<<

ThePennsylvaniaStateUniversity

TheGraduateSchool

CollegeoftheLiberalArts

THELATECLASSICORGANIZATIONOFJADEARTIFACTPRODUCTION

INTHEMIDDLEMOTAGUAVALLEY,ZACAPA,

ADissertationin

Anthropology

by

ErickT.Rochette

©2009ErickT.Rochette

SubmittedinPartialFulfillment oftheRequirements fortheDegreeof DoctorofPhilosophy

December2009

ThedissertationofErickT.Rochettewasreviewedandapproved*bythefollowing:

KennethG.Hirth ProfessorofAnthropology DissertationAdviser ChairofCommittee DavidWebster ProfessorofAnthropology GeorgeMilner ProfessorofAnthropology MatthewRestall EdwinErleSparksProfessorofHistory E.PaulDurrenberger ProfessorofAnthropology DirectorofGraduateStudies *SignaturesareonfileintheGraduateSchool.

ii ABSTRACT Objectscraftedfromjadeplayedaprominentsocial,politicalandritualroleinall prehispanicMesoamericanfromatleasttheMiddleFormativeperiod(ca. 1000400B.C.)throughtothetimeoftheSpanishConquest.Basedprimarilyonthe consumptionofjadeartifactsbyancientMayaelites,scholarshavearguedthattheir productionwasunderthedirectcontrolofelitemembersofsociety.Nevertheless,few studieshaverecoveredevidenceofjadeartifactproduction.Thisdissertationpresentsthe resultsofanarchaeologicalprojectintheMiddleMotaguaValley,Zacapa,Guatemala, whereevidencedemonstrateswidespreadproductionofjadeartifactsintheonly positivelyidentifiedjadesourceforprehispanic.Thisfieldresearch involvedarchaeologicalsurveyandtestexcavationtodocumenttheorganizationofjade artifactproductionintheareaduringtheLateClassicperiod(A.D.600900).Thesedata andsubsequenttechnologicalanalysessuggestthatjadearitfactproductiontookplacein avarietyofdomesticandnondomestic,aswellaseliteandnonelitecontexts.This evidencerunscountertomanypreviousmodelsofwealthgoodsproduction,whichhave viewedsuchproductionasanelitedominatedactivity.Further,thedatasetof9,920 jadeiteartifactsrepresentsthelargestcollectionofjadeartifactproductionevidence recoveredtodate,andprovidedtheopportunityforadetailedanalysisofthe technologicalprocessofjadeiteartifactproduction.Thisstudyprovidesvaluableinsights intotheorganizationofwealthgoodsproductioninancientMesoamericaandoffersa contributiontogeneralanthropologicaltheoriesofpoliticaleconomy.

iii TABLEOFCONTENTS LISTOFTABLES...... vii LISTOFFIGURES...... ix ACKNOWLEDGEMENTS...... xii CHAPTER1 INTRODUCTION...... 1 1.1 ProblemDefinition&Significance...... 2 1.2 SpecificIssuesCoveredinthisDissertation...... 10 1.3 MethodologyandDataCollection...... 11 1.4 ChapterOrganizationandContent...... 14 CHAPTER2 APPROACHESTOTHEARCHAEOLOGICALSTUDYOFCRAFT PRODUCTION...... 17 2.1 ArchaeologicalApproachestotheStudyofPreindustrialCraft Production...... 19 2.2 DimensionsofCraftProduction...... 22 2.2.1 Technology&CraftProduction...... 23 2.2.2 CraftProductionUnits...... 26 2.2.2.1Spatial&SocialOrganizationofProductionUnits...... 28 2.2.3 TypesofGoodsProduced...... 32 2.2.4 SociopoliticalContextofProduction...... 36 2.3 ConcludingComments...... 40 CHAPTER3 JADEANDITSSIGNIFICANCEINPREHISPANIC MESOAMERICA...... 43 3.1 WhatisJade?:Jade,JadeiteandGreenstone...... 44 3.1.1 JadeiteSourcesandSourcinginMesoamerica...... 47 3.2 TheCulturalSignificanceofJadeinPrehispanicMesoamerica...... 52 3.2.1 PatternsofFormativePeriodJadeUseinMesoamerica...... 53 3.2.2 PatternsofClassicPeriodJadeUseintheMayaArea...... 66 3.3 Discussion...... 74 CHAPTER4 THEMIDDLEMOTAGUAVALLEY:PREVIOUSRESEARCH, RESEARCHDESIGN&SURVEYRESULTS...... 76 4.1 TheMiddleMotaguaValley:GeologicalandNaturalEnvironment...... 77 4.2 PrehispanicCulturalGeographyoftheSoutheasternMayaZone...... 80 4.2.1 PreviousArchaeologicalResearchintheSEMayaPeriphery...... 80 4.2.2 PreviousArchaeologicalResearchintheMiddleMotagua Valley...... 91

iv 4.3 UnderstandingJadeArtifactProductionintheLowerLatoValley...... 103 4.3.1 PreliminaryWork...... 103 4.3.2 SurfaceSurveyMethodology...... 105 4.4 SurfaceSurveyResults...... 108 4.4.1 LowerLatoRiverValleySites...... 111 4.4.1.1VargasIIA...... 111 4.4.1.2VargasIII...... 115 4.4.1.3Magdalena...... 116 4.4.1.4SitesoutsidetheLowerLatoRiverValley...... 117 4.5 SurfaceSurveyResultsInterpretation...... 118 4.6 Discussion...... 125 CHAPTER5 LOWERLATORIVERARCHAEOLOGICALJADEPROJECT EXCAVATIONS...... 126 5.1 PreviousExcavationsintheMiddleMotaguaValley...... 126 5.1.1 SmithandKidder'sGuaytanExcavations...... 129 5.1.2 Walters'GuaytanExcavations...... 132 5.2 ExcavationsforLowerLatoRiverArchaeologicalJadeProject...... 140 5.2.1 ExcavationMethodology&LocationofExcavationUnits...... 141 5.3 SummaryofexcavationsatGuaytan4...... 147 5.4 SummaryofGuaytan3Excavations...... 157 5.5 SummaryofGuaytan5Excavations...... 158 5.6 SummaryofGuaytan6Excavations...... 158 5.7 SummaryofGuaytan7Excavations...... 159 5.8 SummaryofGuaytan8Excavations...... 161 5.9 SummaryofMagdalenaIExcavations...... 162 5.10 MiscellaneousExcavations...... 163 5.11 DiscussionofExcavationResults...... 164 CHAPTER6 MAKINGTHEJADE:THETECHNOLOGICALPROCESSOFJADE ARTIFACTPRODUCTION...... 167 6.1 PreviousStudiesofJadeArtifactProduction...... 168 6.1.1 PercussionMethods...... 169 6.1.2 Grinding/Abrading...... 173 6.1.3 Sawing...... 176 6.1.4 Drilling...... 181 6.1.5 Incising...... 188 6.1.6 Polishing...... 190 6.2 TypologyofJadeArtifactProductionEvidence...... 192 6.2.1 JadeCobbleorChunk...... 195 6.2.2 LargeJadeFlakes...... 195 6.2.3 SmallJadeFlakes...... 196 6.2.4 JadeBeadPreform...... 197 6.2.5 Broken/UnfinishedJadeBead...... 198

v 6.2.6 JadeHollowDrillCores...... 198 6.2.7 CompleteJadeBead...... 199 6.2.8 CutJadeFragment...... 200 6.2.9 JadeFragmentwithGroundFacet...... 201 6.2.10 Hammerstones...... 202 6.2.11 ChertBladeFragments...... 202 6.2.12 ChertDrills...... 202 6.2.13 OtherLithicandShellArtifactAnalyses...... 203 6.3 OperationalChainofJadeBeadProductionintheMiddleMotagua Valley...... 204 6.4 NonBeadJadeArtifactProductionintheMiddleMotaguaValley...... 212 6.5 OtherProductionEvidenceintheMiddleMotaguaValley...... 213 6.6 Discussion...... 214 CHAPTER7 ORGANIZATIONOFJADEARTIFACTPRODUCTIONINTHE MIDDLEMOTAGUAVALLEY...... 216 7.1 AncientMayaWealthGoodsProduction...... 217 7.2 MiddleMotaguaValleyWealthGoodsProductioninContext...... 225 7.2.1 ProductionMethods&TechnologyintheMiddleMotagua Valley...... 225 7.2.2 ScaleandStructureofProductionUnits...... 235 7.2.3 NatureoftheGoodsProduced...... 237 7.2.4 SociopoliticalContextofProduction...... 244 7.2.5 MiddleMotaguaValleyWealthGoodsProductionSummary..245 7.3 AlternativeModelsofMMVWealthGoodsProduction...... 246 7.3.1 DomesticEconomyModel...... 247 7.3.2 PoliticalEconomyModel...... 251 7.3.3DiscussionofDomesticandPoliticalEconomyModels...... 253 7.4 Conclusion...... 257 CHAPTER8 CONCLUSIONS...... 258 8.1 Technology...... 258 8.2 OrganizationofJadeiteArtifactProduction...... 263 BIBLIOGRAPHY...... 269 APPENDIXASURFACESURVEYDETAILS...... 306 APPENDIXBTESTEXCAVATIONDETAILS...... 321 APPENDIXCLITHICARTIFACTANALYSESDETAILS...... 357 APPENDIXDMIDDLEMOTAGUAVALLEYCERAMICS...... 363

vi LISTOFTABLES Table2.1 Modelsofcraftspecialization...... 27 Table4.1 Walters(1982)sitehierarchyfortheMiddleMotaguaValley...... 99 Table4.2 Walters(1982)jadeworkshopclassesfortheMiddleMotaguaValley..100 Table4.3 Artifactsrecoveredfromlooter’strenchesatVargasIIA...... 114 Table4.4 SurfacecollectionsfromVargasIII...... 116 Table4.5 DefinitionofsitehierarchyintheMiddleMotaguaValley...... 119 Table4.6 Totaljadeandlapidaryproductionevidencefromsurfacecollections...121 Table4.7 Totalproductiontoolsandlargejadecobblesfromsurfacecollections..122 Table4.8 Totaljadeandlapidaryproductionevidencefromsurfacecollections,by hierarchicalsitetype...... 123 Table4.9 Totalproductiontoolsandlargejadecobblesfromsurfacecollections,by hierarchicalsitetype...... 123 Table4.10 PeriodsofoccupationbasedonsurfacecollectedceramicsfromMiddle MotaguaValleysites...... 124 Table5.1 Artifactscollectedin1msquaresatGuaytan4priortoexcavations...... 144 Table5.2 Artifactsrecoveredinexcavationunits1A1and1A2...... 151 Table5.3 ArtifactsrecoveredfromOperation1Dexcavations...... 153 Table5.4 ArtifactcountsfromOperation1Eand1Fexcavationunits...... 161 Table5.5 ArtifactsrecoveredinOperation1CexcavationsatGuaytan3...... 157 Table5.6 ArtifactsrecoveredinOperation6AexcavationatGuaytan6...... 159 Table5.7 Artifactsrecoveredinexcavationunits3A1and3A2...... 160 Table5.8 Artifactsrecoveredinexcavationunits4A1and4A2...... 162 Table5.9 ArtifactsfromMagdalenaItestunits...... 163 Table5.10 Artifactsfrommiscellaneoustestunits...... 164 Table5.11 Artifacttotalsfromallexcavationsatallsites...... 164 Table6.1 Listoftypologicalcategoriesforjadeiteartifactsusedinthis dissertation...... 194 Table6.2 Measurementsofhollowdrillcoresfromsurfacecollections& excavations...... 199 Table6.3 Otherlithicandshellartifactsfromexcavationsandsurface collections...... 204 Table6.4 Sizegradesofsmalljadeflakesfromsurveyandexcavations...... 207 Table6.5 Hollowdrillcores,broken/unfinishedbeads,andcompletebeadsshowing evidenceofgrindingononeormoresurfacespriortodrilling...... 208 Table6.6 Comparisonofdiameterofjadebeaddrillholeswiththicknessofchert drilltips.Tipsofmanydrillsweretooworntoobtainaccurate measurements...... 209 Table7.1 Chertdrillsandbladesfromsurfacecollections...... 227 Table7.2 Chertdrillsandbladesrecoveredfromtestexcavations...... 229 Table7.3 Sitesatwhichbeadsbrokenorabandonedduringtheprocessofdrilling wererecoveredfromsurfacecollections...... 230 Table7.4 Evidencelinkedtopossiblejadebeadproductionfromexcavationsand surfacecollections...... 239

vii Table7.5 Comparisonofaveragediameterofholesincomplete,brokenand abandonedbeadswiththediametersofhollowdrillcores...... 242 Table7.6 Comparisonofdiametersofinteriorholesofbroken,abandonedand completedrilledbeads(“Holes”)andhollowdrillcores(“Cores”), bysitetype...... 243

viii LISTOFFIGURES Figure1.1 MapshowingMayaarea,withMiddleMotaguaValleyinbox...... 12 Figure3.1 Worlddistributionofknowngeologicalsourcesofjadeitejade...... 49 Figure3.2 LocationofMotaguaFaultanditscooccurrencewith serpentinerockbeds...... 49 Figure3.3 JadesourcessampledbyHammondandcolleagues...... 52 Figure3.4 LateFormativejadesfrom...... 65 Figure4.1 MapofMayaareawithmajorarchaeologicalsites...... 78 Figure4.2 ExtentoftheMiddleMotaguaValley...... 81 Figure4.3 MapoftheSoutheastersnMayaPeriphery...... 82 Figure4.4 MapofMiddleMotaguaValleyfromWalters(1982)...... 97 Figure4.5 MapofSAAAZsitesfromareainsidetriangleinFigure4.3...... 98 Figure4.6 MapoftheeasternMiddleMotaguaValley,showingextentofarea surveyedaspartofdissertationresearch...... 102 Figure4.7 Jadeitedebitage(examplescircledinred)atGuaytan4...... 105 Figure4.8 LowerLatoValleysurveyarea...... 109 Figure4.9 MapofGuaytan,dashedboxisareaofinsetbelow(fromLopeznd.)....112 Figure4.10 MapofGuaytanshowinglocationofsiteswithjadedebitagescatters...112 Figure4.11 ExtensivelootingatVargasIIA...... 113 Figure4.12 JadeproductionevidencefromVargasIIAlooter'strench(Op.5I1)....113 Figure4.13 StonerecoveredatVargasIIA,possiblyusedforgrindingbeads...... 115 Figure4.14 MapofsouthernportionofMagdalenaI...... 117 Figure4.15 JadeitedebitagefromKM92III...... 123 Figure5.1 MapofMiddleMotaguaValley...... 128 Figure5.2 MapofGuaytan,withlocationsofstructuresnotedby Smith&Kidder...... 131 Figure5.3 Structure24atGuaytan...... 132 Figure5.4 MapofGuaytan,withapproximatesurveyareaboundaries(hatchedlines) describedbyWalters(1980a,1980b)...... 133 Figure5.5 ContourmapofAreas3,4&5(Walters1980b:88)...... 135 Figure5.6 PlanviewofArea4,Excavation16(Walters1980b)...... 136 Figure5.7 PlanmapofexcavationunitsinArea3andthefloorplanofLateClassic featuresrevealedinthoseexcavations(Walters1980b)...... 138 Figure5.8 MapofexcavationunitsfromArea4(Walters1980a:13)...... 139 Figure5.9 Locationofsitesexaminedaspartofthisdissertationresearch...... 142 Figure5.10 MapofGuaytan,hatchedlinesindicatelimitsofmapinsetshownin Figure5.11(modifiedfromLopezn.d.,inRamonRamirez2006)...... 144 Figure5.11 DetailofsouthernportionofGuaytan,indicatinglocationofareas withjadeartifactproduction,identifiedduringarchaeological surfacesurvey...... 145 Figure5.12 Mapshowinglocationofstructures,gridsestablishedforexcavationsand looter'strenchesatGuaytan4...... 146 Figure5.13 MapofsouthernportionofGuaytan4,showinglocationofexcavation units...... 147 Figure5.14 PanoramicviewlookingsouthtowardGuaytan4...... 149

ix Figure5.15 Excavationprofileofunit1A1...... 151 Figure5.16 PlanphotooffloorinUnit1B1,whereexcavationwasterminated...... 152 Figure5.17 CacheofbladecoresfromexcavationatGuaytan4...... 155 Figure5.18 FragmentsofworkedshellrecoveredfromGuaytan4excavations...... 156 Figure5.19 Possiblejaguarclawrecoveredfromcontentsofobsidian bladecorecache...... 156 Figure5.20 ViewofGuaytan3,lookingtothenorth...... 157 Figure5.21 ViewofGuaytan5,lookingwestbysouthwest...... 158 Figure5.22 Stratigraphicprofileofunit3A1atGuaytan7...... 160 Figure5.23 StingrayspineanddrilledobsidianfromGuaytan8excavations...... 162 Figure6.1 Jadeiteflakesproducedbyhardhammer,directedpercussion...... 171 Figure6.2 EarlystagepercussionflakesandjadeceltpreformsfromCenegal...... 172 Figure6.3 PossiblejadeanvilatCenegal....... 173 Figure6.4 Artist'srenditionofMaorinephriteadzegrinding...... 174 Figure6.5 Maoritechniqueofsawingnephriteusingasandstonesaw...... 185 Figure6.6 WorkersinPekingcuttingjadeiteblockusingawoodframewiresaw..179 Figure6.7 Sectiondrawingsofcutjadefragmentsfrom...... 180 Figure6.8 CutfragmentofjadeitefromGuaytan4excavations...... 180 Figure6.9 Stringsawanchorrecoveredat...... 181 Figure6.10 Olmecjademask.Notedrillingtoformnostrilsandeyesofmask...... 183 Figure6.11 HeaddressornamentrecoveredfromCancuen...... 183 Figure6.12 ChertdrillsrecoveredfromNativitas,Puebla,...... 185 Figure6.13 Jadebeadbrokenduringuniconicaldrilling...... 185 Figure6.14 AlabastertabletfromIxtapaluco...... 186 Figure6.15 JadeitehollowdrillcoresfromGuaytan4excavations...... 187 Figure6.16 CarvedbeadsfromKaminaljuyu....... 187 Figure6.17 Depictionofapumpdrillshowingflywheelandhafteddrilling element(fromDigby1964:16)...... 188 Figure6.18 SlateslabsandlimestoneearflarepolisherfromCancuen...... 192 Figure6.19 LimestoneearflarepolisherrecoveredfromCancuen...... 192 Figure6.20 JadecobblecollectedfromKM91III...... 195 Figure6.21 LargeflakesfromVargasIV...... 196 Figure6.22 SmalljadeflakesfromGuaytan4excavations(1A2001)...... 197 Figure6.23 JadebeadpreformsfromVargasIIIsurfacecollections...... 197 Figure6.24 JadehollowdrillcoresfromGuaytan4excavations...... 199 Figure6.25 Completejadebeads...... 200 Figure6.26 Drawingofanexampleofcutjadeitefragmentfrom1A1005...... 200 Figure6.27 JadeitehammerstonerecoveredfromGuaytan8excavations...... 201 Figure6.28 Examplesofartifactsclassifiedasgroundjadefragments...... 202 Figure6.29 ChertdrillsrecoveredfromVargasIII...... 203 Figure6.30 OccurrencesofjadeintheMiddleMotaguaValley...... 206 Figure6.31 JadebeadpreformfromGuaytan4excavations...... 207 Figure6.32 ChertdrillsandjadeitebeadfromGuaytan4excavations...... 209 Figure6.33 Flowchartdepictingoperationalsequenceofjadeitebeadproductionin theMiddleMotaguaValley...... 211 Figure6.34 Jadeiteartifactsshowingevidenceofhavingbeencut...... 213

x Figure6.35 FragmentsofworkedshellandstonefromGuaytan4...... 214 Figure7.1 Chertdrillsandbladesfromsurfacecollections,bysitetype...... 228 Figure7.2 Chertdrillspercubicmeterfromexcavations...... 229 Figure7.3 Chertdrillspercubicmeterfromexcavations,averagedpersitetype....229 Figure7.4 Surfacecollectedbeadsbroken/abandonedduringdrillingbysitetype..231 Figure7.5 Hollowdrillcoresrecoveredfromsurfacecollection,bysitetype...... 231 Figure7.6 Smalljadeflakesurfacecollectionsbysitetype...... 232 Figure7.7 Avg.quantityofsmalljadeflakesfromsurfacecollections persitetype...... 233 Figure7.8 Averagequantityofsmalljadeflakespercubicmeterrecoveredfrom excavations,bysitetype...... 234 Figure7.9 Jadefragmentsshowingevidenceofsawingbysitetype...... 240 Figure7.10 Fragmentswithgroundfacetsfromsurfacecollections,bysitetype...... 241 Figure7.11 HollowdrillcoresrecoveredfromGuaytan4excavations...... 241

xi ACKNOWLEDGMENTS Noworkthattakessomuchtime,effortandstresstocompletecouldeverhave beenaccomplishedwithouttheassistance,encouragmentandguideanceofmanypeople.

Inthisspace,IcanonlyattempttoacknowledgetheenourmousdebtthatIowetothe

manypeoplethathaveindulgedmyignorantquestions,requestsforhelp,ranting,andall

theotherthingsthatgoalongwithcompletingadissertation.

Iwouldliketothankmyadvisor,KenHirth,forbeingaconstantsourceof

encouragementandintellectualinspiration;withoutyourinsightandassistancethis

dissertationwouldneverhavebeenpossible.Iwouldalsoliketothankmyother

committeemembers:DavidWebster,GeorgeMilnerandMatthewRestall.Throughtheir

discussionsandcommentsonthisdissertationtheyhaveshownmethat"received

wisdom"shouldneverbeaccepteduncritically,norassumedtobewisdom.

Dissertationsarecostlyacademic,personalandfinancialendeavors,andthis

researchwouldhaveneverbeenpossiblewithoutthegeneroussupportoftheFoundation

fortheAdvancementofMesoamericanStudies,Inc.,theWilliamT.SandersDissertation

Award,theHillFoundationDissertationImprovementAwardandaDissertation

ImprovmentAwardandDissertationReleaseTimefromthePennStateResearchand

GraduateStudiesOffice.

IoweaspecialdebtofgratitutetothehelpoftheInstitutodeAntropologíae

HistoriadeGuatemala(IDAEH)forprovidingmewiththeopportunitytoconductmy

researchintheMiddleMotaguaValley.IwouldespeciallyliketothankGustavoAmarra

ofIDAEHforhishelpinmakingthisfieldworkandthesubsequentartifactanalysesa

sucess.

xii Thisdissertationfieldresearchwouldhavebeenwithoutthehelpofmyco

directorLicenciadaMónicaPellecerAlecio,whoworkedtirelesslyinarrangingthe

logisticsofthisprojectandensuringthatourresourcesweremorethansufficient.

Mónica,graciasportodocontodasinceridad,yesperotrabajarcontúenelfuturo.

Fieldresearchalwaysinvolvesmultiplepersonstodothenecessarywork,and

therearemanypeoplewhosedilligent,hardworkmadethisallpossible.Thanksto

LicenciadaErikaGomezforhermeticulousexcavationandnotes,withoutwhichIwould

havebeenlost.ThankyoutoLicenciadaElisaMencosforherhardwork,friendship,and

excellentdrawings,whichwerefarbetterthanIcouldhaveeveraccomplishedonmy

own.Many,manythankstoLicenciadaSelketCallejasforhertremendouswork

completingtheceramicanalysis.IowemoregratitudethanIcaneverexpresstoDon

GustavoGuillenandSergioGonzalesCastrofortheirhardwork,friendship,and

hospitality.IwouldalsoliketothankallthechildrenofGuaytan,forprovidingan

endlesssourceofamusementandhelpduringourexcavations.Despitethelong,hot,

dustyworkdays,IwillalwayslookbackfondlyonmydaysspentintheMiddleMotagua

Valleyduringthisdissertationresearchbecauseofyouall.

MytimeinGuatemalawouldhavebeenimmenselymoredifficultifitweren'tfor themanygreatfriendsandcolleaguesthathelpedkeepmesaneandgrounded.Thanksto

Dr.KarlTaubeandDr.ZacharyHrubyforintroducingmetothewondersof"jadefever" andforstartingmeoutintheMiddleMotaguaValleyresearch.ThankstoLicenciado

LuisRomeroandthelateLicenciadoJoséHéctorParedesfortheirhelpinplanningthis projectfromitsinception.Mydeepestgratitudetoallthefollowing,whoinonewayor anotherprovidedtremendoussupport:JessicaCraig&AdamStokesforputtingmeupin

xiii Antigua;EdwinRoman,TomGarrison,RobGriffinforallowingmetocrashoncouches;

andJohnRexerandeverybodyatCafeNoSefordrinkingwithme.

IwouldcertainlyneverhavesurvivedwithoutthetrulyincrediblefriendsthatI

havemadeduringmytimeatPennStateUniversity;Icouldprobablywriteanentire dissertationlengthbookabouthowmuchyouhaveallmeanttome:JasonDeLeon,Eric

Jones,SharonDeWitte,HollyDunsworth,NiaBharti,SamSholtis,MariaInclan,Craig

Goralski,KirkFrench,KirkStraight,EllenQuillen,GeoffVasile,RobGriffin,Corey

Sparks,AbbyBigham,BrendaFrazier,LaurelPearson,BlancaMaldonando,Ryan

Aadms,RyanPeterson,DawnMiller,JessBurgett,ScottHammerstedt,Johanna

YngvassonBissat,andLeilaRodriguez.

SpecialthanksalsogotothededicatedstaffofPennStateAnthropology,without

whosehelpIwouldhavemissedinnumerabledeadlinesandfineprint:WendyDiebler,

DianeSnyder,KimMiller,FayeMaring,BettyBlair,andMelissaStrouse.

BecauseIamsimplystandingontheshouldersofgiants,Iwouldliketo

acknowledgemyundergraduateadvisorNormanHammond.Withoutyourhelpand

example,noneofthiswouldhavebeenpossible.

IoweeverythingthatIamtomyparents,HaroldandKaarina.Youhavealways

shownmethatIcandowhateverIsetouttoachieve,andthisdissertationisatestament

toyouboth.Icanneverhopetorepayyouforallthatyouhavedoneforme,butIhope

thatthisservesasbutasmalldemonstrationofhowtrulywonderfulyouare.Thanks,

andIloveyoumomanddad!

Ifthereisoneperson

xiv GARYREXWALTERS????

wasindispensabletothesuccessofthisresearch.Iwouldalsoliketothankthe followingforinsightfulcommentsthathaveimprovedthispaper:KennethHirth,David

Webster,CraigGoralski,JasonDeLeon,J.HeathAnderson,KirkStraight,KirkFrench, andScottSpeal.Specialthanksalsotomycodirector,,andtoallwhohelpedmakethis researchasuccess,especiallyKarlTaube,ZacaryHruby,ErikaGomez,ElisaMencos,

SelketCallejas,DonGustavoGuillenandSergioGonzalezCastro.Last,butcertainlynot least,IwouldliketothankmyparentsHaroldandKaarina,andespeciallymywifeSarah, fortheirsteadfastsupportandunderstandingthroughtheprocessofcompletingthis project.

MariaInclan

xv CHAPTER1

INTRODUCTION

Objectscraftedfromjadeplayedaprominentsocial,politicalandritualroleinall prehispanicMesoamericancivilizations.BytheMiddleFormativeperiod(ca.1000400

B.C.),jadewasusedwidelythroughoutMesoamerica(Garberetal.1993;Ortizand

Rodríguez2000;Taube2005)anditsuseandcirculationcontinuedtoexpanduntilthe

timeofSpanishConquest(Lange1993).JadewassopreciousthatAztecofficials presentingagiftofseveraljadestoCortesnotedthat“eachone[is]worthmoreand[is] esteemedmorethanagreatloadofgold”(Díaz1956:7677).Beyonditseconomicvalue, jadewasreveredforitscosmologicalassociations,beingconsideredaphysical representationoffertility, water,,centrality, breath,andthesoul( Fields1991;

Freidel1990;MillerandSamayoa1998;Taube2000,2005 ).

TheimportanceofjadefortheancientMayaisdemonstratedbytheinclusionof

elaborateandabundantjadeobjectsinmanyeliteburialsandfromthemanymurals,

stelaeandpaintedvesselsdepictingeliteswearingabundantjadejewelry(Digby

1964;Proskouriakoff1974;Garberetal.1993;KrejciandCulbert1995;Taube2005).

Despitethisconspicuoususe,weknowlittleabouthowjadewasacquired,howitwas

shapedintoobjectsofvalue,andhowthisproductionanddistributionwasorganized.

Moregenerally,manycompetingproposalshavebeenpresentedaboutthenatureof

ancientMayapoliticalsystemsandtheireconomicbases(MassonandFriedel2002;

McAnanyandIsaac1989;Scarboroughetal.2003;ScarboroughandClark2007).

Thisstudyevaluatescurrentargumentsabouttheorganizationofproductionof jadeandotherwealthgoodsinancientMayasocietythroughaninvestigationofthe

1 organizationandtechnologyofprehispanicjadeartifactproductionintheMiddle

MotaguaValley,DepartmentofZacapa,Guatemala.Itisimportantbecauseitisthefirst

studytoidentifyandreconstructsystemofwealthgoodsproductiononaregionallevel.

Furthermore,itisimportantbecauseitprovidesnewdatathatruncontrarytoassumptions

oftraditionalmodelsofwealthgoodsproduction.

1.1 ProblemDefinitionandSignificance

Understandingtheorganizationofeconomicsystemsiscrucialforunderstanding thestructureandfunctioningofancientsocieties.Alleconomicsystemsaremadeupof threecomponents:production,distributionandconsumption.Thestudyofproduction systemsisparticularlyimportantbecauseitcanyieldinformationrelevanttoabroad rangeoftheoreticalissues,suchasdomesticandpoliticaleconomy,socialorganization, andsocioculturalevolution,amongothers.Furthermore,inmanyinstanceseconomic activityassociatedwithproductioniseasiertoidentifybecauseofthevisiblematerial remainsthatarecreatedasabyproductofproductiveactivity.

Archaeologistshavelongrecognizedthatelitesoftenseektomaintainand increasetheirpowerbycontrollingtheproductionordistributionofvaluableornecessary resources,materialsorfinishedgoods(BrumfielandEarle1987;D'AltroyandEarle1985;

Earle1997;FrankensteinandRowlands1978).Despitethevarietyofmeansbywhich elitesmightachievetheseends,morestudiesfocusondefiningtheroleofelitesin controllingthedistributionandexchangeofwealthgoodsratherthanonhowproduction wasorganizedwithinparticularpolitiesorsocieties(Hirth1992,1996).Thismayresult fromthenotion,expressedbyCarolSmith(1976:311),thatcontrolofthedistributionof

2 scarceorvaluableresources,ratherthantheirproduction,isthecriticalbasisbywhich

rankingandstratificationareupheldinagrariansocieties.However,evenin sociopoliticalsystemswherecontrolofthedistributionofnecessaryrawmaterialsor

craftedgoodsisvitaltosociopoliticalandsocioeconomicinequality(cf.Frankensteinand

Rowlands1978;Sinopoli2003),themannerinwhichproductionisorganizedisstill

importantforunderstandingthenatureofpoliticalpowerandeconomicorganization withinthosesocieties.Forexample,whilesomevaluablegoodsmayhaveserved disproportionatelytovalidateandsymbolizeeliteauthoritywithinthepoliticaleconomy, wecannotassumethattheirproductionwasdirectlycontrolledbyelites(Arnoldand

Munns1994).Furthermore,itmustbedemonstrated,ratherthanassumed,thatthe productionofwealthgoodstookplaceoutsideofthedomesticeconomy,inwhich productionwasgearedtowardthesupportofindividualhouseholds,ratherthanthe politicalelite.Inthisdissertation,Iusethemoregeneralterm"wealthgoods"toreferto whathavetraditionallybeencalled"prestigegoods"intheliteraturetoavoidinterpretive problemsrelatedtotheterm"prestigegood,"whichimpliesaparticulartypeof"prestige goodssystem"tomanyscholars.

Aparticularconcernformanyarchaeologistshasbeendocumentingvariationin theorganizationofcraftproductionsystems(BrumfielandEarle1987;ClarkandParry

1990;Costin1991,2001).Oneofthemostprominentmodelsforancientchiefdomsand statesdichotomizescraftproductionbasedonthenatureofthegoodsproducedandthe degreetowhichproductioniscontrolledbypoliticalelites(Earle1981;Brumfieland

Earle1987). Inthismodel,itisarguedthateverydayutilitariangoodstendtobe producedbyindependentspecialistswhoproduceforgeneraldemand,whilewealth

3 goodstendtobeproducedbyattachedspecialistswhoproduceforpatronsondemand

(Earle1981;BrumfielandEarle1987).Althoughthisdistinctionisuseful,ithasbeen criticizedasoverlytypologicalandtoocloselytiedtoculturalevolutionarytrajectories

(ClarkandParry1990;Costin1991;ArnoldandMunns1994;Inomata2001).

Anumberofrecentstudieshowever,havefocusedondocumentingvariabilityin

theorganizationofdifferentsystemsofcraftproductionwithinasinglesociety(e.g.

Costin1996;MassonandFriedel2002;Underhill1991;WellsandDavisSalazar2007a;

Wright1998).Thislineofresearchiscongruentwiththecrossculturalsurveyofcraft productioncompiledbyClarkandParry(1990:320),whichshowsthatthereisageneral correlationbetweengreaterpolity/communitysize,sociopoliticalcomplexity,anda greaterdiversityoftypesofspecializedcraftproduction.Takentogether,thisresearch

demonstratestheneedforstudiesofcraftproductioninawiderangeofpoliticaland

socialcontextsthatclarifytherelationshipbetweenpoliticalandeconomicstructures

(Costin2001:274).

ThisisespeciallytruefortheClassicMaya(A.D.3001000),wherearguments

aboundaboutthepossibleeconomicbasesofelitepower(e.g.Blantonetal.1996;

Demarest1992;Foxetal.1996;MassonandFriedel2002;McAnanyandIsaac1989;

Sanders1989;Scarboroughetal.2003;ScarboroughandClark2007;Tourtellotand

Sabloff1972).SomescholarsarguethatancientMayaelitesatcertainsitesmaintained powerbycontrollingandmanagingvitalnaturalresourcessuchasagriculturalland(e.g.

Adams1975,1981;ChaseandChase1987;HarrisonandTurner1978;Healyetal.1983;

Kunen2001,2004)orwater(e.g.Matheny1976;Scarborough1993,1998,2003).Other

scholarshavenotedtherolethatMayaelitesatsomesitesplayedincontrollingthe

4 distributionofcraftgoodsorrawmaterialsgenerally(e.g.HesterandShafer1984),and ofwealthgoodsmorespecifically(e.g.Aoyama1999;Rathje1970,1972).

Controllingtheproductionofwealthgoodscanbeaparticularlyeffectivestrategy forenhancingorlegitimatingpoliticalauthority,becausedoingsomeanshaving de facto controloftheirdistribution(Lewis1996).Elitesmayattempttocontrolcraftproduction systemsinanumberofways.Theymaysponsorproductioninattachedfacilitiesor undertakeproductionwithintheirownhouseholds(e.g.Ball1993;Inomata2001).They mayobtainfinishedorsemifinishedcraftproductsfromnonelitehouseholdswithinor outsideoftheirpolitiesthoughavarietyofmobilizationorexchangemechanisms.An exampleofthelatersituationcomesfromtheAztecempireduringthePostclassicPeriod, whensomewealthgoodsusedbyeliteswereproducedbyindependentspecialistsaspart oftributepayments,butoverwhoseproductionverylittledirectcontrolwasexercised

(Berdan1994;SmithandBerdan2003:93).Alternatively,productionofwealthgoods maybeanactivityinwhichnonelitehouseholdsengagedwhenthenecessaryresourcesto dosowereavailableaspartofadomesticeconomy,creatingasituationinwhichthe abilityofelitestocontroldistributionandacquisitionofthesefinishedgoodswasof paramountimportance.

Nevertheless,fewstudieshavedocumentedancientMayasystemsofcraft production.Thosestudiesthathavedonesohavegenerallyfocusedontheproductionof utilitariangoods(Andrews1983;Aoyama1999;HesterandShafer1984;Mallory1984;

McKillop2003;Michels1979;ShaferandHester1983).MoststudiesofancientMaya wealthgoodsproduction,however,havereliedonsecondaryevidencesuchas distributionpatternsandchemicalsourcingtoinfertheorganizationofsystemsofwealth

5 goodsproduction(Ball1993;LeCount1999;RandsandBishop1980;ReentsBudet

1998).Thissituationispartiallyattributabletotheverycharacteristicsfromwhich

wealthgoodsderivetheirvalue:theirscarcity,the(oftenexotic)rawmaterialsfrom

whichtheyaremanufactured,andtheallegedlyspecializedskillsandknowledge

sometimesneededtocraftthemproperly(WellsandDavisSalazar2007b).These

factorshaveoftenmadeitdifficultforarchaeologiststodocumentmanyclearexamples

ofwealthgoodsproductionintheMayaarea.Studiesthathavebeenableto

convincinglydocumentwealthgoodsproductionareexceedinglyrare,andofteninvolve

single,specializedcontexts(Inomata2001;Kovacevich2007;Widmer2009).This

dissertationresearchisimportantbecauseitisthefirsttoreconstructaregionalsystemof

wealthgoodsproductionintheMayaareaindetail.

Workingfromtheseincompletesourcesofevidence,somescholarshave

characterizedancientMayaeliteauthorityandpoliticaleconomyasbeingbasedonor

significantlyenhancedbytheproduction,consumptionanddisplayofelaboratewealth

goodssuchasjadebeadnecklaces,earspools,polychromeceramicsandfeatheredhead

dresses(e.g.Demarest1989,1992; Blantonetal.1996;WellsandDavisSalazar2007a).

Further,theseauthorscharacterizeClassicMayaeconomyasoneinwhichMayaelites

exercisedlittle,ifany,directcontroloverthesubsistencebaseoftheirpolities,but

insteadwhereelitesfocusedeffortsoncontrollinganddirectingwealthgoodsproduction

(Demarest1989,1992;Hendon1991;Inomata2001;McAnany1993;ReentsBudet

1998).Thisreconstructionisoftencastintermsof"competitivestatusrivalry"(e.g.

Marcus1993;Webster1998),whereelitescompetewithoneanotherforpurposesof prestige,territorialexpansionand"aggrandizement"(Webster1998:311),andusewealth

6 goodstodemonstratetheirelevatedsocialstatus(c.f.WellsandDavisSalazar2007b).

Accordingtothesemodels,bycontrollingwealthgoodsandtheirproduction,Mayaelites

effectivelycontrolledthe"materialization"(c.f.DeMarris,CastilloandEarle1996)of

ideologiesandritualsthatlegitimatedtheirelevatedpositionwithinsociety.

Thesepropositionsleadtotwobasicquestions.First,wastheproductionof

wealthgoodscontrolledordirectedinanydemonstrablewaybyancientMayaelites?

Demonstratingcontroloftheproductionofcraftgoodsbyelitesisanotoriouslydifficult

taskforarchaeologists,andthisisespeciallythecasefortheancientMayabecauseofthe paucityofevidenceofwealthgoodsproduction.Wherethereisevidenceforelite

involvement,itistypicallyarguedtobewithinthecontextofa"palaceeconomy"where

elitesproducedgoodswithintheirownhouseholdsfortheirownuses(Ball1993;Ball

andTaschek1991;Inomata2001;McAnany2004;Widmer2009).Somehaveargued

fornoneliteparticipationintheproductionofwealthgoods(Ball1993;PotterandKing

1995;RandsandBishop1980),buttheevidenceforthisparticipationisnot

straightforwardandisopentointerpretation.

Asecondquestionwemustaskiswetherallwealthgoodsusedinthesame mannerbyancientMayaelitesandcommoners?DecadesofresearchatancientMaya centershasdemonstratedthedisproportionateconsumptionofhighlycraftedexotic objectsbytheelite.Nevertheless,amajorinterpretiveproblemforunderstandinghow wealthgoodsproductionwasorganizedderivesfromaninsufficientrecognitionofthe variedusesofmanyofthesegoodsintheMayaarea.Emphasisisoftenplacedonthe rawmaterialfromwhichtheywereproduced,ratherthanonthestylisticcharacteristicsof particularformsofwealthgoods.Thisisespeciallytrueforartifactsproducedfrom

7 exoticrawmaterialssuchasjade.JadeobjectswerecertainlyofhighvalueintheMaya worldandbeyond,butnotalloftheseobjectsweretreatedwiththesamereverenceor usedinthesamecontexts(Freidel1993;Taube2005).

Thevarietyofwaysinwhichwealthgoodswereusedbyindividualsandsocial groupsofdifferingstatuscanbeenseenatafewsitesintheMayaarea(e.g.Krejciand

Culbert1995).InastudyofLateClassicartifactdistributionintheCopanValley,

Zeleznik(2002)concludedthatalthoughjadewasfoundmorefrequentlyandwithgreater artisticandstylisticelaborationinelitecontexts,itwasstillpresentatalllevelsofthe

socialhierarchy.Whilejadewascertainlyarawmaterialwithstrongcosmologicaland

symbolicassociations,itsusewasnotrestrictedtoelites.Hirth's(1992:23)admonitionis

applicableinthisregard:

"Archaeologistsmustdiscardthenotionthatthecirculationofprimitive valuablesthroughinterregionalexchangenetworkswasstimulatedbyadesire toobtainstatusmarkers...andbegintoexaminethemorespecificwaysin whichprimitivevaluablesareusedintheformationofstatushierarchies" Eliteswouldhavesoughttomanipulatethesharedrecognitionbetweenthemselvesand commonersofthecosmologicalsignificanceofjadeinwaysthatlegitimatedtheir authority.Therefore,itisessentialthatweexaminethewaysinwhicheliteand commonerusesofjadebothoverlappedanddiverged.Lesure(1999)suggeststhatto betterunderstandtheuseandsignificanceofvaluablegoods,weshouldfocuson understandinghowdifferentartifactformsproducedfromthesamerawmaterial(s)were used,bothintermsofthekindsofsocialrelationshipstheymediatedandtheway particularartifactformswerevalued.InChapter3,Iexplorethechronological developmentofjadeuseinMesoamericafromtheEarlyFormativeperioduntilthetime ofSpanishConquest.Recognizingthediversityofusesofjadeartifactsdemonstrates

8 thatsimplylabelingthemwealthgoodsfailstocaptureadequatelytheirroleinMaya

societyandhindersourabilitytounderstandthesystemsofcraftproductionofwhich

theywereapart.

Thiscontextualdiversityhasimplicationsforourunderstandingofhowelites

mighthavesoughttocontrolbothrawjadeiteanditsproductionintofinishedartifacts.

AsIdiscussinChapter2,characterizingtheproductionofwealthgoodsasfull/parttime

orattached/independentspecializationdoeslittletoadvanceourunderstandingofhow productionwasorganized.Furthermore,thisoversightpreventsusfromfully

recognizinghowdifferenttypesofwealthandutilitariangoodswereexchangedor

transferredbothamongstandbetweenelitesandcommoners.Putsimply,ifjadeite

consumptionvariedwidely,thenitcannotbeassumedthatcontrolovertherawmaterial,

itsproductionandexchangemechanismsdidnotsimilarlyvary. DuringtheColonial period,Spanishusedavarietyofpreexistingtributeandexchange

networkstomobilizeresourcesintheMayaareaandthroughoutMesoamerica(Feldman

1971;Restall1997:184188).ItislikelythatClassicperiodMayaelitesalsoused

multipleexchangeanddistributionnetworkstomeettheirneeds,justastheydidinthe

Aztecempirethroughdirectsponsorshipofproductionandmobilizationoftribute(Smith

andBerdan2003).Understandingthevarietyofwaysinwhichresourcesweremobilized

iscrucialifwearetoaccuratelyreconstruct ClassicMayasystemsofcraftproductionand politicaleconomy.

The purpose of this dissertation is to understand the technological process of jade

wealth goods production and the organization of jade artifact production in the Middle

Motagua Valley, Guatemala.

9 1.2 SpecificIssuesCoveredinthisDissertation

Theresearchpresentedinthisdissertationfocusesonansweringtwospecific,but interrelatedquestions.First,Iseektounderstandthetechnologicalprocessor chaîne opératoire ofjadeartifactproductionintheMiddleMotaguaValley.Descriptionsof theseprocesses,basedontechnologicalanalysisofjadeiteproductiondebitagerecovered fromsurveyandexcavation,arepresentedinChapter6.Fewotherattemptshavebeen madetounderstandtheprocessofprehispanicjadeartifactproduction.Themajorityof studiesthathaveattemptedsuchreconstructionshavebeenbasedprimarilyonthe examinationoffinishedartifacts(Easby1968;Kidder,Jennings,andShook1946;

Lothrop1955).Stillfewerstudieshaveexaminedjadeproductionbyexaminingdebitage andtoolsfromtheproductionsequence(Hirthetal2009;Kovacevich2006,2007;

Walters1982),owingprimarilytothescarcityofjadedebitagerecoveredatmostancient

Mayasites.Therefore,thisstudyisauniqueandimportantcontributiontothesmall bodyofliteratureonprehispanicjadeartifactproduction.

Second,Iaddresshowtheproductionofjadeartifactswasorganizedduringthe

ClassicPeriod(ca.A.D.3001000)intheMiddleMotaguaValley.AsInotedearlier, scholarshavediscussedClassicMayaeconomicsystemsbycontrastingtheorganization ofproductionoftwoclassesofgoods:utilitarianand“prestige”orwealthgoods.Asthe argumentgoes,elitessoughttocontroltheproductionordistributionofwealthgoods

(includingjade),whilepayinglessattentiontothecontroloftheproductionandexchange ofutilitariangoods(Rathje1975;BrumfielandEarle1987;Fash1991;Ball1993;

Demarest1992;PotterandKing1995;ReentsBudet1998;Aoyama1999;LeCount

1999;West2002;Kovacevich2007;Foias2007).Manyofthesemodelspositthat

10 attachedcraftproducers,andinsomecaseselitesthemselves,madewealthgoods(c.f.

McAnany1993;Inomata2001).Thisdichotomyismoreoftenbasedontheoretical

modelsandassumptionsaboutthestructureofancientMayapoliticalandpowerrelations

thanonempiricalevidence,atopicIdiscussinChapter2.

Archaeologistshavehadexceedinglyfewopportunitiestodirectlyinvestigateand

documenttheproductionofwealthgoods(Inomata2001;Kovacevich2006).Thisstudy

isunique,therefore,becauseoftheabundantevidenceofwealthgoodsproductionthat

wasrecoveredfromavarietyofsocioculturalcontexts.InChapter7,Ievaluateanumber

ofmodelsofwealthgoodsproductionagainstthisdataset.Theevidenceindicatesthat

domesticcraftproductionofwealthgoods,inthiscasetheproductionofjadeiteartifacts,

wasmorewidespreadandmorevariedinitsorganizationthanpreviouslybelieved.

1.3 MethodologyandDataCollection

Thepresentstudywasdesignedtospecificallyaddresstheissuesnotedinthe previoussectionthroughacombinationofarchaeologicalsurveyandexcavation.The goaloffieldresearchwastogatherdataonthesystemofjadeartifactproductionfrom theinitialgatheringofrawjadethroughtheprocessingofjadeartifactstothecomplete manufactureoffinishedjadeartifacts.Thesedataareusedtoconstructamodelforthe productionofjadeartifactsintheMiddleMotaguaValleythatprovidesabaselinefor determiningthetechnologicalprocessesandorganizationofproductionofjadeartifacts.

Thesegoalswereaddressedthroughaprogramofsurfacesurvey,surfacecollection,test excavation,experimentalreplicationstudiesandlaboratoryanalysis.

FieldresearchwasconductedintheLowerLatoRiverValley,intheMiddle

11 MotaguaRiverValley,DepartmentofZacapa,Guatemala(Fig.1.1).Ichosethisarea beacuaseapilotsurfacesurveyinJune2004identificatiedfoursurfaceconcentrationsof jadeproductiondebitagenearthemoderntownofGuaytan.Theseincludedangular debitagefromtheinitialreductionofrawjade,aswellasbyproductsofotherproduction techniquessuchasdrilling,grindingandpolishing.

Figure1.1MapshowingMayaarea,withMiddleMotaguaValleyinbox.

12 WiththesupportofFAMSIandthePennsylvaniaStateUniversity,Iconducted systematicarchaeologicalfieldresearchfromOctobertoDecember2005aspartofthe

ProyectodeInvestigaciónSobrelaProduccióndeJadeenelRíoLato(PJ2005).The fieldresearchinvolvedintensivesurfacesurveyof8.5km 2centeringonLowerLato

RiverValleyandlimitedtextexcavationsateightsitescontainingevidenceofjade artifactproduction.Thisfieldresearchwasdesignedtoachieve four objectives:

1) Locate,surfacesurveyandmakesurfacecollectionsatallsitesintheLower LatoRiverValleyandsurroundingarea,aswellastolocatejadesources. 2) Undertaketestexcavationsinareaswithevidenceofjadeiteartifact productiontoconfirmthepresenceof in situ productionactivityandtoobtain samplesfromstratifieddepositswithwhichtodateproductionactivities. 3) Analyzelithicmaterialfromexcavationsandsurfacecollectionstounderstand theprocessofjadeiteartifactproduction. 4) Usetheresultsofthesefieldandlaboratoryinvestigationstoevaluatemodels ofwealthgoodsproductionfortheMiddleMotaguaValley. Aspartofthesurfacesurvey,welocatedandsurfacecollected32sites,butno jadesourcesoroutcropswereidentifiedduringthesurvey;5,375lithicandshellartifacts wererecoveredfromsurfacecollections,includingevidenceofallstagesofjadebead production.ThearidenvironmentandsparsevegetationoftheMiddleMotaguaValley providedidealconditionsfortheidentificationofproductiondebristhroughsurface survey,whichisnotpossibleinmanyotherpartsoftheMayalowlands,wheredense tropicalvegetationobscuresthegroundsurface.Whilethetestexcavationprogramfailed toyield in situ evidenceofjadeartifactproduction,wedidrecoverover5,757piecesof jadeinvariousstagesofproductionfromexcavations,allofwhichproduceddeposits datingtotheLateClassicperiod.

13 1.4 ChapterOrganizationandContent

Chapter 2 presentsthetheoryandmodelsusedbyarchaeologistsinthestudyof

craftproduction.Inparticular,Ifocusondimensionsalongwhichcraftproductionmay

varyinordertoprovideameansforevaluatingarchaeologicalmodelsofcraft production.Indoingso,Ihighlightwaysinwhichthesedimensionsvaryindependently

ofoneanotherinordertohighlightproblemswithcurrentassumptionsaboutcovariation betweenaspects.Chapter2alsooffersanoverviewofdefinitionsandconceptsrelevant tothisresearchinordertoprovideacommonlanguageandlogicforsubsequentchapters.

Chapter 3 providesanoverviewofthesignificanceofjadeinancient

Mesoamericansocietiesanditschronologicaldevelopment.Duringthedevelopmentof

thepresentstudy,Irecognizedthelackofatheoreticalperspectivethatcouldaddress jadeartifactsasbothrestrictedwealthgoodsandgoodsavailabletononelitemembersof

ancientMayasociety.Therefore,Chapter3providesatheoreticalbackgroundand

comparativeperspectiveforunderstandingthevariousrolesthatartifactscraftedfrom jadeplayedinancientMayasociety,drawingonevidencefromarchaeological,

epigraphic,iconographicandethnohistoricsources.

Chapter 4 presentsadescriptionofthemethodsusedandasummaryofthe

findingsofarchaeologicalsurfacesurveycarriedoutintheLowerLatoRiverValley.

Thechapterprovidesanintroductiontothestudyarea,includinginformationofthe

naturalandgeologicalenvironmentoftheMiddleMotaguaValley.Thisisfollowedbya

summaryofpreviousarchaeologicalresearchconductedintheMiddleMotaguaValleyin

general,aswellasabriefsummaryofarchaeologicalresearchconductedinthegreater

southeasternzoneoftheMayaarea.Thebroadscopeofthisinformationisnecessaryfor

14 tworeasons.First,thepresentstudyisoneofthefewstudiestoperformarcheological

researchintheMiddleMotaguaValley.Therefore,abroadreviewofthisinformationis

necessarybecauseofthepaucityofpublishedinformationaboutthearea.Second,the

structureofthelocaljadeproductionindustrycannotbefullyunderstoodwithout referencetoexternalfactorsinfluencingitsdevelopmentandorganization.Afterthis overview,Ipresenttheresultsofthearchaeologicalsurveyandsurfacecollectionsthat werecompletedaspartofthisdissertationfieldresearch.Descriptionsofthesettlement pattersinthesurveyareaarepresented,aswellassummarydataofmaterialsrecovered

fromsurfacecollectionsatthesesites.Iincludetechnologicalcategoriesofjadeartifacts

inthesesummaries;descriptionsofthesecategoriesarefoundinChapter6.

Chapter 5 presentsthemethodsandresultsoftestexcavationsundertakenaspart

ofthisdissertationresearch;fulldescriptionsoftheexcavationsareprovidedin Appendix

B.Inaddition,IsummarizepreviousarchaeologicalexcavationsatthesiteofGuaytan.

Chapter 6 presentsthetechnologicalanalysisoftheprocessofjadeiteartifact productionintheMiddleMotaguaValley.FirstIsummarizehistoric,ethnohistioric,

ethnographicandarchaeologicalevidenceregardingtechnologicalcategoriesrelatedto jadeandotherlapidaryproduction.Ithenmoveontodiscussthetechnologicaltypology

ofjadeartifactsdevelopedbasedonmaterialsrecoveredfromtheMiddleMotagua

Valley.Finally,Ipresentatechnologicalmodelfortheproductionofjadeartifacts, particularlyjadebeads,intheMiddleMotaguaValleyduringtheLateClassicperiod.

Chapter 7 evaluatespreviousmodelsofancientMayawealthproductionand

comparesthemagainsttheevidencefromtheMiddleMotaguaValley.Theevidence

regardingthesocialandtechnologicalorganizationofjadeartifactproductioninthe

15 MiddleMotaguaValleyaresummarizedanddiscussedwithregardtothesemodels.I

arguethatthedatafromthisdissertationfieldresearchdonotmatchexpectationsof currentmodelsoftheorganizationofwealthgoodsproduction.Baseduponthecurrent

evidence,IproposetwomodelsoftheproductionofjadeitewealthgoodsintheMiddle

MotaguaValley,onebasedonapoliticaleconomyandanotherbasedonadomestic economy.

Chapter 8containstheconclusionsforthisdissertationresearchandsuggestions forfurtherworktoclarifythenatureofjadeartifactproductionintheMiddleMotagua

Valley.

Appendix A containsdetaileddescriptionsofallsitesencounteredduring archaeologicalsurfacesurveyintheMiddleMotaguaValley.

Appendix B presentsdetaileddescriptionsofthetestexcavationsundertakenas partofthisdissertationresearch.

Appendix C providesdetailsaboutofthemeasurementstakenaspartofthelithic materialsrecoveredfrombothsurfacesurveyandtestexcavationsduringthe2005field season.

Appendix D presentsdetailsofMiddleMotaguaValleyceramictypesrecovered aspartofthisdissertationresearch,alongwithadescriptionoftheceramicchronology usedtodateexcavationlots.

16 CHAPTER2 APPROACHESTOTHEARCHAEOLOGICALSTUDY OFCRAFTPRODUCTION

Allhumansmustmeettheirneedsanddesiresformaterialgoodsbyproducing themforthemselvesorbyacquiringthemthroughexchangeorthroughdirect expropriationfromothers.Thewaysthattheymeettheseneedsvarywidelyandhas beenamajorfocusofresearchinthesocialsciencesandanthropology.Inparticular, archaeologistshavelongbeeninterestedinancientcraftproduction.Studiesofcraft productionhavebecomeafundamentalpartofarchaeologicalresearchbecauseofthe potentialtheyprovideforexaminingabroadrangeofsubstantive,methodologicaland theoreticalinterests,includingtechnology,materialculture,ecology,economy, sociopoliticalorganizationandpoliticaleconomyinabroadrangeofancientsocieties

(e.g.BrumfielandEarle1987;Childe1951;ClarkandBlake1994;Costin1996;

D'AltroyandEarle1985;Earle1987,1990;Helms1993;Peregrine1991b;Rice1981;

Service1962;Stein1998;Wailes1996).

Despiteavoluminousliteratureonpreindustrialcraftproduction,thereislittle agreementaboutkeyconceptsrelatedtocraftproductionandhowtooperationalizethese conceptsusingarchaeologicaldata.Inaddition,studiesofcraftproductionoftenframe investigationswithinlargerresearchprograms,typicallytheexaminationofexchange systems,politicalstructureandsocioeconomicdifferentiation,ratherthaninvestigating thestructureofcraftproduction before assumingtheexistenceofparticularformsof economicorpoliticalorganization.Further,manystudiesofcraftproductionassume, a priori ,thatthereisanormalandregularlinkbetweenparticularsystemsofcraft

17 productionandparticularformsofsociopoliticalandeconomicorganization(Kenoyeret al.1991:49).

Beforethesereconstructionsaremade,the actual contexts,intensityandmethods

ofcraftproductionneedtobeestablishedusingarchaeologicaldata.Inthisdissertation,I presentevidenceofprehispanicjadeartifactandotherlapidaryproductionintheMiddle

MotaguaValley,Guatemala,duringtheClassicperiod(A.D.300900).Indoingso,I

makenoassumptionaboutthelinkbetweentheobservedpatternsofarchaeological

evidenceofcraftproductionandparticularpoliticaloreconomicstructures.Rather,this

dissertationresearchisanattempttounderstandtheorganizationoflapidarycraft productionintheMiddleMotaguaValley.Althoughthisresearchhasimplicationsfor

ourunderstandingofancientMayaeconomicorganizationandpoliticaleconomy,the primaryfocushereisonestablishingthecharacterofcraftproductionitself.

Inthischapter,Isummarizearchaeologicalapproachestostudyingcraft production.Inparticular,Ifocusonwaysinwhichcurrentdebateshavebeen

unproductiveforcharacterizingandunderstandingsystemsofpreindustrialcraft production.Ibeginbyexaminingthewaysinwhicharcheologistshavetraditionally

approachedstudiesofpreindustrialcraftproduction,particularlywithregardtodebates

aboutthesignificanceofspecializedproduction.Ithenpresentanumberofwaysin

whichtheorganizationofpreindustrialcraftproductionmayvary.Indoingso,Ipresent

abasicframeworkforunderstandingprehispanicsystemsofcraftproductionandtheir

relationshiptobroaderissuesofpoliticalandeconomicorganizationdiscussedinlater

chapters.

18 2.1 ArchaeologicalApproachestotheStudyofPreindustrialCraftProduction

CraftsaredefinedinWebster’sNinthNewCollegiateDictionaryas“theproducts

ofartisticproductionorcreationthatrequireahighdegreeoftacitknowledge,arehighly

technical,requirespecializedequipmentorfacilitiestoproduceandinvolvemanual

labor.”Whilethisdefinitionmaybesufficientformodernconcerns,itisinsufficientfor

recognizingthebroadrangeanddiversityofcraftsproducedorpracticedinpreindustrial

economicsystems.Forthepurposeofthisdissertation,Iadoptadefinitionofcraftgoods

thatencompassesnoncomestiblematerialgoodsthatmaysurviveinthearchaeological

record,thatrequire some degreeofspecializedknowledgeandtechniquestoproduce,and

whosemanufacturewasintendedforoneormoreconsumersotherthan,orincluding,the producerhimselforherself(Sinopoli2003:8).Idefinecraftgoodsinthismanner becauseitleavesopenthepossibilitythatcraftproducersmayproducefortheirown

consumption,fortheconsumptionofothers,orforboth,dependingontheirownneeds

anddesires.Suchadefinitionincludesthe'conventional'craftcategoriesreferredtoby

archaeologistsinterestedincraftproduction,andexcludesothercategoriesthatmightbe

consideredcrafts(e.g.poetry,singing,foodpreparationandvariousservices)whichare

difficulttoidentifyinthearchaeologicalrecord(butseepapersinHrubyandFlad2007

forsomealternativestothisapproach).Thuscraftproductionherereferstothe

“investmentoflaborby(moreorless)skilledpractitionerswholabortotransform potentialintofinishedproducts”(Sinopoli2003:16).

Craftproductionisfoundtosomeextentinallhumansocieties,pastandpresent,

regardlessofsociopoliticalcomplexity(Cobb1993;Cross1993;Sassaman1998).What

hasbeenaparticularconcernformanyarchaeologistshasbeentheappearanceand

19 expansionof specialized craftproduction,particularlybecauseofthewaysinwhichit mayservetolinkcraftproducerswithoneanother,aswellaslinkthemwithnon producers(e.g.Childe1951;Wailes1996).Despitethisimportance,thereislittlegeneral consensusaboutthemeaningsofspecializationandspecialist.Somescholars(e.g.

ArnoldandMunns1994;BrumfielandEarle1987:5;Evans1978;Longacre1999;

Muller1984;Rice1991)definespecializationintermsofadivisionoflaborbetween producerandconsumer.Thekeyelementofspecializationforthesescholarsisthat specialistproducersmeetsome,ifnotmostorall,oftheirsubsistenceneedsfromthe exchangeofthegoodsthattheyproduce.Forexample,Muller(1984:490)definesa

“producerspecialist”assomeonewhose“livelihooddependsonacertainactivity."Such definitionsrelyonanotionofeconomicspecialization,derivedfromearlierworksabout theroleofcraftspecializtioninculturalevolutionbyEmileDurkheim(1893),Adam

Smith(1776),andKarlMarx(1867),thatstressesasocialdivisionoflaborwherevarious specializedproducersaredependentononeanotherwithinalargereconomicsystem(see

Clark1995foradiscussion).

Otherscholarsdefinespecializationintermsoftheratioofproducersto consumersforanyparticularclassofcraftgood(e.g.Clark1995:279;ClarkandParry

1990:297;Costin1991:4,2001:276;Inomata2001:322;ShaferandHester1983;Stein andBlackman1993:29).Accordingtothisperspective,aspecialistissomeonewho

“controlsasetofskillsthatmostofhis[ sic ]communalfellowsdonotcontrol”(Rodgers

1966:410).Suchdefinitionsshiftthefocusofstudiesofcraftspecializationtoan examinationofcraftgoodswherethereisahigherratioofconsumersinrelationto producers.Toexpandonthedefinitionpresentedearlierthen,specializedcraft

20 productioncanbedefinedhereas“theinvestmentoflaborby(moreorless)skilled practitionerswholabortotransformpotentialintofinishedproducts that were in turn consumed by non-producers ”(Sinopoli2003:1,emphasisadded).Keytothisdefinition isthefactthatcraftspecialistsproducemoreofaclassofobjectsthantheyconsume themselves(c.f.Costin2001:276).Further,thisdefinitiondoesnotassumethat specialistsproducegoodstomeetthemajorityoftheirsubsistenceneeds;specialists,by thisdefinition,includeproducersthatexchangeveryfewcraftgoodstosupplementtheir ownsubsistenceproduction.

Despitetheoppositionalpositionsoftentakenindebatesoverthedefinitionof craftspecialization,theseperspectivesneednotbemutuallyexclusive.Craftproducers mayspecializeinthesensethattheyproducegoodsthatfewothersinsocietyproduce whilestillmeetingthemajorityoftheirsubsistenceneedsthroughagriculturalproduction.

Asanalternativetothefull/parttimespecializationdichotomy,Hirth(2009a:18)has recentlyintroducedtheconceptof intermittent crafting toreferto“discontinuousor periodiccraftproductionthattakesplacewithindomesticcontextsalongsideother subsistencepursuits.”Inaddition,householdsmayengagein multicrafting byproducing multiple,butpossiblyrelatedgoods.Characterizingthesevariouscraftsasfullorpart timedoeslittletoadequatelydescribetheirrolehelpinghouseholdsmeettheir subsistenceneeds(seediscussionbelowinSection2.2.1).Forexample,Feinmanand colleagues(Feinman1999;FeinmanandNichols2000,2004;Feinman,Nicholsand

Haines2002)havedocumentedproductionofavarietyofcraftsinClassicPeriod householdsintheValleyofwhichappearstohavebeenperformedasa supplementtonormalhouseholdmaintenanceandsubsistenceactivity.

21 Therefore,itisessentialtomovebeyondtypologicalrepresentationsofcraft productionandspecializationandbegintounderstandthespecificwaysinwhichcraft productionwasorganizedinparticularsocieties.Onlybydocumentingvariationincraft productionsystemswillwebeabletoconstructcrossculturalmodelsthatreflectthe archaeologicaldata.Inthenextsection,Idiscussvariouswaysinwhicharchaeologists haveapproachedthetopicofvariationinsystemsofcraftproduction.

2.2 DimensionsofCraftProduction

Theorganizationofcraftproduction,whether"specialized"ornot,mayvary

alonganumberofimportantdimensions(Costin1991,2001,2005).Theseincludethe

identityoftheproducers,thetechnologyofproduction,thesocialandspatialorganization

ofproduction,thetypesofobjectsproduced,andtherelationshipbetweenproducersand

consumers.Anyparticularsocietymaycontainmultiple,overlappingsystemsofcraft productionandconsumption,rangingfromhighlyvaluablegoodsconsumedbyonlya

limitedsegmentofthepopulationtomorewidelyconsumedgoodsproducedformore

utilitarianormundanepurposes.Thesocial,political,spatialandtechnologicalcontexts

ofcraftproductionmaysimilarlyvary,buttheremaybelittlecorrespondencebetween

variationinthecontextsofproductionandthetypeofgoodsbeingproduced.

Inthefollowingsections,Idiscusssomewaysinwhichtheorganizationofcraft productionmayvary,providingarchaeological,ethnohistoricandethnographicexamples

toillustratethisvariation.Inparticular,Ifocusonaspectsofcraftproductionvariability

thataregermanetothisdissertationresearch:(1)productionmethodsandtechnology,(2)

scaleandstructureofproductionunits,(3)thenatureofthegoodsproduced,and(4)

22 sociopoliticalcontextofproduction.Archaeologicalmodelsofcraftproductionoften

expectcovariationamongthesedimensionsofvariation,whichhaveledtoanumberof

inappropriateexpectationsofparticularformsorsystemsofcraftproduction(c.f.

Feinman1999;Hirth2006,2009a).Thisisbynomeansanexhaustiveoverviewof

archaeologicalcraftproductionstudies,butisintendedtoprovidethereaderwitha backgroundforlaterdiscussionsofcraftproductioninMesoamericaingeneral,andin theMayaareainparticular.

2.2.1 TechnologyandCraftProduction

Craftproductionfundamentallyinvolvestheuseoflabor,skillandtechnologyto transformrawmaterialsintofinishedproducts.Technologycanbeunderstoodasthe seriesofstepsthatareinvolvedinthistransformation,includingboththeknowledgeof theproductionprocessandthetoolsusedtoeffectthistransformation(e.g.Merrill1968:

576577).Technologycanrangefromsimpletechniquesusingadhoc oreasily procured/producedtools,tocomplexproductionsequencesinvolvingspecializedtools andfacilities.Therefore,examinationsofpreindustrialsystemsofcraftproductionneed toconsiderthetechnologiesinvolvedintheproductionofparticularcrafts,andthe possibilitiesandconstraintstheypresentforvariationinproduction(e.g.Arnold1985;

Underhill2002;vandeLeeuw1976).Despitethepossiblerangeofvariationin productivetechnologies,artisanswithknowledgeofaproductionprocesswillbelimited intheirabilitytopracticeparticularcraftsby(1)theavailabilityofrawmaterials necessaryfortheproductionprocess,(2)theneedforspecializedfacilitiestopractice particularcraftsand(3)theavailabilityoftoolsnecessaryforproduction.

23 Anumberofresearchershaveattemptedtoexplaindifferentialparticipationin craftproduction(i.e.whyinsomesocietiesonlyalimitednumberofpeopleundertake productionofcertaingoods)intermsofecologicalandenvironmentalconditionsand demography(e.g.Arnold1985;WilsonandBlinman1995).Suchadaptationalist approaches(Costin2001a:307308)explainsuchdifferentialcraftproductioninrelation totheabundanceorscarcityofparticularresources,suchasadequateagriculturalland

(Hagstrum2001;Halstead1989)andlocalavailabilityofmaterialsneededforparticular crafts(Arnold1987;ArnoldandMunns1994;Muller1997).Viewedfromanother perspective,theabilitytopracticecertaincraftsmaybe facilitated bythelocal availabilityofrawmaterialsnecessaryfortheproductionofparticularcraftgoods, regardlessofpressuretoadoptcraftproductionfromdemographicorenvironmental circumstances.Forexample,thepresenceofabundantrawmaterialsnecessaryforthe productionofshellbeads(purpleoystershellandchertformicrodrills)ontheChannel

IslandsofCaliforniaisarguedtohavestimulatedthedevelopmentofintensiveshellbead productionontheislands(Arnold1987;ArnoldandMunns1994).Thus,givensufficient demandforparticulargoods,artisansmaypracticecraftproductionasaresultof opportunitiesaffordedbylocalavailabilityofrawmaterials,especiallywhencrafts requirelittlespecializedknowledgeortools.

InthisdissertationIdealwithlapidaryproductionofstoneandshellartifacts, whichinvolvesareductivetechnologicalprocessinthesensethatgoodsareproducedby removingfragmentsfromrawmaterials,ratherthancombiningrawmaterialstoproduce finishedgoods.Althoughtheskillsneededtocraftdesiredgoodsmaybecomplex

(especiallywhenartifactformsordesignsrequirespecializedknowledgeoriconography

24 toexecuteproperly),thetoolsandrawmaterialsneededforlapidaryworkneednotbe

complexorelaborate.Thetechnologicalbasisoflapidaryproductionminimallyinvolves

theapplicationofabrasivesofsufficienthardnesstostoneorshellinordertoproduce finishedgoods(seediscussioninChapter6).Whilethischaracterizationoflapidary productionmaybeoverlysimplistictodescribethetechnology(i.e.skill)involvedinthe productionofintricatelycarvedgoods,itcertainlyappliesbroadlytotheproductionof simplelapidarygoodssuchasbeads.Thus,theabilitytopracticesimplelapidary productionasacraftislimitedbytheavailabilityofsufficientsuppliesofabrasive materialandrawmaterials(e.g.shellandjadeandotherstones)fromwhichtoproduce finishedgoodswhicharedesiredbyothers.Thiscanbecontrastedwiththepracticeof jadelapidaryproductioninChina,wheremetalandwheeldriventoolswereavailable, whichallowedforagreaterelaborationofartifactforms(Hansford1950:fig.11;Saxetal.

2004).

Simpletechnologiesmayalsofacilitatetheeasewithwhichcraftproducersmay expandtherangeofgoodstheyproduceorthecraftstheypractice(Feinman1999;Hirth

2009b).Recently,Hirth(2006,2009a)andShimada(2007)haveusedtheconceptof multicrafting torefertoproductionby"thesameorcloselyrelatedartisansperforminga majorpartortheentiretyoftwoormorecraftsinvolvingdifferentmediaorrawmaterials incloseproximitytoeachothertoproduceitemsprimarilyforsuprahousehold consumption"(Shimada2007:5).Forexample,craftsbasedonsimilartechnologies, suchasshellandstonebeadproduction,maybeundertakenbythesamecraftproducers

(Feinman1999)using intersecting technologies (c.f.Hagstrum1992)thatinvolvemany ofthesametoolsandtechnologicalprocesses.Thispointisimportantbecausemost

25 studiesofcraftproductionsystemstendtoconsiderdifferentcrafts(e.g.ceramics,textiles, stonetools)asdistinctanalyticalcategories,ratherthanaddressingtherelationships amongthem(Shimada2007:3).AsIargueinthefollowingsection,archaeologistsoften inappropriatelylinkcharacterizationsofthesimplicityorcomplexityofcraftproduction technologytootherdimensionsofcraftproductionvariation,suchasthecontextof productionorthetypesofcraftgoodsproduced(Hegmon1998:278).

2.2.2 CraftProductionUnits

Oneofthemostbasicunitsofproductioninallhumansocietiesisthehousehold,

whichisorganizedtomeettheeconomicandsocialneedsofitsmembers(Hirth2009a;

Wilk1989).Whileindividualsarecertainlyimportanteconomicactors,itisthe

householdthathasservedasaprimaryfocusofeconomicactivityforpeoplein preindustrialagrariansocieties.Ethnographicandhistoricaccountsdemonstrate

tremendousvariabilityinthesize,compositionandstructureofcraftproductionunits

acrosstimeandspace(e.g.D.Arnold1985;Hassig1985;Matson1965;Nadel1942;

Peacock1982;RyeandEvans1976;Spence1981;Stark1985).Whilemanyscholars

recognizetheimportanceofhouseholdproductionformeetingtheinternalsubsistence

needsofhouseholdmembers,manyarchaeologicalstudieshavefocusedgreaterattention

onotherproductionunitswhenconsideringancientsystemsofcraftproduction.

Inaninfluentialandoftcitedpaper,vanderLeeuw(1977,seealso1984) presentedasixpartmodelofcraftproduction,drawnfrom(primarilyOldWorld)

ethnographicandhistoricdescriptionsofpotteryproduction.Subsequently,hismodel

wasslightly,thoughnotsignificantly,modifiedbyothers(Peacock1982;Rice1981;

26 Santleyetal.1989).Thesemodelsdescribeaseriesofproductionarrangements,defined primarilybythenatureandcompositionofprimaryproductionunits(e.g.household,

workshop,factory;seeTable2.1below).Inthem,householdproductionispresentedas

themostbasicformofproduction,andischaracterizedassmallinboth scale (ameasure

oftherelativesizeoftheproductionunit)and intensity (ameasureoftheoutputof production)(vanderLeeuw1977:72,Table1;1984:Fig.1).Householdproductionis

furthercharacterizedas"parttime"(Santleyetal.1989:108)or"occasional"(vander

Leeuw1984:722,Fig.1),"amateur"inskillorexecution,andusingsimple,impermanent

technologies.Incontrast,higherorderproductionunits(e.g.workshopsand

manufactories)arecharacterizedby"fulltime,"highintensityproduction,dedicated productionfacilitiesandlargerworkgroups,madeupofindependetspecialists.

vanderLeeuw(1977,1984) Santleyetal.(1989) Largescaleindustry Manufactory Villageindustry Nucleatedindustry Workshopindustry Workshopindustry Individualindustry Tetheredspecialization Householdindustry Householdindustry Householdproduction Householdproduction Table2.1Modelsofcraftspecialization.

Suchtypologies,whileusefulforbringingordertoanarrayofcrosscultural productivearrangements,areinappropriateforunderstandingvariabilityincraft productionwithinparticularsocieties.Particularly,suchmodelsimproperlygroup

dimensionsofvariabilitythatoughttobekeptanalyticallydistinct.Forexample,the

termhouseholdproductionisadescriptionofthecontextorlocationoftheproduction

unit,andhasnodirectandinvariantrelationshipwithotherdimensionsofvariabilityof

27 craftproduction,suchasintensityofproductionorthenatureofgoodsproduced.

Nevertheless,standardmodelsofcraftproductionunitsmuteandsubsumevariabilityand

hinderourabilitytoaccuratelycharacterizepreindustrialsystemsofcraftproduction.I

arguethatsuchtypologiesofcraftproductionunitsneedtobeunboundfromtheother

measuresofvariabilityincraftproduction,andneedtobeconsideredseparatelyfromone

another(Costin1991,2001;Feinman1999;FeinmanandNicholas2000;Hirthn.d.;

Shimada2007).Therefore,Iconsiderhereanumberofwaysinwhichcraftproduction

unitsthemselvesmayvary,bothspatiallyandsocially.

2.2.2.1SpatialandSocialOrganizationofProductionUnits

Theidentificationoflociofcraftproductionisimportantbecausetheyprovide basicinformationaboutthephysicallocationofcraftingandcluesaboutthesocial organizationofcraftproduction.Craftproductionlociaredirectlyidentifiedusingthree primarylinesofarchaeologicalevidence:(1)productionrelatedfacilities,(2)tools,and

(3)debris.Formalproductionrelatedfacilitiesarerarelyencounteredinpreindustrial systemsofcraftproduction.IntheNewWorld,thesefacilitiestypicallyincludefeatures suchaskilnsusedforpotteryproductionandmetallurgy(Arnoldetal.1993;Goldstein andShimada2007;Santleyetal.1989;ShimadaandMerkel1991).Nevertheless,as

Santleyetal.(1989:110)caution,lackofpermanentfiringfacilitiesdoesnotprecludethe presenceofpotteryproduction(seeMaldonado2007forasimilarargumentconcerning copperproductionintheTarascanempire).NewWorldlapidaryproductionhowever,is unlikelytohavebeenaccomplishedusingspecialpurpose,permanentfacilities,owingto thelimitedtechnologyassociatedwithsuchproduction(seeSection2.2.1above).

28 Therecoveryofproductionrelatedtoolsisasecondlineofevidenceusedto

identifylociofcraftproduction.Forlapidaryproduction,archaeologicallyrecoverable toolsmayincludestonehammerstones,mortarsforpreparingabrasives,chisels,adzesor axes,scrapers/abraders,saws,awls,microdrills,polishersandblades(Arnold1987;

FlanneryandWinter1976:39;Yerkes1983,1989,1991).Metaldrillsandsawswere alsolikelyusedwhereavailable;Sahagún(15471558)mentionstheuseofmetaltools forPostclassicperiodAzteclapidaries(DibbleandAnderson1959:7982).

Identificationoftheselapidarytoolsmaybeproblematichowever,assomemayhave beenusedforpurposesotherthanlapidaryproduction,andthereforemayhavebeen recycledorcuratedinwaysthatwouldreducetheirvisibilityinthearchaeologicalrecord

(Aldenderfer1991).Further,perishablelapidarytoolsofwood(Clark2006)orbone

(Holmes1919:351352)mayhavebeenusedinplaceoffunctionallyequivalentstone andmetaltools(alsoKidder,JenningsandShook1946;Widmer1991).

Finally,manufacturingbyproductsordebris(i.e.debitage)arethemost frequentlyusedlineofevidenceforidentifyinglociofstonetoolandlapidaryproduction.

Manufacturingdebrismayinclude:exhaustedorpartiallyworkedcores;partiallyworked stoneorshellartifacts;toolsorornamentsbrokenintheprocessofproduction;and chippedstoneflakes.However,identificationofproductiondebrisisnotunproblematic orstraightforward.Forexample,caremustbetakentodistinguishtoolsorornaments brokenduringproductionfromthosebrokenduringorafteruse.Further,datafromthe archaeologicalandethnoarchaeologicalstudiescautionagainstuncriticallyequatingthe lociofrecoveryofproductiondebriswiththephysicallocationofpastproduction

activity(Clark1986,1990;DealandHayden1987:288;MoholyNagy1990,1997;

29 SantleyandKneebone1993;Schiffer1987).Identifyingmanufacturingdebrisassociated withthefinalstagesoflapidaryproduction(e.g.grinding,carvingandpolishing)canbe

especiallyproblematic,asthesestagesproduceverylittleinthewayofmacroscopic

debitageotherthanbrokenpiecesintheprocessofmanufacture,andinsteadproduce microscopicpiecesasanobjectisabradedintoshape(Chenault1986).Analternative approachhasbeentousemicroscopicanalysisofintactfloordepositstoidentifyprimary locationsoflapidaryproduction(Feinman1999;FeinmanandNichols2000;Kovacevich

2007;Widmer1991).

Reliableidentificationofcraftproductionlocimustthereforerelyonsome combinationofthesethreelinesofevidence.Iftoolsassociatedwithlapidaryproduction

(e.g.microdrills,polishers)arefoundindirectassociationwithbyproductsoflapidary production(e.g.unfinishedorbrokenartifacts,debitage),itisreasonabletoproposethat productiontookplacewithinthevicinity(c.f.Clark1990).Whensuchaccumulationsare foundwithinclosespatialproximitytoidentifiablestructures,itmaybepossibletoinfer acorrespondencebetweenthetwo,particularlyforsmallscaleproductionloci,suchas householdsinnonurbanenvironments(SantleyandKneebone1993:45).

Oncecraftproductionlociareidentified,archaeologistsneedtoidentifythe

spatialcontextand"concentration"(c.f.Costin1991:1315)ofproductionby

characterizingtherelativedispersaloraggregationofproductionloci.Contextrefersto

theactuallocationofproduction,whileconcentration“describestherelativedispersalor

aggregationofproducersservingadefinedgeographicareaorpopulation”(Costin2001:

295).Concentrationofproductionmaybeinfluencedbyanumberoffactors,including:

accesstorawmaterialsneededforproducts,toolsorproduction(e.g.ArnoldandMunns

30 1994;ShaferandHester1991;alsoseeSection2.2.1);accesstolabor(e.g.Kenoyeretal.

1991);accesstotransportationroutes;orlocationofconsumersorsponsors(Hayashida

1995).Therefore,concentrationmayvaryfromthepresenceofmanyproducersevenly

distributedthroughoutagivenpopulationtodenseconcentrationsofproducersina definedlocation.

Concentrationofcraftproductioncanalsovaryintermsofscale(smalltolarge) andinternalsocialcomposition(kinbasedtononkinbased)ofindividualproduction units,andcanincludedomestichouseholds,workshopsandmanufactories.Scaleisoften definedintermsoftherelativephysicalsizeofthestructuresorfacilitieswithwhich productionevidenceisassociated(e.g.vanderLeeuw1977,1984;Peacock1982).Scale andinternalsocialcompositionareoftenassumedtocovary,suchthatsmallscale productionunitsarecomposedofkinmembers,whilelargerscaleproductionunits consistofnonkinworkgroups(Santleyetal.1993:110;vanderLeeuw1984:756).

Whileitisreasonabletoassumethatsmallscaleproductionunitswerecomposedofkin basedworkgroups,itisnotclearthatlargerscaleproductionunits,suchasworkshops, werenotsimilarlycomposed.Forexample,intheearly20 th centuryNupekingdomof

Nigeria,blacksmithworkshopswereoftenstandalonefacilitiesnearfamilycompounds

(i.e."medium"to"large"scale)inoperationyearround,andwereoperatedbymembers

ofthesamefamily(i.e.kinbased)(Nadel1942:263264).Therefore,researchersmust becarefultodisentanglethedimensionsofscaleandinternalsocialcompositionwhen constructingmodelsofpreindustrialcraftproduction(seeAmes1995;Janusek1999).

31 2.2.3 TypesofGoodsProduced

Moststudiesofpreindustrialsystemsofcraftproductionmakedistinctionsamong avarietyofclassesofgoodsbasedontheirperceivedvalue,utilityandmeaninginpast societies.Commonly,adistinctionismadebetweentwogeneralclassesofgoods:so calledwealthgoodsandutilitarianornecessarygoods.Indrawingthisdistinction, scholarspositafundamentaldivergenceinthenature,productionandvalueofthegoods inquestion.Utilitariangoodsareoftendefinedasthosethatsatisfybasichousehold subsistenceneeds,andarevaluedandusedbyallmembersofagivensocietyfor biologicalandsocialends(Brumfiel1987;BrumfielandEarle1987:4).Othertermsthat appearinthecraftproductionliteratureinclude"staples"(D'AltroyandEarle1985),

"practicaltechnologies"(Hayden1998),and"subsistencegoods"(BrumfielandEarle

1987).Regardlessofthetermapplied,allpointtotheusefulnessofthesegoodsfor humanphysicalsurvival,andemphasizethattheiruseorpossessionisnotlimitedby customorlawtoparticularclassesofindividualswithinsociety.Inthisdissertation,I usetheterm"utilitariangood"torefertotheseobjects,despiteproblemsofdistinction

(notedbelow).

Incontrast,wealthgoodsareseenasthoseartifactsorobjectsthatareusedin

"display,ritual,andexchange"(BrumfielandEarle1987:4),particularlyasmarkersof socialidentity(Peregrine1991:1),andarelimitedintheirdistributiontoonlycertain classesofpeoplewithinsociety.Wealthgoodshavealsobeenreferredtoas"prestige goods"(Costin2001b;FrankensteinandRowlands1978;Hayden1998;Junker1993;

Peregrine1991),"luxuries"or"luxurygoods"(Appadurai1986;BlantonandFeinman

1984;Childe1951;Inomata2007),"primitivevaluables"(ArnoldandMunns1994;Earle

32 1982);"preciosities"(Wallterstein1976)and"elitegoods"(Wells1982).Inthe archaeologicalliteratureoncraftproduction,thesetermsareoftenusedinterchangeably andarerarelyexplicitlydefined,despitethefactthateachtermimpliesaparticularkind ofvalue,meaningoruseforthegoodsorobjectsbeingdescribed(FladandHruby2007:

10).

Nevertheless,allofthesetermsshareabroadsimilarityinthatthegoodsinvolved areseenas(1)desiredbymanybutrestrictedindistribution(bylaworprice)toalimited grouporclassofindividuals("elites");(2)beingsemioticallyrich(i.e.capableof communicatingcomplexmessages,c.f.Appadurai1986:38);and(3)capableofbeing controlled.Inthisdissertation,Iusethegeneralterm"wealthgood"torefertothese classesofartifactsfortwoparticularreasons.First,thetermleavesopenthepossibility thatthegoodsmaysimultaneouslypossessbotheconomic and socialvalue,meaningand utility.AsIdiscussfurtherinChapter3,goodscraftedfromjadeitewerecharacterized bygradationsofvalue,withsomejadeitegoods(suchasbeads)distributedmoreevenly thanothers(e.g.carvedpendantsanddiadems).Thus,differentartifactformsmayhave beendistributedandconsumedindifferentways.Second,Iwishtoavoidinterpretive problemsrelatedtotheterm"prestigegood,"whichimpliesaparticulartypeof"prestige goodssystem"inwhichsuchgoodsareneededforsocialreproduction(c.f.Frankenstein andRowlands1978;Meillassoux,1978).Specificdistinctionssuchastheseneedtobe demonstratedforparticularcultures,agoalthatisnotfeasibleinthisdissertation.

Becausethefocusofthisstudyistheproductionjadeitewealthgoods,Inowdiscusshow suchgoodsmightbeidentifiedarchaeologically.

FollowingtheworkofHelms(1993),somescholarshavearguedthatwealth

33 goodsaretypicallymanufacturedfromexotic,nonlocalrawmaterialsorinvolvehigh

inputsoflabortoproduce(Earle1987:89;Flannery1968:100;Rathje1972;Peregrine

1991).Wealthgoodsmanufacturedfromnonlocalrawmaterialsareseenasenhancing

socialstatusbecauseofthemessagesthattheycommunicateregardingtiestoforeign

(andmystical)landsandpeoples(Helms1993:7),whilethoserequiringhighlaborinputs

orgreatskilltomanufacturetestifytoanenhancedabilitytocontrolorotherwisedirect

thelaborofothers(Meillassoux1978).Thecommonassumptionofthesemodelsisthat

theyarguethatwealthgoodsarethosethatinvolvegreatlaborinput,eitherinthe procurementofmaterialsorthemanufacturingofthefinishedgoods.Furthermore,they positthatthesecharacteristicsallowthemtobemoreeasilycontrolledbyelites,thus reinforcingtheirvalue.

Ekholm(1972:100)defineswealthgoodsas“productswhichwerenotneededfor actualmaterialsupportoflife,butweredefinitelyneededforsocialandpoliticalposition withinthesociety.”Thoughwealthgoodsarenotnecessaryfortheeveryday provisioningofhouseholds,somemaybemanufacturedinformssimilartoutilitarian

goods.Clark(1996:193)callstheseitems"hypertrophic"goodsthatare"unusableas

toolsbecausetheyaretoofragileorelaboratelydecorated."Insomecasesthesegoods

aremanufacturedfromvaluable,nonlocalmaterialsthatmaybeexpensivetoprocure.

Forexample,inthehighlandsofPapuaNewGuinea,large(2030cmlong)axes,

unsuitableforagriculturalwork,wereassembledandusedinbridewealthtransactions,

andservedasasymbolofwealthandsocialpositionforthosethatpossessedthem

(Burton1989;Strathern1971:105).Modernexamplesmightincludeitemssuchasfine

chinathatconveysocialmessagesregardingprestige,wealthandtaste.

34 Basedonacrossculturalethnographicstudy,Peregrine(1991)arguesthat archaeologistsneedtoexercisecautioninidentifyingwealthgoods.Focusing specificallyonethnographicallyknownprestigegoodssystems,heidentifiedfourbasic categoriesofgoodsthatareheretermed"wealthgoods":(1)fursandotherrawmaterial;

(2)shellbeads(especiallystringsofshellbeads);(3)personalornamentsofdurableand preciousmaterials;and(4)larger,morecomplexpersonalornamentsmanufacturedfrom plantandanimalmaterialssuchasfeathersandplantfibers(Peregrine1991:4).

Interestingly,hefoundthatceramicsdidnotfunctionasprestigegoods,possiblybecause oftheirnecessityandtotheeasewithwhichtheycouldbeproduced.Thisfindingruns contrarytoargumentsfortheClassicMaya,whereanumberofscholarshavearguedthat elaboratelydecoratedceramicvesselswereusedtosolidifyintereliterelationships,and insomecasestomaintaintheloyaltyofcommoners(LeCount1999;ReentsBudet1994,

1998;Rice2009).

Thereareofcourse,othermeansbywhichstatusandprestigedifferencesmaybe expressed,suchasthroughgreaterelaborationofdomesticarchitectureorthroughthe sponsoringofpublicworksofvariouskinds.Theparticularmixofstrategieschosenfor markingstatusdifferencesvarywidely,buttheywouldbeexpectedtoberedundantwith eachotherinmarkingtheenhancedprestigeorstatusofparticulargroupsorindividuals.

Thus,whenattemptingtoidentifyprestigegoodsinthearchaeologicalrecord,care shouldbetakentoexamineredundancyofthesegoodswithotherpotentialmarkersof prestigeorstatus.Simplyshowingthataparticularartifacttypehasadifferential distributiondoesnotdemonstratebyitselfthatitservedasawealthgood.A demonstrationoftheartifacttype'sredundancywithotherproposedwealthgoodsand

35 withothermeansofmarkingstatusisneeded.Ifsuchredundancycannotbe

demonstrated,thenthereisthepossibilitythattheartifacttypeinquestionmayhave

servedotherpurposes,suchastomarksocialgroupaffiliation,occupation,orsomeother

socialrole.

Thecontextinwhichtheyarefoundisanotheressentialcriterionfortheproper

identificationofwealthgoods.Becausetheywerehighlyvalued,itisunlikelythat

complete,finishedwealthgoodswillbefoundregularlyindomesticmiddens.However, wemightexpecttofindevidenceoftheproductionofwealthgoodsinmiddens,

especiallywhentheirforms,andnotthematerialfromwhichtheywereproduced,was

whatwasconsideredvaluable.Conversely,iftherawmaterialiswhatwasvalued,we

mightexpectthatbyproductsfromproductionmightbecuratedorotherwisetakenoutof

circulationbyinclusionincachesorburials(MoholyNagy1997).Furthermore,if particularformsofwealthgoodsweredesiredorrequired,wemightalsoexpecttosee productioncontrolledorsponsoredinsomeway,andissuetowhichInowturn.

2.2.4 SociopoliticalContextofProduction

Thesociopoliticalcontextofproductionreferstothelocationofproductionin

socialspace(c.f.Costin2001a:297),includingthesocialrankorstatusorartisans,and

therelationshipofproducerstoconsumers.Inmodelsofcraftproduction,thesetwo

dimensionsofproductionareoftendiscussedtogether,andassuch,Iwilladdressthem

simultaneouslyinordertohighlightsomewaysinwhichmodelslinkingtheseconcepts

havecausedinterpretivedifficultiesforunderstandingparticularsystemsofcraft production.

36 Inahighlyinfluentialandfrequentlycitedmodelofcraftproductioninancient

societies,BrumfielandEarle(1987;alsoEarle1981)dichotomizecraftproductionbased

onthenatureofthegoodsproduced(addressedaboveinsection2.2.3)andthedegreeto

whichproductioniscontrolledbypoliticalelites.Intheirmodel,theyarguethat

everydayutilitariangoodstendtobeproducedbyindependentspecialistswhoproduce

forgeneraldemand,whileprestigeorwealthgoodstendtobeproducedbyattached

specialistswhoproduceforpatronsondemand(BrumfielandEarle1987:5;alsoCostin

1991:7172).Thus,independentproductionisdepictedfromtheperspectiveofthe producerandseenasmotivatedbyadesireforprofit(howeverdefined),whileattached productionisoftenviewedfromtheperspectiveofthesponsorandseenasbeing motivatedbythedesiretocontroltheproductionprocess(Costin2001a:298).As

Hayashida1995:12)pointsouthowever,thesearetwodifferentkindsofproduction,not endsonacontinuum(astheyareoftendepicted),anditisoftendifficulttofitparticular caseswithinthisframework.Itisbetter,therefore,toexaminewaysinwhichthe motivationforproductionandthecontroloffinalproductsvariedindividually,rather thanassumingthattheyvarieduniformly.

Costin(2001a:298)arguesthatintheseterms,somedegreeof"attachment"of producertoconsumerexistswhendecisionmakingaboutanyaspectofproductionis madebyindividualsorinstitutionsoutsideoftheproductionunit.Thiscaninclude decisionsaboutrawmaterialsortechnologiesusedinproduction,theorganizationofthe productionunit,thestyleorappearanceofthegoodsproduced,ortheultimate

distributionoffinishedgoods(Costin2001a:298).However,ClarkandParry(1990:298)

notethatwhileattachedproducersareobligedtomanufactureparticulargoods,no

37 physicalcontrolofproducers,theproductionprocess,orthetotaloutputofproducersis implied.Santleyetal.(1989:108)usetheterm"tetheredspecialization"inasimilar mannertodescribeproduction"foreliteuseorconsumptionbythestateinstitutional system,eitheronacommissionedbasisorasaresultofobligationsowedtospecific highrankingindividuals."Themostcommondistinctioniscontrolofthedistributionof finishedproducts,whichisanaspectofdistribution,andnotproductionperse.

Costin(1991:25)suggeststhatcontrolofproductionbyattachedproducerswill oftenhavecleararchaeologicalcorrelates.Forexample,shearguesthat"workshopsof attachedspecialistsmostoftenarephysicallyassociatedwithelitedomesticstructuresor governmentfacilities[or...]maybephysicallyseparatedfromotheractivityareas,in placeswhereaccesscanbeeasilymonitoredoraccessrestricted."Anumberof ethnographicallyandarchaeologicallyknownexamplesofthistypeofsituationcanbe provided,includingthoseoftheInka(Costin1991),Hawaii(Earle1987)andClassic

Maya(Inomata2001;Widmer2009).Nevertheless,asnotedearlier,productionneednot bephysicallycontrolledormonitoredinordertobeconsidered"attached"(Stein1998:

20)

Sponsorshipofattachedspecialistsisnottheonlymeansopentoelitesfor

controllingproductionanddistributionofprestigegoods.Elitesmayalsocontrol

distributionthroughthemobilizationoffinishedgoodsfromdispersedproducersinthe

formoftribute.SuchastrategyisknownforanumberofprehispanicNewWorld

societies,includingtheAztec(Brumfiel1987;Berdan1992,1994)andtheInca(Costin

1996;Earle1987).Undersuchastrategy,individualhouseholdsarerequiredto

contributeaspecifiedamountofparticulargoodsforusebyelitesorstateinstitutions.

38 Forexample,womeninconqueredprovincesoftheIncaempirewererequiredtoprovide

threadandclothtothestateforuseinthepoliticaleconomyandaspaymenttoimperial beauracrats(Costin1998). Thegoodsproducedundersuchasystemaretypically

manufacturedfrommaterialsavailabletononelitehouseholdseitherthroughdirect procurementortradeandexchange.Furthermore,theyaregoodsthatmaybeproduced byagreatmanyhouseholdsbecausetheyeitherdonotrequireagreatdealofskillto produceordonotrequiretheuseofcomplextechnologies.Undersuchasystem,we

wouldexpecttofindevidenceofproductiondispersedamonghouseholdsregardlessof

socialrankorstatus.Inaddition,wewouldexpectthatthosehouseholdsshowing

evidenceofproductionwouldconsumeonlyasmallproportionoftheirproducts.

CharacterizingstrategiesforthecontrolofwealthgoodsproductionasIhave

doneheredoesnotprecludethefactthatanyparticularsystemmayhaveinvolvedallof

thesestrategiesatonce.Forexample,withintheTarascanempire,metalobjectsusedas

ceremonialandwealthgoodswereproducedbyattachedspecialistsandmobilizedinthe

formoftributefromnonelites(Pollard1987).Theparticularstrategyorstrategiesthat

wereemployedarehighlydependentonthemeansavailabletoelites(Hirth1996).In

fact,asrecentevidencesuggestsfortheancientMaya(discussedinChapter7),theremay

havebeenmultiplestrategiesemployedintheproductionofwealthgoods.

Nevertheless,demonstratingthesocialrankorstatusofproducersandthedegree

ofcontrolexertedontheproductionprocessmaybeparticularlydifficult.Untilrecently,

craftproducersinpreindustrialsocietieshaveoftenbeendepictedassociallyor

economicallymarginal(e.g.Rice1981).However,itisincreasinglyevidentthatthe

statusofproducersandtheirabilitytonegotiatethetermsoftheirproductionvaried

39 widely,andcraftproductionbyeliteshasbeenreportedinawiderangeofsocieties

(Ames1995;Brumfiel1998;Costin1993;Inomata2001;Lass1998;ReentsBudet1994,

1998;Sinopoli2003).Identifyingthesocialrankofproducersmaybemore

straightforwardwhenevidenceofcraftproductionisrecoveredfromdomestic,nonelite

contexts(e.g.Wattenmaker1998;Feinman1999).Thetaskisconsiderablymore

difficultwhenproductionevidenceislocatedwithineliteornondomesticcontexts.The

interpretivedifficultiesareexemplifiedbyArnoldandSantley(1993:242)whenthey

arguethatkilnfiredceramicproductionatanelitehouseholdatMatacapanwasdoneby

nonelitecraftworkers,ratherthanbytheeliteresidentsthemselves,despitealackof

evidencetosupportthisclaim.

Identifyingthesocialstatusofproducersdoesnotnecessarilydemonstratethe

natureoftheproducerconsumerrelationship.Demonstratingattachedproduction

requiresevidenceofboththecontextsofproductionANDconsumption.Inotherwords,

archaeologistsmustdemonstratethatproductionlevelssurpassedtheconsumptionlevels

ofindividualproductionunits.Intheabsenceoflargescaleexcavationshowever,sucha

determinationmaybedifficult.Thisisespeciallytruewhenoneconsidersthatproducers

mayretainrightstothedistributionorconsumptionofaportionofthegoodsthey produce(Hayashida1995:17).

2.3 ConcludingComments

Archaeologistshavelongrecognizedtheimportanceofcraftproductioninthe structureandfunctionofcomplexsocieties.Nevertheless,thematerialevidenceforcraft productionispotentiallyambiguousbecauseofthevariouswaysinwhichcraft

40 productionsystemsmaybeorganized.Thisvariation,andtheambiguityofthe archaeologicalevidence,hasgeneratedagreatdealofdiscussionregardingthestructure ofthesesystemsofcraftproduction.

Inthischapter,Ihavefocusedonsomedimensionsalongwhichpreindustrial systemsofcraftproductionmayvary,particularlywithregardtothetechnologyof production,theorganizationofproductionunits,thenatureofgoodsbeingproducedand thesociopoliticalcontextofproduction.Thetechnologyinvolvedintheproductionof particularcraftsmayvaryalonganumberofdimensions,includingtheskillsneedto practiceacraft,theavailabilitytoolsandrawmaterialsneededforproductionandthe possibilityofproducingitemswithmultiplerawmaterialsusingintersectingtechnologies.

Variationinthesedimensionsmayinfluencetheabilityofindividualsandhouseholdsto practiceparticularcrafts.Theorganizationandstructureofthephysicallociinwhich productiontakesplacemayvaryfromdomestichouseholdcontextstotheuseof specializedfacilitiesinwhichindividualproducersmaynotberelatedbytiesofkinship.

Thetypesofgoodsproducedmayrangefromgoodsneededforphysicalsurvivaltothose thathavenodirectbearingonphysicalsurvival,butratherhavemoreprimarysocial significance.Thesegoodsmaybemoreorlesselaborateandmayinvolvetheuseraw materialsthatareeasyordifficulttoacquire.Finally,craftproductionsystemsmayvary intermsofthedegreeofattachmentandsociopoliticalrelationshipbetweenproducers andconsumers,althoughthesemaynotvary directly withtheoveralloutputofproducers.

Therearemanymoredimensionsthatmightbeaddedtothesecontinua,butthose discussedinthischapterpresentaframeworkforaddressingvariationintheorganization ofpreindustrialsystemsofcraftproduction,especiallywithregardtolapidarywealth

41 goodsproduction.Usingthesedimensions,itshouldbepossibletodiscussparticular systemsofcraftproductionandcomparethemtoseehowandifthesedimensionsco vary,particularlywiththegoaloflinkingthesystemsofcraftproductiontootheraspects ofpolitical,culturalandeconomicvariation.

Inthefollowingchapters,Iexaminetheproductionofwealthgoods(particularly jadeiteartifacts)inprehispanicMesoamerica,particularlyinreferencetotheClassic periodMayasociety.Indoingso,Iexaminevariabilityinthedimensionsofcraft productiondiscussedinthischapter,andtheimplicationssuchvariationhasfor

understandingprehispaniceconomicandpoliticalorganization.

42 CHAPTER3 JADEANDITSSIGNIFICANCEINPREHISPANICMESOAMERICA AlthoughjadeobjectsaremostoftenassociatedwithChinainthepopular

imagination,theyhadimportantritual,political,andeconomicsignificanceforall prehispanicMesoamericancivilizations.Jadewashighlyvaluedasatoughstonecapable ofbeingworkedintobothdurableutilitarianobjectsandfinelycraftedobjects.The cosmologicalsignificanceofjadeforbotheliteandnonelitemembersofsocietyseems tohavedevelopedearly,duringtheEarlyFormativeperiod(BlakeandClark1999;Coe andDiehl1980;Lange1993;Lesure1999),andcontinueduntilthetimeoftheSpanish

Conquest.Thecommonrecognitionofthevalueofjadeobjectsprovidedanopportunity forelitemembersofancientMayasocietytodistinguishthemselvesusingalready establishedassociationsofjadewithconceptssuchascentralityandfertility.Inthis chapter,IdiscussthevariousmeaningsandusesofjadeintheMayaarea,andtheir implicationsforunderstandingtheorganizationofjadeartifactproduction.

Ibeginthischapterwithadescriptionofthemineralogicalcharacterofjade, focusingparticularlyonjadeite,theonly'true'lapidaryjadefoundinMesoamerica.Next,

IexaminethechronologicaldevelopmentofjadeuseinprehispanicMesoamerica, particularlyfortheancientMaya.Ifocusspecificallyonhowjadewastransformedfrom astonewithritualmeaningandsignificancetoallmembersofancientMayasocietyinto asymbolofeliteauthority.Recognizingthevariedusesofjadeartifactsfortheancient

Mayaprovidesthepropercontextforinterpretingandunderstandingtheorganizationof jadeartifactproductionintheMiddleMotaguaValley.

43 3.1 WhatisJade?:Jade,JadeiteandGreenstone

Theexactoriginsoftheterm"jade"areobscure,butitisclearhowever,thatthe

termderivesfromSpanishandPortugueseaccountsinthe16thcenturywhichreferredto

greenstonefromChinaandMesoamericaas piedra de hijada becauseofthecurative powersthatthestoneswerebelievedtopossess(Desautels1986:23).Specifically, piedra de hijada ,or"loinstone,"reflectedthebeliefthatwavingthestoneovertheloins orabdomencouldhealailmentsofthespleen,kidneysandliver(MillerandTaube

1993:102).TheEnglishterm"jade"isderivedfromtheFrenchwordforthestone, pierre de l'ejade (Desautels1986:3).Itisunclearwherethepracticeofusingjadeforhealing originated.Desautels(1986:3)suggeststhattheideaoriginatedinChina,anddidnot haveantecedentsinMesoamericanfolkmedicine,whileThouvenot(1982:131132,cited inTaube2004:204)arguestheconceptwasMesoamericaninorigin.

Inthearchaeologicalliterature,theterm“jade”isacommonlyusedcatchallfora mineralogicallyandchemicallydiversesetofgreenstones.Rocksthathavebeentermed

“jade”inthearchaeologicalliteratureofMesoamericaincludejadeite,serpentine, bowenite,albitite,andvariousquartzesandquartzites(Harlow1993:10).“True” lapidaryjades,however,includeonlythemineralsjadeiteandnephrite.Nephrite,an amphibolemineral,doesnotoccurnaturallyinMesoamericaandwasusedonlyinAsia,

NewZealandandtheArcticregionsofNorthAmerica;therefore,itsmineralogical propertieswillnotbediscussedindetailinthisdissertation.

Jadeiteisapyroxenemineralcomposedofsodium,aluminum,andsilicates

(NaAlSi 2O6).Initspurestate,jadeiteiswhiteincolor,butobservedcolorsofjadeite

varydependingonitschemicalcomposition,andincludeshadesofgreen,blue,lavender,

44 andblack.Thegreenshadesofjadeitethatwerehighlyprizedinprehispanic

Mesoamericaoccurasaresultofthepresenceofchromiumandnickel(Harlow1993:17).

Themosteasilyrecognizedcharacteristicofjadeiteisitshardness,whichisintherange of6.5to7ontheMohsscale(talcisthesoftestwithahardnessof1,whilediamondis

thehardestwithahardnessof10).Theindividualcrystalsofjadeiteareverygranular,

andmuchofthetoughnessofjadeiteisattributabletothecloseinterlockingofthese

grains.Jadeitehasaspecificgravityofabout3.3to3.6anddoesnotfracturepredictably

alongregularcleavageplanes.

Jadeiteismostoftenfoundnotinitspuremineralform,butratherasarock composedmostlyofjadeiteandotherminerals.Mostjadeiterockcontainssmaller amountsofrelatedmineralsthattypicallyformundersimilargeologiccircumstances includingalbite,diopside,acmite,andchloromelanite.Ifthesodiumandaluminumin jadeitearereplacedbycalciumandmagnesium,forexample,theresultisomphacite, diopside,orenstatite(amagnesiumrichdiopside)(Harlow1993:20).Jadeiteisalso unstable,andasburieddepositsofthemineralcomeclosertothesurfaceandexperience higherwatersaturation(especiallybelowvolcanicsediments)theycanchemicallybreak downintoanalcimeoralbite(Harlow1993:16).Manyofthesemineralscanoccurwitha greencolor,andsomeevenhavesimilarpropertiestojadeite(thoughnotthesamesuite ofmineralogicalcharacteristics).Nevertheless,jadeitewascertainlyfavoredby prehispanicMesoamericanartisansforitssuperiorcolor,luster,andworkability(Foshag

1957).

Inadditiontojadeiteandthemineralsmentionedabove,anumberofother greenstoneswereworkedbyprehispanicartisansthathavebeenreferredtoas"jade"in

45 thearchaeologicalliterature.Theseincludesoapstone(sometimescalledsteatite), serpentine(amuchsofterrock),agate(acryptocrystllinesilicate),amazonite(atypeof

quartz),muscovite,andjasper(relatedtoquartz).Allofthesestones,however,aresofter thanjadeiteanddonotretainafinepolishlikejadeite,nordotheyhavethesamebright

luster.Inthisdissertation,thetermjadewillbeusedtorefertoallgreenstonerecovered

archaeologicallyintheMiddleMotaguaValley,becauseitistheonlypositively

identifiedjadeitesourceregioninMesoamerica.

Aztecethnohistoricsourcesrefertojadebyanumberoftermsthatreflectthe physicalpropertiesofdifferentvarietiesofthestone. Chalchihuitl wasthe genericterm forjadeandallitsvarieties,andisderivedfromtheword xalxihuitl ,or xalli,

sandorjeweland xihuitl, herborherbcolored(Foshag1957:7).Sahagún(Dibbleand

Anderson1963:221229)describedthemanydifferenttypesofgreenstoneforthe,

dependingoncolorandquality: Quetzalitztli, oremeraldgreenjade,wasabrightemerald

green; Quetzachalchihuitl wasdescribedashighquality,transparent,andwithout

imperfections; Xiuhtomoltetl wasdescribedasgreenandwhitemixed,butwasreferredto

asturquoiseinothersources.Sahagún(DibbleandAnderson1961:168)alsodescribed poorquality“chalchihuitesfingidos”thatwereusedbythecommonerswhowerenot permittedtousejade(citedinFoshag1957:9).

ThevarietyoftermssuggeststhatmanyAztecscitizens(bothcraftspersonsand

thegeneralpublic)coulddiscerndifferentlevelsofqualityforgreenstones,possibly

accordingeachdifferentamountsofprestige.Itispossible,butbynomeansclear,that

differencesinthetypesofgreenstonedisplayedbyAzteceliteswererepresentativeof

rank.Meosamericanscholarshavearguedthatsumptuarylawswereonemeansbywhich

46 nonelitemembersofsocietywerepreventedfrompossessingsymbolsofrankand

authority(Anawalt1980).AlthoughthedistinctionsnotedabovebySahagúnsuggest

discernmentaboutvarioustypesofgreenstones,itmaybethecasethatthesymbolsor

ornamentsintowhichgreenstonewascarvedwasmoreimportantthantheprecise

material.

3.1.1 JadeiteSourcesandSourcinginMesoamerica

Anumberofjadesourceregionshavebeenidentifiedintheworld,allwidely

separatedfromoneanother.Ofthesehowever,onlysixaresourcesofjadeitejade(Fig.

3.1).Thenaturalrarityofjadeiteisattributabletothefactthatitformsinunique

geologicalenvironmentswherehighpressureandlowtemperatureconditionsinthe

earth’scrustareassociatedwithmajortectonicfaultzones,ofteninassociationwith

serpentinerock(Harlow1993).AllthreeoftheseconditionsarefoundintheMiddle

MotaguaRivervalleyinGuatemala,whichfollowstheMotaguaFaultZone(Fig.3.2).

TherecognitionoftheMiddleMotaguaValleyasanimportantjadeitebearingregion firstcamewhenRobertLesliedocumentedthelocationofextensive in situ jadeite

sourcesatManzanotalin1952(FoshagandLeslie,1955).Sincethisdiscoveryhowever,

therehasbeenconsiderabledebateaboutwhethertheMotaguaValleywastheonly prehispanicjadeitesourceinMesoamericaandgreaterCentralAmerica.Somescholars

notethedistinctvisualdifferencesbetweenjadeitefromtheknownMotaguasourcesand

thefinebluegreenjadeiteusedbytheOlmecandancientculturesofCostaRica.This

apparentdiscrepancyhasledsomescholarstoproposethatother,asyetunidentified jadeitesourcesexisted,possiblyinorCostaRica(Coe1968:100103;Easby

47 1968:87;1981:138;Griffin1993:203;Hauff1993:93;Langeetal.1981;Bishopetal.

1985).

DatafromInstrumentalNeutronActivationAnalysis(INAA)performedon jadeiteartifactsfromsitesintheMayaareaandsamplesfromknownjadeitesourcesin theMotaguaValleyledBishopandcolleagues(Bishopetal.1985;BishopandLange

1993)toarguethattheMotaguaValleywasnottheonlyjadeitesourceexploitedin prehispanicMesoamerica.Theirargumentisbasedprimarilyontheobservationofthe chemicalandstructuralvariabilitybetweenjadesfoundatMayasitesandjadescollected fromtheknownMotaguasources.Thisledthemtosuggestthatthereweremultiple jadeitesourcesexploitedinancientMesoamericathathavesincebeenexhaustedorare

yetundiscovered.Forexample,Bishopandcolleagues(Bishopetal.1985;Bishopand

Lange1993)notethatthechemicalsignaturesofjadeitesamplestakenfromtheMotagua

regionclusteredintodistinctgroups(theMotaguagroupswerecomposedofMotagua

Light,MotaguaDark,MotaguaExceptionalandChichenGreengroups).However,there

wasmoreobservedchemicalheterogeneitybetweentheMotaguasamplesandjadeite

artifactsfromMayasitesthantherewaswithintheMotaguasamples(i.e.therewasmore

similaritybetweentheMotaguasourcesamplesthantherewasbetweentheMotagua

sourcesamplesandthesampledjadeiteartifactsfromMayasitesasawhole).

48 Figure3.1Worlddistributionofknowngeologicalsourcesofjadeitejade. (Source:Lange1993:3,Fig.1)

Figure3.2MapsshowinglocationofMotaguaFaultanditscooccurrencewith serpentinerockbeds.MotaguaFaultshownasMinupperimage (Source:AvéLallemant2005).

49 Inaddition,Bishopandcolleaguesincludedgreenstoneartifactsfromsitesin northwesternCostaRica,wheretheywereusedalmostexclusivelyasburialgoodsfrom

300B.C.toA.D.700(LangeandBishop1988).Ingeneral,theCostaRicanjadeite samplesalsoclusteredintolightanddarkgroups,butwerecompositionallydistinctfrom theknownMotaguasamples.Only10artifactsfromtheMayaregionmatchedthe chemicalcompositionoftheCostaRicansamples,andonly5CostaRicanartifacts matchedtheMotaguadata.Thus,theyarguedthattheCoastRicancultureshadaccessto, orexploited,someunidentifiedjadeitesourceinCostaRicaorelsewhere(Bishopetal.

1985).

Morerecentchemicalcharacterizationwascompletedon27piecesofgreenstone debitagefromtheancientMayasiteofCancuen,GuatemalabyKovacevichand colleagues(Kovacevich,NeffandBishop2005)usingLaserAblationInductively

CoupledPlasmaMassSpectrometry(LAICPMS).Theresultsparalleledthoseofthe earlierINAAstudiesinanumberofrespects.First,theCancuensamplesclusteredinto lightanddarkgroups,reflectingcompositionalvariationsinchromiumandnickelcontent.

Additionally,LAICPMSconfirmedthatrocksfromthesamesourcelocation,aswellas differentpartsofthesamerock,exhibitthesamevariationinlightanddarkcomposition

(Kovacevich,NeffandBishop2005:51).Importantly,thestudydidnotproducesecure, specificsourceattributionsformostoftheartifacts,indicatingthatmoresourcesampling isneeded.Interestingly,thestudyshowedtheCancuensamplestocompositionally distinctfromtheknownMotaguasources,butcompositionallysimilartosamplesfrom sitesintheSalamaValleyintheAltaVerapaz,Guatemala(SharerandSedat1987).

50 Kovacevich(2006:138)arguesthatthisresultmayindicatethatCancuenandtheSalama

Valleysiteswereexploitingsomeunidentifiedjadeitesource.

Harlow(1993)however,hasarguedthatjadeitesourcescontainenoughchemical

heterogeneitythatinadequatesourcesamplingandthepresenceofunidentifiedsources withintheMiddleMotaguaValleycouldeasilyaccountforthedifferencesinthe

chemicalcompositionsnotedbyBishopandcolleagues.Thus,hearguesthat

demonstratingthechemicalandstructuralvariationbetweendocumentedjadeitesources

andsampledjadeiteartifactsdoesnotprecludethepossibilitythatalljadeiteusedin prehispanicMesoamericaderivedfromtheMiddleMotaguaValley.

Despitethisscholarlyinterestinidentifyingjadeitesourcesexploitedin prehispanicMesoamerica,relativelyfewactualsourceshavebeendocumented.Aspart

oftheirresearchattemptingtocompositionallycharacterizejadeitesources,Hammondet

al(1977)documentedsevenjadeitesourcesalonga10kmstretchofthenorthsideofthe

RioMotagua,anarealocatedabout10kmeastofGuaytan,thelargestsiteintheMiddle

MotaguaValley(Fig.3.3).AnumberofshopsinAntiguacontinuetoexploitsourcesin

theregionforcommercialpurposes,althoughthelocationofthesesourcesisaclosely

guardedtradesecret.ErosioninthevalleyandthesurroundingSierradelasMinasand

SierradeChuacúsmountainrangescausedbyHurricaneMitchin1998ledtotherecent

discoveryofanumberofjadeitesources,significantlyincreasingtheknownextentofthe jadeitebearingzone(Broad2002;Seitzetal2001).Theseincludesourcesatthe

headwatersoftheRioElTambortothesouthandRioTeculutantothenorth(Taube,

HrubyandRomero2006).Thesesourcesawaitfurtherinvestigationandmayprovetobe

someoftheunidentifiedjadeitesourcesalludedtobycompositionalstudies.Most

51 importantly,no in situ jadeitesourceshaveyetbeenidentifiedoutsideoftheMiddle

MotaguaValley.Therefore,themostparsimoniousexplanationoftheavailabledatais

thattheMotaguaregionwastheonlyjadeitesourceregionexploitedinprehispanic

MesoamericaandgreaterCentralAmerica.

Figure3.3JadesourcessampledbyHammondandcolleagues (Source:Hammondetal.1977:fig.3)

3.2 TheCulturalSignificanceofJadeinPrehispanicMesoamerica

JadehadcosmologicalandritualsignificanceforallprehispanicMesoamerican

culturesfromtheEarlyFormativeperiod(ca.20001000B.C.)untilthetimeofthe

Spanishconquest(Lesure1999;CoeandDiehl1980;Lange1993).Becauseofthe

ambiguousdescriptionsofthemineralogyofgreenstoneobjectsrecoveredatmany

Mesoamericansites,Iwillbetreat greenstone and jade objectsasequivalentinthis discussion.Currentarchaeologicalevidencesuggeststhatjadeobjectswerefirstusedas markersofsocialstatusduringtheMiddleFormativeperiod(Lesure1999), althoughthe

symbolicandritualsignificanceofjadewasestablishedearlier,intheEarlyFormative.

Althoughjadeuseisoftentreatedasamarkerofelitestatusinthearchaeological

52 literatureontheancientMaya,jadeisoftenfoundinsmallamountsinnonelite

householdsaswell(e.g.A.Chase1992;HavilandandMoholyNagy1992;Krejciand

Culbert1995;MoholyNagy1997;Palka1997;Zeleznik2002;Guderjan2007).

Inthissection,IsummarizetheevidenceofearlyjadeuseinMesoamerica, throughtheendoftheLateFormativeperiod.Theterm"Formative"isgenerallyapplied inMesoamericanchronologytoearlysitesoutsideoftheMayaarea.IntheMayaarea, theterm"Preclassic"isgenerallysynonymouswith"Formative."Iwillusetheterm

"Preclassic"torefertothisearlytimeperiodonlyforsiteslocatedintheMayaarea,and use"Formative"forallothersites.FromthereIfocusspecificallyontheuseofjadein theMayaareaduringtheClassicandPostclassicperiods.Examiningjadeuse chronologicallyhighlightshowjade'ssignificancewasfirstestablishedduringtheearliest periodsofvillagelifeinMesoamericaandwaslaterusedasameansoflegitimizingelite

authorityassociopoliticalcomplexitydevelopedinMesoamerica.Indoingso,I

highlightthemultipleusestowhichjadeartifactswereputbybotheliteandnonelite

membersofancientMayasociety.

3.2.1 PatternsofFormativePeriodJadeUseinMesoamerica

JadeartifactswerealreadywidelytradedandusedinMesoamericaasearlyas

1500B.C. , andcurrentevidencesuggeststhattheideologicalandritualsignificanceof jadehadalreadybeenestablishedbythisearlyperiod.Oneoftheearliestmanifestations

ofjadeuseoccursduringtheinitialphasesoftheEarlyFormative(16001200B.C.)at

PasodeLaAmada,intheMazatánregionofthePacificCoastof,Mexico,an

areacharacterizedbysomeoftheearliestsettledvillagesinthearea.Thereislittle

53 evidenceofinternalsocialdifferentiationatthesesites,whichdoesnotbegintoappear untiltheendoftheEarlyFormativeperiod(BlakeandClark1999).

Duringthisearlyperiod,jadeappearsinmanyprosaiccontexts,including(in descendingorderoffrequency):constructionfill,middens,occupationsurfaces,floors, burialsandofferings(Lesure1999:42).Residentsinallareasofthesite,includingthose inplatformandnonplatformresidences,hadaccesstosmallquantitiesofjade,withno significantdifferencesbetweenhouseholds(LesureandBlake2002).Mostnon utilitarianjadeartifactswereobjectsofpersonaladornment,typicallysinglebeadsor smallpendants.Moreelaborateformssuchasearspoolsareabsent,asistheuseof carvedorincisediconographyonjade.JadeceltsoccuratPasodeLaAmada,butthey werepredominantlyutilitarianobjectsfoundinfill,middensandoccupationsurfaces,and themajoritywerewellusedpriortodisposal(Lesure1999:45;Blake1991:40).Lesure

(1999:42)arguesthatjadewasalreadyimbuedwithspecialceremonialandideological significanceatthistime.Hisinterpretationisbasedprimarilyontheplacementofa singlejadeceltbeneaththefloorofalargebuildingdatingtoaround1400B.C.andthe placementofajadebeadinasubfloorcacheinabuildingofmodestsize,datingto around1250to1100B.C.Lesure(1999:44)furtherarguesthatitemsofpersonal adornmentmayhavebeeninalienablepersonalpossessionsthatservedasmarkersof personalidentity,butwerenotyetusedasmarkersofsocialstatusorprestige.

ThemostconspicuousEarlyFormativeritualuseofjadeoccursduringtheManatí

APhase(ca.16001500B.C.)atthesacredspringatElManatí,insouthern

(OrtizandRodriguez1999;OrtizandRodriguez2000;RodriguezandOrtiz2000).The earliestdepositsatElManatíincludejadeaxesthatappeartohavebeendepositedby

54 tossingindividualaxesintothedeepestpartsofthenaturalpoolatthesite(Ortizand

Rodriguez1999:246).Allofthejadeaxesarehighlypolishedandveryfinelycrafted,

demonstratingahighlevelofcraftsmanshipthatappearstohavebeenintendedto

highlightthematerial,form,colorandsurfacefinishofthejadefromwhichtheaxes

weremanufactured(OrtizandRodriguez2000:87).Itisinterestingtonotethattheseare

hypertrophicversionsofutilitarianforms,whichcontraststhetheadzeformsfoundat

PasodelaAmada.Especiallyintriguingisthelocationofthejadeaxesinthecenterof

thepool,repeatingthecentralplacementofajadeaxeinMound6atPasoDeLaAmada

around1400B.C.(Blake1991:40).Itthusappearsthatjadewasalreadyassociatedwith

theconceptofcentralityatthisearlytime,whichisanassociationthatcontinueduntilthe

timeoftheSpanishConquest(Taube2005).Despitetheseritualassociations,jadewas

notyetusedasasymbolofstatusandprestigeineitherregion.

ItisduringthelaterstagesoftheEarlyFormativeperiodwhenarchaeological evidencesuggestssomeofthefirstusesofjadeobjectsasmarkersofsocialdistinction andprestige.DuringtheSanJosephase(1150850B.C.)atTomaltepecintheValleyof

Oaxaca,jadebeadsandceltsappearasburialgoodswithindividualsofproposedhigh status(Whalen1981:61).NoexclusiveconnectionexistsatTomaltepecduringthistime betweenhighstatusindividualsandjade.Instead,theplacementofjadebeads(anumber

ofwhichwereplacedinthemouthsofthedeceased)indicatesthatjadewasritually

significantandavailabletomostindividualsregardlessofstatus.Nevertheless,theuseof jadebeadsintheformofnecklacesandthefactthat88%ofalljadebeadswerefound

withflexed(presumedelite)burialsmayindicatethatjade,andtheabilitytoprocureand

wearlargeamountsofit,hadbecomeasymbolofstatus(MarcusandFlannery1996:97).

55 Theseinitialstepstowardtheuseofjadeasamarkerofelevatedsocialstatusarealso

evidentatSanJoséMogote,whereasimilargradientofaccesstojadeisapparent,and

wherecertainforms,suchasearspools,appearinalimitednumberofburials(Marcus

andFlannery1996:104).

IntheValleyofMexico,patternsofjadeusagearesomewhatdifferent,butstill suggesttheritualmanipulationofjadeanditspossibleuseasamarkerofsocialstatus.

AtCoapexco,twojadebead"blanks"werereportedfromhouseholdexcavation;nojade wasreportedinburials(Tolstoy1989 ).At,ontheotherhand,jadewasfoundin anumberofburials,whereitisrestrictedtogravescontaining10objectsormore

(Tolstoy:109).Nojadebeadswereplacedinthemouthsofdeceasedindividuals.

Instead,jadebeadswereapparentlywornasnecklaces,incombinationwithshellbeads.

Joyce(1999)arguesthattheevidenceatTlatilco,whilefallingshortofdemonstratingthe presenceofanemergentelite,demonstratestheengagementofdifferentsocialgroupsin thecompetitivedisplaysofwealthtoattractfollowers.Interestingly,CoeandDiehl

(1980)reportverylittlejadeatSanLorenzoontheGulfCoastofMexico,oneofthe largestceremonialsitesofthetimeperiod.Thus,whilejadeappearstohavehadritual andsymbolicsignificance,itsuseasamarkerofdifferentialsocialstatuswasnotyet establishedthroughoutMesoamerica,evenintheOlmecareawhereelitesatsiteslikeSan

Lorenzodidnotuseittorepresentstatus.

DuringtheMiddleFormativeperiod(1000400B.C.)numerousrankedsocieties emergedthroughoutMesoamericaanditiswithinthissociopoliticalmilieuthatjade’s ritualandsymbolicsignificancewasexpandedandconsiderablyelaborateduponatmany sites.Iconographythathadpreviouslyappearedonceramicvesselsbegantoappearwith

56 increasingfrequencyonjadeartifacts,asemergingelitessoughtamorerestricted

mediumforiconographicexpression(Garberetal1993:213;Lesure1999:40).For

example,“babyface”figurinesthatwerepreviouslymadefromclaywerereplacedby jadefigurinesduringtheMiddleFormativeperiod.Nevertheless,althoughjadewas becomingamaterialmanipulatedbyelitesformaintainingsocialdistinctions,itsusewas

notrestrictedtoelites,andthearchaeologicalcontextsinwhichjadeisrecoveredfrom

thistimeperiodvariesconsiderably.

Patternsofjadeuseat,,Mexicosuggestthatjadeartifacts

servedtodefinemultiplesocialidentities,andwerenotitemsthatwereexclusivetothe

elite.Fragmentsofjadearefoundineveryhouseareaatthesite,suggestingthatall

householdshadsomeaccesstojadeartifacts(MerrydeMorales1987:99).The

distributionofjadeinChalcatzingoburials(n=116),however,suggestsadifferential

abilitybysomeindividualstohavejadeartifactsincludedasburialfurniture.Whilethe

majorityofburials(84%,n=98)donotincludeanyjaderegardlessofgravetype,halfof

thesimpleintermentsthatcontainjade(n=6)haveonlyasinglejadebeadplacedinthe

mouthofthedeceased;singlejadebeadsarefoundonlyinsimpleinterments.Onlytwo burials(2%)containmorethanasinglebead;bothburialsareslablinedgraves

associatedwiththelargeststructureatthesite(PCStructure4),andhavetheonly

completejadejewelry(necklaceandbelt,respectively)atChalcatzingo,alongwith

unbrokenjadeearflares.Tenburials(9%)havenonbeadjadeartifacts,includingtwo

gravesthatcontainedbrokenjadeite"awls,"whichmayhavebeenusedasbloodletters,

suggestinganattemptbyChalcatzingoelitestoreplicaterituallysignificantitemsin

morerestrictedmedia.BrokenjadeartifactsarealsoreportedatCerros,,during

57 theLatePreclassic,suggestingthatthesmashingofjadeartifactswasawayofremoving

themfromcirculation,thusincreasingtheirvalueorindicatingtheirspecificityor

inalienability(Garber1993).Theevidencesuggeststhatwhilejadebeadswereavailable

forritualorstatuspurposestomostmembersofChalcatzingosociety,moreornate jewelrysuchasearspoolsandjadebeadsinlargequantitieswererestrictedtoelites,and

mayhavebeenpersonal,nontransferablepossessions.

EvidenceelsewhereinMesoamericasuggestssimilarpatternsofuse,wherejade

artifactsbegantobeusedtomarksocialdistinctionsbeyondthoseofageandsex.

DuringtheEarlyMiddlePreclassicperiod(1250650B.C.)at,Belize,jadewas

recovered(althoughrarelyandinsmallquantities)inadiverserangeofburial

assemblages,withfewindicationsofdifferentiationbetweenindividuals(Hammond

1999).DuringthesubsequentLateMiddlePreclassicperiod(650400B.C.),jade

continuestoberareinburialassemblages,butisfoundonlywithadultmales,incontexts

thatsuggestjadebeadswerewornasjewelry(probablybracelets),andincombination

withshellornaments.Hammond(1999:55)interpretstheoverallpatternatLateMiddle

PreclassicCuellotobereflectiveofsocialdifferentiationthatwasnotevidentpreviously.

AlongthePacificcoastofGuatemala,anumberofcentersshowsimilarpatterns

oflimitedjadeuse.AtLaBlanca(Love1991),15piecesofjadewererecovered,while

atLaVictoria(Coe1961)onlyonepieceofjadewasfounddatingtotheMiddle

Formative;unfortunatelythetypeofcontextsinwhichjadewasfoundwerenotreported.

AtElMesak,Guatemala,twosmallfragmentsoffinelypolishedjadeadzeswerefound

indomesticmiddens,suggestingthattheywerepossiblyutilitarianitemsusedatthesite

(PyeandDemarest1991:91).

58 InsoutheasternMesoamerica,particularlyinandElSalvador,jadeuse waswidespreadduringtheMiddleFormative.Joyce(1992:243)reportsthatmost

"costumeornaments"inHonduranburialsweremanufacturedfromgreenstone.InaJaral phaseintermentinthesummitofthedominantStructure1atLosNaranjos(Baudezand

Becquelin,1973:49,9193;citedinJoyce,1992:246),aneliteindividualwasburied withadoublestrandedjadebeadbelt,ajadecollarandtwolargejadeearflaresthatwere apparentlypartofanelaborateheaddress.AtCopan,Fash(1985;citedinJoyce,1992:

245)reportsaburialwith8jadeceltsand300jadebeads,alongwithotherindicatorsof highstatus.AtPuertoEscondido(JoyceandHenderson2001:13),jadeappearsatthe sametimeastheconstructionofthefirstlargeearthenplatformatthesite,andrefuse fromjadeproductionisfoundinstructurefill.AtKaminaljuyu,however,nojade artifactsoccurredwithanymoundburials(Brown1984).

Incontrasttothevariedcontextsinwhichjadeartifactsarefoundelsewhere,the

mostelaborateusesofjadeduringtheMiddleFormativeoccurattheOlmeccenterofLa

VentaintheGulfCoastregion.Jadeartifactsappearprimarilyintwotypesofcontextsat

LaVenta:burialsandcaches(Garberetal.1993:214).Drucker,HeizerandSquier

(1959)reportnumerous"offerings,"someofwhichwerelikelyburialsinwhichthe

humanremainshavenotpreserved.Anumberofthesepossibleburialscontainelaborate

combinationsofpersonalornamentsofjadesuchascelts,pendants,earspoolsandbeads.

AswasthecaseatChalcatzingo,anumberofburialsincludedjade"awl"bloodletters.

FourteencacheswerealsouncoveredatLaVenta,alongthecenterlineofComplexAor

inassociationwithmajormonumentsorfeatures(Garberetal.1993:215).Themajority

ofthesecachesincludejadeandserpentinecelts,ranginginquantityfromtwoto51celts.

59 Manyofthesejadeceltsshowsignsofbatteringandusewear(Druckeretal.1959:139),

suggestingthattheyservedmoreprosaicpurposesbeforebeinginterredinaritual

manner.Otherformsofjadeartifactsincachesincludefigurines,"canoes"and"spoons."

BytheendoftheMiddleFormativeperiod,jadehadbecomeawidelyrecognized

mediumforexpressinganumberofcosmologicalthemes,continuingandexpanding

uponearliersymbolicusesofjadeartifacts(c.f.Lesure1999).Thecolorofjadewas

associatedwiththecolorofthemaizecropandfertility,asymbolicrelationshipthat

likelyreflectstheincreasingimportanceofmaizeinearlyfarming

communitiesthroughoutMesoamerica(Taube2005:23).MiddleFormativecacheswith jadeartifactsatanumberofsitesincludejadeceltsandotherjadeartifactsorientedtothe

cardinaldirections(Smith1982:245;Taube2000:301;EstradaBellietal.2003).In

someofthecaches,jadeceltsareplaceduprightatthecardinaldirectionsandlaidflatat

thecenter,suggestingthatthecachesservedasminiaturemodelsofthefoursidedworld,

acosmologicalmodeloftheworldthatcontinuedinMesoamericaintothePostclassic period(Taube1998:429432,2005:23).Thus,bytheendoftheMiddleFormative period,jadehadbecomeaninstrumentalcomponentofdevelopingiconographicsystems andcosmologicalpracticesthroughoutMesoamerica.

Atthesametime,certainformsandcombinationsofjadeartifactswere increasinglyappropriatedassymbolsofstatusandprestigeinsomeregionsof

Mesoamerica,thoughcertainlynotinauniformmanner.Jadeitselfdoesnotseemto havefunctionedasawealthorstatusgood.Rather,itwastheformsintowhichjadewas manufacturedthatwereimportantsymbolsofstatus,althoughonepossibleexceptionis

SanJoseMogote,whereWinter(1984:205)notesthatjadeearspoolsarefoundinboth

60 highandlowstatusgraves.DuringtheMiddleFormativethepracticeoftransferring

iconographyontojadeobjectsbegantospreadinsomeregions,possiblyasameansby

whichelitescouldfurtherseparatethemselvesfromnonelites(Joyce1999;Lesure1999).

Nevertheless,inHonduras,wherejadewasmorereadilyavailablebecauseofthe proximitytotheMotaguaValleysources,jadewaswidespreadenoughthatelitesappear nottohaveattemptedtotransferthisiconographytojade,butinsteadcontinuedto inscribeiconographyonceramics(Joyce1992:249).Ratherthantherebeingasingle trendinMiddleFormativeMesoamericatowardtheuseofareveredandexoticmaterial fortheexpressionofsocialdifferences,weseeamuchmoremosaiclikepattern,where elitesindifferentregionsattemptedtosignifytheirgreaterstatusandprestigethrough locallymeaningfulavenuesofexpression.

AnumberofscholarsnotethatitwasduringtheMiddleFormativeperiodthat jadewasfirstclearlysymbolicallyassociatedwithwaterandfood,specificallysprouting maize(Joralemon1971,1988:38;Coe1988:225;Fields1989;MillerandSamayoa1998;

Taube2000,2005;Wagner2001).AsFriedelandcolleaguesnote:"jadeandgreenstone werethusanchoredintothehopesandneedsoffarmersinwaysthatpromotedthe desirabilityofthematerialamongthem"(Friedel,ReeseTaylorandMoraMartin2002:

45).Forexample,theselinkagescanbeseeninnumerousMiddleFormativeOlmec incisedjadeceltsthatportraytheOlmecmaizegod(Taube2005:24,Fig.1ab).Taube

(2000:303)furtherarguesthatthejadeceltsthemselvesrepresentedceltiformearsof maize,especiallywhenplacedatthecardinaldirectionsofcaches,suchastheone recoveredatfromtheLateMiddlePreclassicperiod(ca.500B.C.)(EstradaBelliet al.2003).

61 BytheLateFormativeperiod(400B.C.A.D.200),jadehadbecomea widespreadsymbolofwealth,statusandauthorityinMesoamericathatwasprimarily associatedwithelitesandeliteritualcontexts,althoughjadecontinuedtobeusedtoa limiteddegreeandinsmallerquantitiesbynonelites(KrejciandCulbert1995).Inthe

ValleyofGuatemalaatKaminaljuyuandothersites,Brown(1984:223)notesthatjade doesnotbecomeanelitegooduntilafter200B.C.,eventhoughjadehadbeenavailable topeopleinthevalleyforover600yearsandthevalleyislocatedwithin100kmofthe

MiddleMogtaguaValley.AtCuello,jadeisnowfoundonlywithmalesburiedin ceremonial/ritualcontexts,andofteninplacementssuggestingitwaswornasjewelry

(RobinandHammond1991:221).Thesechangessuggestthatjadeartifactshadbecome arequisitepieceofeliteregalia.Elitesbythistimeappeartohaveeffectivelycoopted thesymbolicmeaningsofjadeandassociatedthemselveswithjadesoastoenhancetheir claimstosupernaturalconnections,attemptsthatareclearlyvisibleonmonumental architecture(Friedeletal.,2002).

Inadditiontotheuseofjadeasanelitestatusmarker,theuseofjadeinrituals, especiallythoseassociatedwithstructurededicationandtermination,becameevenmore widespreadintheLateFormative,especiallyintheMayaarea.Hammondand colleagues(Hammond1987;Justeson,NormanandHammond1988)andhavenotedthe similaritiesbetweenthreeelaborateLatePreclassiccachesthatallcontainjadeartifactsat thesitesofCerros,andPonoma,alllocatedinBelize.Allthreecaches containedcombinationsofjadeartifacts,deliberatelyplacedincentrallocationswithin ceremonialstructures.Thispatternofjadeuseincacheswithinstructuresisparalleledat

Caracol,wheremanyLatePreclassiccacheshavebeenrecovered(ChaseandChase

62 1998).Taube(2005:2425)arguesthatthisrepeatedpatternisanexpressionofthe

symbolicassociationsofjadewithcentrality,directionalityandthe axis mundi ,which parallelsthecentralplacementofjadeduringtheEarlyFormativeatPasodelaAmada

notedearlier(Lesure1999).

TheuseofjadeinstructurededicationandterminationritualsatCerros,Belize

hasbeendetailedbyGarber(1983,1989,1993).AtCerros,jadeartifactswererecovered

fromavarietyofcontexts,butneverfromburials.Strikingly,themajorityofjade

artifacts(187of236)recoveredwerebrokenandhavebeeninterpretedtobedepositedas partofterminationritualsinLatePreclassicandEarlyClassicstructures.Theremaining jadeartifactswererecoveredfromcaches(n=31)andothercontexts,including

constructionfill,humus,wallfall,anddomesticmiddens.Alljadesrecoveredfrom

cacheswerewholeartifacts,while92%(n=172)ofjadesfromterminationritualswere broken(Garber1993:167,Table12.1).Intriguingly,108jadefragments(including

fragmentsofbeads,earflaresandcelts)atCerroswererecoveredfromaresidentialzone

associatedwithadockingfacility,orwharf(Garber1993:168).Thereasonforthis patternofdepositionisunclear,thoughCliff(1982)suggeststhatthefragmentswerepart

ofaterminationritualinthispartofthesite.Asimilarpatternhasbeendocumentedat

SalitrónViejoincentralHondurasduringtheLateFormative/EarlyClassicperiod(Hirth

1982;HirthandHirth1993).AlthoughSalitrónViejoislocatedoutsideoftheMayaarea, patternsofjadeitedisposalshowstrikingsimilaritytothatnotedbyGarber,wherebroken jadeobjectsweredepositedincachesaspartofritualsassociatedwiththeterminationof

structuresbeforenewconstruction.Asimilarpracticeofsmashingjadeartifactsis

documentedforChichenItza,whereover20,000jadeartifactshavebeenrecovered,a

63 greatmanyofwhichwereintentionallysmashedorotherwisedamagedpriorto

deposition,althoughitisimpossibletodeterminewhentheseobjectsweredepositedand

thus,whenthepracticebegan(Proskouriakoff1974).

Overall,theLateFormativeperiodsawanexpansionandelaborationoftheforms

ofjadeartifactsintheMayaarea.Inadditiontothosealreadymentioned(i.e.beadsand

celts),thesenewformsincludeelaboratependantsandearflares,spangles,inlays,

mosaics,andavarietyofelaborate,portablecarvings.Oneparticularformthatappears

duringthisperiodisthebibstyleheadpendant(Fig.3.4),examplesofwhichhavebeen

recoveredfromanumberofLatePreclassicsites.FriedelandSchele(1988)arguethat thesependantsfunctionedaselementsofaroyalcrownwhichwerelaterincorporated intotheClassicperiodsystemoficonographyassociatedwithrulership.Ahaupectorals

(Fig.3.4)alsofirstappearduringtheLatePreclassicandbecomeacommonpartofthe regaliaofClassicPerioddepictionsofelitesonstelaeandpaintedceramics.Recently,a jadeahaupectoralwasfoundwiththeoldestknownroyalburialintheMayalowlandsat thesiteofSanBartolo(Taube2005).Thus,bytheLatePreclassicperiod,Mayarulers andelitesincreasinglytransferrediconographyrelatedtotheirsuperordinaterankwithin societyontojade,whichprovidedthemwithbothamediumoflowavailabilitytoexpress theseideas,aswellasamediumwithwellestablishedsymbolicandcosmological meaningsforMesoamericanpeoples.Atthesametime,Mayaelitesbegantousejadein evermoreelaboratewaysintheirpersonaladornment.LatePreclassicimagesofelites oftendepictthemwithlargeamountsofjadejewelryamongtheirregalia,apatternthat canalsobeseeninanumberofLatePreclassicburials(ScheleandMiller1986:105107).

AtKaminaljuyu,LatePreclassicburialsofroyalelites,includingthatoftherulerburied

64 Figure3.4LateFormativejadesfromCerros.Left:"bibsytle"headpendant. Right:Ahaupectoral.(modifiedfromFriedelandSchele1988:fig.7) inthetombonStructureEIII3,includedgreatnumberofjadeobjectsandregaliaas

gravegoods(ShookandKidder1952). Similarlyextravaganteliteburialshavebeen excavatedatRioAzul(R.E.W.Adams1992)andCopan(Fash1991:6870).

DuringthecourseoftheFormativeperiodinMesoamericaweseethe developmentofawidespreadsystemofideologicalandritualmeaningattachedtojadeas aculturallymeaningfulrawmaterialthatcomesgraduallytobeassociatedwithhigh statusandauthority.Todate,nojadehasbeenfoundincontextsdatingtopriortothe

Formativeperiod,thoughmoreprojectsdesignedtouncoversuchdepositsmayyield moreinformationonthepossibleoriginsofjadeuse.Nevertheless,jadebeganitscareer intheEarlyFormativeasamaterialusedforthemanufactureofrituallyimportantobjects andasameansofpersonaladornmentavailabletomostmembersofsociety.Bythe

MiddleFormative,jadeobjectsworninlargeamounts,ormanufacturedincertainforms, appeartobecomemeansbywhichhighstatusindividualscouldmateriallyrepresenttheir status.

ThisprocesswasnomeansuniformthroughoutMesoamericaandcertainregions seemtohavebeenlessinclinedtousejadeasastatussymbolatthispoint.Tosome degreethismayhavebeenduetotheavailabilityofjade.Inareaswhereitwasavailable onlyintermittently,jadeappearstohavebeenutilizeddifferentlythanitwasinareas

65 wheresuppliesweremorereliable.Inareaswherejadewasabundant,suchasHonduras,

itappearsthatwhileitwasstillutilizedasawealthgoodandstatussymbol,local

materials(includinganimalboneandteeth,amphiboliteandreddishbrownstones)were

usedtoreplicatetheartifactformsthatwereimportanttoemergentelites(Joyce1992;

1999).Nevertheless,jadewasstillavailabletoindividualsofvaryingstatusandhadnot

yetbecomethenearexclusivedomainofelitesyet.BytheLateFormative,however, jadehadclearlybecomeoneoftheprimarymeansofmateriallyrepresentingauthority

andstatus.Elitesbythistimeappeartohavealsocooptedthesymbolicmeaningsof jadeandassociatedthemselveswithitsoastoenhancetheirclaimstosupernatural

connections,attemptsthatareclearlyvisibleonmonumentalarchitectureandothermedia

depictingeliteswithelaboratejaderegalia(Friedel,ReeseTaylorandMoraMartin2002).

BytheendoftheLateFormativeperiod,thestagehadbeensetfortheexplosionofjade

usebyelitesamongtheancientMayathatweseeinthearchaeologicalrecordrepresented bylavishtombsandelaboratecachesandbyhypertrophicdisplaysofjadegoodsdepicted inClassicMayaart.

3.2.2 PatternsofClassicPeriodJadeUseintheMayaArea

BytheClassicPeriod(A.D.300–1000),jadehadbecomeoneoftheprimary symbolsofMayaelitestatusandrulership(ScheleandMiller1996).Taube(2005:23) emphasizesthispointbynotingthat"oneofthemorecommonwaysofportrayingthe abjectandpatheticstateofcaptiveelitesistohavethemstrippedoftheirjadefinery."

EvenacursoryexaminationofClassicperiodMayaartillustratestherangeofjade

artifactformsthatwereusedasitemsofpersonaladornment,including:flares(wornboth

66 asearflaresandattachedtobeltsandbracelets);necklacesofsphericalbeads,sometimes withpectoralpendants,plaquesortubularbeads;braceletsofsphericalandtubularbeads; beltsofbeads,oftenwithsuspendedcelts;andnumeroustypesofheaddressornaments

(Digby1964).ThemostcommoncontextsforrecoveryofjadeartifactsfromtheClassic

Periodaretombsanddedicatorycaches;jadesaremuchlessfrequentlyrecoveredfrom mundanecontexts,suchasconstructionfillandmiddens.Nevertheless,jadewasbyno meansanexclusiveitemofeliteconsumption,andisoftenfoundinsmallquantitiesin nonelitehouseholds(Zeleznik2002).

TherarestcategoriesofClassicperiodjadeartifactswerethosethatcontained certaintypesoficonographyandwererestrictedtotheupperechelonsofMayasociety, typicallytheroyalelite.Theseitemsincludelargerthanaveragelargeearflares(e.g.

Pendergast1998),ahaupendants(Friedel1993;FriedelandSchele1988;Scheleand

Friedel1990),androyaldiademelements,suchasthejestergodornaments(Eberland

Inomata2001;ScheleandMiller1986),whichwerewornbyClassicperiodrulers.

Thesetypesofitemsarefoundalmostexclusivelyinroyalburialsandwerelikely personalitemsandthatweretheinalienablepossessionsoftheindividualsthatpossessed them.AsIdiscusslaterinChapter7,evidencefromtheMayasiteof,

Guatemala,demonstratesthatsomeoftheseartifactswerecraftedbymembersofthe

Mayaelite(Inomata2001).Ifthisisthecase,itstandstoreasonthatmanyofthemost iconographicallycomplexitemswornbyClassicMayarulerswerecraftedspecifically fortheirpersonaluse.

OfthemanyexceptionaljadesproducedduringtheClassicperiod,themosaic jadeburialmaskoftherulerK'inichJanaab'Pakalstandsoutasaremarkable

67 specimen.AsTaube(2005)andDigby(1964)note,masksofthistypewereelaborations

oftheearlierpracticeofplacingajadebeadinthemouthofthedeceaseduponburial.

Jadewasparticularlyassociatedwithwind,the"carrierofrain"andthebreathspirit

(Taube2005:30).Coe(1988:225)notesthattheClassicMayapracticeofplacingajade beadinthemouthofburiedindividualslikelyhadthesamemeaningasthesixteenth

centuryfuneraryritualperformedatthedeathofPokomMayalords.LasCasas

(translationinMiles1957:749)notesthat“[w]henitappears[...]thatsomelordisdying,

theyhadreadyapreciousstonewhichtheyplacedathismouthwhenheappearedto

expire,inwhichtheybelievethattheytookthespirit,andonexpiring,theyverylightly

rubbedhisfacewithit.Ittakesthebreath,soulorspirit."Thus,theelaboratejademasks

foundinroyalMayaburialswerehypertrophicextensionsofmuchmoreancientpatterns

ofjadesymbolisminMesoamerica.

Inadditiontotheincreaseinelaboratejadecarving,somescholarsnoteageneral

trendofdecreasingquantityofjaderecoveredatMayasitesfromtheEarlyClassictothe

LateClassicperiod,withjadebecomingincreasinglyrestrictedtotheelitelevelofMaya

society(Rathje1970;MoholyNagy1994,1997;Guderjan2007).Onepossibilityisthat

duringtheLateClassicperiod,eliteswereabletorestricttheuseofjadestatusgoods

throughtheenforcementofsumptuarylawsorthecontrolofproductionandexchange

networks(Rathje1972;Kovacevich2006:147).Theideathatsumptuarylawsmayhave beeninplaceisalludedtoinethnohistoricsourcesincentralMexicoatthetimeof

Spanishconquest.

Amajordifficultywithevaluatingthislineofargumentistheconsiderablelackof

adequatedistributionalstudiesatClassicperiodsitesthatexaminebotheliteandnonelite

68 contexts.MoststudiesintheMayaareahavefocusedonthemostelaborate,elite portionsofancientMayasites,oftenneglectingthegreatmajorityofnonelite householdsthatlieattheperipheriesofthesesites.Asaresult,ourunderstandingof regionalpatternsofdistributionofjadeartifactsinbotheliteandnonelitecontextsis limited.ThisbiashasonlyrecentlybeguntobeaddressedbyresearchprojectsatMaya centersintentonsystematicallyrecoveringarepresentativesampleofbotheliteandnon elitecontexts,especiallytheexcavationofnonelitehouseholds(seeWebsterandGonlin

1988;Robin2003;LohseandValdez2004).Nevertheless,takentogether,wecansketch ageneralpictureofClassicperiodjadedistributionatanumberofMayasiteswherethis typeofresearchhasbeenconducted,supplementingthemwithmoreanecdotalevidence fromelitecenters.

EvidenceatanumberofMayasitessuggeststhatjadewasvaluablebothasaraw materialandasfinishedartifacts.Somescholars(Digby1964;Chenault1986)notethat jadewassohighlyvaluedthatmanytimesnopieceofdebitagewaswasted,andwere insteadshapedinsmallobjects.Thevalueofjadeartifactsisalsoattestedtobythe specialcontextsinwhichtheyweredeposited,especiallyincachesandburials.Jadeis rarelyencounteredinhouseholdrefuseatmanyClassicperiodMayasites.Whenitis recoveredfromsuchcontexts,itisoftendepositedaspartofterminationrituals,like thosenotedearlierforCerros(Garber1983,1993;seealsoPendergast1976;Potter1980,

1982;Hammond1982,1986).Raworpartiallyworkedpiecesarealsorarely encounteredatClassicMayasites;whentheyare,theyarecachedinstructuresorunder monuments(Willey1978;MoholyNagy1997).Sitescontainingjadeindomestic contexts(notdepositedaspartofterminationrituals)includeCeren,ElSalvador(Sheets

69 2000),Copan(Widmer2009),Cancuen(Kovacevich2003,2006,2007;Kovacevich,

NeffandBishop2005)andthesitesintheMiddleMotaguaValleyjadesourceregion

(SmithandKidder1943;Walters1980,1982;Rochette2007,2009;Rochetteand

Pellecer2006,2008;PellecerandRochette2006).Alloftheseareextraordinaryin

certainrespects.AttheMiddleMotaguaValleysites(thefocusofthisdissertation),

CopanandCancuen,jadewasrecoveredfromdomesticcontextsinproductionareas(the productiondatafromCopanandCancuenaredetailedinChapter7).AtCeren, extraordinarypreservationofthesiteasaresultoftheeruptionoftheLomaCaldera volcanoinA.D.595preservedthe in situ locationsofjadeartifactsinnonelite households,eachofwhichhadatleastonejadeaxe(Sheets2000:221).

JadeuseatthesiteofPiedrasNegras,Guatemalarevealsomeinterestingpatterns ofaccesstothematerialandtheuseanddepositionoffinishedartifacts.Overall,Piedras

Negrascontainsrelativelylowamountsofjade,eveninthemostelitecontexts

(KovacevichandHruby2005).Threeproposedeliteburialsatthesitecontainonlyfive totensmalljadebeadseach.EventhetombsofRulers3and4containlowamountsof jadeforClassicperiodroyalburials,themajorityofwhichweresmalljadebeads.

Interestingly,bothtombscontainedmanyclaybeadsthatwerepaintedblueinorderto imitatethecolorofjadebeadsandfunctionassubstitutes(Kovacevich2006:149).

Similarly,anotherEarlyClassicelitetombatthesitecontains24bluequartzbeadsinthe samenecklaceasanumberofjadebeads,althoughthequartzbeadswerebyfarthe largestinthenecklace.KovacevichandHruby(2005)arguethatthepaucityofjadeat

PiedrasNegraswastheresultofthesite'sbeing"cutout"ofthejadetradebecauseofthe highlevelsofwarfareintheregion.Regardlessofthecause,thepaucityofjadeat

70 PiedrasNegras,aswellastheuseofalternatematerialsmeanttoimitatejade demonstratesboththesymbolicandeconomicvalueofthematerial.

Forthesiteof,Guatemala,MoholyNagy(1994,1997)hasdocumentedthe widevarietyofdepositionalcontextsofjadeartifacts,furtherdemonstratingjade'svalue.

Inall,shedescribes13,343piecesofjade,including7,611finishedartifacts(morethan

2,500werebeads)and5,723piecesofdebitage.Unfortunately,neithertheoriginalnotes fromwhichMoholyNagyworked,norherdescriptionsprovideacleardefinitionofwhat typesofmaterialweredeemedtobejadedebitage.Thedepositionalcontextsofjadeat

Tikalparallelthosealreadymentioned:monumentcaches,structurecaches,burial(both chambertombsandotherstypes),aswellas"problematicdeposits,"whichweredefined ascontextswhere"significantamountsofdomesticrefusewereincludedinwhat otherwisewouldhavebeenclassifiedasaburialorcache"(MoholyNagy1997:299).

Thevalueofjadeatthesiteisattestedtobythefactthatmostofthematerialwasnot recoveredindomesticcontexts,butwasinsteaddeposited,alongwithotherdomestic

refuseattimes,inspecialcachesorinburials.Nevertheless,somejadedebitagewas

recoveredfromgeneralexcavations(theexacttypeandlocationsarenotspecified),and

sometimesinnonelitecontexts(n=21).MoholyNagy(1997:308)interpretsthismaterial

asevidenceofthepossibleproductionofjadeartifactsatTikal.Unfortunately,the

locationofthisproductionisnotknown,becausethegreatmajorityofthematerialwas

encounteredinsecondarydepositionalcontexts.MoholyNagy(1994:89)alsonotesthat themanyjadeartifactsarenearlyexclusivelyrestrictedtoelitechamberburialsinthe

LateClassic,followingtheexpectationsofanincreasingrestrictionofjadeuseduring thattimeperiod.

71 Thispatternofincreasingrestrictionofjadetoelitemembersofsocietythrough

theClassicperiodissupportedbyrecentexcavationsatthesiteofBlueCreek,Belize,

where1,350jadeartifactshavebeenrecovered(Guderjan2007).Themajority(n=

1,253)oftheseartifactsarefromLatePreclassicandEarlyClassiccontexts,recoveredin

associationwithpublicarchitectureintencachesandburials.Incontrasttomanyother

ClassicMayasites,148piecesofjadewererecoveredfromnonelitecontexts,aboutone

thirdofwhichwerefromburialsandcaches.Theremainingjadeartifactswere

recoveredfromgeneralexcavations,with48piecesfoundaspartofa"ceramic

concentration"ofunknownfunction(Guderjan2007:143).Inlinewiththecasesalready

mentioned,intheLateClassicperiodjadeuseatBlueCreekisnearlyabsent(3small

fragmentsandonecelt).Guderjan(2007)suggeststhatthisisaresultofaconsolidation

ofpoweratlargerMayasitesthatmayhavecontrolledaccesstojadeintheregion.

ThesiteofCopaninHondurasisoneofthemostthoroughlyexcavatedClassic periodMayasites,withexcavationsatalllevelsofthesitehierarchy(Webster,Freterand

Gonlin2000;Fash1991).InastudyofLateClassicartifactdistributionintheCopan

Valley,Zeleznik(2002)concludedthatalthoughjadeitewasfoundmorefrequentlyand

withgreaterartisticandstylisticelaborationinelitecontexts,itwasstillpresentatall

levelsofthesocialhierarchy.ThemajorityofjaderecoveredatCopancamefrom

mortuarycontexts,whereitwasremarkablycommon,whilejadewasrarelyencountered

indomesticcontexts.ThecloseproximityofCopantotheMiddleMotaguaValley(ca.

60km)mayexplaintheabundanceofjadeatthesiteduringtheLateClassicperiod.

Nevertheless,Palka(1997)hasalsorecoveredjadeatalllevelsofthesettlement

hierarchyatthesiteofDosPilas,Guatemala.

72 ItisclearthatduringtheClassicperiodjadeandjadeartifactshadbecomea primarymeansofmarkingelitestatus,bothbecauseoftheintrinsicrarityofjadeat mostlowlandMayasites,butalsobecauseofthecosmologicalandritualmeanings thathadalreadybeenattachedtojade.Nevertheless,althoughjadeiscertainlyfound primarilyinelitecontexts,itsusewasnotrestrictedtoelites.Jadecontinuedto functioninmanyofthesamewaysthatithadpreviously:asameansofperforming smallscaleritualanddefiningsocialrelationships.Itislikelythatasthecurrent trendofstudyingandexcavatingnonelitecontextsproceeds,wewillbegintogeta morecompletepictureofjadeusebyancientMayacommoners.

BythePostclassicperiod(A.D.10001521),jadeuseintheMayaareahad declinedgreatlyandisnearlyabsentatmanyMayasites(Garberetal.1993:229).

ThemostnotableexceptionisthemanyjadesdepositedintheCenoteofSacrificeat

ChichenItza,althoughmanyofthesewerecarvedinthe""style,whilesome wereheirloomobjectsfrommuchearlier(Proskouriakoff1974:1517).

Proskouriakoff(1974:16)notesthatafterthefallofChichenItza,jadeworking declinedrapidlythroughouttheMayaarea.At,oneofthemostpowerful lowlandPostclassicMayasites,fewpiecesofjadehavebeenrecovered(Massonand

Lopez2007).AtNebaj,intheGuatemalanhighlands,Postclassicjadesarerare

(Smith1951;Becquelin1969).Friedel(1993;Friedeletal,2002)arguesthatitems suchasshellandjadeitebeadswerefungiblecurrenciesthatcouldbeusedin quotidianmarkettransactions.Theevidence(seeTozzer1941:96)tosupportthis claim,however,isequivocal.Furthermore,evidenceofmarketsinancientMaya societybeforethePostclassicisconspicuouslyabsentorambiguous.Regardlessof

73 theparticularusestowhichitwasputduringthePostclassicperiod,itisclearthat jadehadbecomemuchlesssignificantintheritualandeconomiclivesofmostMaya.

3.3 Discussion

Jadeandjadeartifactswereritually,cosmologicallyandeconomically

significantforallprehispanicMesoamericancultures,especiallytheancientMaya.

ThesignificanceofjadeinMesoamericadatestothetimeoftheearliestvillagelife,

whenjadeartifactsservedasmarkersofsocialdistinctionthatweremeaningfulin

markingindividualsocialidentityandinsmallscaleritualbehavior(Lesure1999).

Throughtime,jadeanditsattendantsymbolismandmeaningwerecooptedbyelites

attemptingtoassociatethemselveswithacosmologicallysignificantmaterialasa

meansoflegitimatingtheirelevatedsocialstatusanddemonstratingtheirdifferential

abilitytocommunicatewithandcontrolthespiritualrealmonwhichalldepended

(c.f.Helms1993).Despitethedifferentialaccesstojadethateventually

characterizedancientMayasociety,itwasstillusedbymembersofalllevelsof

ancientMayasocietyuntilthetimeoftheSpanishConquest.

Thiscontextualdiversityhasimplicationsforourunderstandingofhowelites mighthavesoughttocontrolbothrawjadeiteanditsproductionintofinished artifacts.Characterizingtheproductionofstatusgoodsasfull/parttimeor attached/independentspecializationdoeslittletoadvanceourunderstandingofhow productionwasorganized.Furthermore,thisoversimplificationpreventsusfrom fullyrecognizinghowdifferenttypesofstatusandutilitariangoodswereexchanged ortransferredbothamongstandbetweenelitesandcommoners.Putsimply,ifjadeite

74 consumptionvariedwidely,thenitcannotbeassumedthatcontrolovertheraw

material,itsproductionandexchangemechanismsdidnotsimilarlyvary.InChapter

7,IdiscusshowthismorenuancedunderstandingofjadeuseintheMayaareamay contributetomorecompleteinterpretationsofsystemsofstatusgoodsproduction, suchastheonepresentintheClassicperiodforjadeartifactsintheMiddleMotagua

Valley.InChapters4through6,Ipresentevidencefromthisdissertationresearchof thenonelite,domesticproductionofjadeiteartifactsintheMiddleMotaguaValley.

75 CHAPTER4 THEMIDDLEMOTAGUAVALLEY: PREVIOUSRESEARCH,RESEARCHDESIGNANDSURVEYRESULTS

AsIdiscussedinthepreviouschapter,archaeologistshavelongrecognizedthe ritual,social,politicalandeconomicsignificanceofjadeandjadeartifactsinall prehispanicMesoamericancivilizations,includingthatoftheancientMaya.Despitethis recognition,weknowverylittleabouthowpeopleinprehispanicMesoamericaobtained jadeartifacts,especiallyhowtheirproductionwasorganized(seeChapter2).This situationispartiallyattributabletotheverycharacteristicsfromwhichwealthgoods derivetheirvalue:theirscarcityandtheoftenexoticrawmaterialsfromwhichtheyare manufactured.Therefore,archaeologistsintheMayaareahavehadfewopportunitiesto studytheorganizationandcontextsofwealthgoodsproduction.Inthisregard,the

MiddleMotaguaValleyisauniquesettinginwhichtoexamineancientMayawealth goodsproductionbecauseoftheampleevidenceofsuchproductionknownforthearea

(Kidder1935;SmithandKidder1943;Foshag1957;Feldmanetal1975;Hammondetal

1977;Walters1980a.1980b,1982,1989).

Inthisandthefollowingchapter,IsummarizepriorresearchintheMiddle

MotaguaValleyandthegoals,methodsandsummaryresultsofthisdissertationresearch.

Inthischapter,Iprovidebackgroundontheprehispanicculturalgeographyofthe southeasternMayaperipheryandthearchaeologicalsurfacesurveyandsurface collectionscompletedaspartofthisdissertationfieldresearch.Ibeginthischapterwith adiscussionofthegeologicalandnaturalenvironmentoftheMiddleMotaguaregion.

ThenIdiscussthehistoryofarchaeologicalsurveyandresearchintheMiddleMotagua

76 Valleyandsurroundingregions,toprovidecontextforunderstandingthecurrentresearch.

NextIsummarizethesurveymethodsemployedinthisdissertationfieldresearch.

Finally,Ipresenttheresultsofthearchaeologicalsurfacesurveycompletedaspartofthis dissertationresearch.

4.1 TheMiddleMotaguaValley:GeologicalandNaturalEnvironment

TheMiddleMotaguaValley(Fig.4.1)islocatedineastcentralGuatemalaand includestheMotaguaRiverValleybetweenthemoderncommunitiesofPaloamontonado onthewestandRioHondoontheeast(SmithandKidder1943).Thevalleyisbounded tothenorthbytheSierradelasMinasrange,1530kmwidefromnorthtosouth,whose highestpeakisCerroRaxón,at3,015mabovesealevel.TheSierradelasMinasare composedofrugged,metamorphicformationsthatwerecreatedbytectonicactivityfrom theMotaguaFault,astrikeslipfaultthatrunsgenerallyparalleltotheMotaguaRiver.

ThehighestelevationsoftheSierradelasMinassupportdense,lushvegetation, includingcloudforestenvironmentsinplaces;anareaof2363km²iscurrently designatedastheSierradelasMinasBiosphereReserve.TheSierraareimportant sourcesofmarbleandtimberformodernindustry,inadditiontobeingpartoftheonly positivelyidentifiedsourceregionforjadeiteexploitedinprehispanicMesoamerica(see

Chapter2).Tothesouth,thevalleyisboundedbyruggedterrainthatformsthefoothills oftwomountainranges:theSierradelEspirituSantototheeastandtheSierrathe

Chuacústothewest.Higherelevationsintheserangessupportalpineforests.Although notmentionedoftenindiscussionsofthesourceregion,jadeitesourceshavebeen documentedsouthoftheMotaguaRiver,includingalargeoutcropof"Olmec"blueand

77 bluegreentranslucentjadeiteintheUpperRioElTamborregion(Taube,Hrubyand

Romero2005).

Figure4.1MapofMayaareawithmajorarchaeologicalsites. MiddleMotaguaValleyisindicatedbyboxsurroundingGuaytan.

78 TheMiddleMotaguaValleyliesentirelyinthe tierra caliente altitudinalzone, withanaltitudeonthevalleyfloorof275matthewestto160mabovesealeveltothe east(SmithandKidder1943:109).Theenvironmentonthevalleyfloorhasbeen describedasaridandsemidesert,withannualrainfallinthevalleyaveragingabout500 mm,whichoccursalmostexclusivelyduringtherainyseasonbetweenMayandOctober

(Simmons,TaranoandPinto1959:83).Vegetationonthevalleyfloorconsistsmainlyof low,thornyscrubbrushandotherxerophyticvegetation,aswellasvariousspeciesof cactus.Lushtropicalvegetationdoesoccurinlimitedareasofthevalleybottoms however,wherehighwatertablesexist.Mostrainfallislostintheformofrunoff becauseittypicallyfallsinshort,hardshowersandthelocalsoilsandsteepslopes effectivelypreventwaterretention.Thelackofsufficientvegetationandhigh temperatures(32°Caverageannualtemperature)resultinthelossofabout10%of annualrainfalltoevaporation,thehighestrateinallofGuatemala,makingitamarginal, highriskareaforrainfallagriculture(Walters1982:17).

Today,agriculturewithouttheuseofmoderntechniquesandindustrialequipment isonlypracticalonthefloodplainsoftheMotaguaRiverandafewofitstributaries.

Elsewhere,rainfallagricultureofmaizeandothersubsistencecropsispracticedwith varyingsuccess(Simmons,TaranoandPinto1959:83).Bedrockintheareaconsists primarilyofserpentineandschists,andthesoilsthattheygenerateare“shallow,infertile,

highlysusceptibletoerosion,andpoorforagriculture”(Simmons,TaranoandPinto1959:

83).Theexceptionstothispatternincludethewidealluvialplainofveryfertilesoils

alongthebanksoftheRioMotaguabetweenElJicaroandElRancho(Fig.4.2).This

amountstoabout5,000haofland.Theotherexceptionistheabout600haof“shallow,

79 heavytexturedsoilformedoversemiconsolidateddepositsofvolcanicashnearthe southernsideofthealluvialplain”whichisintermediateinfertilitybetweenthetypical valleysoilsandthealluvialdeposits(Simmons,TaranoandPinto1959:83).

4.2 PrehispanicCulturalGeographyoftheSoutheasternMayaPeriphery

TheMiddleMotaguaValley(MMV)isgenerallyconsideredtobepartofthe southeasternzoneoftheMayaarea(Leventhal1981;SmithandGifford1965),andis oftenreferencedinarchaeologicaldiscussionsoftheSoutheasternMayaPeriphery(Fig.

4.3),whichincludescentralandwesternHonduras,easternGuatemala,andallofEl

Salvador(BooneandWilley1988;UrbanandSchortman1986).Iusedtheterm

"periphery"toencompassbothMayaandnonMayapopulationsandsitesintheregion.

Despiteover100yearsofresearch,outsideofthesitesofCopan(Baudez1983;Fash

1983,1991;Webster1999;Websteretal2000);andQuirigua(Schortman1993;Sharer

1978a,1990),theareatodayremainslesswellknownthantheLowlandMayaregionsto thenorthandtheGuatemalanHighlandstothewest.Nevertheless,researchinthearea overthelastthreedecadeshasbeguntoclarifythenatureandextentofprehispanic settlementinthearea(Ashmore2007;BooneandWilley1988;Douglass2002;Robinson

1987;SchortmanandNakamura1991;SchortmanandUrban1986a;SharerandSedat

1987).

4.2.1 PreviousArchaeologicalResearchintheSoutheasternMayaPeriphery

Archaeological,ethnohistoricandlinguisticevidencedemonstratethatthe

SoutheasternMayaPeripherywasanareaofintenseinteractionbetweenvariousethnic

80 BoxindicatesextentofmapinFigure4.6. Figure4.2ExtentoftheMiddleMotaguaValley.

81 Figure4.3MapoftheSoutheasternMayaPerhiphery.

82 groupswhichsharedculturaltraitswithbothMayagroupsandwithnonMayagroups

southofMesoamerica(Brinton1887;Fash1983;Feldman1998;Joyce1986,1991;

LangeandStone1984;Lothrop1939;Miles1957;Schortman1986;Schortmanand

Nakamura1991;UrbanandSchortman1986;Wisdom1940).Althoughscholarshave

longdebatedtheexactlocationofthesoutheasternboundarybetween"Maya"and"non

Maya"populations,recentarchaeologicalresearchintheareasuggeststhatnoclear boundaryexisted(Joyce1986;Schortman1986;SchortmanandNakamura1991;Sheets

2000;UrbanandSchortman1986).Instead,prehispanicpeoplesintheareacycled betweendifferentethnicandculturalaffiliationsthroughtime,especiallyatthelevelof

eliteculture(Brown1984;SchortmanandNakamura1991;Sheets2000).Muchofthis

interactionwasstructuredbytheweboftradenetworksthatdevelopedthroughoutthe

areabeginningintheEarlyPreclassicperiod,whichspurredthedevelopmentofmany

regionaltraditions(seeSharer2000foranoverview).

PrehispanicoccupationinthesoutheasternMayaperipherydatesbacktoatleast

theEarlyPreclassic(ca.20001000B.C.)andcontinuedthroughtothetimeofSpanish

conquestinthe16 th century(Willey1988).Althoughevidencefromtheoldestportionof theEarlyPreclassichasrarelybeenrecovered,thearchaeologicalrecordfromthelater portionsofthisperiodmarktheappearanceofearlyagriculturalvillagesbyasearlyas

1400B.C.intheCopanValley(Websteretal.2000:22),and1200B.C.atChalchuapain westernElSalvador(Sharer1978b)andintheValleyofGuatemala(PopenoedeHatch

2002:279;ShookandPopenoedeHatch1999:291).CeramicsatChalchuapafromthis periodaresimilartothosefoundintheMayaareaalongthePacificcoastofGuatemala

(CoeandFlannery1967).

83 TheMiddlePreclassicperiod(ca.1000400B.C.)markssomeoftheearliest populationexpansionsandsociopoliticaldevelopmentsinthesoutheasternperiphery.

MiddlePreclassicdepositscontainevidenceoftheearliestoccupationintheNacoValley

(SchortmanandUrban1996),AltaVerapaz(Arnauld1986),theValleyofGuatemala

(Michels1979),andLaEntradaregion(InomataandAoyama1996).Bytheendofthis period,theCopanValleyhadthrivingvillagepopulationswithsomeevidenceofsocial ranking(Fash1991:6771).Furthersouth,Chalchuapadevelopedintoaregional chiefdom,withmonumentalarchitectureandevidenceofcontactwiththeGulfCoast

Olmec(Sharer1978b).Someofthemostprecociousdevelopmentsofsociopolitical complexityinHondurasduringthisperiodareseenatLosNaranjos(Baudezand

Becquelin1973)andPlayadelosMuertos(Kennedy1981),wherechiefdomlevel societiesseemtohavedevelopedbyaround600B.C.IneasternandsouthernGuatemala, thereisevidenceofthepossibledevelopmentofregionalchiefdomscenteredonLos

MangalesandElPortonintheSalamaValley(SharerandSedat1987)andcenteredon

KaminaljuyúintheValleyofGuatemala(Michels1979:135;PopenoedeHatch2002:

279280).Interestingly,noevidenceofMiddlePreclassicoccupationhasbeenrecovered fromtheMiddleMotaguaValleyitself(Rochette2009;Walters1982).Basedonthe presenceof"unfinishedjadeornaments[and]workshopdebris"inMiddlePreclassic deposits,SharerandSedat(1987:90)arguethatElPortonwastheprimaryproduction anddistributionnodeforMiddleMotaguajadeatthetime.

Trendsofincreasingsociopoliticalcomplexityandpopulationexpansion continuedduringtheLatePreclassicperiod(ca.400B.C.A.D.100)throughoutthe southeasternMayaperiphery.Bythistimeanumberoflargecentershaddeveloped,

84 markedbytheconstructionofcomplexesofmonumentalarchitectureforpublic

gatheringsandrituals,elaborateeliteresidencesandburials,andnonportablecarved

monuments.Kaminaljuyúemergedasarguablythelargestandmostpowerfulsiteinthe

southernMayaareaatthistime(Sharer2000:465).Duringthisperiod,thepopulationof

theValleyofGuatemaladoubled,andanumberofsmallersitesaroseinthevalley,most

ofwhichappeartohavebeensatellitesofKaminaljuyúatonetimeoranother(Brown

1984).Kaminaljuyú'sprominencehasbeenpartiallyattributedtoitslocationonthe

dividebetweenthePacificandCaribbeanwatersheds,whichallowedittobenefitfrom

theflowofhighlandgoodslikejadeiteandobsidianthatmovedalonganumberoftrade

routesintheregion(Brown1984;Michels1979;PopenoedeHatch2002;Shookand

Kidder1952).TheSalamaValley,whichshowssteadyincreasesinsociopolitical

complexitythroughouttheLatePreclassic,seemstohavesufferedamajorpopulation

declineorreorganizationtowardstheendofthisperiod,possiblyasaresultofdominance byKaminaljuyu(SharerandSedat1987:434).

AlthoughavailabledatafromLatePreclassicperiodsitesindicateregional variationinculturaldevelopment,similaritiesineliteburialpracticesandarchitectureat manysitecenterssuggestpoliticaloreconomictiesbetweenindependentpolitiesinthe southeasternMayaperiphery.Aparticularlyvisibleexpressionofthisregionalunityat theelitelevelisseeninthewidespreadappearanceofUsulutanwareceramics.The distinctivelydecoratedware,withcreamcoloredswirling"resist"linessetagainstan orangebackground,isfoundatsitesthroughoutthesoutheasternMayaperipheryandhas beenrecoveredasfarawayasthenorthernMayalowlandsatElMiradorandTikalandat

ChiapadeCorzoinChiapas(Goralski2008;Sharer2000:469).Althoughrare,Usulutan

85 ceramicsareamongsomeoftheearliestsherdsrecoveredintheMiddleMotaguaValley

(Rochette2009;alsoseeAppendixD).

ThetransitionfromtheLatePreclassictotheEarlyClassicperiods(ca.A.D.

100600)marksashiftinoccupationandorganizationatmanysitesthroughoutthe southeasternMayaperiphery.Ingeneral,theLatePreclassicEarlyClassictransitionis characterizedbydramaticchangesintheregionalsociopoliticalgeography,ascenters thathadbeenprominentgivewaytonewpowersthatappearintheClassicperiod.These changesareparticularlydramaticinwesternElSalvadorandalongthesoutheastern portionofthePacificcoastofGuatemala.ExcavationsatChalchuapaandCerensuggest thatmuchoftheareawasdevastatedbytheeruptionoftheIlopangovolcanosometime aroundA.D.200,whichmadeagricultureimpossibleintheaffectedregionformany generations(Sheets2000:422;2002).AtKaminaljuyú,constructionactivityandthe erectionofmonumentshadceasedbytheendoftheSantaClaraphase(ca.A.D.100

200),andmuchofthevalleywasabandoned,possiblyasaresponsetointrusionand encroachmentbyforeigngroupsfromthenorthwest(PopenoedeHatch2002:288290).

IntheSalamaValley,thepopulationdeclinesthatbeganduringtheendoftheLate

Preclassiccontinued,withmanysitesbeingcompletelyabandonedandsparsesettlement concentratedinthesouthernportionoftheValley(SharerandSedat1987:434436).

TheEarlyClassicmarkstheestablishmentofroyaldynastiesatCopanand

Quirigua,whichwouldeventuallybecomethetwomostprominentandperhapspowerful centersinthesoutheasternMayaperipheryduringtheLateClassicperiod.Notably,both royaldynastieswereestablishedinA.D.426(Looper2003:36;ScheleandMatthews

1998:134).Althoughtheevidenceislimited,theestablishmentoftheroyaldynasties

86 seemstobeconnected,andtheyappeartohavebeenlinkedtoinfluencefromforeign

groupsorpowers,possiblyTikal(Fash2001:7576;Looper20033638).Furthermore,

theseeventstranspirealongwiththerelativelysuddenappearanceofmanyofthe

materialtrappingsofeliteidentityassociatedwithLowlandMayacenterstothenorth,

whichwerenotablydifferentfromlocalandregionalstylesandtraditions(Websteretal.

2000:2324).

AsisthecaseelsewhereintheMayaarea,theLateClassicperiod(ca.A.D.600

900)inthesoutheasternMayaperipheryischaracterizedbyexplosivepopulationgrowth andexpansion,theelaborationofelitearchitectureandassociatedmaterialculture,and vigorousinterregionalinteraction(SchortmanandUrban1994;WilleyandBoone1988).

Copanprovidessomeofthemostvisibleexamplesofthesetrends,andappearstohave beenthemostprominentcenterattheoutsetoftheLateClassicperiod,withitsroyal elitescompletingaseriesofmonumentalconstructionsintheMainGroup(Fash2001;

Websteretal2000).QuiriguashowssimilarmanifestationsofLateClassiceliteMaya culture,withtheerectionofnumerouselaboratelycarvedstelaeinitssitecenteraswell

(Looper2003;Ashmore2007).Althoughnotaselaborate,similarincreasesin populationandmonumentaleliteconstructionareseenatanumberofsitesthroughout thesoutheasternMayaperiphery(BaudezandBecquelin1973;Henderson1992;

Hendersonetal.1979;InomataandAoyama1996;Schortman1986;Schortmanand

Nakamura1991;SchortmanandUrban1994;Sharer1978a).

SociopoliticalrelationsbetweenpolitiesduringtheLateClassicperiodareseem mostreadilyatsitecentersandamongtheelitelevelofsociety.Asnotedearlier,Copan andQuiriguaseemtohavehadaparticularlycloserelationship,withCopanasappearing

87 tobedominantoverQuirigua(Fash2001;Looper2003).Thissituationchanged,atleast

temporarily,afterA.D.738,whenhieroglyphictextsatbothCopanandQuiriguarecord

thecaptureandkillingoftheCopanruler18RabbitbytheQuiriguarulerCauacSky

(JonesandSharer1986).SomescholarshavearguedthatCopanwasinterestedin

dominatingQuiriguainordertocontroltheimportanttradenetworksforjadeand

obsidianalongtheMotaguaRiverfromwhichQuiriguawasstrategicallylocatedto benefit(Fash1988:160;Hammond1972;Sharer1990:101102,106107).

SomescholarshavearguedthattheinfluenceofCopan,andbyextension,

lowlandMayamaterialculture,onlocalelitesduringtheLateClassicperiodcanbeseen

atanumberofothersitesinthesoutheasternMayaperiphery.SchortmanandUrban

(1987)notethispatternintheNacoValley,Hondurasattheprimarycenterof

Gualjoquito,locatedapproximately100kmnortheastofCopan.LocalnonMayaelites

atGualjoquito,whichwasstrategicallylocatedalongmajortradeandcommunication routes,emulatedthesymbolsofstatusandwealthusedatCopan,possiblyasareflection

oftheirparticipationinregionaleliteinteractionnetworks(SchortmanandUrban1987:

22).OutsideofGualjoquitohowever,hinterlandpopulationscontinuedtoadheretolocal

traditionsthroughouttheLateClassic.ThevariablereachoflowlandMayasymbolic

expressionishighlightedbytheabsenceofcarvedstelaeandtheirsecludedlocationsat

site(ratherthanplacementinopenplazaareas)andtheabsenceofelitewealthitems

(suchasjade,carvedshellorflintandobsidianeccentrics)atallsitecentersinLower

MotaguaValleyotherthanQuirigua(Schortman1986,1993).SitecentersintheLa

Entradaregion,however,showsuchclosetiestolowlandMayapatternsthattheyare

discussedas"Maya"centers(InomataandAoyama1996;SchortmanandNakamura

88 1991;SchortmanandUrban1994).Despitethisvigorousinteractionandtheinfluenceof

CopanandlowlandMayaelitematerialcultureseenatmanysitessoutheasternperiphery sites,thereislittleevidencetosuggestthatCopan,oranyothersiteforthatmatter, controlledinterregionaltradenetworksinanymeaningfulsense(Websteretal,2000:

192).

TheeffectsandseverityofthelowlandMayacollapsethatmarksthebeginningof thePostclassicperiod(ca.A.D.9001500)werevariablyfeltinthesoutheasternMaya periphery.BothCopanandQuiriguasufferedthecollapseoftheirdynasticlinesbyA.D.

900(Fashetal.2004;Looper1999;MartinandGrube2000:225),whiletheirhinterlands

werelargelydepopulatedbythebeginningoftheearlyPostclassic(Ashmore2007;Fash

etal.2004;Websteretal.2004).Neitherareaappearstohaverecovered

demographicallyfromthiscollapseuntilwellintotheColonialperiod.Sharer(1978) postulatesthatthecollapseoftradenetworksalongtheMotaguaRiverattheendofthe

LateClassicprecipitatedQuirigua'scollapse,thoughthisispurelyspeculation.

Regardlessofthecause,muchoftheMotaguaRiverValleyappearstohaveabandoned

duringthePostclassicperiod,withonlysmallpocketsofpopulationremaining(Ashmore

2007;Feldman1998;Miles1957;Walters1982).

MostregionsinthesoutheasternMayaperipheryarecharacterizedbyanumberof

newculturaldevelopments,includingtheemergenceofanumberofgroupsthatseemto

havebeenrecentmigrantsfromoutsideoftheMayaarea.Themostpronouncedofthese

culturalchangesoccurredafterA.D.1000intheGuatemalanhighlandstothewestofthe

southeasternMayaperipheryproper,althoughthesedevelopmentsmayhavehad

significantimpactsonculturalpatternswithintheregion.AtthetimeofSpanishcontact,

89 theGuatemalanhighlandswereapatchworkofethnolinguisticallyrelatedMayagroups

engagedin"anincessant,Machiavellianwebofnegotiations,alliance,betrayal,andwar"

(Hill1991:15).TheCakchiquelandQuichéwerethetwomostpoliticallyand

territoriallydominantethnolinguisticgroupsinthehighlands(Brown1985;Fowler1989;

Fox1987;Hill1991;HillandMonaghan1987;Kelly1988).Indigenoushistoriesclaim

thattheelitelineagesinQuichéCakchiquelsocietyweredominatedbyforeigngroups

thathadmigratedtotheareainthelastfewcenturiesbeforecontactandsubjugatedthe

indigenouspopulation(Carmack1981:4344;butseeBrown1985foranalternative

interpretationofQuichéCakchiqueloriginmyths).Theavailableethnohistoricand

archaeologicalevidencesuggeststhatindividualpolitiesweregeographicallysmallunits.

AlthoughtheareastheydominatedlikelyextendedintotheUpperMotaguaValley,their

dominationdoesnotseemtohaveincludedtheMiddleMotaguaValley(Carmack1981;

Fox1987).TheappearanceofcentralMexicancharacteristicsearlyinthePostclassic periodisseenincentralandwesternElSalvadoratChalchuapa(Sharer1978b)and

Cihuatan(Kelly1988).

AlthoughpopulationsinsomeregionsofthesoutheasternMayaperipheryseem tohavereboundeddemographicallybythelaterpartofthePostclassicperiod(ca.A.D.

12001500),thereisnoevidenceofmajorcentersonparwiththoseoftheLateClassic period(Henderson1992:168;Sheets2000:437).Nevertheless,Naco,innorthwest

Honduras,thrivedduringthistimeastradingcommunity,linkedtothecircumYucatan tradingnetworkthatextendedintocentralMexico(Wonderly1986:321).The ethnolinguisticaffiliationofpeoplesatNacoisdebated,withHenderson(1977) proposingChontalMayaoccupation.Incontrast,Healy(1984)arguesforaNahua

90 speakingPipilpopulationatthesite,thoughthetwoproposalsneednotbemutually

exclusive,asmultipleethnicgroupscouldhaveoccupiedtheimportant"international"

tradingcentersimultaneously.

OntheeveoftheSpanishConquest(ca.A.D.1524),thesoutheasternMaya peripherywasinhabitedbyavarietyofethnolinguisticgroups,manyofwhomwere linkedtogetherbyeconomicandpoliticalties(Feldman1971).Evidenceoftheethnic characteroftheinhabitantsoftheMiddleMotaguaValleyatthistimeisextremely fragmentaryanddifficulttoassess.LatePostclassicarchaeologicalremainsfromthe

MiddleMotaguaValleyarevirtuallynonexistent(SmithandKidder1943;Rochette

2008;Walters1982).Inaddition,thereareexceedinglyfewdirectreferencestotownsin theMiddleMotaguaValleyintheearlyethnohistoricliterature(Waltersetal1982:595).

Whilesomescholars(Brinton1887)havearguedforthepresenceofNahuaspeaking

PipilMayaatSanCristobalAcasaguastlanandSanAgustinAcasaguastlan,others(Miles

1957)havecounteredthatthepresenceofNahuaspeakerswasaresultofpostConquest resettlement.StillothersourcessuggestthatMiddleMotaguaValleyinhabitantwere

ChortiMayaspeakers(Feldman1998:3334).Regardlessofitsspecificethnic affiliations,theMiddleMotaguaValleywassparselyinhabited,withonlyafewhundred tributarieslistedfortheareainearlyColonialdocuments(Alvarado1526;Cerratoetal.

1549;bothcitedinWaltersetal1982:595).

4.2.2 PreviousArchaeologicalResearchintheMiddleMotaguaValley

ThefirstdescriptionofarchaeologicalremainsintheMiddleMotaguaValleywas madein1878bytheparishpriestofSanCristobalAcasaguastlan,DonJoseInocente

91 Cordon(quotedinBrinton1887).Thereportfocusesprimarilyondescriptionsofalarge archaeologicalsiteattheconfluenceoftheMotaguaandTeculutanRivers,whichis todayknownasVegaDelCobán.Importantly,Cordonalsonotedthepresenceof continuousmoundgroupsonbothsidesoftheMotaguaRiverbetweenTeculutanand

SanCristobalAcasaguastlan.Later,Sapper(1895,citedinWalters1982)andSeler

Sachs(1900,citedinWalters1982)brieflyreportedthepresenceofarchaeological remainsnearSanAgustinAcasaguastlan.

ThefirstarchaeologicalresearchintheMiddleMotaguaValleywascarriedout byKidderandcolleagues(Kidder1935;SmithandKidder1943)attherequestofDr.

GustavoEspinoza,directoroftheInstitutoDeAntropologiaeHistoria.Datafromthese initialexplorationsledKiddertoconcludethatthearchitectureatsitesinthevalleywas unlikeanypreviouslyreportedfortheMayaarea.Thedatafromtheceramiccollections indicatedalongperiodofoccupationandincludedceramicsassociatedwithneighboring regionsinGuatemalaandHonduras.ThesetwoobservationsledSmithandKidder(1943:

109)toundertakefurther"explorationandexcavation"inthearea"todefinethelocal cultureandestablishitsgeographicallimits[and]providechronologicallinkagesbetween itandotherMayacultures."Thisfieldresearchtookplacein1940andconsistedoftwo monthsofexcavationatGuaytanandtendaysdevotedtoahastysurveyofthevalleyin searchofarchaeologicalsites.Theresultsofthesurveyaredescribedhere;descriptions oftheexcavationsareprovidedinChapter5.

Surveyofthevalleyindicatedthatthegreatestconcentrationofarchaeological siteswasinthelowerLatoRiverValley;archaeologicalremainsbecame"smallerand morescattered"awayfromthiscorezone(SmithandKidder1943:112).Observations

92 ofthearchitecturalfeaturesatGuaytanandtheresultsoftheirsurveyledSmithand

Kidder(1943:116)tolabelthearchaeologicalremainsbetweenthetownsof

PaloamontonadoandRioHondoastheMiddleMotaguaCulture(Fig.4.2),basedonthe

observationthatsettlementwasalmostabsentbeyondthesepoints.Inall,Smithand

Kidder(1943:112)noted1,600moundsbetweentheRioMorazanonthewestandthe

RioSunsapote(nowknownastheRioPasabien)ontheeast.Themajority(over1,000)

ofmoundswerelocatedonthenorthernbankoftheMotaguaRiverbetweenthemodern

settlementsofSanGertrudisandLosChaguites,with142moundsreportedforthesiteof

Guaytanitself.Inadditiontositesinthevalleyitself,SmithandKidder(1943:113,131

133)brieflyvisitedtwositesintheSierradelasMinastothenorthoftheMotaguaRiver:

LosCimientosandSanJoseApantes.Architectureandstructurearrangementsatboth siteswasdifferentfromthatfoundinthevalleysites,leadingSmithandKidder(1943:

133)toarguethattheywerenotpartofthe“MiddleMotaguaCulture,”butweresimilar toarchitectureatthesiteofRabinalintheBajaVerapaz.

ParticularlystrikingwasthelackofcarvedstelaeatanysitesintheMiddle

MotaguaValley,acharacteristicthatsettheareaapartfromthenknownMayasites.

SmithandKidderalsoidentifiedauniquetombstylenotfoundelsewhereintheMaya

lowlandsthatconsistedofsubsurfacechamberscenteredbelowmounds,withwallsof

schistorwaterwornstonesthatwerecappedwithlongslabsthatspannedthechamber

walls,orwitharoughcorbeledarchformedbytwoorthreerowsoflargestoneslabs

(SmithandKidder1943:129130).Eachtombhadanarrowentrancethatpermittedits

continueduseafterintermentoftheburiedindividual,andmanyofthetombsshow

93 evidenceofhavingbeenusedcontinuouslyforsuccessiveinterments(seediscussionin

Chapter5).

Despitetheuniquetombstyleandthelackofcarvedstelae,manyother architecturalfeaturestypicallyfoundelsewhereintheMayaareaarepresentinthe

MiddleMotaguaValley.SmithandKidder(1943:118119)recordedtwelveballcourts duringtheirexplorations,twoofwhichwereatGuaytan;thespecificlocationsoftenof theseballcourtswerenotprovidedinthereport.Theballcourtsresemblethosefoundin theGuatemalanhighlands,northwesternElSalvadorandwesternHonduras(Smithand

Kidder1943:178179),withlong,narrowplayingalleys,wideslopingbenchesand tenonedstoneheadsabovetheplayingalley.Otherarchitectureandstructure arrangementswerenotedastypicaloftheMayaarea,includinglowplatformssupporting thinwalledsuperstructures,multichamberedbuildingscontainingmultiplerooms separatedbylowwalls,andsmall,multistructureplazagroups.Orientationofindividual structuresandstructuresgroupsvariedconsiderably,withlittleevidenceofconsistent formalizedpatternsofsiteplanning(SmithandKidder1943:113).

Ceramicanalysisindicatedthreeperiodsofoccupationinthevalleybetween400

B.CandA.D.1000(SmithandKidder1943:174).Althoughsubsequentreanalysisof theceramicsledSmithandGifford(1965)toidentifysixperiodsofoccupationspanning from1000B.C.toA.D.1250,laterworkbyWalters(1982)confirmedtheinitialceramic chronologydevelopedbySmithandKidder.Someoftheearliestmaterialincluded ceramicssimilartoMiraflores(400B.C.A.D.250)phasematerialsfromKaminaljuyu, aswellaspossibleUsulutanceramicsfromHonduras(SmithandKidder1943:174175).

Followingthisperiod,SmithandKidderproposedtwosubsequentoccupationphases,

94 LatoandMagdalena,althoughspecificchronologicaltimeperiodswerenotassignedto

thesesequentialphases.Generally,theLatoandMagdalenaphasesappearedto

correspond,respectively,withtheEarlyandLateClassicperiods.

Duringtheirsurvey,SmithandKidderdidnotmentionthepresenceofany

surfaceappearanceofjadeproductiondebrisfromsitesintheMiddleMotaguaValley

(seeChapter5fordescriptionofjaderecoveredfromtheirexcavations).Duringsalvage

operationsatthesiteofPuenteHatoin1952,Espinozarecoveredajadebeadcore producedbyahollowdrill,twounpolishedandunperforatedsphericalbeads,andan

unworkedfragmentofjade(Espinoza1952,citedinWalters1982:37).Followingthese

initialreports,evidenceofjadeartifactproductionwasreportedfromtheManzanaljade

source(FoshagandLeslie1955;BequelinandBosc1973).Feldmanandcolleagues

(1975)reportedextensiveevidenceofjadeworkingatthe"Terzuola"site,whereover

twentypoundsofjadedebitagewerecollected,includingtwodrillcoresandaground

fragmentwithacutgrooveononeface.Eightsmall,residentialmoundswerereported

forthesite.

ThemostextensivearchaeologicalprojectundertakenintheMiddleMotagua

Valleybeganinthelate1970swhenWalters(1982)conductedasurfacesurveyofthe

SanAgustinAcasaguastlanArchaeologicalZone(SAAAZ),locatedinthelowerLato

Valley,aspartofhisdissertationresearch(Fig.4.4).Hisresearchyieldedanumberof

importantinsightsaboutthechronology,settlementpatternsandthejadeiteprocessing

industryintheregion.Atotalof32siteswererecordedduringhissurvey;anadditional

ninesitesdescribedbyGuatemalanarchaeologistsandlocalinformantsareincludedin

hisdissertation,butwerenotexamineddirectly(Fig.4.5).Ceramiccomparisons

95 indicatedthattheMiddleMotaguaValleywasoccupiedduringtheLatePreclassic,

MiddleClassic,LateClassicandLatePostclassicperiods.Itwasunclearfromhis

researchwhethersitesinthevalleywereabandonedintheinterveningperiodsorifthe

ceramicchronologywasinsufficienttoidentifythesetimeperiods(Walters1982:129).

Basedontheresultsofthesurfacesurvey,Walterscreatedafourlevelsite

hierarchyforclassifyingsitesinthevalley(Table4.1).Theclasseswerebasedonthe occurrenceofcombinationsofmoundtypesandheightsandthepresenceorabsenceof otherarchitecturalfeatures(Walters1982:47).Ceramicanalysisofsurfacecollections allowedforthereconstructionofthelocalsitehierarchyduringtheMiddleandLate

Classicperiods.TheearliestClassicperiodoccupationintheSAAAZdatestoca.A.D.

500,withtheappearanceofathreetieredsitehierarchy(Walters'Classes13).Bythe

LateClassicperiod,afourtieredsettlementhierarchyhademerged,withfoursites occupyingthehighest(4 th )tier.Walter's(1982:131)datasuggestedthattheareahad beenlargelyabandonedbyA.D.850.

96 gicalZone 20) locationoftheSanAgustinAcasaguastlanArchaeolo withintriangle.(modifiedfromWalters1982:Fig. Figure4.4MapofMiddleMotaguaValley,showing

97 riangleinFigure4.3. Figure4.5–MappofSAAAZsitesfromareainsidet

98 Class1/non Class2/ Class3/ Class4/ mounded small medium large Culturaldebrisonly X X X X Moundsover2mtall X X X Moundsover5mtall X Platformsw/thin Maybe X superstructurewalls Multiroomstructures Maybe X Funerarymonuments Maybe X Ballcourt(s) Maybe X Table4.1Walters'(1982:47)sitehierarchyfortheMiddleMotaguaValley. AprimaryaimofWalters'researchwasthereconstructionofthejadeprocessing

systemintheMiddleMotaguaValleyandhowitchangedthroughtime.Basedonthe

surfaceremainshowever,hewasonlyabletoreconstructtheLateClassicjadeite processingsystembecauseoflimitedevidenceofPreclassicandPostclassicproduction

sites.Allofthesiteswhereherecoveredevidenceofjadeartifactproductioncontained

ceramicsdatingtotheLateClassicperiod,whileonlyonejadeworkshop,Guaytan

Castillo,couldbesecurelydatedtotheMiddleClassicperiod(Walters1982:133).He

definedfourtypesofjadeiteworkshops(simpletocomplex):TypesI,II,III,andIV

(Table4.2).TypeIworkshopswerecharacterizedentirelybyjadeitedebitageproduced byshattering,orstrongpercussionblows(flakes>5cm).TypeIIworkshopsconsisted

exclusivelyof"flakesproducedbypecking"(flakes<5cm).TypeIIIworkshops

containedpeckingflakes,aswellasdebitageshapedbyabrading,drillingandpolishing.

TypeIVworkshopscontainedalltheevidenceofTypeIIIworkshops,plusevidenceof

sawingandincising(intheformofbrokenorunfinishedartifacts).Ingeneral,hisdata

indicatedthatthemostcomplexjadeiteworkshops(TypeIV)wereconfinedtothelargest

99 sitesinthesitehierarchy(Class4),allofwhicharelocatedintheLowerLatoRiver

Valley.TypeIIIworkshopswerefoundatsomeClass3sites.TypeIIworkshopswere

foundinallsiteclasses.Finally,TypeIworkshopswereonlylocatednearjadeite

outcrops.

Large Small Drilling Abrading/Polishing Sawing/Incising Flakes Flakes TypeI X TypeII X TypeIII X X X TypeIV X X X X Table4.2.Walters'(1982:6162)jadeworkshopclassesfromtheLateClassic intheMiddleMotaguaValley. WaltersproposedamodelforthemovementofjadeitewithintheMiddle

MotaguaValleythatreliedheavilyonanassumptionofcompleteelitecontroloverall

aspectsofthejadeprocessingsystem.Inhismodel,TypeIworkshopswerecontrolled byelitesatClass3andClass4sites.TypeIworkshopsextractedjadeitefromoutcrops

andprovidedrawmaterialtoTypeII,IIIandIVworkshopsforfurtherprocessing

(Walters1982:134).TypeIIworkshopsservedprimarilyasplaceswhererawjadeite

wouldbepartiallyworked,butwerenotlocationswherefinishedjadeiteartifactswere produced.Instead,Walters(1982:135)arguedthatallfinishedjadeiteartifactswere producedatTypeIIIandTypeIVworkshops.TypeIIIworkshopswerecontrolledeither

indirectlybyelitesatClassIVsites,ordirectlyby"secondary"elitesatClassIIIsites,for

theirownconsumption.Walters(1982:135)arguedthatmostfinishedjadeiteartifacts producedatTypeIIIworkshopswerechanneledtothe"primaryelite"atClass4sitesfor

"redistributionwithinthesystemorforexport."Finally,allfinishedjadeiteartifactsfrom

TypeIVworkshopswouldhavewentdirectlytotheeliteatClass4sites.Insum,

100 Waltersproposedasysteminwhichsimplerjadeiteworkshopspassedraworpartially

workedjadeitetohigherordersitesandmorecomplexworkshops,whichperformedthe

finalstagesofartifactproduction,positinganelitecontrolmodelfortheMiddleMotagua

Valley.

Basedonceramictieswithneighboringareasandwiththelevelofproduction evidence,Walters(1982:135138)speculatedaboutthedistributionofjadeiteartifacts beyondtheMiddleMotaguaValley,butcouldnotdiscernwhetherdirectorindirect modesofexchangewereinvolved.Hisspeculationisbasedprimarilyonthepresenceof

MotaguajadeinarchaeologicalassemblagesrecoveredinCostaRica,thoughhenoted some"CostaRicanproducts"wererecoveredintheMiddleMotaguaValley;hedoesnot specifythetypesof"products"(Walters1982:137).Itisdifficulttoevaluatethese argumentsbecauseWaltersdoesnotprovidespecificdatatosupporttheseclaims.

Walters'researchendedin1981withthespreadoffightingfromtheGuatemalan civilwartopartsoftheMiddleMotaguaValley.Researchpickedupagaininthelate

1980sandcontinuedintothe1990s,withvariousprojectsdirectedbyGuatemalan archaeologists.TheProyectodeArqueológico,directedbytheUniversidadde

SanCarlosdeGuatemalaandinitiatedin1986,undertookaprogramofsurfacesurvey southoftheMotaguaRiverinthedepartmentofElProgresso,includinginvestigationin themunicipiosofSansareandElJícaro(Fig.4.2).Theprojectproducedaninventoryof sitesintheregionandmadepreliminaryplanmapsofeverysite,including22newsites alongthemarginsoftheMotaguaRiver(RámonRamírez2006:18).

In1997,theprojectcontinuedunderthedirectionofJoséHéctorParedesandLuis

RomerounderthenameProgramadeAqueologíadelMotaguaMedio(PAMM).The

101 focusofthesenewinvestigationswasfurthereastintheMiddleMotaguaValley,inthe

municipiosofRíoHondoandEstanzuela(Romero1999).Researchfocusedona

continuedprogramofsurfacesurvey,aswellassystematicexcavationsatanumberof

sites,includingLaVegadelCoban,thelargestsiteintheeasternpartoftheMiddle

MotaguaValley(Fig.4.2).ExcavationsinPlaza3ofGroupDatLaVegadeCoban

uncoveredasmalljadeworkshop,althoughthiswastheonlyjadeproductionevidence

recoveredbyPAMM(Paredes2003:3,citedbyRámonRamírez2006:23).More

intriguingisthefactthatdespitetheextensivesurveyandexcavationsundertakenbythe project,jadeartifactswererarelyrecoveredfromfunerarycontexts(RámonRamírez

2006:31).

Despitetheimportantcontributionsoftheseprojects,wewerestillleftwitha vagueandincompletedescriptionoftheorganizationofjadeiteartifactproductioninthe

MiddleMotaguaValleyandhowitarticulatedwiththebroaderdomesticandpolitical economy.Waltersprovidedonlygeneraldescriptionsofthesitesheencounteredbutdid notincludedetailedinformationabouttheirspatialconfigurations,ortheareasofthesites whereevidenceofjadeartifactproductionwasrecovered.Further,Waltersdidnot provideinformationaboutthelocationofparticularstagesofjadeiteartifactproductionat eachsite.Forexample,wedonotknowwhetherproductionwassituatedcloseto“elite” residencesorcompounds,orevenatsitecenters.

AnotherdifficultyisthatWaltersreportedonlythepresenceorabsenceofjadeite productiondebitageateachsite,ratherthanthequantitiesofdebitagerecovered; quantitativedataofjadeiteproductionevidencerecoveredinthelimitedexcavations undertakenduringhisfieldworkwereneverpublished.Althoughcollectionsand

102 summarycountsofthedebitageweremadeduringthecourseofhisfieldwork,theseare

nolongeravailablebecauseofthedestructionofmuchofhisdatainafireatthe

UniversityofMissouribeforethedissertationworkwascompleteandthelossofthe

artifactsthemselves(Walters2003,personalcommunication).

4.3 UnderstandingJadeArtifactProductionintheLowerLatoValley

Thisdissertationresearchisconcernedwithunderstandingtheorganizationof prehispanicjadeartifactproductionintheMiddleMotaguaValley,DepartmentofZacapa,

Guatemala(Fig.4.6).Giventhelackofdetailaboutthestructureofthejadeprocessing

industrynotedabove,morefocusedandrigorousarchaeologicalresearchintheMiddle

MotaguaValleyhadthepotentialtoproduceapowerfuldatasetregardingthestructure

ofthelocaljadeiteprocessingindustry.

Thepurposeofthisstudyistoidentifythecontextsofjadeartifactproduction

throughanexaminationofthelocationandstagesofjadeiteartifactproductionatsitesin

theMiddleMotaguaValley.Theresultswouldprovidethefirstdetaileddocumentation

ofaregionwidesystemofjadeartifactproductionintheMayaarea.Further,theywould provideadatasetwithwhichtoevaluatethetypesofsitesinwhichwealthgoods productiontookplaceduringtheClassicperiod.Thisworkrepresentsthefirstfully

reportedstudyofcommunitywidewealthgoodsproductionforprehispanicMesoamerica.

4.3.1 PreliminaryWork

Beforeinitiatingfieldresearch,IundertookasmallpilotprojectintheMiddle

MotaguaValley,withfundingfromtheDepartmentofAnthropology,PennState

103 Figure4.6–MapoftheeasternMiddleMotaguaValley,showingextentofarea surveyedaspartofdissertationresearch.TheRioMotaguaservedasthesouthern limitofthesurveyarea. University,todeterminewheresystematicarchaeologicalresearchcouldyielddata

relatedtojadeiteartifactproduction.OverthecourseoftwoweeksinJuly2004Ivisited

knownarchaeologicalsitesandjadesourcesthroughoutthevalleyandsurrounding

mountainswiththeassistanceofLicenciadoLuisRomeroandlocaljadeprospector

CarlosGonzalez.Specifically,Ifocusedonlocatingareaswithevidenceofjadeartifact production.

Basedontheresultsofthepilotproject,Idecidedthatsystematicresearchinthe

LowerLatoRiverValley,coveringmuchoftheareapreviouslyreportedbyWalters,

wouldprovidethegreatestamountofdataaboutlocaljadeiteartifactproduction.This

determinationwasmadefortworeasons:1)archaeologicalevidencewashighlyvisible

onthesurfaceand2)itwasalreadyknownthatjadeiteartifactproductiontookplaceat

104 sitesintheLatoValley.Examinationofsitesinthisarea confirmedthepresenceof prehispanicevidenceofjadeartifactproduction,includingdenseconcentrationsofjadeite percussiondebitageandevidenceoflaterstageofjadeiteartifactproduction(Fig.4.7).

Figure4.7–Jadeitedebitage(examplescircledinred)atGuaytan4.

4.3.2 SurfaceSurveyMethodology

Walters'(1982)surveyoftheSanAgustinAcasaguastlanArchaeologicalZone

(SAAAZ)identifiedtwentyeightsiteswithintheLowerLatoRiverValley,alongwith associatedconcentrationsofjadeiteproductiondebitageatanumberofthosesites(Fig.

4.5).Asnotedearlier,Walters'reportsonlyprovidevaguedetailsaboutthelocationand natureofjadeiteartifactproductionatthesesites.WiththeassistanceofLicenciado

MonicaPellecer,inOctober2005Iinitiatedarchaeologicalsurfacesurveytolocate archaeologicalsites,jadeiteproductionareasandjadeitesourcesaspartoftheLower

LatoRiverArchaeologicalJadeProject(Fig.4.6).Oureffortsfocusedonresurveying

105 theareaexaminedbyWalterstoconfirmthebasicdetailsofhisresearchandgenerate

newdata.Approximatelysixweeksweredevotedtosurveying,mappingandmaking

surfacecollectionsoveranareaof8.5squarekm(Fig.4.8).

Theprincipalgoalsofthearchaeologicalsurveyweretoidentifyanddefinethe

extentofallsitesinthesurveyarea,theirperiodsofoccupation,andtolocateandsurface

collectevidenceoflithicproduction,particularlyofjadeiteartifacts.Forthepurposesof

thesurvey,Idefineda"site"asacollectionofculturalmaterial(regardlessofthe presenceofarchitecturalremains)thatwasseparatedfromthenearestsuchcollectionby atleast50morbysomenaturalfeature,suchasa quebrada (anaturallyformedravineor gully).SurveyareaswereidentifiedonWalters'mapsandonthecorresponding1:50,000

SanAgustinAcasaguastlanmapoftheInstitutoGeográficoNacional(NAD83/WGS

84). Systematicsurfacesurveywascarriedoutinallparcelsoflandinthesurveyareato whichwecouldgetaccessfromlocallandowners,includingagriculturalfields,cattlepasture, andresidential,commercialandpublicproperties.Unfortunately,wecouldnotnegotiate accesstoallareasofinterest.Additionally,thelocationofthecommunitiesofMagdalena andGuaytanovermuchofsurveyareapreventedusfromdefiningthefullextentof prehi spanicoccupation.

Atwoorthreepersonsurveyteamledbymyselfconductedanintensive

archaeologicalsurfacesurveyofeachsurveyarea.Becauseoftheruggednatureofthe

terrain(withmanysteepsidedquebradas)andinformationprovidedbylocalinformants,

weconcentratedoursurveyonareasoflevel,orgentlyslopingterrain.Spotchecksof

steepsidedterrainnearareaswithdenseconcentrationsofartifactsorarchitectural

remainsconfirmedtheabsenceofsitesinthesetypesofterrain.Weusedparcel boundarylinesasreferencepointsratherthanfollowingagridsystemwheneverpossible.

106 Fullcoveragesurveyofallareasandparcelstowhichwecouldgainaccesswasdirected towardagoalofobtainingasampleofthevariabilityinjadeproductioncontexts.

Ateachsiteencountered,theteam(1)tookGPSreadingsofacentralpoint(and bordersoflargersites),(2)recordedobservationsregardingthenumberanddimensions ofstructures,sitedisturbance,currentlanduseandabundanceofsurfacematerial,(3) drewamapofthesiteusingacompassandtape(whentimepermitted)and(4)made surfacecollectionsofartifactsforevaluatingsitefunctionandperiodofoccupation.At eachsite,ateammemberwasassignedtomakeafullcoveragesurveyofaquadrantor halfofthesite,dependingonsitesize.Eachquadrantorhalfwasdefinedbythecentral pointofthesite,whichwasdeterminedbyquickreconnaissanceafterthesitewas identified.

Weattemptedtomakecompletesurfacecollectionsofalljadeiteproduction debrisateachsurveyedsite.However,ifdenseconcentrationsofjadeiteproduction debriswerefound,collectionwashaltedsothattheirlocationscouldberecordedbefore collection.Thisallowedustoidentifyparticularlociatindividualsiteswherejadeite artifactproductionpotentiallytookplace.Inadditiontojadeiteproductiondebitage,we alsomadecollectionsofotherartifactclasses.Weattemptedtocollectallexamplesof otherlapidaryartifacts(includingshellandstoneproductiondebitage),andnotedin surveynotebookswhereproductionevidencewasencountered.Inadditionwecollected samplesofobsidianartifacts,payingparticularattentiontothelocationofnonblade flakesofobsidianthatseemedtorepresentthepresenceofobsidianartifactproduction activities.Thelocationsoflargeartifactssuchasmanosandmetateswerenoted,but theseitemswerenotcollectedbecauseofissuesoftransportandstorage.Finally,

107 diagnosticceramicsherdswerecollectedtoprovideachronologicalframeworkforeach

site.

SitedesignationsweremadeasmodificationsofthesitenamesusedbyWalters

(1982).SiteslocatedinthecoreGuaytanzonealongtheRioLatoweregiven designationsthatreflectedthenameofthesiteandthesector(e.g.Guaytan4;VargasI;

MadgalenaI).SiteslocatedinthesurveyareaalongtheMotaguaRiverweregiven namesthatcorrespondedtothekilometermarkernearestthelocationofthesite,aswell asasitenumber(sitenumberprogressedwesttoeast).Forexample,KM93IIislocated totheeastofKM93I.Detaileddescriptionsofallsites,alongwithfigures,arepresented inAppendixA.Theresultsofthearchaeologicalsurfacesurveyaresummarizedbelow.

4.4 SurfaceSurveyResults

Archaeologicalsurfacesurveyidentifiedatotalof28sites,rangingfromartifact

scatterswithoutassociatedarchitecturetoclustersofresidentialandcivicceremonial

architecture(Fig.4.8).Allsiteshavebeenextensivelylootedandmanyhavebeen partiallydestroyedbymodernconstructionoragriculture.Sitesweremostdensely

clusteredalongthebanksoftheLowerLatoRiverandbecamemoredispersedandless

numeroustotheeastandwestoftheLatoRivervalley.

SitesalongtheMotaguaRiveraregenerallylocatedalongthesouthernedgeof thebluffsthatoverlookthenorthernbanksoftheriver(about15mabovetheriver’s floodplain)andarefoundonlevelorgentlyslopingterrain,oftenimmediatelyadjacent tosteepquebradas.Wewereunabletosurveysomeofthemoreruggedfoothillsofthe

SierradelasMinasbecauseoftimeconstraintsandlackofpermissiontoaccessland.

108 LowerLatoValleysurveyarea. e4.8 Figur

109 Nevertheless,outsideoftheLowerLatoRivervalley,weencounteredonlyonesitenorth oftheCA9.Inaddition,wewereunabletomakesurfacecollectionsattwosites(KM

91IandKM93IV)becausewecouldnotobtainpermissionfromlandowners.

Ingeneral,sitesconsistofsmallgroupsof4to6structures,sometimesorganized aroundplazas,thoughnoconsistentsiteplanwasevident.Sitesrangefromsimple(non elite)residentialhousemoundgroupstolargerceremonial/residential(elite)groupswith moreelaboratearchitecture.Structurecategoriesincludedlowsubstructureplatforms thatlikelysupportedthatchsuperstructures,vaultedfunerarymonuments(identifiableby lootedslablinedtombs),andmultiroomedplatformswithlowmasonrywallsthatlikely supportedperishablesuperstructures.Thelargestandmostarchitecturallyelaboratesites inthevalleycontainedmonumentalarchitecture(structuresofabout4minheightor larger)andballcourts,includingGuaytanCiudadela(nowaprotectedarchaeologicalpark wherewewerenotallowedtoexcavate,Fig.4.9),andportionsoftheMagdalena,Vargas andElTerronsites.Inaddition,welocatedtwositesthatcontainednostructures,but consistedentirelyofsurfacedebris.

Thelargestsites(intermsofthenumberofstructures)andlargeststructuresinthe

surveyareaarefoundinthelowerLatoRivervalleyatGuaytan,Vargas,Magdalena,

PuenteHato,andElTerron.Asnotedearlier,Guaytanhasbeenthefocusofnumerous

archaeologicalprojectsandhasbeenmapped,soourgoalwastolocateevidenceof jadeiteartifactproductionatthesite.ThepresenceofthemodernvillageofGuaytan

overmuchoftheancientsitelimitedoursurveytothoseareasunderprotectionby

IDAEHandtheareasofthesitesouthoftheresidentialcoreofthemodernvillage.We

locatedfourareasofjadeiteartifactproductionatGuaytan(inadditiontothoselocatedin

110 July2004):Guaytan5,Guaytan6,Guaytan7,Guaytan8(Fig.4.9,4.10).Descriptionsof

testexcavationsintheseareasareprovidedinChapter5.

4.4.1 LowerLatoRiverValleySites

PortionsofallofthelowerLatoRivervalleysitesshowevidenceofelite occupation,indicatedbylarger,moreelaboratestructuregroupsandthepresenceofball courtsatGuaytan(GuaytanCiudadela,Guaytan6),VargasI,andElTerron.Walters

(1982)notedthepresenceofaballcourtatMagdalenaII,butwecouldnotconfirmthis report.LocalinformantsindicatedthatWaltersmayhavebeenreferringtoapartofthe sitethathassincebeendestroyedbytheconstructionofadrivewayandprivate residentialoutbuildingonpartofthesite.Althoughweencounteredevidenceofjadeite artifactproductionatallsitesinthelowerLatoRiverValley,thedensestconcentrations werefoundatGuaytan4,VargasIIA,VargasIII,MagdalenaI,andElTerronNorte;

Guaytan4isdescribedalongwithsummaryofexcavationsinChapter5.Full descriptionsofallsitesareprovidedinAppendixA.

4.4.1.1VargasIIA

JadeiteproductionevidenceatVargasIIAwasassociatedwithacoreofelite architecturethathasbeenbadlydestroyedbylootingandmodernconstruction(Fig.4.11).

Ceramicscollectedfromlooter'strenchesandsurfacecollectionsindicateoccupation

fromtheLatePreclassicthroughtheLateClassic,andincludeLatePreclassicperiod

importedUsulutanceramicsandlocallymadeimitationsofUsulutanvessels,including platesandbowls(CraigGoralski2005,personalcommunication).Evidenceof

111 Figure4.9MapofGuaytan,dashedboxisareaofinsetbelow(fromLopeznd.)

Figure4.10MapofGuaytanshowinglocationofsiteswithjadedebitagescatters (ModifiedfromLopeznd.)

112 jadeproductionwasconcentratedbehindthelargeststructureofthesite,onalarge artificialplatformatopabluffoverlookingtheRioLato.Collectionshereincluded evidenceofallstagesofjadeitebeadproduction,aswellasevidenceindicating productionofbeadsfromotherstones,suchasjasperandotherunidentifiedstones.

a b Figure4.11ExtensivelootingatVargasIIA.(a)Viewofarchitectureexposedby largetrenchdugintocenterofStructure1;collectionsforOp.5I2weretakenfrom centeroftrench,inforegroundofphoto.(b)Portionofplazafloor(onleftofphoto) exposedbyexcavationanderosioninsouthernplazaarea.

Figure4.12JadeartifactproductionevidencefromVargasIIAlooter'strench(Op. 5I1).Percussiondebitage( a,f) ,brokenbeads( b),polishedfragments( c),bead preforms( d),completebeads( e).

113 CollectionsfromVargasIIAincludematerialobtainedbyscreening360litersof backdirtfromarecentshallowlooter’strench(Op.5I1)dugintothewesternedgeofthe artificialplatform(Fig.4.12);wecouldnotsecurepermissionfromlocallandownersto excavateatthesite(Table4.3).Ceramicsfromthislooter'strenchwererestrictedtothe

LateClassicperiod.Anadditional288litersofbackdirtwerescreenedfromthelarge looter’strenchdugintothecenterofStructure1(Op.5I2,5I3;Fig.4.9a)andincluded onlyLatePreclassicperiodceramics(Table4.3).Unfortunately,becauseofthelevelof disturbance,itisnotpossibletomakeaclearassociationbetweentheLatePreclassic ceramicsandthejadeproductiondebitage.Collectionswerealsomadefromthewallsof looters’trenchesdugintostructuresandplazafloorsthatincludedmaterialsimilartothat foundonthesurface(Fig.4.11b),aswellascutjadeitepiecesandastonewithcircular depressionsthatmayhavebeenusedforgrindingorpolishingjadeitebeads(Fig.4.13).

Itissignificantthatjadeiteproductionevidencewascollectedfromplazafloorlevelsthat alsocontainedsomeoftheUsulutanceramicsmentionedabove.Takentogether, evidenceatVargasIIAsuggestslapidaryproductionofwealthgoodsdirectlyassociated withelitecivicceremonialandresidentialarchitecture.

VARGASIIAArtifactType Quantity(5I1) Quantity(5I2&5I3) JadeFlakes 85 40 FinishedJadeBeads 6 0 Partial/BrokenJadeBeads 30 12 JadeiteBeadPreforms 8 3 JadeBeadDrillCores 1 1 Polished/GroundJadeFragments 3 0 ChalcedonyDrills 1 0 ObsidianBlades/BladeFragments 7 5 ObsidianFlakes 23 26 Nongreenstonebeadfragments 4 2 Table4.3Artifactsrecoveredfromlooter’strenchesatVargasIIA.

114 Figure4.13StonerecoveredatVargas IIA,possiblyusedforgrindingbeads. Notelargeconcavityatbottom,and threesmalleroneinupperleft.

4.4.1.2VargasIII

ThesiteofVargasIIIcontainstwogroupsofstructures.Inthenorthernportion ofthesite,12structuresrungenerallyeastwestalonggentleslopes;onlyonegroupof fivestructuresformedpartofatypicalMayaplazagroup.Themajorityofthestructures inthenorthernsectorare1mtallplatformterracesbuiltintogentlyslopingterrain;there arealsotwovaultedfunerarymonumentslessthan2mtall(bothwithlootedtombs).

Threeadditionalgroupsoflowplatformstructures(twotothreestructurespergroup, ninestructuresinall)arelocated20mfurthersouthwest,closertotheriver;nomapwas madeofthesitebecauseoftimeconstraints.

Littlejadeiteproductionevidencewasfoundwithinthecentralportionornorthern perimeterofthenorthernportionofthesite.Themajorityofproductiondebitageand

associatedproductiontools(i.e.chertdrills)werefoundscatteredaroundthesmallest platformstructuresatthesite.Thesestructuresarelocatedonthewesternand

southwesternperimeterofthenorthernportionofthesiteandtheirfunctionisdifficultto

assesscurrently,butthestructuresformasmallpatiogroupoffourstructureslocated

20mawayfromtheneareststructuregroup.AswasthecasewithVargasIIA,evidence

115 ofallstagesofjadeartifactproductionareinthisportionofthesite,withsmaller

amountselsewhereinthenorthernportionofthesite(Table4.4).Surfacecollectionsof

ceramicsindicatedoccupationfromtheLatePreclassicthroughtheLateClassic.

VARGASIIILithicArtifactType Quantity Quantity TOTAL (SW) (other)

SmallJadeFlakes 310 97 407 JadeFragmentw/GroundFacet 6 0 6 Partial/BrokenJadeBeads 2 1 3 JadeBeadPreforms 3 0 3 CutJadeFragments 1 0 1 JadeCobbles/Chunks 1 1 2 LargeJadeFlakes 3 1 4 JadeHammerstone 0 1 1 ChertMicrodrills 2 4 6 ObsidianBlades/BladeFragments 58 20 78 ObsidianFlakes 13 10 23 ManoFragments 1 0 1 Table4.4Artifactrecoveredfromsurfacecollectionsinsouthwestern(SW)andall other(other)portionsofVargasIII.

4.4.1.3MagdalenaI

MagdalenaIisthenorthernmostgroupofstructuresthatformpartoftheelite coreofthesiteofMagdalena;thesiteiscomprisedofmorethan25structuresonthe bluffsabovetheeasternedgeoftheLatoRiverandisboundedtothesouthbyasmall quebrada.Unfortunately,wecouldnotsecurepermissionfromalocallandownerto exploreaportionofthesite.Evidenceofjadeiteartifactproductionwasconcentratedon theeasternandwesternperipheriesofMagdalenaI(Fig.4.14).Theeasternportion consistsofeightstructures,someofwhicharesituatedonalargeartificialplatformbuilt intothenaturallyslopingterrain.Jadeitedebitagewasfoundaroundtwolowplatform

116 structuresofuncertainfunctionandStructure3,a2mtall,rectangular,multiroomed

structure.Significantconcentrationsofdebitagewerealsofoundindirectassociation

with,aswelldownslope,fromtwomultiroomed,stonewalledstructuresonthewestern perimeterofthesite.Theentiregroupwasalmostcertainlyaneliteresidentialand

ceremonialgroup.CeramicscollectionsindicateoccupationfromtheLatePreclassic

throughClassicperiods.

Figure4.14SouthernportionofMagdalenaI.Testexcavationsaredescribedin Chapter5. 4.4.1.4SitesoutsidetheLowerLatoRiverValley

OutsideoftheLowerLatoRivervalley,thelargestscattersofproductiondebitage

areatKM93I,whichwasfirstdescribedasthe"Terzuolasite"byFeldmanetal.(1976).

Withtheexceptionoffourlowplatformstructures,theareahasbeenleveledforaloe

117 cultivation.Jadeiteproductionevidencewasconcentratedonthesouthernand southwesternportions.DescriptionsbyFeldmanetal.(1976),Walters(1982)andlocal informantsindicatethatKM93Ilikelyconsistedoftwodomesticpatiogroupsbeforeits

destruction.ThesiteisbisectedbytheCA9highwayandtothenorthofthehighwayare

anadditionaltwomoundswhichhavebeenalmostcompletelydestroyedintheprocessof

fieldpreparationforaloecultivation.

Furthereast,thesiteofKM93IIIcontainednoevidenceofsurfacearchitecture

(theareashowednoevidenceofmoderndestruction,anassessmentthatwasconfirmed bylocalinformants),althoughjadeiteproductiondebitageandbrokenbeadfragments werefoundinsurfacescatterswithdomesticrefuse(e.g.bowlandjarfragments).Still furthereast,thesiteofLosChaguites02consistsofaseriesofthreegroupsoflow domesticstructures(alllessthan2mtall;sevenstructuresinall).Beadproduction evidencewasconcentratedonthesouthernandeasternperipheriesofthesite.

4.5 SurfaceSurveyResultsInterpretation

Basedonthesurveyresults,afivelevelsettlementhierarchyfortheMiddle

MotaguaValleywascreatedbasedon:numberofmounds/structuresateachsite, mound/substructureheights,presenceofmultiroomedmasonrysuperstructures,and presenceof'elite/ceremonial'featuressuchasballcourtsandstelae(Table4.5).

Characteristicsusedtodefineeacharenotconfinedtothatspecificsitetype,butmaybe alsopresentinhigherordertypes.Forexample,VargasIIA(TypeVsite),includesa ballcourt,onemultiroomedstructureover2meterstall,and2mtallvaultedfunerary monuments,butalsoincludesthreelowsubstructureplatformslessthan50cminheight.

118 Hierarchical Characteristics SiteType TypeI Unmoundedornoarchitecture(i.e.onlyculturalmaterial/artifacts) TypeII Lowmoundsonly(alllessthan1mtall) Allmoundslessthan2mtall TypeIII Multiroomedmasonrysubstructures Somemoundsgreaterthan2mtall TypeIV Multiroomedmasonrysuperstructureswithhigh(>.5m)stonewalls Multiroomedmasonrystructuresover2mtall TypeV Vaultedfunerarymonumentsgreaterthan4mtall Ballcourt(notfoundatallTypeVsites) Table4.5.DefinitionofsitehierarchyintheMiddleMotaguaValley. Thesecriteriawerechosenbecauselarger,moreelaborateresidentialarchitecture

isgenerallytakenasindicativeofgreatersocialrankoftheinhabitants.Allsites,

regardlessoftheirdesignationwithinthelocalsitehierarchy,containedstructuresand

artifactsthatsuggestresidentialfunctions.TypeIsitesaside,allothersitescontainlow

moundswhichlikelyservedassubstructuresforperishable,thatchedsuperstructures;low

moundsbetween1to2minheightarethemostcommonmoundtypeswithinthesurvey

area.Principleofabundancewouldthussuggestthatthemostfrequentstructuretypesin

anysettlementpatterlikelyrepresentdomestic,residentialstructures.Additionally,many

ofthesestructuresaregroupedaroundpatios,apatterntypicalofdomestichouseholdsin

theMayaarea(Ashmore1981).Inaddition,allsitescontaineddomesticartifacts,

includingmanosandmetates,anddomesticceramicforms,suchas comales ,bowlsand jars.

Inregardtocraftproduction,thesurveydataandsurfacecollectionsshowthat jadeiteartifactproductionwaspresentat all levelsofthesitehierarchy(Tables4.6and

4.7).Whileitispossiblethathigherorderssitesreflectlengthofoccupation,orthe functionofthesite,ratherthanthesocialstatusofitsinhabitants,theimporantpointis

119 thatnomatterhowthesitehierarchyisconstructed,theirisevidenceofjadeartifact productionatallsitesintheMiddleMotaguaValley.Tables4.8and4.9further underscoresthispointbybreakingdownthesetotalsaccordingtothelocalsitehierarchy.

Intotal,4,072piecesofjadewererecoveredinthesurfacecollections,representing almostallthestepsinvolvedintheproductionofjadeitebeads,aswellasfragmentsof polishedplaquesandpossiblypendants.Wefoundnoevidenceofmoreelaborateartifact

forms,suchastubularbeads,diadems,figurines,oranyevidenceofincisingorcarving.

Themajorityofthematerial(96%)consistedofjadeflakes(n=3,910),whichresemblea

coarsegravel(Fig.4.15).Inaddition,29jadeitecobbleswerecollectedduringthe

archaeologicalsurfacesurvey.AnalysesofthesematerialsaresummarizedinChapter6.

Ceramicsurfacecollectionsprovidedperiodsofoccupationat23sites;fivesites

didnotyieldtemporallydiagnosticceramicsherds(Table4.10).Theearliestceramics

datetotheLatePreclassicperiod(Motaguaphase,200B.CA.D.200)andwere

recoveredfromsevensites.ThemostabundantceramictypesrecoveredintheMiddle

MotaguaValleydatetotheClassicperiod(A.D.200900).Nineteensitesyielded

evidenceofEarlyClassicperiod(A.D.200600)occupationintheHuisajoceramic phase(A.D.200550).AllsitesshowevidenceofoccupationduringtheLateClassic period(A.D.550900),intheManzanal(A.D.550650)andMagdalena(A.D.650

900)ceramicphases.Mostsites(n=17)showevidenceofcontinuedoccupationduring

thesubsequentEarlyPostclassicperiod(Palmillaphase,A.D.9001150),whileonly

sevensitesyieldedceramicsfromtheLatePostclassicperiod(A.D.11501600).Afull descriptionoftheceramictypologyisprovidedinAppendixD.

120 Jade beads Flakes Broken

SiteName CutJade Preforms TOTALS JadeBead Fragments Fragments DrillCores JadeBeads JadeBeads JadeHollow GroundJade Nongreenstone HierarchyType Guaytan3 I 29 ― ― ― ― ― ― 29 Guaytan4 II 145 ― 6 ― 5 ― 1 2 158 Guaytan5 II 16 1 1 ― ― ― ― ― 18 Guaytan6 V 73 ― ― ― ― 1 1 ― 75 Guaytan7 V 51 ― 1 ― ― ― ― ― 52 Guaytan8 IV 29 ― 1 ― 1 ― 5 ― 36 PuenteHato IV 2 ― ― ― ― ― ― ― 2 VargasI V 3 ― ― ― ― ― 1 ― 4 VargasIIA V 178 7 50 11 2 1 4 6 259 VargasIIB III 212 1 4 1 ― ― 1 5 224 VargasIII III 407 ― 3 3 ― 1 6 ― 420 VargasIIIA II 36 1 ― ― ― ― 1 ― 38 VargasIV IV 47 ― 1 ― ― ― ― ― 48 MagdalenaI V 397 1 ― ― 1 2 ― 1 402 MagdalenaII III 22 ― ― ― ― ― ― ― 22 ElTerronN. V 86 ― ― ― ― 1 2 ― 89 ElTerronS. IV 18 ― ― ― ― ― 3 ― 21 KM912 IV 50 ― 1 ― ― ― ― ― 51 KM913 III 31 1 ― ― ― ― 1 ― 33 KM914 III 177 ― 2 ― ― ― ― ― 179 KM921 III * ― ― ― ― ― ― ― 0 KM922 II 23 ― ― ― ― ― 1 ― 24 KM923 III? 626 ― 1 6 1 1 10 ― 645 KM931 II 819 ― 1 1 3 2 1 ― 827 KM933 I 42 ― 2 ― ― ― ― ― 44 KM934 III? * ― ― ― ― ― ― ― 0 LosChaguites1 II 321 ― ― ― 1 1 3 ― 326 LosChaguites2 III 70 ― 1 ― ― 1 ― ― 72 TOTALS 3910 12 75 22 14 11 41 14 4098 Table4.6Rawcountsofjadeandlapidaryproductiondebitagefromsurface collections.

121 Hierarchy Jade LargeJade Jade SiteName ChertDrills Type Cobbles Flakes Hammerstones Guaytan3 I ― ― ― ― Guaytan4 II ― ― ― 31 Guaytan5 II ― ― ― ― Guaytan6 V 1 1 ― 9 Guaytan7 V ― 1 ― 1 Guaytan8 IV ― 3 ― 3 PuenteHato IV ― 2 ― 1 VargasI V ― ― ― ― VargasIIA V 1 3 ― 2 VargasIIB III ― 2 ― 6 VargasIII III 2 4 1 4 VargasIIIA II 1 ― ― ― VargasIV IV 3 1 ― 4 MagdalenaI V 3 1 ― 16 MagdalenaII III ― ― ― ― ElTerronN. V ― 3 2 ― ElTerronS. IV ― ― ― ― KM912 IV 1 ― ― 1 KM913 III 4 1 ― 2 KM914 III 4 7 2 5 KM921 III ― ― ― ― KM922 II ― ― ― 2 KM923 III? 4 7 ― 8 KM931 II 4 ― ― 2 KM933 I ― ― ― 2 KM934 III? 1 1 ― ― LosChaguites1 II ― 9 1 6 LosChaguites2 III ― ― ― ― TOTALS 29 46 6 105 Table4.7Rawcountsoflapidaryproductiontools,largejadeflakesandjadeite cobblesrecoveredfromsurfacecollectionsatMiddleMotaguaValleysites.

122 SiteType Jade beads Broken Debitage CutJade Nonjade Preforms JadeBead JadeBead Fragments Fragments DrillCores JadeBeads JadeBeads GroundJade I 71 2 II 1360 2 9 1 9 4 17 2 III 1592 2 10 10 1 2 12 IV 99 3 1 5 5 V 391 8 51 11 2 5 13 7 TOTALS 3910 12 75 22 13 11 47 14 Table4.8Rawcountsofjadeandlapidaryproductiondebitagefromsurface collections,groupedbyhierarchicalsitetype. SiteType JadeCobbles LargeJadeFlakes JadeHammerstones ChertDrills I 2 II 5 9 1 41 III 15 22 3 25 IV 4 6 0 9 V 5 9 2 28 TOTALS 29 46 6 105 Table4.9Rawcountsoflapidaryproductiontoolsandlargecobblesofjadeite recoveredfromsurfacecollections,groupedbyhierarchicalsitetype.

Figure4.15JadeitedebitagefromKM92III.

123 Site Late Late Early Colonial Preclassic Postclassic Postclassic LateClassic EarlyClassic ElTerrónN. ElTerrónS. X X X Guaytán3 Guaytán4 Guaytán5 Guaytán6 X X Guaytán7 X X X Guaytán8 X X X KM91II X X X X X KM91III X X X X KM91IV X X X X X X KM92I KM92II X X KM92III X X X X KM93I X X X X X KM93III X X X X KM93IV X X LosChaguites01 X X X LosChaguites02 X X X X MagdalenaI X X X MagdalenaII X X PuenteHato X X X VargasI X VargasIIa X X X X X X VargasIIb X X X VargasIII X X X VargasIIIa X VargasIV X X X Table4.10Periodsofoccupationbasedonsurfacecollectedceramics fromMiddleMotaguaValleysites.Xindicatesceramicsfromthatperiod.

124 4.6 Discussion

Inthischapter,IhavedescribedtheMiddleMotaguaValleyandthemethodology

andsummaryresultsofarchaeologicalsurfacesurveyconductedaspartofthis

dissertationfieldresearch.Thesummaryoftheprehispanicculturalgeographyofthe

southeasternMayazoneprovidedthebackgroundinformationnecessarytoputtheresults

ofthisdissertationfieldresearchintotheirlargerregionalcontext.Inaddition,the

characterofthenaturalenvironmentinfluencedpatternsofeconomic,culturaland politicaldevelopmentintheMiddleMotaguaValley.Althoughafullexplorationofthe

interactionbetweenthenaturalandculturalenvironmentisbeyondthescopeofthisstudy,

thegeneralsociopoliticalandnaturalenvironmentlikelyinfluencedculturalpatternsat

MMVsites,apointtowhichIwillreturninChapter7.

Thearchaeologicalsurveydataprovidevaluablenewinformationregardingthe

organizationofjadeartifactproductionintheMiddleMotaguaValley,Guatemala.

Archaeologicalevidencedemonstratesthatjadeiteartifactproductiontookplaceonsome

scaleat all siteswheresurfacecollectionscouldbemadeaspartofthisdissertationfield

research.Themajorityofthisevidence(96%)consistsofsmalljadeitepercussionflakes,

althoughtheevidencesuggeststhattheproductionofjadeitebeadstookplaceatevery

siteinthesurveyarea.Thesesitesrangedfromsmall,amorphoussurfacescattersof

artifactsnotassociatedwithmoundsorarchitecture,toeliteresidentialandceremonial

siteswithmultiplestonewalledstructures.Ceramicevidencerecoveredduringthe

surfacesurveysuggeststhatallsitesinthesurveyareawereoccupiedthroughoutthe

Classicperiod,whilesomesitesshowevidenceofPreclassicandPostclassicoccupation

aswell.Themajorityofceramicevidence,however,datestotheLateClassicperiod.

125 Althoughthesurfacesurveyandcollectionsprovideagreatdealofnewdatafor addressingthegoalsofthisdissertationresearch,evidencefromexcavationsarerequired toconfirmthesedata.IntheChapter5,Idescribetheexcavationundertakenaspartof thisdissertationfieldresearch.Theseexcavationswereintendedtoprovideevidencethat subsurfacedepositswerereflectiveofsurfacecollectionmaterial.Inaddition, excavationscouldprovidemoresecurelydatedcontextsforevaluatingthetimeperiods duringwhichsiteswereoccupiedintheMiddleMotaguaValley.Excavationdata,in additiontoevidencefromsurfacesurvey,provideabasisforunderstandingthe technologicalprocessandorganizationofjadeartifactproductionintheMiddleMotagua

Valley.

126 CHAPTER5 LOWERLATORIVERARCHAEOLOGICALJADEPROJECTEXCAVATIONS Thisdissertationresearchisconcernedwithunderstandingtheorganizationof prehispanicjadeartifactproductionintheMiddleMotaguaValley,Guatemala.AsI

notedinthepreviouschapter,oneoftheprimarygoalsofthisdissertationresearchwasto

undertaketestexcavationsinareaswithevidenceofjadeiteartifactproductiontoconfirm

thepresenceof in situ productionactivityandtoobtainsamplesfromstratifieddeposits withwhichtodateproductionactivities.Datafromtheseexcavationscouldalsoprovide asubstantialdatabaseforobservationsaboutthetechnologicalprocessesofjadeartifact production.

Inthischapter,Isummarizethemethodsandresultsofthetestexcavations undertakenaspartofthisdissertationresearchatthesitesofGuaytanandMagdalena.I beginbysummarizingtheresultsofpreviousexcavationsundertakenatGuaytan(Kidder

1935;SmithandKidder1943;Walters1980a,1980b,1989),inordertoprovidethe readerwithcontextaboutpreviousarchaeologicalresearchcarriedoutatthesesites.

Next,Idescribetheexcavationmethodsemployedinthisarchaeologicalfieldresearch.I thensummarizetheresultsoftheseexcavations.Finally,Idiscusstheexcavationdatain regardtotheobjectivesdescribedinSection4.3

5.1 PreviousExcavationsintheMiddleMotaguaValley

PreviousarchaeologicalexcavationsintheMiddleMotaguaValleyhavefocused ontwoparticularsites:GuaytanandLaVegadeCoban;inthissection,Idescribeonly excavationsatGuaytan,asLaVegadeCobanislocatedtowardtheeasternlimitofthe

127 MiddleMotaguaValley,andiswelloutsidetheareacoveredaspartofthisdissertation research(Fig.5.1).Excavations MiddleMotaguaValley Figure5.1

128 atGuaytanwerecompletedbyEspinoza(1952)in1934,SmithandKidder(1943)in

1940andWaltersin19791980(1980a,1980b,1982,1989).Inthissection,Idescribe

thelocationandresultsofexcavationsofthelatertwoprojects,toprovidethereaderwith

aframeofreferenceforcomparingtheexcavationmethodologyandresultsofthis

dissertationfieldresearch.Espinoza'sexcavationsaresparselydocumentedand

consistedoftunnelingintotenstructurestoexaminetombs.

5.1.1 SmithandKidder'sGuaytanExcavations

Inadditiontothe"hastyexploration"ofruinsalongtheMotaguaRiverdescribed

inthepreviouschapter,SmithandKidder(1943;Kidder1935)completedaseriesof

excavationsinsomeofthelargestmoundsandtwoballcourtsatGuaytaninanattemptto

definethelocalceramicchronologyandmaterialcultureoftheMiddleMotaguaValley

(Fig.5.2);hereIwillsummarizetheexcavationsthatarewelldescribedinthepublished

reports.

ExcavationsatMound23,along,lowstructure(25mx9mx2m),revealeda10 room"multichambered"structurewithfewceramicsherdsandnoburials,leadingSmith andKidder(1943:120)tohypothesizethatthestructurewas"neverapermanent residence"thatmayhavebeenoccupied"duringcertainceremonialoccasions."

ExplorationofMounds9and9a,locatedinthecentralportionofGuaytan,revealedtwo nearlysquarestructures,bothpossiblyofLateClassicconstruction(SmithandKidder

1943:122).SubfloorexcavationsinMound9auncoveredacryptburialcontainingthe decayedremainsoftwochildren,oneofwhichhadajadebeadlayinginsideitslower jaw,inafashionsimilartopracticesdiscussedearlierinChapter3.Excavationof

129 Mound24,describedasaconicalmound12mindiameter,and3mhigh,uncovereda

seriesofthreebuildingphases,eachassociatedwithatombofthetypedescribedearlier

inChapter4.Thelowertwotombs(TombsIIandIII)contained11and37individuals,

respectively;anadditionalfourburialswereuncoveredsurroundingthestructureitself

(Fig.5.3).ExcavationswereinitiatedintoMound25,thelargestatGuaytan,butwere

nevercompletedbeforetheendofthefieldseason;theyyieldedceramicsfromthe

Early/LateClassictransition(SmithandKidder1943:129).

BasedontheirexcavationsandexaminationoflootedstructuresatGuaytanand

othersites,SmithandKidder(1943:172)notedthat"MiddleMotaguaValleysites

servedtoanunusuallygreatextentascemeteries."Especiallyperplexingwasthefact

manyofthestructuresappearedtohavebeenerectedoverthetombsandburials,rather

thancontainingintrusiveburials.Thisconclusion,however,mustbeviewedinlightof

thefactthatSmithandKidderconcentratedtheirexcavationsonthelargeststructuresat

Guaytan,whicharemorelikelytohaveservedasmortuaryfacilities.Nevertheless,itis

difficulttoevaluatetheseclaimsbecauseofthesparsereportingofthefullextentoftheir

excavations,whichincludedmoremoundsthanthosethatweredescribedintheeventual publications(Kidder1935;SmithandKidder1943).Interestingly,SmithandKidder

reportedrelativelyfewpiecesofjadeartifactproductiondebitagefromtheirexcavations,

themajorityofwhichcamefrommortuarycontexts.Whatlittlematerialtheydidrecover

wastermed"Jadeworker'sMaterial(?)",including"subsphericalbeadsinprocessof

manufacture;shapedbutunpolishedandunperforated(n=3);conicaldrillcores(n=3);

restsmallwaterwornpebbles,sawedpieces,brokenfragments,someoffinestone"

(SmithandKidder1943:165).ThesepieceswerefoundscatteredinthefillofStructure

130 24,locatedapproximately150mfromtheareadesignatedasGuaytan4inoursurvey.

Theydonotreportfindingtoolsrelatedtojadeartifactproductioninanyoftheir excavationsintheportionsofwiththemostelaboratearchitectureandtombs.

Figure5.2MapofGuaytan,withlocationsofstructuresnotedinthedescriptions ofworkbySmithandKidder(modifiedfromLopezn.d.,reproducedinRámon Ramírez2006)

131 Figure5.3Structure24atGuaytan(Source:SmithandKidder1935:Figure10b).

5.1.2 Walters'GuaytanExcavations

Between1978and1980,Walters(1980a,1980b)completedexcavationsineight areasatGuaytan,themajorityofwhichwereinthesouthernportionofthesite(Fig.5.4).

Inadditiontotheseexcavations,thecaretakeroftheprotectedzoneofGuaytan,Don

GustavoGuillen,toldmeoflimitedexcavationsthatWaltersundertookatMagdalena andElTerron(bothsitesaretotheeastofGuaytan,acrosstheRioLato);theresultsof theseexcavationswerenotmentionedorpublishedbyWaltersoranyothermembersof theSanAgustinAcasaguastlanArchaeologicalProject.

132 Figure5.4MapofGuaytan,withapproximatesurveyareaboundaries(hatched lines)describedbyWalters(1980a,1980b)(modifiedfromLopezn.d.,inRámon Ramírez2006).

133 Walters'onlypublishedexcavationsoutsideofthesouthernportionofGuaytan

werelocatedimmediatelynorthoftheCiudadelaelitemoundcomplex,wherehe

completedfourexcavationsinanundisturbedportionoftheplazathatrevealedaseriesof

Classicperiodfloors;depositsbelowthelowestofthesefloorscontainedLatePreclassic periodceramics(Walters1980a:8).Nootherdescriptionoftheartifactsrecoveredfrom

theseexcavationswaspublished.

InthesouthernportionofGuaytan,Walters'concentratedhisexcavationsinsix

surveyareas(Fig.5.4).InArea2,Waltersexcavatedasingle1x1munitintoasmall,

heavilydamagedLateClassicperiodstructureatthetopofanaturalhill,whichyielded

fewartifacts(Walters1980a:11).Fifteenexcavationunitsofvaryingsizewere

completedinArea6,andwerefocusedonanareaofdomesticdebristhatWalters believedtobetheremainsofahousehold;excavationsrevealedthepresenceofaLate

Classictombandassociatedstructurethathadbeenlootedinantiquity(Walters1980a:

25).InArea7,Waltersexcavatedatombthathadbeenlootedpreviously,though

incompletely,inordertoobtain"datathathadbeenmissedbythelooters"(Walters

1980a:27);thetombdatedtotheLateClassicperiod.Interestingly,excavationofthe

floorofthetombchamberrevealedasubgravecacheconsistingofaceramicvessel

containing"overapoundofcrushedjade"(Walters1980a:31).Asimilarcachewas

foundduringexcavationsinArea6.InArea8,noexcavationswereinitiated,althougha

lootedLateClassictombwasclearedout,revealingamassburialof15individuals

(Walters1980a:35).

ThemajorityofWalters'excavationsfocusedonthejadeworkshopthatcovers portionsofhisAreas3and4(Fig.5.5).Area3containedthreeextensivelylooted

134 mounds;Area4,adjacentandnorthofArea3,contained"anumberoflowmounds,allof

whichhavebeenextensivelylooted"(Walters1980a:12).Allstructuresareassociated

withasunkenpatio,andWalters'excavationswerelocatedonthewestern,northernand southernperimetersofthewalls

Figure5.5ContourmapshowinglocationofstructuresandexcavationsinAreas3, 4and5(Source:Walters1980b:88).TheportionofArea3thatliesimmediately southofthemodernfenceisnowcoveredbythelocalelementaryschooland adjacentconcreteschoolyard.

135 definingtheplaza,inareaswithsurfaceevidenceofjadeiteartifactproduction.

Excavationsinbothareaswerecompletedoverthecourseoftwofieldseasonsin1979 and1980(Walters1980a,1980b,1989).

Onthewesternedgeoftheplatform(Fig.5.5,areamarkedby“1320”),eight2x2 munitswereexcavated,revealingtwooccupationlevels,oneLateClassic(A.D.800

1000)andoneMiddleClassic(A.D.650800),whichwereseparatedbyasingeinstance ofrebuilding(Walters1982b:114).Oneunitexposeda10cmtallretainingwallof schistslabswithnomortar,whichdefinedthewesternedgeofthesunkenpatio.Inthe westernsideofthesameunit(Excavation16),Waltersuncoveredasmall(25cmx50cm) stonelinedbox,coveredbythreeschistslabs,containingasmallvesselfilledwithred pigmentononeendandtwoobsidianprismaticbladesontheother(Fig5.6). Walters

(1980b:110)arguesthattheboxwasasubfloorstorageunitfor"preciousorritual items".Althoughthecontentscouldnotbedated,Waltersproposesthatitwasdeposited duringtheLateClassicperiod,basedondatesfromceramicsintheassociated stratigraphiclevels(Walters1980b:110).Althoughhedoesnotprovideartifactscounts,

Walters(1980b:114)notesthattheexcavationsinthewesternedgeoftheplaza containedgreaternumbersofimportedpolychromepottery,andsuggestsitwas"the focusofthecontrollerelitewhodirectedthespecializedactivitiesoftheplazagroup."

Figure5.6PlanviewofArea4,Excavation16, showingthelocationoftheplatformwallontheright andstonelinedboxwithcontentsontheleft(from Walters:1980b:111).

136 Theevidenceforsuch"specializedactivities"comespredominantlyfrom excavationsonthenorthern(Area4)andsouthern(Area3)edgesofthesunkenpatio.

Twentyone2mx2munitswereexcavatedalongthesouthernperimeterofthepatio, whereWaltersreportsheavyconcentrationsofjadeandobsidiandebitage.Excavations revealedanaccessrampdescendingfromsouthtonorthintothesunkenpatioarea(Fig.

5.7).Excavationstothenorthofthesouthernretainingwall(i.e.insidethesunkenpatio) uncovered14cachesofexhaustedobsidianbladecores(n=5199),clusteredtotheeast andwestoftheentranceramp,andincontextsdatingtotheLateClassicperiod(Walters

1989).Inadditiontothebladecores,excavationsinthesouthernportionofpatiogroup uncovered4,500obsidianfragmentsfromClassicperiodcontexts.Walters(1989:256 doesnotelaborateonthespecificportionsoftheClassicperiod,oraboutthetypesof obsidianfragmentsrecovered(i.e.bladesfragmentsvs.earlystagepercussionreduction debris).Only200fragmentsofjadeitewererecoveredfromexcavationsinthesouthern portionofthepatiogroup;the"vastmajority"ofartifactsrecoveredwere"domesticand foreignceramicfragments"(Walters1980b:103104).Basedonthisevidence,Walters

(1980b:104)arguesthatthesouthernportionofthepatiogroupwasoccupiedbya domestichouseholdfocusedontheproductionofobsidianblades,foreitherinternal consumptionwithinthepatiogroup,orforexternalconsumption.Allofthestructuresin thesouthernportionofthepatiogroupweredestroyedbytheconstructionofthelocal elementaryschoolinthelate1980s.

Excavationsinthenorthernperimeterofthesunkenpatiowerelocatedwithinthe areathatWaltersdesignatedArea4;intotal,eight2mx2mandthree1mx1munits wereexcavated(seeFig.5.5).Whenoneoftheunits(Area4,Excavation4),revealeda

137 seriesoffloorsextendingtoadepthof1.8metersbelowthesurface,Walters(1980a:12)

openedeight2mx2munitsorientednorthsouthinthevicinityofExcavation4.The

northernretainingwallofthe

Figure5.7PlanmapofunitsexcavatedinArea3andthefloorplanofLateClassic featuresrevealedinthoseexcavations.Romannumeralspointtothelocationof cachesofobsidianbladecores(modifiedfromWalters1980b:90). patiogroupwasencounteredinExcavation11and12,andtheseunitswereleft unexcavated(Fig.5.8).Unitslocatednorthofthewall(Excavations58)revealedan occupationalhistoryspanningfromtheLatePreclassicthroughLateClassicperiods, whileExcavation9and10,locatedtothesouthofthewall,containedonlyLateClassic periodcontexts(Walters1980a:12).Althoughnoartifactcountsareprovided,Walters

138 (1980a:18)notesrecoveringjadeiteproductiondebitageandtoolsassociatedwithjadeite

debitageproduction(e.g.jadeitehammerstonesandpolishingstones)inalllevelsof

Excavations48,withthehighestconcentrationsintheupper(LateClassic)levelsofthe

units.InExcavation9and10,jadeitedebriswaslimited,but"numerousobsidiancores

andcoreandbladefragments"wererecovered.Thegreaterquantitiesofjadeitedebris

recoveredfromthenorthernportionofthepatiogroupledWalters(1980a,19880b,1989)

toarguethatcraftspecializationwasinternallysegmentedwithinthepatiogroup,with

residentsofthesouthernportionproducingobsidianblades,thenorthernportion producingjadeiteartifacts,andthewesternportionofthepatiodirectingtheseactivities, aswellaspracticingalimitedamountofjadeartifactproduction.

Figure5.8MapindicatingthelocationofexcavationunitsfromArea4 (fromWalters1980a:13)."Groundsurface"indicatesprofileofgroundlevelfrom XtoYonsketchmap. DatafromexcavationtheexcavationsofSmithandKidder(1943;Kidder1935)

andWalters(1980a,1980b,1989)providedimportantindicationsabouttheprehispanic

inhabitantsofGuaytan.AlthoughLatePreclassicceramicswererecoveredfromMiddle

MotaguaValleysitesduringthearchaeologicalsurveyconductedaspartofthis

dissertationresearch,previousexcavationsrarelyrecoveredceramicsfromthattime period.Inaccordwiththeresultsofoursurvey,thegreatmajorityofceramicsfrom

139 SmithandKidder'sandWalters'excavationsdatetotheClassicperiod,withLateClassic ceramicsbeingmostabundant.

Despitetheimportantcontributionsofbothoftheseprojects,wewerestillleft withanincompleteandfragmentarydatabaseforunderstandingtheprehispanic organizationofjadeartifactproductionatGuaytan.Particularly,neitherSmithand

KiddernorWalterspublishedanydetailsabouttheevidenceofjadeartifactproduction recoveredintheirexcavations.Becauseofthislackofspecificdata,furtherexcavations werenecessaryfordetailingandreconstructingthestructureofjadeartifactproduction.

Themethodologyandresultsofexcavationscompletedaspartofthisdissertation researcharesummarizedbelow.

5.2 ExcavationsforLowerLatoRiverArchaeologicalJadeProject

Acriticalpartofthisdissertationresearchinvolvedexcavationinareasidentified inJuly2004aspossiblejadeiteworkshopsbasedonthepresenceofhighconcentrations ofsurfacedebitage.Thegoalsoftheseexcavationsweretwofold:(1)todetermine whetherthesurfaceevidencewasindicativeof in situ jadeiteworkshops;and(2)to collectevidenceregardingthesocialcontextofthisjadeiteartifactproduction(i.e. specializedvs.domesticcontexts).ExcavationsbeganonOctober17,2005andfocused onthreeofthesepreviouslyidentifiedareas:Guaytan3,Guaytan4andMagdalenaI.In addition,eighttestpitswereexcavatedatGuaytan5(3testpits),Guaytan7(2testpits),

Guaytan8(2testpits)andKM93I(1testpit). Asummaryoftheresultsofthese

excavationsareprovidedhere;fulldescriptionsoftheexcavationscanbefoundin

AppendixB.

140 5.2.1 ExcavationMethodologyandLocationofExcavationUnits

Asnotedabove,inJuly2004,archaeologicalreconnaissanceidentifiedsurface

scattersofjadeitedebitageatthesitesofGuaytan(Guaytan3andGuaytan4)and

MagdalenaI(Fig.5.9).Basedonthesurfaceremains,Idecidedtoundertakeaprogram

oftestpittingintheseareastolocate in situ evidenceofjadeartifactproductionandto

obtainastratifiedsampleofjadeproductiondebitageandceramicmaterial.Test

excavationswereimperativeformyresearchprojectinordertoassessthequality,

significanceandrepresentativesofthesurfacecollections;approximatelysevenweeks

weredevotedtotestexcavations.

WorkbeganatGuaytan4(Operatin1A&1B),thelargestanddensestsurfacedebitage

scatteratGuaytan,wherea25mx30mgridwasimposedinordertoprovide provenienceforasystematiccollectionofsurfacearchaeologicalmaterials,and

subsequentlyforexcavation(Fig.5.10,5.11,5.12,5.13).Thegridwasorientedto

magneticnorth,andgridunitswereorganizedaccordingtoacoordinatesystem,usingan

arbitrarydatumpointlocatedtothesoutheastofthedebitagescatterastheorigin.Using

theestablishedgrid,nine1mx1mgridunitswereimposedoverthedebitagescatterand

allarchaeologicalartifactswerecollectedwithineachunit(Fig.5.12).Thesurface

collectionsinthe1mgridsquaresservedasadirectcheckagainstwhichtocomparethe

subsurface,stratifieddepositsoflithicmaterials(Table5.1).

Afterthecompletionofsurfacecollections,two1mx1mexcavationunits

(N6E12andN7E12)wereselectedbecauseofthehighdensityofsurfaceartifactsand

theirlocationalongtheoutsideperimeteroftwolowstructureretainingwalls(these

excavationsaredescribedinsection5.3).Excavationsproceededbyarbitrary10cm

141 Figure5.9–Locationofsitesexaminedaspartofthisdissertationresearch. levels,unlesscleardepositionallayerswereobserved.Allexcavatedmaterialwas

screenedthrough1/8”meshscreenstoensurethecollectionofallsizegradesofjadeite

debitageandotherarchaeologicalmaterial.A10cmx10cmcolumnwasleft

unexcavatedineachunitforthecollectionofsoilsamplestobeusedformicroscopic

examinationofparticlesofjadeiteandpossibleabrasivesusedtogrindandpolishjadeite,

suchasgarnetorquartz;thesehavenotasyetbeenexamined.Wehadhopedtocollect

charcoalsamplesduringexcavationsforC14dating,butdidnotencounteranygood

samplesinthecourseofexcavations.

Aftertheexcavationsoftheseunitsfailedtoyieldstratified in situ workshop

deposits,adeterminationwasmadetochangeexcavationstrategies.Aprogramoftest pittingusing50cmx50cmunitswasinitiatedintwootherareasoftheGuaytan4(Fig.

5.13)containingjadeitesurfacesscatters(Op.1D,1Eand1F),aswellasintheGuaytan3

142

Jade drills Chert Flakes fragments Drill Cores Drill jadebeads JadeHollow Groundjade Broken/patial 1A-N5E10 14 - 1 - 1 1A-N5E11 1 - - - 1 1A-N5E12 5 1 - - - 1A-N6E10 24 - 1 - 3 1A-N6E11 27 - - 1 - 1A-N6E12 8 1 1 - - 1A-N7E10 19 - 1 - - 1A-N7E11 6 - - - 3 1A-N7E12 5 - 1 - 3 TOTALS 107 2 5 1 11 Table5.1Artifactscollectedin1msquaresatGuaytan4priortoexcavations(see Fig.5.12forlocationofgrid).Theseartifactswereincludedinsurfacecollections (presentedinChapter4)forGuaytan4. site(Op.1C).Excavationsof50cmx50cmtestpitsproceededbyarbitrary20cm

levelsafterobservationsfromtheOp.1Aand1Bexcavationsrevealedthat10cmlevels

weretoounnecessarilytimeconsumingforidentifyingstratifieddeposits.Nevertheless,

whencleardepositionallayerswereencountered(e.g.floors,subfloorfill),thesewere

usedtoidentifystratigraphiclayers.

FurtherreconnaissanceatGuaytanidentifiedadditionalareascontainingsurfaceevidence

ofjadeartifactproduction(Guaytan5,Guaytan6,Guaytan7,andGuaytan8).We

excavated50cmx50cmtestunitsineachoftheseareastodeterminethenatureofthese

surfaceconcentrations(Fig.5.11).TestexcavationswerealsomadeatMagdalenaI,and

KM93I;wewereunabletosecurepermissiontoexcavatefromlocallandownersatthe

VargasIIIsite.Wherenecessarybecauseofthedepthofarchaeologicaldepositsor becauseofthedensityofrecoveredmaterial,excavationunitswereexpanded

horizontallytoenableartifactrecovery.Atotalof32unitswereexcavatedtobedrockor

143 sterilesoil.Theresultsoftheseexcavationsaresummarizedbelowanddetailed descriptionsofallexcavationsareprovidedinAppendixB.

Figure5.10MapofGuaytan,hatchedlinesindicatelimitsofmapinsetshownin Figure5.11(modifiedfromLopezn.d.,inRámonRamírez2006).

144 Figure5.11DetailofsouthernportionofGuaytan,indicatinglocationofareaswith jadeartifactproduction,identifiedduringarchaeologicalsurfacesurvey.

145

Figure5.12Mapshowinglocationofstructures,gridsestablishedforexcavations andlooter'strenchesatGuaytan4.Op.1Aexcavationunitsareshaded ingreyon3mx3mgrid.

146 Figure5.13SouthernportionofGuaytan4,showinglocationofexcavationunits. 5.3 SummaryofexcavationsatGuaytan4

OurmostintensivetestexcavationswerecarriedoutatGuaytan4,aTypeIIsite inthelocalsettlementhierarchylocatedalongthesouthernportionofGuaytan(Fig.5.11,

5.12,5.13).Guaytan4isborderedonthewestbyasmallquebrada,andisborderedon

147 theeastbythemodernroadtoGuaytan;thesouthernedgeofthesiteisdefinedbythe fencethatsurroundsaroundtheelementaryschoolthatwasbuiltinthelate1980s.The southernandsouthwesternperimetersoftheGuaytan4werethelocationofthe"Area3" and"Area4"excavationsbyWalters(1980a,1980b,1989)thatweredescribedearlierin thischapter.Theconstructionofthelocalelementaryschoolhassincedestroyeda portionofthesite(Area3)(Fig.5.4,5.5,5.7).Althoughitislocatedapproximately100 metersfromtheportionofGuaytanthatWalters(1982)identifiedasbeingapossible eliteresidentialarea(Areas5and8inFig.5.4),Guaytan4itselfisofmodest constructionandsize.

Guaytan4iscomprisedoftwogroupsoflowstructureslaidoutoveraseriesof smallplatformsbuiltintogentlyslopingterrain(Fig.5.12).Inthenorthernportionofthe sitearefourstructures,allofwhichhavebeenextensivelylooted.Structure1islocated immediatelyadjacenttothemodernroadtoSanAgustinAcasaguastlan,andis12mx8m, orientedroughlynorthsouth.Structure2isa5mx5msquaremound, approximately.5mtall.Structure3islocatedninemeterstothesouthofStructure2,and isanother5mx5msquaremound,approximately.5mtall.Structure4islocatedonthe westernedgeofthenortherngroup,andisasmall(1mtall)mound,locatedatthebaseof asteepslopetothewest.Alooter'strenchdugintothecenterandsidesofthestructure revealedthepresenceofalootedslablinedtomb.Verylittlejadeevidenceofjade artifactproductionwassurfacecollectedinthisarea.

Approximately25meterstothesouthwestofStructure4aretheedgesoflow terracewalls(lessthan25cm)builtintothegentlyslopingterrain(Platforms1and2,Fig.

5.12).InJuly2004,archaeologicalreconnaissanceidentifieddenseconcentrationsof

148 jadeitedebitagethissouthernportionofGuaytan4(Fig.5.12,5.14).Allsurface collectedandexcavatedevidenceofjadeiteartifactproductionwasrecoveredin associationwiththesouthwesterncornersofPlatforms1and2(Operations1Aand1B) andthenorthernandwesternperimeterofasunkenpatioareabuiltinthelowpointof twoslopes(areaofOperations1D,1E,1F;seeFig.5.5forcontourmapofsouthern portionofGuaytan4).ThesunkenpatioisboundedonthenorthbyPlatform3andon

thewestbyasimilarplatformwallidentifiedbyWalters(1980b)inhisexcavationsof

thearea(Fig.5.6).BecauseofdensevegetationinthewesternportionofGuaytan4,we

wereunabletodefinethelimitsofthewesternedgeofthesunkenpatio.Structure6sits justatoptheplatformwall,althoughIcouldnotdiscernthisisthesamestructure identifiedandpartiallyexcavatedbyWalters(1980b).Asnotedabove,thesouthern portionofthesunkenpatiowasdestroyedintheprocessofbuildingthelocalelementary school,althoughWalters(1980b)excavatedthisarea,asdescribedearlierinSection

5.1.2).InthecenterofthesunkenpatioaretheremainsofStructure5,anextensively lootedmoundbuiltoveraslablinedtomb.

Figure5.14Panoramicviewlookingsouth;thesouthernportionofGuaytan4 istotheleftofthefootpathextendingfromtheleftforegroundofthephoto.

149 FollowingthecompletionofsurfacecollectiondescribedinSection5.2.1,two1m x1munitslocatedoffthesouthwestcornerofaPlatforms1and2wereselectedfor excavation(Fig.5.13).Excavationunit1A1(surfacecollectionunitN6E12)andunit

1A2(surfacecollectionunitN7E12)werechosenforexcavationbecausetheywere believedtoprovidethebestopportunityforrecovering in situ evidenceofjadeartifact production.Theirselectionwasalsobasedontheobservationthattheunitsquares locatedtothewest(N6E10andN6E11)containedthedensestconcentrationsofjade debitage(Table5.1),andthatthismaterialmayhaveerodedfromdepositsfurther upslope,wherethetwoexcavatedunitswerelocated.Thetwounitswereexcavated simultaneously.Constrainingourselectionofotherexcavationunitsinthisareawasthe factthatIDAEHhadexplicitlyforbiddenexcavationwithinstandingarchitecturewithout priorauthorization.TheintentattheoutsetofexcavationswastoexcavateunitsN6E10 andN6E11uponcompletionofthefirsttwoexcavationunits.Unfortunately,time constraintsquicklymadethisunfeasible,astheexcavationsprovedtootimeconsuming forthelimitedpersonnelavailable.Additionally,itwassoonapparentthatrecoveryof in situ jadeartifactproductionwasunlikelyintheseareas.

Units1A1and1A2uncoveredaseriesoftworesurfacings,possiblyofaplaza floor.Thefirstfloor,locatedapproximately50cmbelowthenaturalsurface,wasaburnt plasterfloorthathadbeenplacedoverasubflooringoffine,compactedsoilthat containedpiecesofjadeitedebitageandotherartifactualmaterial(Fig.5.15).Asecond floorwasencounteredatapproximately80cmbelowthenaturalsurface,whichappearsto havebeentheearliestplazafloor;thenaturalbedrockwasencountered25cmbelowthis floorinUnit1A2,withfewartifactsintheinterveninglevel.Excavationinunit1A1

150 washaltedatthelevelofthesecondfloorupondiscoveryofasmall30cmx40cmx

11cmfirepit.Althoughjadeproductionevidenceandotherlithicandceramicartifacts wererecoveredateverylevelwithinbothunits,no in situ evidencewasuncoveredin

eitherunit.Inaddition,despitethetwofloorresurfacings,allexcavatedlevelscontained

atleastsomeLateClassicperiodceramics.Table5.2presentsasummarycountofthe

artifactsrecoveredfromUnits1A1and1A2.

Figure5.15Excavationprofileofunit1A1. Op.1AArtifactTypes n Table5.2Artifactsrecoveredin excavationunits1A1and1A2. JadeFlakes 693 JadeBeads 3 JadeBeadPreforms 6 Broken/PartialJadeBeads 4 JadeHollowDrillCores 2 CutJadeFragments 3 GroundJadeFragments 21 LargeJadeFlakes 3 ChertDrills 125 WorkedShellFragments 10 ObsidianBlades 570 ObsidianFlakes 79 ObsidianBladeCores 1 Nonjadebeads 1 Hammerstones 1

151 Anadditional1mx1munit(1B1)waschosenforexcavationinsideofthelow platformwallslocatedtothenortheastof1A1/1A2,inordertodetermineifthewall

visibleonthesurfacewastheedgeoflowplatformstructureorpartofthenaturalterrain

(Fig.5.13).Excavationofthisunitwasabandonedsoonafterasurfaceofarchitectural

stoneswasencounteredatadepthof33cmbelowthesurface,asexcavationinto

standingarchitecturewasprohibitedbyIDAEH(Fig.5.16).Fewartifactswererecovered

fromtheunitandthemajorityofexcavatedceramicswerefromtheLateClassicperiod.

Figure5.16Planphotooffloor inUnit1B1,whereexcavation wasterminated.

Aftercompletionoftheseexcavations,Idecidedtoswitchexcavationstrategiesto enablemorerapidtestpitting.Forallotherexcavations,weexcavated50cmx50cm unitsinordertogetagreaternumberofsamplesfromdifferentcontexts.Sixunitswere selectedforexcavationinanareaofheavyjadesurfacedebitagetodeterminethenature ofthesurfacescatters(1D1thru1D6).Theunitswerelocatedattheedgeofthe quebradathatmarksthewesternedgeofGuaytan4(Fig.5.13).Allunitswereexcavated

152 tobedrock,whichrangedfrom40cmto1mbelowthenaturalsurface.Intwoofthe

excavationunits,alevelofcompactsoilwasnotedthatappearedtobetheremainsofan

erodedplazafloor,butthiscouldnotbeconfirmedacrossalltestunits.Ceramicmaterial

intheseunitsdatedtotheEarlythroughLateClassicperiods,butonceagain,alllevels

containedLateClassicperiodceramics.Jadeproductionevidencewasrecoveredfrom

allunitsofOperation1D(Table5.3). Unit Cores Preforms JadeBead Fragments JadeBeads JadeFlakes ChertDrills GroundJade Broken/Partial Obsidianflakes Obsidianblades JadeHollowDrill 1D1 1 0 16 0 0 0 0 5 1D2 9 0 208 0 0 0 2 25 1D3 17 10 86 2 2 0 5 16 1D4 4 1 67 0 0 0 0 11 Table5.3Artifacts 1D5 18 8 48 0 0 0 0 12 recoveredfrom 1D6 14 1 135 0 3 0 0 13 Operation1D Totals 63 22 560 2 5 0 7 82 excavations.

Fiveadditionalunits(Operation1Eand1F)wereexcavatedfromeasttowest alongPlatform3,along,platformretainingwallthatformsthenorthernedgeofthe sunkenpatiointhesouthernportionofGuaytan4.Excavationwasinitiatedtoobtaina stratifiedsampleofproductiondebitage,basedonthepresenceofhighsurface concentrationsofjadeitedebitagelocatedatopandbelowtheplatformwall.Theareais thenorthernportionofthegroupexcavatedbyWalters(1980,1989),inwhichhe reportedfindingdensedepositsofjadeitedebitage.Fouroftheunits(1E1thru1E4) wereplacedbelow(southof)theplatformwall.Anadditionalunit(1F1)wasplacedon theplatformitself,approximately1mnorthoftheplatformwall.Allunitswere

153 excavatedtobedrock,whichrangedfrom84cm(1F1)to1.8m(1E3)belowthenatural

surface.Afterexcavation,itwasobservedthatunits1E3and1E4werebothnorthof

theplatformretainingwall.

Unfortunately,no in situ evidenceofjadeiteartifactproductionwasuncoveredas partofOperations1Eand1F.Nevertheless,allexcavationunitsyieldedsignificant amountsofjadeiteproductionevidence,includingflakedebitage,completeand incompletebeads,sawnjadepieces,jadefragmentswithevidenceofgrindingand polishing,andnumerouschalcedonydrills,typicallyrecoveredaspartofsubfloorfill

(Table5.4).Inaddition,Operations1Eand1Falsoyieldedevidenceofthepossible productionofobsidianblades(Fig.5.17)andproductionofshellartifacts(Fig.5.18).All unitsyieldedLateClassicperiodceramics,althoughEarlyClassicceramicswere recoveredfrommostunitsaswell.Allshowevidenceofmultipleepisodesoffloor construction,mostofwhicharebadlyerodedandpoorlypreserved,theearliestofwhich wereconstructedonlyafewcentimetersabovethetalpetate.

Unit Obsidianblades Obsidianflakes ObsidianBladeCores JadeFlakes JadeBeads JadeBeadPreforms Broken/Partial JadeBeads JadeHollowDrillCores CutJadeFragment GroundJadeFragment ChertDrill WorkedShell NonGreenstoneBeads 1E1 42 14 83 1 1 8 1 1 3 3 1E2 62 30 248 83 4 1 3 17 2 1E3 100 33 855 1 10 37 4 6 2 4 2 1E4 37 11 121 1 3 1 1 2 1F1 13 8 32 1 2 1 1 1 1 TOTALS 244 92 248 1174 3 1 25 42 6 14 23 6 2 Table5.4ArtifactcountsfromOperation1Eand1Fexcavationunits.

154 Especiallyintriguingwasthediscovery,inthesouthwesterncornerofunit1E2, ofacacheofexhaustedobsidianbladecoresplacedatthebaseoftheplatformwall(Fig.

5.17).Thecachewaswelldefined(40cmindiameter,22cmdeep)andwascoveredwith anumberoflargeceramicfragmentsandunworkedstones,placedoneontopoftheother,

Figure5.17Cacheofobsidian bladecoresfromexcavationat Guaytan4.Right:Definitionof cacheddeposit.Above:Upperlevel ofcacheafterremovaloflarge ceramicfragments.

155 Fig.5.18FragmentsofworkedshellrecoveredfromGuaytan4excavations: (left)brokenshellearspool,(right)fragmentofworkedshell. withoutanyobviouspattern.Thelargestceramicpiecewasafragmentofalargeurn witharaisedzoomporhicface;fragmentsoftheborderofsomecomalesandunidentified bodysherdsalsocoveredthecache.Thecachewasexcavatedin5cmlevelstoensure carefulrecoveryofit'scontents.Intotal,thecachecontainedatotalof245obsidianblade cores;anadditionalthreeobsidianbladecoreswererecoveredfromotherlevelsofthe sameunit.Theonlyothercontentsofthecacheincludedapossiblejaguarclaw(Fig5.19) andfourpiecesofjade(twoflakes,onedrillcoreandonefragmentwithevidenceof grinding).Theplacementofthecachealongtheexteriorfaceofaplatformwallis consistentwiththeplacementofsimilarcachesinthesouthernportionofthisgroupthat wereexcavatedbyWalters(1980b,1989)beforetheyweredestroyedbytheconstruction oftheschoolthatnowcoversaportionofthegroup.

Figure5.19Possiblejaguarclawrecoveredfromcontentsofobsidianbladecore cache(scaleincentimeters).

156 5.4 SummaryofGuaytan3Excavations

ThesiteofGuaytan3(TypeIsite)islocatedtothenorthofGuaytan4ona narrowbluffattheconfluenceoftwosmallquebradas;therearenostructuralremainsat thesite(Fig.5.20).Theareawaschosenforexcavationbasedonthepresenceofa surfacescatterofjadeitedebitage,inthehopesthatexcavationmightclarifythenatureof thisdeposit.Weexcavatedthreesmall50cmX50cmtestpitstoassessthesignificance ofthesurfacedebitageobservedinthearea.Allexcavationsterminatedat60cmindepth uponreachingbedrock.Fewartifacts(andnoceramicmaterial)wererecovered, althoughlimitedevidenceofjadeiteartifactproductionwascollected (Table5.5).The natureofthesurfacescattersremainsunclear.

Figure5.20ViewofGuaytan3,lookingtothenorth. Op.1CArtifactTypes n Table5.5Artifactsrecoveredin JadeFlakes 113 Operation1CexcavationsatGuaytan3. GroundJadeFragment 1 ObsidianBlades 6 ObsidianFlakes 2

157 5.5 SummaryofGuaytan5Excavations

TestexcavationsatGuaytan5(aType2site)wereintendedtoassessthenature ofsurfacescattersofjadeiteandobsidiandebitage.Thesiteislocatedacrossaquebrada tothesouthwestofGuaytan4andacrossaquebradatothesouthofGuaytan6;thesiteis comprisedofagroupofthreelowplatforms(lessthan25cminheight)(Fig.5.21).

Unfortunately,allthreeofourexcavations(Operation2,Units2A1,2A2,and2A3) wereterminatedatamaximaldepthof20cmuponreachingbedrock.Nosubsurface ceramicsorevidenceofjadeiteartifactproductionwasrecoveredfromanyofthe excavations;twoobsidianbladeswererecoveredfromoneunit.

Figure5.21ViewofGuaytan5,lookingwestbysouthwest.

5.6 SummaryofGuaytan6Excavations

Guaytan6(aTypeVsite)islocatedtothenorthofGuaytan5andtothewestof

Guaytan4,separatedfrombothgroupsbysmallquebradas.Thesitewasdescribedby

SmithandKidder(1943)andWalters(1982)asaseriesofeliteresidential,ritualand

ceremonialgroupsconstructedatopanaturalhill(Fig.5.11).Themajorityofstructures

158 atGuaytan6havebeenextensivelydestroyedbylootingwithsomestructuresbeing

reducedtoapileofdiscardedstonesandlooters'backdirt;somelooter'spitsareusedas

garbagedumpsbyvillageresidents.AlthoughreportsofGuaytan6indicatethepresence

ofaballcourt,nonecouldbeidentifiedfromtheremainingstructures.

Oneunit(Operation6,unit6A1)wasexcavatedinasurfaceconcentrationof jadedebitagelocatedonthesoutheasternperimeterofthesite,behindagroupoflow,

masonrysubstructureplatformsimmediatelyadjacenttotheedgeofthequebrada

separatingGuaytan6fromGuaytan4.Giventhesurfaceconcentrationofjadeite

debitage,chalcedonydrills,obsidianandceramics,theunitwasexcavatedinthehopeof

revealingadumpfromthenearbystructures.Theunitwasterminatedatadepthof60

cmuponreachingsterilesoil.Onlytheupperlotyieldedceramicsthatcouldbedated;

themajoritydatetotheEarlyClassicperiod,butincludeLateClassicceramicsaswell.

Jadeiteproductionevidenceconsistedsolelyofflakesandchalcedonydrills(Table5.6) .

Op.6AArtifactTypes n Table5.6Artifactsrecoveredin JadeFlakes 62 Operation6AexcavationatGuaytan6. ChertDrills 23 ObsidianBlades 3 ObsidianFlakes 3

5.7 SummaryofGuaytan7Excavations

Guaytan7isasectorofthesouthernportionofGuaytanthatcontainsacoreof eliteresidentialstructuresthatwerestudiedandexcavatedbybothSmithandKidder

(1943)andWalters(1980)(Fig.5.11).ItisaTypeVsiteinthelocalsitehierarchy.

Duringsurveyofthissectorofthesite,asmall,widelyscatteredcollectionofjadeite debitagewasobservedinasmallplazaontheeasternedgeofthesitesector,whichhas

159 partiallydestroyedonitswesternedgebytheroadtoSanAgustinAcasaguastlan.Two small50cmX50cmunits(Op.3A1and3A2)wereexcavatedtorapidlyassessthe significanceofthissurfacematerial.Anerodedplasterfloorwasuncoveredatadepthof approximately50cmbelowthesurfaceintheeasternmostofthetwoexcavationunits

(Fig.5.22);jadedebitagewasrecoveredfrombelowthisplasterfloor.Bothunitsyielded significantamountsofjadeitedebitageflakes,butfewcategoriesofevidenceofother typesofjadeartifactproduction(Table5.7).CeramicsdatedtotheClassicperiod generally,withthemajorityfromtheLateClassicperiod.Bedrockwasreachedat approximately1.3mbelowsurfaceinbothunits.

Figure5.22Stratigraphicprofileof unit3A1atGuaytan7.Solidblack layerindicateserodedplasterfloor. Maximumdepth=1.4m.Northwall ofexcavationunitis50cmwide.

Op.3AArtifactTypes n Table5.7Artifactsrecoveredin JadeFlakes 1051 excavationunits3A1and3A2. Jade(PartialBeads) 1 Jade(Polished) 3 ChalcedonyDrills 7 ObsidianBlades 88 ObsidianFlakes 15

160 5.8 SummaryofGuaytan8Excavations

Guaytan8(aTypeIVsite)isasectorofthesiteofGuaytanlocatedatthefar southernperimeterofGuaytanCiudadela,approximately150mtotheeastofGuaytan4 and50mtothesouthoftheGuaytan7testexcavations(Fig.5.11).Althoughno architecturalremainsarevisibleonthesurfaceofthissector,itshouldbenotedthatthe sectorliesdirectlytothesouthofaheavilylootedareaofeliteresidentialarchitecture thatsitsonasmallnaturalplateauabovethefield.Duringsurvey,35piecesofworked jadeitewerecollectedinthefield,whichhadbeenusedformaizecultivationasrecently as2002.Aftertalkingwiththelocallandowneranddeterminingthatthefieldhadonly beenplowedbyhorsedrawnplows,Idecidedtoexcavatetwosmalltestunitstoassess thecharacterofdepositslocatedbelowtheplowzone(Operation4,units4A1,4A2).

Unfortunately,excavationshadtobeabandonedbeforecompletionwhenthelandowner’s sonschangedtheirmindsaboutgrantinguspermissionandaskedustoleave.

Althoughrecoveredfromdisturbedcontexts,thetwotestunitsyieldedsome unusalfinds,includingtwostingrayspines,twopiecesofdrilledobsidian(Fig.5.23), alongwithobsidianbladesanddebitageandevidenceofjadeitebeadmanufacture

(predominantlyjadeiteflakes,butalsoajadeitehammerstone)(Table5.8).Ceramics datedprimarilytotheClassicperiod,thoughPostclassicmaterialwasrecoveredfromthe upperlevelinbothunits.Noundistrurbed,stratifiedcontextswereencounteredineither unit,althoughfragmentsofburntclay,possiblyfromtheexteriorofawaddleanddaub structure,wererecoveredinunit4A1.

161 Figure5.23Stingrayspine(left)anddrilledobsidian(right)fromGuaytan8 excavations.Unitsonscaleare1cm. Op.4AArtifactTypes n Table5.8Artifactsrecoveredin JadeFlakes 588 excavationunits4A1and4A2. Jade(PartialBeads) 1 JadeBeadCores 1 ChalcedonyDrills 13 WorkedShellFragments 1 ObsidianBlades 113 ObsidianFlakes 54 Hammerstones 1

5.9 SummaryofMagdalenaIExcavations

ThesiteofMagdalena(locatedontheedgesofthemodernvillageofthesame name)occupiesaseriesofriverterracestotheeastoftheRioLato(Fig.4.14); itisa

TypeVsiteinthelocalsettlementhierarchy.Waltersdividedthesiteintothreesurvey sections,eachseparatedfromoneanotherbynaturalquebradas;MagdalenaIisthe northernmostsectorofthesite.InJuly2004,wefoundjadeitedebitagescattersinthe westernandeasternperimetersoftheeliteceremonial/residentialcoreofMagdalenaI,in directassociationwitheliteresidentialarchitecture.MagdalenaIhasbeenheavilylooted, makingitdifficulttofindundisturbedlocationsfortestpitting.

Seventestpits(Operation8)wereexcavatedatMagdalenaI:onetestpitinthe easternperimeterofthesite(8A1),onetestpitinthecentralplazaarea(8A3),andfive

162 testpitsinthewesternportionofthesite(8A2,8A4,8A5,8A6,and8A7)(Fig.5.24;

Table5.9).Noneoftheexcavationsreachedmorethan80cmbeforeterminatingin sterilesoiloratbedrock.Units8A1and8A6,excavatedintheeasternandwestern perimetersofthesiterespectively,producedthegreatestamountsofjadeiteproduction

evidence,thevastmajorityofwhichweresmallflakes(Table4.12). Threeunits(8A4,

8A6,8A7)wereexcavatedintoconcentrationsofjadeitedebitagelocateddownslopeof

theeasterngroupofstructuresinthehopesoffindingarefusedump,butallunitsyielded

fewartifactsbelowtheuppermostlevels.AlllevelsofallunitsyieldedLateClassic periodceramics,alongwithsignificantamountsofEarlyClassicperiodceramics . Unit Jade Jade Non Shell Drills beads Chert Flakes Flakes Blades Ground Worked Preform Obsidian Obsidian Fragment JadeBead greenstone 8A1 5 1 817 1 2 1 1 8A2 5 29 37 8A3 1 8A4 14 1 67 7 8A5 1 1 8A6 10 2 165 2 10 8A7 3 TOTALS 35 33 1091 3 2 17 1 1 Table5.9ArtifactsfromMagdalenaItestunits.

5.10 MiscellaneousExcavations

Onetestunitwasexcavatedineachofthefollowingsites:VargasIIB(Operation

7,Unit(7A1),KM93I(Operation9,Unit9A1),andKM92III(Operation10;Unit

10A1).Eachunitwasexcavatedinareaswithsurfaceconcentrationsofjadeitedebitage, althoughnoneweresuccessfulinlocatingdense,stratifiedjadeitedeposits(Table5.10).

Fewceramicswererecoveredineachunit,themajorityofwhichdatedtotheLate

Classicperiod.

163 Jade Jade Jade Shell Non Bead Drills Chert Flakes Flakes Blades Hollow ebeads Worked Obsidian Obsidian Preforms

Unit greenston DrillCore 7A1 45 23 67 1 1 1 1 9A1 15 22 95 2 10A1 2 1 5 TOTALS 62 38 167 1 2 1 1 1 Table5.10Artifactsfrommiscellaneoustestunits. 5.11 DiscussionofExcavationResults

Oneoftheprimarygoalsofthisdissertationresearchwastoundertaketest excavationstoconfirmthepresenceof in situ productionevidenceinareaswithdense surfaceconcentrationsofjadeiteproductiondebitage.Unfortunately,noneofthe excavationsyielded in situ evidence,butthetestexcavationsdidrecoveragreatdealof materialrelatedtojadeartifactproduction.Atotalof5,744piecesofjadewere recoveredfromallexcavations.Inaddition,toolsassociatedwithjadeartifactproduction werealsorecovered,including296chalcedonydrillsanddrillfragmentsand2 hammerstones(Table5.11).

Artifact Types - All Excavations n Table5.11Artifacttotals Jade Flakes 5,585 fromallexcavationsatall sites. Complete Jade Beads 6 Jade Beads Preforms 12 Broken/Partial Jade Beads 36 Jade Hollow Drill Cores 48 Cut Jade Fragments 9 Jade Fragments with Ground Facet 49 Chalcedony Drills 296 Worked Shell Fragments 33 Obsidian Blade and Blade Fragments 1,223 Obsidian Flakes 351 Obsidian Blade Cores 249 Non-jade beads or bead fragments 7 Hammerstones 2

164 Takentogether,theresultsofthetestexcavationssuggestthatsurfaceevidenceof jadeartifactproductionisasomewhatreliableindicatorofthepresenceofsubsurface depositsofjadeartifactproductionatMiddleMotaguaValleysites.In20of32(63%) excavationunits,jadeartifactswererecoveredbelowtheuppermoststratigraphiclevel, although12unitsyieldedjadeinonlytheuppermostlevel.However,onlythe excavationsatGuaytan4andGuaytan7yieldedevidenceofjadeiteartifactproductionin clearlysealedcontextsbeneathplazaresurfacings.Thisindicatesthatsurfacescattersare indicativeofjadeproductionactivityinthevicinityofthelocationofthosescatters,but maynotberepresentativeofthefullrangeofproductiveactivitiespresentatindividual productionareasatsitesintheMiddleMotaguaValley.Inaddition,allexcavationunits containedLateClassicceramicsinallexcavationlevels.

Anotherprimarygoalofthisdissertationfieldresearchwastoobtainsamples fromsubsurfacedepositstousealongwithsurfacecollectionstounderstandthe technologicalprocessofjadeiteartifactproductionintheMiddleMotaguaValley.Our excavationsrecoveredevidenceofarangeofartifactsfromdifferentstagesofjadebeads andotherformsofjadeartifacts.InChapter6,Iusethesurfacecollectionand excavationdatafromthisfieldresearchtoreconstructthetechnologicalprocessofjadeite artifactproductionintheMiddleMotaguaValley.

Datafromtheexcavationsandsurfacecollectionsalsosuggestthatotherlapidary goodswereproducedatsomesiteswithevidenceofjadeartifactproduction.Surface collectionsatMagdalenaI,VargasIIAandGuaytan4includedbeadsofstonesotherthan jadeitethatwerebrokenduringproduction.Evidenceoftheproductionofshellartifacts wasrecoveredfromsurfacecollectionsatMagdalenaIandVargasIIB.Thesesurface

165 collectiondatawerecomplimentedbyexcavationdata.ExcavationsatGuaytan4,

Guaytan7andVargasIIByieldedevidenceofnonjadestonebeadproduction,while

onlyexcavationsatGuaytan4yieldedevidenceofshellartifactproduction.Theco occurrenceofthesedifferenttypesoflapidaryproductionareexaminedinfurtherdetail inChapters6and7.

166 CHAPTER6

MAKINGTHEJADE: THETECHNOLOGICALPROCESSOFJADEARTIFACTPRODUCTION Aprimarygoalofthisdissertationresearchistousearchaeologicalsurface collectionandexcavationdatatoreconstructthetechnologicalprocessofClassicperiod jadeartifactproductionintheMiddleMotaguaValley.Understandingthetechnological processesinvolvedinjadeartifactproductionandtheirmaterialsignaturesprovidesa meansforexaminingtheorganizationofproductionacrosstimeandspace,throughan examinationofthecontextsinwhichevidenceisrecovered.Whatweknowofthe prehispanicprocessofjadeartifactproductionhascomefromethnohistoricsources

(Sahagún19501982)orstudiesoffinishedartifacts(Kidder,JenningsandSkook1946:

118124;Lothrop1957;Foshag1957:4457;Digby1964:1420;Proskouriakoff1974:

817;Taube200).Recentstudiesofjadeproductiondebitage(Walters1982;Kovacevich

2006,2007;Rochette2009)havesignificantlyaddedtoourunderstandingofthe processesofjadeartifactproduction.

Inthischapter,Iprovideanoverviewofthetechnologicalprocessesinvolvedin prehispanicjadeartifactproductionbasedonethnohistoric,ethnographicand archaeologicaldatafromMesoamericaandfromotherjadelapidarytraditionsaroundthe world.ThenIdiscussthelithicartifactanalysesundertakenaspartofthisdissertation researchandhowtheseanalysesarelinkedtoanunderstandingofthetechnological processofjadeartifactproduction.Usingtheresultoftheseanalyses,Ithenpresenta modelfortheoperationalchainforjadeartifacts,particularlyjadebeads,intheMiddle

MotaguaValley(MMV).Inaddition,Iaddressthepresenceofothertypesoflapidary

167 productionatMMVsites,whichsuggestthatsomehouseholdsmayhavebeeninvolved in multicrafting ofdifferentlapidaryproductsthroughtheuseofoverlappingor intersectingtechnologies.

6.1 PreviousStudiesofJadeArtifactProduction

Althoughjadeandjadeartifactsweresymbolicallyimportantandhighlyvalued throughoutMesoamericasincetheEarlyFormativeperiod(Chapter3),jadeuseand knowledgeofjadesourcesandproductiontechniquesseemstohavedisappearedrapidly aftertheSpanishConquest.Ethnohistoricaccountsregardingjadeartifactproductionand theidentitiesofthoseinvolvedincraftingjadearesomewhatvague,butprovideabasis forunderstandingMesoamericanlapidaryproduction.Theonlyethnohistoricaccountof lapidaryproductiontechniquescomesfromSahagún's(15471558)descriptionsofAztec lapidaries:

"Thelapidary[is]wellreared,welladvised;acounselor,informedinhis art;anabrader,apolisher;onewhoworkswithsand;whoglues[mosaic]with thickglue,workswithabrasivesand,rubs[stones]withfinecane,makesthem shine.Hemakesthemshine. Thegoodlapidary[is]acreatorofworksofskill.[Heis]adroit,adesigner ofworksofskill,agluer[ofmosaicsofstone].Theyareglued.Hecreates,he designsworksofskill.Hegrindsdown,hepolishes,heappliesabrasivesand[to stones].Herubsthemwithfinecane;hemakesthemshine;heglues[mosaicsof stone],ofturquoise.Hecuts[stones],cutsthemintopieces,grindsthemdown, cutsthemintotriangles,formsdesignsofthem. Thebadlapidary[is]onewhoscrapes[thestones],whoroughensthem; whoraisesaclatteringdin.[Heis]stupid,bird[like].Hescrapes[thestones]; roughens,shatters,pulverizes,ruins,damagesthem;raisesaclatteringdin." (DibbleandAnderson1961:26) "Themasterlapidariescutrockcrystal,andamethysts,andgreenstones, andemeraldgreenjade,withabrasivesand,andhardmetal.Andtheyscraped themwithaworkedflinttool.Andtheydrilledthem;theyboredthemwitha metaltubulardrill.Thentheyslowlysmoothedthesurfaces;theypolishedthem; theygavethemametallicluster.Andthentheyfinishedthemoffwithapieceof wood[andveryfineabrasive].Theypolishedthemsothattheygleamed,they

168 sentforthraysoflight,theyglistened.Orwithapieceoffinecane[containing silica]thelapidariespolished,finished,perfectedtheirartifacts." [Bloodstone]couldnotbecutwithabrasivesand,butcouldonlybe brokenintopieces,beatenwithastone;anditsroughpieces,whichwerenogood, whichcouldnotbepolished,werecastaway."(DibbleandAnderson1959:8081) "[Ordinaryjades]areformedinthismanner:theyareround,reedlike,like anavel,likeatomato,triangular,cutintriangles,formedintotriangles,thin formedintosquares.Theyarepolished,ground,workedwithabrasivesand, gluedwithbatexcrement,rubbedwithafinecane,madetoshine.Theyglisten, theyaretransparent;therelightappears"(DibbleandAnderson1963:223). Takentogether,thesepassagesprovideavaluablestartingpointforreconstructing theprehistorictechniquesusedintheproductionofjadeandotherlapidarygoods.

AlthoughthedescriptionscomefromcentralMexicoafewdecadesafterSpanishcontact, theyareuseful,withcertaincaveats,forunderstandingtechniquesusedbytheancient

Maya,giventhecontinuityofastoneandwoodbasedtechnologybetweenClassicMaya andPostclassicAztectimes.Basedonthedescriptions,twoprimarytechnological categoriesareevident:percussion(shatteringandpecking)andabrasion(grinding, sawing,drilling,incisingandpolishing).Inthefollowingsections,Iaddressthevarious techniquesofjadeproduction,andthetypesofarchaeologicalsignaturesthateachwould haveproduced.Inthesedescriptions,Iincludeinformationfromarchaeological, ethnohistoricandethnographicsources.

6.1.1 PercussionMethods

Percussiontechniquesincludeanymethodsofartifactproductionthatinvolve strikingonebodyforcefullyagainstanother,withtheobjectiveofrapidlyremoving fragmentsfromoneofthebodiesincontact.Althoughinthepassagecitedabovethe

"badlapidary"isdescribedasonewho"shatters"stones,percussionwascertainlyan importantinitialstepinpreparingjadeforproductionintofinishedartifacts,asSahagún

169 notesforlapidariesworkingwithbloodstone,astonesimilartochert.Percussionwould

havebeenespeciallyexpedientincaseswhereanoduleorpieceofjadesuitablefora particularartifactwasnotavailable,asitwouldhavebeenamuchquickermeansof producingaworkableblankthangrindinganobjectintoshape.Thematerialcorrelates

ofpercussiontechniquesinclude(1)debitageflakes,(2)piecesofjadewithvisible, patternedflakescars,and(3)thetoolsusedtoachievetheremovalofflakes,suchas

hammerstones,punchesandanvils.Percussioncaninvolveoneofthreetechniques:(1)

directpercussion,(2)undirectedpercussion,and(3)pecking.

Directpercussionisperformedby“holdingthematerialtobeflakedinthe unsupportedhandanddirectingthepercussionorpressureimplementwiththeotherhand todetachflakesorblades,”withblowsbeingdirecttowardplatformsfromwhichthe detachmentisinitiated(Crabtree1972:59).Flakesinclude“anypieceofstoneremoved fromalargermassbytheapplicationofforce”(Crabtree1972:64),andwhichare typicallycharacterizedbyaplatform(theflatsurfaceuponwhichaflakewasstruck)and bulbofpercussion(bulbarpartontheventralsurfaceandproximalendofaflake).

Flakesmaybeofanysizeordimension,dependingonthestrengthandangleoftheforce appliedtotheplatformfromwhichitwasstruck.Whiledirectpercussionusinghard, forcefulblowswouldproducelargerflakes,theirregularfracturepatternsofjadeitealso resultinsmallerflakesthatfollownaturalirregularitiesinjadeandareoftenimpededby thedensecrystallinestructureofjadeite.InasmallreplicationexperimentthatI conductedusingjadefromtheMiddleMotaguaValley,hardblowsusingajadeite hammerstoneproducedflakeslarger and smallerthan5cm(Fig.6.1).

170 Figure6.1Jadeiteflakesproducedbyhardhammer,directpercussion. NotethatflakesarelargerANDsmallerthan5cminlength.

Undirectedpercussionisperformedbyrestingacoreoflithicmaterialonananvil

andstrikingitwithahammerstone,althoughblowsusingthismethodarenotdirectedat preparedplatformsonthecore,astheyarewithdirectpercussiontechniques(c.f.

Crabtree1972:42).Undirectedpercussionproducesflakesandshatter,thesizeofwhich

dependontheamountanddirectionofalliedforce.Inpractice,itmaybedifficultto

differentiatebetweenflakesproducedbydirectversusundirectedpercussionforfine

grained,densestonessuchasjadeite,owingtoitscrystallinestructure,whichcancause placestoterminateunexpectedly.DuringthepilotstudyintheMiddleMotaguaValley

thatIconductedinJuly2004,Ivisitedthesitelocallyknownas"Cenegal"withDr.Karl

Taubeandalocaljadeprospector,CarlosGonzalez.Itcontainedalarge,20mwide

scatterofearlystagereductionflakesassociatedwithjadeceltproduction(Fig.6.2).In

additiontotheseflakes,wealsofoundwhatappearedtobeajadeboulderwithpock

marksononesurfaceindicatingitspossibleuseasananvil(Fig6.3);noarchitectureor

ceramicswereevidentatthesite.Unfortunately,thesitewasdestroyedthefollowing

year,apparentlybyjadedealersusingabackhoetolookforajadeoutcrop.Inthis

171 dissertation,nodistinctionismadebetweenflakesproducedfromdirectversus undirectedpercussion,astheirmaterialsignaturesanddifficulttodistinguish.

Peckingisperformedto“formoverlappingsuperimposedcones[ofpercussion],

usuallywiththedirectionofforcebeingappliedtothesurfaceofthematerialina perpendiculardirection”(Crabtree1972:80).Peckingwasusedasameansofinitially shapingroundbeads,celts,andearflaresafterasuitableblankhadbeenselectedfor production.isdonetoshapeanartifactthroughthegradualreductionoftheobject.

Unlikedirectandundirectedpercussion,peckingdoesnotproduceflakes,butinstead producessmall“dust”orsmallfragmentslessthan1mminsize,whicharenotreadily recoverablefromexcavations.However,thesesmallpercussionscarswouldhavebeen undesirableandwouldhavebeenremovedthoughsubsequentabrasion.Nevertheless,

Taube(2004:21)notesthatafewjadeiteceltsintheDumbartonOakscollectionretain evidenceofpecking,evenaftergrinding.Thetermpeckingwillonlybeusedtoreferto casesinwhichobjectsshowsignsofmodificationconsistentwiththistechnique.

a. b. Figure6.2(a)EarlystagepercussionflakesatCenegal.(b)Abortedjadecelt preformsfromsurfacecollectionsatCenegal.(Penusedforscaleis14cmlong.)

172 Figure6.3PossiblejadeanvilatCenegal.Areaincenterofphoto isslightlyconcave.(Penusedforscaleis14cmlong.)

Percussionreductionofjadeartifactsrequirestheuseofhammerstonesof sufficienthardness(greaterthan6.5–7.0MOHSscale)anddensitytobeeffective.

Archaeologicallyrecoveredhammerstonesassociatedwithjadeartifactproduction includejadehammerstonesatGuaytan(Walters1980b;Rochette2009)andCancuen

(Kovacevich2006),aswellasquartziteandcherthammerstones(bothMohs7)at

Cancuen.

6.1.2 Grinding/Abrading

Althoughtheterm carving isoftenused,itis,inastrictsense,inappropriatefor describingtheshapingofjadeartifacts.Carvinginvolvesthecuttingofanobjectby removingmaterialthroughthedirectuseofatoolofsomesort.Unlikewoodorsofter stoneswhichcanbecutdirectly,thehardnessofjadeite(Mohs6.57)rendersmosttools relativelyineffective.AsSahagúnnotes,prehispaniclapidarieshadtorelyontheuseof abrasivestofacilitatetheprocessofshapingjadeiteartifactsintodesiredforms.Itisthe abrasivesthateffectivelydidtheworkinshapingtheseartifacts.Therefore,grindingor abradingisamoreappropriateterm,involvingtherubbingoftwoobjectspastone

173 another,typicallywiththeadditionofanabrasive,withthegoalofmassreductionofthe

originalformornoduleofjade(c.f.Walters1982:52).Asnotedearlier,peckingis

typicallydonetoroughlyshapeanobjectbeforeitisgroundintoform.

Grindingcanbedonethroughoneoftwomeans.Onepossiblemethodis

grindingajadeartifactagainstasolidabrasiveblockofmaterialssuchassandstone.

Chapman(1891:500501)andDesautels(1986:94)notethatMaoriadzeswereground

intoshapewiththeuseofwaterandslabsorblocksofsandstoneorslate(Fig.6.4).At

archaeologicalsitesinIdzumoProvince,Japan,West(1963:11)reportstherecoveryof brokenandunfinishedjadebeadsalongwithgrindingstonesof"granite,withparallel

groovesandlargecirculardepressions."Stoneswithsuchlinearorcircularimpression

wouldlikelyprovidetheonlyeasilyidentifiableevidenceofsuchproductionactivitiesat

archaeologicalsites,asthegrindingprocesswouldproducemicroscopicdustthatwould bedifficulttodiscernfromasurroundingmatrix.InMesoamerica,grindingstonesused

forlapidaryartifactproductionhavebeenidentifiedatTlajinga33at

(Widmer1991),atOtumba(Charlton1993)andatCancuen(Kovacevich2006).Onlyat

Cancuenhasevidenceofjadeiteproductionbeenrecovered,wherethegrindingtools

includedslabsofschistandgreenstone(Kovacevich2006:167).

Figure6.4Artist'srenditionofMaorinephriteadzegrinding. (fromDesaultes1986:101)

174 Alternatively,shapingofanartifactcouldalsohavebeenachievedbygrinding

thejadeiteartifactwitha"flintlike"tool,sometimescalleda“rasp”(Adams2002:79),

ratherthanapplyingthejadeartifacttoanabrasiveslab.Foshag(1957:52)arguesthat

raspingwouldhavebeenusedonlyforreducingpiecesintendedformosaicstoan

appropriatethickness.Intheabsenceofatoolthatcanbeidentifiedasaraspingtool,in practice,itwouldbedifficulttodifferentiatebetweenraspingandotherformsofgrinding.

Therefore,inthisdissertation,thetermgrindingwillbeusedtodescribetechniquesthat

wereintendedtoroughlyshapethesurfaceofanartifactthroughabrasion.

Inmostcasesgrindingwouldhavetobeperformedalongwiththeuseofloose

abrasivesofsufficienthardnesstogrindjade,asnotedinthepassagesfromSahagún

earlier.PossibleabrasivesavailableinMesoamericaincludegarnet,quartz,andcrushed jade.InapossibleEarlyClassicjadeworker'sburial(nohumanremainswerefound)at

Kaminaljuyu,Kidder,JenningsandShook(1946:85,120)reportfindingunfinishedjade

artifactsalongwithabrasivesthatincludedpulverizedjadefragments(maximumgrain

size=3mm)andquartzsand,whichwouldhavebeenthemostreadilyavailableabrasive

inmostareas(quartz=7MOHs,equaltoorgreaterthanjadeite).Foshag(1957:50)also

mentionsthepossibilityofusingcrushedgarnet(Mohs6.57)asanabrasive,buttomy

knowledge,nogarnetshavebeenrecoveredfromarchaeologicalsitesinMesoamerica.

Archaeologicalidentificationoflocationswheregrindingtookplacewould

requirethepresenceofgrindingtools,suchasthosementionedabove,orabrasives,asthe processofgrindingitselfdoesnotproducereadilydetectabledebitage.Inhisworkat

Tlajinga33inTeotihuacan,Widmer(1991)successfullyusedheavyfractionflotationto

recovermicrodebitageofgreaterthan1mmfromsoilsamplestodemonstratethe

175 intensityoflapidaryproductionacrosstheapartmentcompound.Whilesuchrecovery methodswouldcertainlyaidinidentifyingparticulartypesoflapidaryproductionthat werenotrecoverablethroughstandard1/8"inchmeshscreening,theywouldnot necessarilyresultintheidentificationofabrasivesusedinlapidaryproductionbecauseof thedifficultyofdistinguishinganthropogenicallygeneratedfromnaturalquartzgrains

(Widmer1991:145).Theresultsofgrindingactivitiesmaybedetectedonunfinishedor incompleteartifactsthatshowevidenceoflinearstriationsorsmoothedfacetsresulting fromthegrindingprocess.

6.1.3 Sawing

Sawinginvolvescuttingjadethroughtheuseofanimplementmovedlaterally sidetoside(c.f.Walters1982:52).AlthoughSahagún(DibbleandAnderson1959:80

81)describedAzteclapidariesascuttingjade"withabrasivesand,andhardmetal,"the useofmetalforlapidarytoolswaslikelyaSpanishintroduction(Foshag1957:46).Like grinding,sawingofjadeitecouldhavebeendonethroughoneoftwobasicmethods:by usingastoneofequalorgreaterhardnessthanjadeite(withorwithouttheaidof abrasives),orthroughtheuseofasawofsoftermaterialalongwiththeapplicationof abrasivesofsufficienthardness.InNewZealand,Chapman(1891:498499)described theuseofslabsof"quartzoseslate"andwatertosawpiecesofnephritejadefrom outcropsbytheMaori(Fig.6.5).Artifactsresemblingstonesawshavenotbeenreported inMesoamerica.

176 Figure6.5Artist'srenditionofMaori techniqueofsawingnephriteusinga sandstonesaw.(fromKeverne1991: fig.32)

ExaminationofjadeiteartifactsatsomeMesoamericansitesdemonstratesthat sawingwasawidelyusedtechniqueforremovingblanksfromlargerjadebodies.At

Kaminaljuyu,alarge(40cmx45cm)lumpofjadeitewasrecoveredfromanEarly

Classiccache,withnumerousscarsononefacefromtheremovalofpiecesbysawing

(Kidder,JenningsandShook1946:119).Aseriesof"wedgeshapedslices"were removedfromtheboulderbysawinginwardfromtwodifferentdirectionstowardsa centralpointthatwasnevermet;instead,thewedgeswerebrokenapartwhensufficiently closetooneanother,leavingaseptumontheboulderwherethedetachmenttookplace.

Foshag(1957:5253)examinedthreejadeplaquesfromNebaj,intheGuatemalan highlands,onwhichtheoriginalsawedsurfacewasvisibleonthebackoftheplaques.

AnunfinishedearflarefromKaminaljuyu(Kidder,JenningsandShook1946:123124) alsoshowsevidenceofhavingbeencutintoshapebeforegrindingorpolishing.

Sawsofmaterialsofterthanstoneormetalcouldhaveincludedhardwoodsaws.

Foshag(1957:52)notesthatmanyofthecutmarksontheboulderatKaminaljuyuwere eitherentirelystraight,orslightlyconcaveatthebottomofthecut,suggestingthatthe

177 implementusedtosawtheboulderwasofahardmaterial.Similarly,Taube(2004:21

22)notesthatmanyOlmecpiecesintheDumbartonOakscollectionsuggestthatthey hadbeencutusing"abrasiveswithabladelikesolidinstrumentofwood."Inasmall replicationexperiment,Clark(2006)wasabletoproduceasmalldepressioninaslabof

MotaguaValleyjadeiteusingatapereddowelrodofoakandcrushedquartzabrasive;his successfuluseofthehardwoodtoolsuggeststhatitmighthavebeenusefulforsawing jadeiteaswell.

Anotherpossibilitywastheuseofastringsaw,whichinvolvedtheuseofsome

sortofcordageandabrasivestocutjade.JadecarversinChinahavebeenobservedto

usedalargebowsaw(Fig.6.6)intheearly20 th centurytocutjadeiteblocks(Whitlock andEhrmann1949:31).Gump(1962:205)describestheprocessofsawing:

"Threemenworkinsawingthestone.Twoworkthesaw( la-suu-tzu ),which consistsofasinglestrandofwire,generallynotched,anddrawntautinabamboo frame.Withaladleathirdmansuppliesthewetabrasivemixturewhichdoesthe actualcutting.Afterbitingintothejade,theabrasiveflowsdownintoabowlset toreceiveit,sinceitwillbeusedagainandagain,untilitcontainstoomuchjade dusttogripeffectively.Weeks,evenmonths,ofconstant,persistent, backbreakingsawingmaybenecessarybeforethestoneiscutintodesired pieces." AsthereisnoevidenceoftheuseofmetalwireinancientMesoamerica,cordsorstrings ofothermaterialswouldhavebeenrequired,suchasmadefromplantfibers,leather

(Lothrop1955:49),oranimalsinew.Althoughlaborioustouse,stringsawsmighthave offeredanumberofadvantagesoverhardwoodorstonesawsfortheprehispaniclapidary.

Lothrop(1955:48)notesthatstringsawswouldhavemadeitpossibletocutcurved interiorlineswithinanobject,whichwouldnothavebeenpossiblewithflatsaws.Taube

(2004)notestheprobablyuseofstringsawingonanumberofOlmecjadesinthe

DumbartonOakscollectiontodefineinteriorfeaturesonfigurines.Basedon

178 experimentalreplicationstudies,Chenault(1986:6467)usedjutetwinecoatedwithlard

andabrasivetocuta1.2cmdeep,4mmwidegrooveinapieceofAlaskannephrite,

suggestingthatsuchaprocedurewouldhaveextremelytimeconsuming.

Figure6.6JadeworkersinPekingcuttingajadeiteblockusinga woodframewiresaw.(fromWhitlockandEhrmann1949:Plate5). Becauseneitherhardwoodsawsnorstringsawswouldsurviveinthe

archaeologicalrecord,othermaterialsignaturesarenecessaryfordemonstratingthe presenceofsawingactivityatarchaeologicalsites.Onelineofevidencewouldbethe

recoveryofunfinishedartifacts,orfragmentsorpiecesofjadeshowingindicationsof

havingbeensawn.Thiswouldincludetherecoveryofartifactswithvisibleseptafrom

theremovaloffragmentsthroughsawing(Fig.6.7).Inaddition,fragmentswithflat

surfaces,terminatingin"ledges"whereapiecewasremovedwouldalsobepresent.In

myownobservationsofsawnjadeiteartifactsfromMiddleMotaguaValleysites,another

indicationofsawingisraised,parallelridgesonthecut,flatsurfaceofanobject(Fig.

6.8).

179 Figure6.7Sectiondrawingsofjadefragmentswithevidenceofsawingfrom Kaminaljuyu.Note"ledges"atbottomofcuts;dashedlinesshowhypothesized shapeofartifact.(fromKidder,JenningsandShook1946:fig.49)

Figure6.8CutfragmentofjadeitefromGuaytan4excavations.Noteseriesof linearstriationsoncutface,and"ledges"atbottomofcut.Scalein1cmunits. Itisdifficult,however,todifferentiatebetweentheuseofstring,hardwoodand stonesawsfromarchaeologicalmaterial,althoughTurner(1957:5253)arguesthat differenttypesofsawswouldleavedistinctivemarksonsawedobjects.Flatedgedstone slabsawswouldlikelyproducecutsthatarestraightalongthelengthofthetermination ofthecut,andproducearoughlyUshapedcrosssection(Chenault1986:54).Hardwood sawswithasharpenededge,ontheotherhand,wouldproducecutsthatareVshapedin crosssection,althoughChenault(1986:54)notesthatstonesawswithsharpenededges mightproducesimilarresults.StringsawswouldproducecutswithUshapedcross sections,aswellaslong,convexcutswiththe"endscutdeeperthanthemiddle,because

180 ofthebendinthestring"(Chenault1986:56).Kovacevich(2006:164)arguesthatthe presenceofstringsawanchorsfromjadeworkingcontextsatCancuensuggeststheuse

ofstringsawsatthesitetocutjade(Fig.6.9).

Figure6.9Proposedstringsawanchor recoveredatCancuen(fromKovacevich 2006:fig.5.15)

Anotherdifficultyregardingsawingofjadeiteartifactsrelatestotheidentification ofthetypeofartifactthatwasbeingproduced.Sawingmayhavebeeninitiatedinorder toproduceablankthatwasintendedtobeworkedintoafinishedobject,suchasaplaque ormosaicinlay.Ontheotherhand,sawingmayhavebeendonetoremoveaportionof anobjectduringtheproductionofanartifactformfromaninitialcoreofmaterial.Inthis case,sawingcouldhavebeenusedtoremovematerialfortheproductionofearflares, tubularbeadsorotherobjectswithgenerallylong,flatsurfaces.Inthesecases,itmaybe difficulttodiscernwhetherarchaeologicallyrecoveredmaterialwithevidenceofsawing werebyproductsoftheproductionofartifacts,orwhethertheyrepresentblanksintended forfurtherelaboration.

6.1.4 Drilling

Inthepassagesquotedearlier,SahagúnnotesthatAzteclapidaries“drilled[jade]; theyboredthemwithametaltubulardrill”(DibbleandAnderson1959:8081).As

181 alreadynoted,thereisscantevidenceoftheuseofmetaltoolsinprehispanictimes.

Instead,itislikelytheprehispaniclapidariesuseddrillsofstoneororganicmaterialfor

drillingjadeartifacts.Inthisdissertation,drillingreferstotheuseofatool,through

rotarymotion,toproduceaholeordepressioninabodyorartifactofjadeite.Drillingof jadeartifactswasdoneforoneoftworeasons:toproduceaholethroughwhichan artifactcouldbesuspended,ortocreateaninteriordesignonajadeartifact.Drillingwas accomplishedthoughtwoprimarymeans:theuseofasoliddrillortheuseofahollow

drill.Itshouldbenotedthatdrillingcouldtakeplaceatalmostanypointinthe productionprocessofjadeiteartifactproduction.Evidencesuggestingtheuseofbothin prehispanicMesoamericaisdescribedbelow.

Soliddrillsorbitsseemtohavebeenusedfrequentlyforjadeartifactandother lapidaryproductioninMesoamerica.Drillingwasnotdonesolelyforthepurposeof creatingsuspensionholesinjadeobjects.Inadditiontocompleteholes,soliddrillswere alsousedtoproducedesignsjadeartifacts,suchasmasksandfigurines.Taube(2004:22) notesthatanumberofOlmecjadeartifactsintheDumbartonOakscollectionsshow evidenceofdrillingusingsoliddrillswithbitsofvariouswidthsfortheplacementof featuresonfigurinessuchaseyesandotherdesignelements(Fig.6.10).From observationsofCostaRicangreenstoneartifacts,Chenault(1986:5658)notesthat drillingwasalsousedtocreateinteriordesignsonartifactsbyplacingaseriesofholesin anartifactwithoverlappingorcloselyspacedtooneanother.Similaruseofoverlapping drillholescanbeseenonajadeheaddressornamentrecoveredatCancuen(Fig.6.11).

182 Figure6.10Olmecjademask.Note useofdrillingtoformnostrilsandeyes ofmask.(fromTaube2004:plate30).

Figure6.11Headdressornament recoveredfrom Cancuen.Noteoverlappingdrillholesatcenterand leftofartifact.(fromKovacevich2006:Fig.5.22)

Soliddrillscouldhavebeenmadeofanumberofmaterials.Asnotedearlier,

Clark(2006)producedasmall,shallowdepressioninajadeitefragmentusingatapered hardwooddowelandabrasives;thewooddrillwasturnedbyhandbetweenthepalms.In hisreplicationexperiments,Chenault(1986:7273)usedawoodeddowelrodofash,

8mmindiameter,withasharpenedend,todrillAlaskannephrite.Drillingfortwohours produceda1mmdeep,8mmdiameter,conicalhole,slightlyroundedatthebottom.

Chenault(1986:73)alsousedarodofsolidbambootodrillthenephrite,withsimilar

183 results.Becausesoliddrillsofwoodorbamboowouldnottypicallybepreserved,they areunlikelytoberecoveredarchaeologically.

Nevertheless,evidenceoftheuseofsoliddrillscanbegleanedfromobservations ofthedrillholesordepressionsondrilledartifacts.Asnotedabove,soliddrillsofwood orbamboowouldlikelyproducedepressionsorholesthathaverounded,Ushapedcross sections,asthedrillbitwouldbecomebluntduringtheprocessofdrilling.Ifdrillingofa holewasdonebiconically(i.e.frombothsidesofanobject),thepointinthecenterofthe object,atwhichtheholewascompleted,wouldcontainridgesthatshowasimilar roundedcrosssection,unlessdrillingcontinuedallthewaythroughtoproduceahole withstraightinteriorwalls.

Soliddrillbitsofcherthavebeenrecoveredfromanumberofsitesin

Mesoamericaandwouldhaveservedwellfordrillingjadeite,becausecherthasaMohs

hardnessof7.0,comparedtoaMohshardnessof6.57forjadeite(Fig.6.12).Atthesite

ofNativitasinPuebla,Mexico,chertmicrodrillswererecoveredinassociationwith

evidenceofjadeartifactproduction(Hirthetal2009).Similarchertmicrodrillshave

alsobeenrecoveredinthejadeworkshopatCancuen(Kovacevich2006,2007)andfrom

thePetenLakesregionwheretheyshowmicrowearevidenceofhavingbeenusedtodrill

afinegrainedstone,suchasjadeite(Aldenderferetal.1989;Aldenderfer1991).

Evidencefortheuseofchertdrillsindrillingjadeitecouldbegleanedfromtwoprimary

linesofevidence.First,therecoveryofexpendedchertdrillsinassociationwithjadeite productionevidencewouldsuggesttheirusefordrillingjadeite.Second,drilledjadeite artifactswithVshapedholesordepressionsmightindicatetheuseofsolidchertdrills

(Fig.6.13).

184 Figure6.12Chertdrills recoveredfromNativitas,Puebla, Mexico(fromHirth2005:fig.13). Rulerforscaleis5cmlong.

Figure6.13Jadebeadbroken during uniconicaldrilling.NoteVshapeddr illhole, likelyfromuseofchertdrillbits,likethose showninFigure6.12.Scalein1cmunits. Becauseofthehardnessofchert,itwouldlikelyholdapointforalongerperiod

ofdrillingthanwouldsoliddrillsmadefromsoftermaterialssuchaswood.This

suppositionissupportedbyexperimentalreplicationbyChenault(1986:7374)usinga

chertdrillbitthatdidnoterodeasrapidlyatthepointasdidthehardwooddrillbit.It

shouldbenotedhowever,thatchertdrillswouldlikelynothavebeeneffectivefor

drillingverydeep,narrowholes,asthewidthofdrillsatthepointofhaftingwouldmake

itdifficulttofitwithinthehole.

Inadditiontosoliddrills,hollowtubulardrillscouldbeusedfordrillingjadeite.

Althoughahollowdrillmadefromjadeitewouldlikelyhaveservedwellfordrilling jadeite,nosuchdrillshavebeenrecoveredinMesoamerica.Otherpossibilitiesinclude

185 hollowdrillsofboneorofreedsorbamboo,alongwithabrasives.Ahollowbonedrill wasfoundintheboreholeofanalabasterplaque(Fig.6.14)atIxtapaluco,nearChalco,

Mexico(Holmes1919:351352).Tomyknowledge,nootherbonedrillshavebeen identifiedinMesoamerica,althoughitispossiblethatsomemayhavebeenrecovered, butnotidentifiedastools.Tubulardrillsofbambooorreedareunlikelytosurvive archaeologically.

Fig.6.14(Left)AlabastertabletfromIxtapaluco.(a)Crosssection,showing locationofbonedrill.(b)Drillfoundintablet.(FromHolmes1919:fig.213) Therefore,thebestevidenceoftheuseofhollowdrillsisthepresenceofthesolid coresthatareproducedasbyproductsinthehollowportionofthedrill(Fig.6.15a).

SuchcoresofjadeitehavebeenrecoveredatGuaytan(Walters1982)andKaminaljuyu

(Kidder,JenningsandShook1946:120).Thesecoresshowevidenceofbothuniconical andbiconicaldrilling(Fig.6.15b).Typically,theendsofthecoresclosesttotheexterior ofsurfacewheredrillingterminatedarewiderindiameterthanaretheendsatthefresh break,owingtheslight“wobble”duringtherotarymotionthatwouldcontinuetowear awaymaterialwheretheholestarted.

186 a. b. Figure6.15Jadeitecoresproducedbyuseofahollowdrill,recoveredinGuaytan4 excavations.(a)Uniconicalcoresfromdrillingfromonedirection.(b)Biconical corefromdrillingfromtwodirections.Notethatdiameterofcoreincreasestoward medialportion,andthatdrillholesdidnotmeetprecisely.(Scalesin1cm increments) Someofthecoresproducedbyhollowdrillsmayhavebeenreusedfortubularbeads,

therebyremovingsomeevidenceofhollowdrillingfromthearchaeologicalrecord.At

Kaminaljuyu,sometubularbeadsshowsometaperingattheirends,whichKidder,

JenningsandShook(1946:120,fig.151)arguetobeevidencethattheywereproduced

fromcoresleftoverfromdrillingotherobjects.Hollowtubulardrillswerealsousedto producedesignsonartifacts.Thistechniquecanbeseenmostreadilyincirculardesign

elementswithcentralcolumnsremainingontheartifact(Fig6.16).

Drillinginvolvesarotarymotionwithaconsiderableamountofpressureand

speedtoproduceadepressionorhole.Therotarymotioncouldhavebeenachieved

Figure6.16–CarvedbeadsfromKaminaljuyu.Notecircularelementsproducedby usingatubularhollowdrill(Kidder,JenningsandShook1946fig.148)

187 thoughtwoprimarymeans,handrollingorthroughtheuseofapumpdrillofsomesort.

EthnographicdescriptionsofMaorilapidarytechniquesshowsthattheyusedchertdrill bitshaftedontoawoodenrodbyrollingthedrillbackandforthbetweenthepalmsand byturningitwithacord(Wills1964).Digby(1964:16)arguestheprehispanic

lapidarieswouldhaveusedpumpdrillswithflyweightsforaddedpressure,ashand

rollingofdrillswouldnothaveproducedsufficientpressureorspeed(Fig.6.17).Todate,

noclearlyidentifiedflyweightshavebeenrecoveredinassociationwithevidenceofjade

artifactproduction.

Figure6.17Depictionofapumpdrillshowingflywheel andhafteddrillingelement(fromDigby1964:16).

6.1.5 Incising

Inthepassagesquoteearlier,SahagúnnotesthatAzteclapidaries"scraped[jade]

withaworkedflinttool,"whichLothrop(1955:48)suggestsisareferencetothelapidary

techniqueofincising.Inthisdissertation,incisingreferstomakingmarksorlinesona

surfacethroughtheuseofasharp,pointedtool,forthepurposeofmakingorotherwise

definingdesignelements.Includedinthiscategoryistheprocessthatothers(e.gRands

1965:574)havecalledgravingorgrooving,whichwasthemeansbywhichmanybas

188 reliefartifactswereproduced.Incisingofjadeitecouldbeaccomplishedbytheuseof pointedstonetoolswithaMohshardnessequalto,orharderthanjadeite(suchaschert, quartzorjadeiteitself).Kovacevich(2006:166)suggeststhatcherttoolswouldhave beenpreferredastheycouldbemoreeasilyshapedattheirpointbypressureflakingto

createpointsofthedesiredthickness.

Incisingcanbeperformedafterinitialgrindinghadcreatedanadequatelysmooth

surfaceonwhichtomakeincisedlines.Alternatively,incisingcouldhavebeendone

afterfinepolishingofanobject.However,basedonreplicationexperimentsusinga

quartzcrystal,Taube(2004:24)arguesthatincisingjadeiteismoreeasilydonebefore

finalpolishing,astheslightlyroughersurfaceallowsmoredirectcontactbetweenthe jadeiteandquartztip.Thompson(1975:106)arguesthatmanyinciseddesignsonOlmec

artifactsweremadebytheirownerswellaftertheobjectswerefinished.

Evidenceofincisingisdifficulttodetectarchaeologicallybecausethetechnique

doesnotproducereadilyobservablebyproducts.Furthercomplicatingtheidentification

ofproductionofincisedartifactsisthefactthatthetoolsusedforincisinglineswere probablyinthesameformsasthechertdrillsdescribedearlier.Foshag(1957:57)argues

that"sharpbittedceltsofjadeiteorchloromelanite"wouldhavebeenusedforsomeform

ofincising.Again,aproblemliesindistinguishingceltsusedforjadeiteartifact productionfromthoseusedforothertasks,suchasfellingtrees,woodworkingor agriculturalwork,whichcanonlybedonethroughexaminationofmicrowearpatternson thetoolsthemselves.Inthisregard,Aldenderferandcolleagues(1989;Alderderfer1991) havenotedthatsomefinechertbifacesfromthePetenLakesregionexhibitmicrowear polishsimilartothatproducedinexperimentsfromworkingfinegrainedstones.

189 Althoughitisnotpossibletodetermineifthispolishwasproducedbyworkingofjadeite

orsomeotherfinegrainedstone,itdoessuggestthepossibilitythatchertbifaceswere

usedbyClassicMayalapidariesforincising.Afurthercomplicationwithidentifying

incisingtoolsisthefactthatjadeceltsmayhavebeenrecycledintootherartifacts.

Giventheseproblemsoftoolidentification,theonlyclearevidenceofthe presenceofincisingasaproductiontechniqueundertakenatalocationistherecoveryof

unfinishedartifactswithpatternedincising.Walters(1982)reportsfindingevidenceof incisingatGuaytan,MadgalenaIIandElTerron,butdoesnotprovideillustrationsof

thesematerials.Nosimilarunfinishedjadeiteartifactsshowingsignsofincisinghave beenreportedinassociationwithevidenceofjadeiteartifactproductionfromelsewhere

inMesoamerica.

6.1.6 Polishing

ThepassagesfromSahagúnquotedearliermakefrequentmentionofAztec

lapidariesmakingjadeartifact"shine"or"gleam,"referringtothepolishingofjadeite artifactstogivethemaglossysheen.Polishingwaslikelythefinalstepintheprocessof creatingjadeartifacts.Sahagúndescribedtheuseofwood,cane,andfineabrasivesfor thisproductionstep.Finecaneorbamboowouldhavelikelyservedasgoodpolishing implements,asthesilicathattheycontainwouldhaveactedasagoodpolishingagent

(Widmer1991:136).

Basedonmicroscopicexaminationofpolishedsurfaceofjadeiteartifacts,Foshag

(1957:5556)arguesthatahardpolisherwithafineabrasivewasprobablyfavoredfor polishingbyprehispanicMesoamericanlapidaries.Hisconclusionisbasedonthe

190 observationthathighspotsarepolished,butthatlower,"intergrain"areasonjadeite

objectsarenotpolished,suggestingthatanobjectwithahard,flatsurfacewaslikely

usedtopolishtheobjects.Basedontheseobservationsaswellaslimitedreplication

experiments,Foshag(1957:56)proposedthatthebroadsurfaceofjadeiteceltswould

haveservedwellforpolishing.Asnotedearlierforincisingtoolshowever,itisdifficult

inpracticetodetermineifapolishedsurfaceonajadeiteceltindicatesitsuseasa polishingtoolorifthepolishedsurfaceonajadeiteceltwaspartoftheproduction processoftheceltitself.Polishingmayhavebeenaccomplishedbyrubbingajadeite

artifactagainstahardsurfacealongwiththeaidoffineabrasives.AtCancuen,aslabof

slatewithacentraldepression(Fig.6.18a)hasbeeninterpretedbyKovacevich(2006:

170)asapolisherforjadeitebeads,similartotheslateslabsmentionedaboveinJapanby

West(1963).AlsoatCancuen,alimestoneblockwithdepressionsthatfitexamplesof

earflaresofallsizesprobablyservedasajadeiteearflarepolisheraswell(Fig.6.18b,

6.19).

Intheabsenceofsuchtoolshowever,identificationofpolishingofjadeiteis

difficulttoidentify.Asisthecasewithincisingthen,theonlyotherpossiblelineof

evidencesuggestingthepresenceofjadeitepolishingactivitywouldberecoveryof jadeiteartifactsbrokenintheprocessofproductionthatcontainpolishedsurfaces.

191 a. b. Figure6.18(a)Slateslabspossiblyusedforpolishingjadeitebeads,recovered fromjadeworkshop.(b)Limestoneearflarepolisherrecoveredfromfillbeneaththe floorofeliteresidentialstructure(fromKovacevich2006:fig.5.23,5.24).

Figure6.19LimestoneearflarepolisherrecoveredfromCancuen, shownwithrecoveredearflaresthatmatchdepressionsinpolisher (fromKovacevich2006:fig.5.25).

6.2 TypologyofJadeiteArtifactProductionEvidence

Akeycomponentofthisdissertationresearchwaslithicartifactanalysistoobtain

informationaboutthetechnologicalprocessofjadeiteartifactandotherlapidary productionatsitesintheMiddleMotaguaValley.Atotalof9,920jadeiteartifactsfrom

surfaceandexcavatedcontextswereanalyzedaspartofthisdissertationresearch;an

192 additional438toolsassociatedwithjadeartifactproductionwerealsoanalyzed(Table

6.1).Iexaminedalllithicartifactsfromatechnologicalperspective,examiningand measuringartifactattributesthatmightprovideinsightintothetechnologicalprocesses involvedintheirproduction.Allnonflakejadeiteartifactswereindividuallymeasured andweighed(andmanyphotographed)aspartofartifactanalysis;jadeflakeswere measuredandweighedinaggregate.

Basedonthetechnologicalprocessesdescribedinsection6.1,Icreateda typologyofjadeiteartifactsandassociatedtoolsrecoveredfromsurveyandexcavationin theMiddleMotaguaValley.Thetypologycontainstwelvecategories:jadecobbleor chunk,largejadeflake(>5cm),smalljadeflake,hammerstone,jadebeadperform, broken/unfinishedjadebead,jadehollowdrillcore,completejadebead,cutjade fragment,jadefragmentwithgroundfacet,chertbladefragments,chertdrill(Table6.1).

Descriptionsofthecriteriausedtodefineeachtypecategoryarepresentedbelow,along withdescriptionsoftheanalysesandmeasurementstaken.Incaseswhereanartifacthad characteristicsofmorethanonecategory,theartifactwasassignedtoonlyonecategory, butitscharacteristicswererecordedinnotes.Forexample,ahollowdrillcorethat showedevidenceofgrindingononeormoreendswascategorizedasahollowdrillcore andcountedinthecategory,butnotedtohaveevidenceofgrinding.

Beforecontinuing,Ishouldnotethatnosystematicdeterminationwasmade aboutthemineralogyofgreenstoneartifactscollectedaspartofthisdissertation(i.e. whethertheywerealljadeiteorsomeotherformofmineralorstone).Forthis dissertation,Iassumethatthegreatmajority,ifnotall,greenstoneartifactsrecovered

193 JadeTypologyCategory Number JadeCobbleorChunk 29 LargeJadeFlake 54 SmallJadeFlake 9,495 JadeBeadPreform 34 Broken/UnfinishedJadeBead 111 JadeHollowDrillCore 62 CompleteJadeBead 18 CutJadeFragment 20 JadeFragmentwithGroundFacet 97 Hammerstone 8 ChertBladeFragment 26 ChertDrill 401 Table6.1Listoftypologicalcategoriesforjadeiteartifactsusedinthisdissertation fromtheMiddleMotaguaValleyarejadeite.Thisisareasonableassumptionfortwo reasons.First,becausetheregionistheonlypositivelyidentifiedjadeitesourcein

Mesoamerica,itisreasonabletoassumethatmuchofthegreenstonebeingusedfor artifactproductionintheMiddleMotaguaValleywasoflocallyavailablejadeite.

Second,fewstudiesintheMayaareamakeadistinctionbetweenjadeiteandnonjadeite greenstones,becausethemajorityofgreenstoneartifactsintheMayaareawereusedina similarmanner,aswealthorstatusgoods.Therefore,makingsuchadistinctionhere wouldbeoflittleutilitybecausefewdataexistwithwhichtocomparesuchdatafromthe

MiddleMotaguaValley.

Inaddition,suchdistinctionsaredifficultwithouttheuseofspecialized equipment,becausejadeiteandmanyothergreenstoneshavesimilarmineralogical characteristics.ExaminationofsevengreenstoneartifactsfromMiddleMotagauaValley sitesbyMaryLouRidingerofJadesS.A.inAntigua,Guatemalashowedthatallsamples

194 fellwithintherangeofjadeiteforspecificgravityandhardnesstests(MaryLouRidinger

2006,personalcommunication).Nevertheless,allgreenstoneartifactsthatwere

significantlydifferentincolor,mineralpatterning,lustre,orothermineralogical

characteristicswerenotedincommentsinourartifactanalysislogs.

6.2.1 JadeCobbleorChunk

Artifactsinthiscategorywereidentifiedaspiecesofjadeitelargerthan5cm,but

thatdonotresembleflakes,eitherbecausetheywere"blockyfragments"withroughly

similarlength,widthandthicknessmeasurements,orbecausetheywereunworked

nodulesofjadeite(Fig.6.20).Themajority(n=21,72%)ofthecobblesorchunks

containedoneormoreflakescars,butwereincludedinthesamecategoryascobbles

withoutflakescarsbecauseofthedifficultyofdifferentiatingbetweenscarsproducedby

naturalfracturingversusthoseproducedbyintentionalpercussion.

Figure6.20Jadecobblecollectedfrom KM91III.Notescaronupperleft surfaceofcobble.(Scalein1cm increments)

6.2.2 LargeJadeFlakes

Jadeflakesmeasuringlongerthan5cminlengthandcontainingeitherastriking platformorventralbulbofpercussionweredefinedaslargejadeflakes(n=54)andwere

195 individuallymeasured,weighedandexamined(Fig.6.21).Inadditiontothemaximum

dimensionsandweightofeachflake,notesweremadeaboutthepresenceofcortexon

anyportionoftheflake,aswellasevidenceofwaterwornsurfacesandofthepresence

ofscarsfromthepreviousremovalofflakes.

Figure6.21LargeflakesfromVargasIV. (Scalein1cmincrements)

6.2.3 SmallJadeFlakes

Smalljadeflakesarethebyproductofdirectandundirectedpercussion

techniquesandmakeupthevastmajority(96%)ofjadeproductionevidencerecovered

aspartofthisdissertationresearch.Inthisanalysis,anyangularorirregularpieceof jadeitedebitagewascategorizedasaflakeifwaslessthan5cminlength(Fig6.22).

Becausejadeitefracturesinanirregularandlargelyunpredictablemannerowingtoit

densecrystallinestructure,analysisofindividualflakesdoesnotprovidereliable

informationaboutthereductionsequenceusedinproducingjadeiteartifacts.Therefore,

alldebitageflakeswerepassedthroughaseriesofnestedwirescreensof1/2",1/4"and

1/8"meshsize;flakesfromeachsizegradewerethencountedandweighedinaggregate.

Thiswasdonetoobtainasmuchdetailaboutdebitagevariationaspossible,andinthe

hopethatitmightprovideinformationaboutvariationinthemanufacturingsequenceof jadeiteartifacts.

196 Figure6.22–Smalljadeflakesfrom Guaytan4excavations(1A2001). Noteirregularityofflakes.(Scalein 1cmincrements)

6.2.4 JadeBeadPreform

Artifactsassignedtothiscategory(n=34)wereidentifiedashavingbeenroughly shapedbygrindingorpercussionintotheformofoneofthebeadshapesdescribedabove inSection6.2.8,butuponwhichdrillinghadnotbeenattempted(Fig.6.23).

Measurementsincludeddiameter,length,width,thickness,andweightofeachbead preform.Manybeadpreformsretainedscarsfrominitialshattering,despiteinitial grindingofsomeofthebeadpreforms.

Figure6.23Jadebeadpreforms fromVargasIIIsurfacecollections. Notefracturesonsurfaceofallthree performsfrominitialpercussion. (Scalein1cmincrements)

197 6.2.5 Broken/UnfinishedJadeBead

Artifactsinthiscategoryweredefinedasbeadseitherbrokenorabandoned

duringtheprocessofdrilling(e.g.Fig.6.13).Measurementsincludeddiameter,length, width,thickness,andweightofeachfragmentarybead.Ifthefragmentarybeadwas drilled,themaximuminteriordiameteroftheholewasmeasured;itwasalsonoted whetherthefragmentarybeadwasdrilledbiconicallyoruniconically.Inaddition,itwas notedwhetherthebeadwasroughlyormorefinelygroundintoshape,asubjective determinationthatwasmadebasedonthecomparativesmoothnessoftheexterior surfacesofthefragmentarybead.Theshapeofeachfragmentarybeadwasalsonoted usingthecategoriesdescribedaboveinSection6.2.3.Themajority(n=91,82%)ofthe brokenorunfinishedbeadswerebrokenduringtheprocessofdrilling,whileonlyasmall portion(n=11,10%)wereabandonedafteronlyasmalldepressionwasmadeinthe bead;inaddition,asmallnumberofbeads(n=9,8%)werebrokenmedially,butwithno

obviousevidenceofdrilling.

6.2.6 JadeHollowDrillCores Artifactsincludedinthiscategoryaredefinedasthebyproductoftheuseof

hollowdrillstomakeholesinjadeiteartifacts(Fig.6.24).Measurementsofallhollow

drillcoresincluded:length,weight,diameterattopofcore,diameteratbottomofcore;

thediameteratthecenterpointofthecorewastakenforbiconicaldrillcores(Table6.2).

Themajority(n=53,84%)ofhollowdrillcoresonlyshowevidenceofuniconical

drilling.Inaddition,observationsweremadeofthepresenceofabsenceofgrinding

exhibitedonbothendsofthehollowdrillcores.

198 HollowDrill Average Average #Rough #Ground #Ground TOTAL CoreType Length MaxWidth BothEnds OneEnd BothEnds Uniconical 6.09mm 4.93mm 36 17 1 54 Biconical 6.97mm 5.80mm 8 1 0 9 TOTAL 44 18 1 63 Table6.2.Measurementsofjadehollowdrillcoresrecoveredfromsurface collectionsandexcavations.

a. b. Figure6.24JadehollowdrillcoresfromGuaytan4excavations.(a)Hollowdrill coresfromuniconicaldrilling.(b)Hollowdrillcoresfrombiconicaldrilling,with visiblecentralportionwhereendsdidnotmeetprecisely.Notevariationof smoothlygroundandroughlyshapedendofbeadcores.(Scalein1cmincrements)

6.2.7 CompleteJadeBead

Artifactsassignedtothiscategoryincludedonlybeadsthatweredrilled

completely.Measurementsforeachbeadincludedmaximumdiameterandthicknessof

thebeaditself,maximuminteriordiameterofthedrilledhole,andweightofthebead.

Allbeadswereexaminedtodetermineiftheyweredrilleduniconically(n=4)or biconically(n=14).Fourtypesofbeadswereobserved:button,donut,sphericaland

tubular.Buttonbeads(n=12)arecircular,butflatandthin,(Fig6.25a).Donutbeads

(n=3)arethickerthanbuttonbeads,andnotcompletelyflatontheirends(Fig.6.25b).

Sphericalbeads(n=1)wereroughlyspherical(Fig.6.25c).Tubularbeads(n=2)are

cylindricalinshape,andgreaterthicknessthandiameter(Fig.6.25d).

199 a. b. c. d. Figure6.25Completejadebeads:(a)Button(b)Donut(c)Spherical(d)Tubular. Notethefracturescarsremainingon(a)and(c)frominitialshattering.(Scalein1 cmincrements) 6.2.8CutJadeFragment

Artifactsassignedtothiscategorycontainatleastoneflatsurface,representing thesurfacealongwhichasawwaspassedtoremoveafragmentofjadeite.Identification ofcutorsawedfragmentswasmadebasedonthepresenceofalipatoneendoftheflat

(cut)facesofanartifact,whichdistinguishtheseartifacttypesfromthosethatwere groundononesurfaceorfacet(Fig.6.26).Allcutjadefragmentsrecoveredinthis dissertationfieldresearchwerefragmentsthatwereremovedfromlargerartifactsby sawing.Measurementsweretakenforalldimensionsoftheartifactitself,aswellasfor thecutsurface(s).Observationsabouttheshape(incrosssection)atthebottomofthe cutwerealsonoted.

Figure6.26Drawingofanexampleofcutjadeitefragment,recoveredfrom 1A1005(allsurfacesotherthancutfacewerenaturallyweatheredsurfaces). DrawingbyLic.ElisaMencos.

200 6.2.9 JadeFragmentwithGroundFacet

Artifactsinthiscategoryincludealljadeartifactsthatcontainedatleastone

groundfacet,butdidnotcontainvisiblesignsofhavingbeenremovedbysawing.

Determinationofwhetherafragmenthadagroundfacetrestedonthepresenceofatleast

onesmoothedsurfacewithvisiblestriationsfromthegrindingprocess,andnotfrom

naturalsmoothing(Fig.6.27).Inmanycases,evidenceofgrindingisnotpresentonthe

entiretyofthesurfaceofajadeartifact,butrestrictedonlytoaportionofthesurface.In thesecases,themaximaldimensionsoftheground,flatsurfacewasrecorded;where multiplesurfacesshowedevidenceofgrinding,eachfacetwasmeasuredindividuallyand recorded.Somefragmentswithevidenceofgrindinglookedsimilartoartifactsassigned tothevariousbeadcategoriesdescribedabove,andmayhavebeengroundartifacts,such asplaques,thatwereintentionallysmashedinordertoproducerecycledfragmentsfor breadproduction.Nevertheless,unlessareasonablycleardeterminationcouldbemade thatthegroundfragmentwasintendedtobeabead,itwascategorizedasaJade

FragmentwithGroundFacet.

Figure6.27Examplesofartifactsclassifiedasgroundjadefragments.(Leftfrom Guaytan4excavations;RightfragmentsfromKM92IIIsurfacecollections).(Scale in1cmincrements)

201 6.2.10 Hammerstones

Hammerstones(n=8)arestonesusedaspercussorstoremoveflakesor fragmentsthroughtheuseofpercussiontechniques.Theywereidentifiedbasedontheir roughlysphericalshape(createdbypecking)andonevidenceofbatteringontheir surface(Fig.6.28).Maximumlength,widthandthicknessofeachhammerstonewas recorded,alongwiththeweight.Allhammerstonesweremadeofjadeite.

Fig.6.28Jadeitehammerstone recoveredfromGuaytan8excavations. Notethebatteringonthesurfacenear thetopoftheimage.(Scalein1cm increments) 6.2.11 ChertBladeFragments

Chertblades(n=26)weredefinedaslong,thinchertartifactswithparallellateral

edges,andflatventralsurfacesanddorsalsurfaceswithoneormoreridges.Hirthetal.

(2009)arguethatchertbladeswereworkedontheirdistalandproximalendsforuseas

drills(seeSection6.2.12).Measurementsincludedmaximumlength,width,thickness

andweightofeachblade,aswellasnoteonthenumberofridgesonthedorsalsurfaceof

thefragment.Incaseswhereonlythemedialsectionofachertartifactwasrecovered,it

wascategorizedasablade,forlackofevidenceofflakingtoproduceadrilloneitherend.

6.2.12 ChertDrills

Twoseparatecategoriesofcherttoolsweredefinedintheconstructionofthe

currenttypology:chertdrillsandchertblades.Chertdrillsweredefinedaslong,thin

202 chertartifactswithparallellateraledges,flatventralsurfaces,dorsalsurfaceswithoneor

moreridgesandwithtapereddistalorproximalendsproducedbytheremovalof

microflakes(Fig.6.29).Measurementsincludedtheweightandmaximumlengthofthe

drill,aswellasthemaximumwidthandthicknessacrossthemedialportionofthedrill.

Inaddition,width,lengthandthicknessmeasurementsofthedrillbitweretakenifthebit

waspresent.Noteswerealsotakenregardingthesubjectivedegreeofwearexhibitedon

thedistalportionofthedrill(e.g.blunt,sharp,semisharp),aswellasthenumberof

ridgesonthedorsalsurfaceofthedrill.

Figure6.29Chertdrillsrecoveredfrom VargasIII.Drillbitsaremissingfromall threeexamplespictured.(Scalein1cm increments)

6.2.13 OtherLithicandShellArtifactAnalyses

Inadditiontojadeiteartifactsandassociatedproductiontools,over3,316other stoneandshellartifactswereanalyzedaspartofthisdissertationresearch(Table6.3).

Theseincludedobsidianartifacts(blades,bladecores,flakesandtwodrilledobsidian ornamentfragments),variousnongreenstoneartifacts(includingbeadsandapartial earflare),shellartifacts(beadsandapartialearflare),greenstoneadzes,andfragmentsof possiblestonetoolsforlapidaryartifactproduction(describedbelow).Allobsidianblade andbladefragmentsweremeasuredandweighedindividually.Standarddimensions

203 (maximumandminimumlength,width,andthickness)wererecordedalongwithother physicalcharacteristics.

Artifacttype Quantity(n) Obsidianbladefragment 1,936 Obsidianprismaticcore 251 Obsidianflake 1,044 Obsidian,ground 2 Shellfragment,worked 20 Shellbead,complete 19 Stonebead,complete 15 Stonebead,broken 7 Adzefragment 8 Misc.workedstones 6 Misc.groundstonetools 6 Table6.3Otherlithicandshellartifactsrecovered fromexcavationsandsurfacecollections.

6.3 ChaîneOpératoireofJadeiteBeadProductionintheMiddleMotaguaValley

Oneoftheprimarygoalsofthisdissertationresearchistoreconstructthe

organizationofjadeiteartifactproduction.Basedontheresultsoftheartifactanalyses,a

numberofinsightsandobservationscanbemadeaboutthetechnologicalprocessand

organizationofjadeiteartifactproductionintheMiddleMotaguaValleyduringtheLate

Classicperiod.IfocusontheLateClassicperiodfortworeasons.First,allexcavated

contextscontainedLateClassicceramics,makingtheassociatedjadeproduction

evidenceareflectionofthattimeperiod.Second,theLateClassicperiodistheonly

temporalperiodrepresentedinthesurfaceceramicsatallsitesexaminedinthis

204 dissertationresearch.Therefore,themostparsimoniousassumptionisthatthemajority oftheevidencereflectsthestructureofjadeproductionduringtheLateClassicperiod.

Jadeitebeadswerethemostcommonformofjadeiteartifactproducedinthe

region;evidencerelatedtobeadproductionwasfoundateverysiteinthesurveyarea.

Thereislessdirectevidenceoftheproductionofotherformsofjadeiteartifacts,suchas plaquesandearflares.Forthisreason,Ifirstmakesomeobservationsaboutthe

organizationjadeitebeadproductionintheMiddleMotaguaValleyandthendiscussthe

evidenceofproductionofotherformsofjadeiteartifacts.

Alljadeiteusedforproductionmustfirstbeobtainedfromavailablenatural

sources.AlthoughjadeitewasquarriedfromlocaloutcropsintheMiddleMotagua

ValleylikethoseatManzanal(Walters1982),cobbleswerealsocollectedfromlocal

rivers,aswellasfromthesurroundinglandscape.Ninelargecobblesrecoveredfrom

MMVsiteshadvisiblecortexonatleastonesurface,suggestingthattheywerecollected

fromsurfacejadeitedeposits.Today,localjadeprospectorscollectloosejadeitethathas

erodedfromoutcropsthroughoutthehillsides(KarlTaube2004,personal

communication;Fig6.30a).Inaddition,eightjadeitecobblesandlargeflakeshad

smoothexteriorsurfacesconsistentwithhavingbeenwaterrolledcobbles(Fig.6.30b).

Althoughthemajorityoflargejadeiteflakesandcobbles(n=64)hadnoclearly

identifiablecortex,thedatasuggestthatMMVartisansproducedartifactsfromavariety

ofabundantlyavailableandeasilyprocuredsourcesofjadeite.

EthnohistoriccomparisonsfromChinaindicatethatriverinematerialmighthave beenpreferredbecauseoftheeasewithwhichitcouldbeobtained,andbecauseriver

rolledcobblescouldhavebeenmorepracticalforartifactproduction.Theconstant

205 a. b. Figure6.30(a)WeatherwornjadeiteboulderdiscoverednearRioHondoby CarlosGonzalez.Noteroughexteriorcortex.(Boulderisapproximately100cm wide,flakescarismodern).(b)LowerRioLaPalmilla.Manyofthebouldersareof jadeite.(Source:Taubeetal.2005). tumblingofjadebouldersandcobbleswouldhavehelpedtoremovethesofter, unconsolidated(i.e.undesirable)material,leavingthehardestandpurestmaterial.In16 th

centuryChina,lapidariespreferredriverinebouldersofnephritefromKhotanover

quarriedmaterial,whichoftenhadfracturesasaresultoftheextractionprocessthat

madeworkingthematerialmoredifficult(Hansford1968:41).Additionally,quarriedor

surfacecollectedmaterialmaterialswouldhavelikelybeenlessdesirablebecausethey

oftencontainathick,orangish"rind"or"skin"ofcortexthatwouldneedtoberemoved

(Gump1962:37).

Thegreatmajority(96%)ofjadeiteartifactsweresmallpercussionflakes

measuringlessthan5cminmaximumlength(Table6.4).Thefactthatthesearethemost

abundanttypeofartifactfoundatMMVsitessuggeststhatpercussionreductionof

cobblesandlargerfragmentswastheprimarymeansbywhichcraftproducersobtained

smallfragmentssuitablefortheproductionofbeads.Thisissupportedbythefactthat

many(n=15,40%)beadpreformsretainedsomeoftheroughangularityofthesesmall

206 percussionfragments(Fig.6.31).Atotalofeightjadeitehammerstoneswererecovered frombothexcavationsandsurfacecollections,almostallofwhichareheavilypitted, likelyfrombeingusedtobreakapartjadeitecobblesbydirectandindirectpercussion methods.

x>1/2” 1/2”>x>1/4” 1/4”>x>1/8” TOTAL Excavations 235 1835 3515 5585 SurfaceCollections 1068 2102 740 3910 TOTAL 1303 3937 4255 9495 Table6.4–Sizegradesofsmalljadeflakesfromsurveyandexcavations.

Fig.6.31JadebeadpreformfromGuaytan4 excavations.Notetheroughangularitythe preformretainsfrominitialshatteringandthe lackoffinegrindingorpolishing.(Blackboxfrom scalebelowpreformin1cmwide). Shatteringofjadeitecobbleswaslikelythemostefficientwaytoproduceblanks

fromwhichtomakebeadsforanumberofreasons.First,sawingorcuttingofjadeite

withouttheuseofmetaltoolsanddiamondtippedsawsisalaboriousandtimeintensive process.Ifthegoalwastheproductionofbeads,itwouldbemoreefficienttoquickly producesmallerfragmentsbydirectpercussionflakingorindirectshatteringoflarger

fragmentstoproducemoremanageablepieceswithwhichtowork.Second,asInotedin

Chapter3,becausejadeiterocksarechemicallyandphysicallyheterogeneous,theyoften

containagreatdealofinternalcolorvariationandphysicalimperfections(e.g.micaand

quartzinclusions).Thiswouldhaveprovidedafurtherincentivetoefficientlyevaluate

thequalityofjadeitecobblesforproducingbeads.Shatteringjadeitecobbleswouldhave

207 allowedartisanstoquicklyidentifyinternalveinsofdesiredcolors,aswellasportionsof

largerstoneswithoutimperfectionswhichmightbemoreeasilyworked.

Afterselectingfragmentssuitableforbeadsbasedonthequalityandcolorof

material,MMVartisansmadejadebeadpreformsbygrindingfragmentsintorough

spherical,donut,buttonortubularshapes,dependingonthedesiredstyleofbead.Itis

afterthisstepthatthereappearstohavebeensomevariationintheproductionprocess.

Examinationofhollowdrillscores,completebeadsandbrokenbeadsshowsthatsome beadswere(a)entirelysmoothedandpolishedbeforedrilling,(b)somewereonly groundsmoothononeend,while(c)themajoritywerenotgroundatallpriortodrilling

(Table6.5).Itisunclearwhatinfluencedartisanstodrillholesinsomebeadspriorto finegrindingorpolishing,butnotinotherbeads.Itispossiblethatsomebeadswere drilledfirstbecausedrillingappearstohaveoftenresultedinbeadbreakage.Infact,91 jadebeadswerediscardedbecausetheybrokeduringbiconicaloruniconicaldrilling.In othercases,beadsmayhavebeensmoothedorpolishedfirsttoensurethatfinalproduct wouldbeofacolorandappearancethattheartisandesired.

HollowDrill Brokenor Complete TOTAL Cores UnfinishedBeads Beads RoughOneEnd 18 10 0 28 RoughBothEnds 43 76 12 131 GroundBothEnds 1 17 5 23 TOTAL 62 103 17 182 Table6.5–Hollowdrillcores,broken/unfinishedbeads,andcompletebeads showingevidenceofgrindingononeormoresurfacespriortodrilling. Drillingofjadeitebeadswasaccomplishedbybothsolidandhollowdrills, possiblydonesequentially,orasindependentsteps.Asnotedearlier,26chertprismatic bladesand401chertdrillswererecoveredfromMMVsites(Fig.6.32a).Insomecases

chertdrillsmayhavebeenusedonlyfortheinitialstagesofdrillingahole,possiblyto

208 formasmalldivotorindentforplacingahollowdrill.Visualexaminationofsome jadeitebeadsbrokenduringdrillingsuggeststheuseofchertdrillsexclusively(Fig.

6.32b).Twoadditionallinesofevidencesuggesttheuseofchertdrillsfordrillingjadeite beads.First,chertdrillsarehardenoughtoabradeanddrilljadeite.Similarchertdrills havebeenfoundinassociationwithjadeiteproductiondebitageatCancuen(Kovacevich

2006,2007)andNativitas,,Mexico(Hirthetal.2009).Second,chertdrilltips, whentheywereintactenoughtobemeasured,overlapwiththesizeofholesinbroken andcompletejadeitebeads(Table6.6).

a. b. Fig.6.32(a)ChertdrillsfromexcavationsatGuaytan4.(b)Jadeitebeadfrom Guaytan4excavations,brokenmediallyduringdrilling.Notethecrosssectionof thedrillholeisvshapedandnarrowstowardthebottom,suggestingthatitwas drilledwithapointedbit,likethosefoundonthechertdrillsontheleft. Standard N Average Deviation Range DiameterofDrillHole 91 1.85mm .90mm .575.8mm ChertDrillTipThickness 14 3.2mm .80mm 2.24.9mm Table6.6Comparisonofdiameterofjadebeaddrillholeswiththicknessofchert drilltips.Tipsofmanydrillsweretooworntoobtainaccuratemeasurements. ChertdrillswerenottheonlytoolusedtodrilljadeitebyMMVlapidaries;atotal

of62hollowdrillcoreswererecoveredfrombothsurfacecollectionsandexcavations.

Thesecoreswereproducedbytheuseofhollowtubulardrillswiththeaidofanabrasive

agent,althoughnohollowdrillswererecoveredinthisdissertationresearch.Analysisof

209 thehollowdrillcoresindicatesthatMMVlapidariesdrilledholesintwodifferent techniques.Themajorityofbeadcoresareuniconical(n=53,85%),suggestingthat drillingofmostbeadswasdonefromonlyonedirection.Incontrast,afewbeadcores showevidenceofdrillingfromtwodifferentdirections(n=9,15%).Thesebeadcores haveabiconicalshapewithaseptuminthecenterwheredrillingwascompleted;often theseptumisnotsymmetricallyaligned.Itisunclearwhysomebeadsweredrilled uniconically,whileothersweredrilledbiconically,butthispatterncontrastswiththat suggestedfortheMayaareabyKidder,JenningsandShook(1946:120),whoobserved samplesinwhichbiconicaldrillingwasthemorefrequentlyusedtechnique.

Afterdrilling,beadsweregroundtoeliminatesurfaceirregularitiesandtosmooth theentiresurface,andthentheywerepolishedtoamediumtohighluster.Among modernagatebeadmakersinKhambhat,India,thesequenceofdrillingandpolishing(i.e. whichisdonefirst)variesdependingontheseasonalavailabilityofbeaddrilling specialistswhodonotengageinbeaddrillingduringthefarmingseason(Kenoyeretal.

1991:53).Althoughthereisnoevidencetosuggestthateachstepinthetechnological processofjadebeadproductionintheMMVwasperformedbydifferentindividuals, timingofdifferentstepswiththefarmingseasonsmayalsohaveoccurred.Forexample, grindingabeadintoshapeislikelytobemorecompatiblewithdiscontinuousor intermittentactivity,suchthatbeadscouldbegroundwhenevertimewasavailable.In contrast,drillingwouldlikelyhavebeenmoretimeconsuming,especiallyifchertdrills neededtobereplacedorsharpenedduringtheprocess.InKhambhat,drillingwasthe mosttimeconsumingpartofagatebeadproduction,andcouldtakeanywherebetween2 and10hourstopenetrate1cm(Kenoyeretal.1991:54).Therefore,drillingwas

210 possiblyanactivityreserveduntiltheagriculturalseasonwasfinishedsomoretimecould bedevotedtoit.Finalpolishingwaslikelydonewithreeds,whichcontainsilicathat providesasurfacesheen.Theentireprocessofjadeitebeadproductionisrepresentedin thediagrambelow(Fig.6.33).

QuarryJadeitefrom CollectJadeiteCobbles Outcrop fromSurface

PercussiontoProduceSmallJadeFlakes

SelectionofFlakesSuitableforBeads

RoughGrindingtoMake BeadPreform

FinelyGrindEntireBead, FinelyGrindPortionof ShapingCompleted Bead

DrillBeadUsingTubular DrillBeadUsingHollow and/orChertDrill and/orChertDrill

FinishFineShaping RemainingRoughPortion ofBead

PolishBead

CompletedBead Figure6.33Flowchartdepictingoperationalsequenceofjadeitebeadproduction intheMiddleMotaguaValley.

211 6.4 NonBeadJadeiteArtifactProductionintheMiddleMotaguaValley

WhilethefocusofmostofthelapidaryworkintheMMVwastheproductionof jadeitebeads,artisansproducedotherformsofjadeiteartifacts,possiblyincluding plaques.Whiletheevidenceofnonbeadjadeartifactproductionistoolimitedtoallow foranevaluationofthecompleteprocessoftheirproductionprocess,somepreliminary

observationscanbemadehere.

Largejadeflakes(>5cminlength,n=54),mayhavebeenintendedasblanksfor

theproductionofplaques.Moredirectevidenceforthepossibleproductionofplaques includes20piecesofjadeiterecoveredfromsurfacecollectionsandexcavatedcontexts thatshowsignsofhavingbeencutwithasawofsomeunknownmaterial.These fragmentscontainone(n=12)ormore(n=8)cutfaces,fromwhichpieceswere removed.Themajorityofthesesawnpiecesappeartobebyproductsfromthe productionofsmall,thinplaques,althoughnofinishedorincompleteplaqueswere recovered(Fig.6.34).Thisisnotsurprisingbecauselargerjadeiteplaqueswouldhave beenunlikelytobreakduringproduction,andthereforeunlikelytobediscarded.Itis alsopossiblethatsomeofthedrillcoresfromhollowtubulardrillswerefromdrilling plaquesforsuspension,butthisisdifficulttodeterminebasedonthecurrentevidence; thispossibilityisdiscussedfurtherinChapter7.

212 Fig.6.34Jadeiteartifactsshowingevidenceofhavingbeencut.(Left)Artifact appearstobeafragmentremovedfromthelateralportionofapartiallyfinished jadeiteplaque.(Right)Artifactcontainscortexonallsurfacesotherthanthecut surface,andisafragmentofacorefromwhichapiecewasremovedfor manufactureofajadeiteartifact. 6.5 OtherProductionEvidenceintheMiddleMotaguaValley

Inadditiontojadeiteartifacts,limitedevidenceoflapidaryproductionofstone andshellartifactswererecoveredatanumberofMiddleMotaguaValleysites.Atotalof sevennonjadeitestonebeadsthatwerebrokenduringdrillingwererecoveredfrom excavationsatGuaytan4andMagdalenaI,aswellasfromlootersbackdirtatVargasIIA.

Inaddition,excavationsatGuaytan4yieldedevidenceofshellartifactproduction, includingasmall"button"ofshell,shellfragmentsthathadbeenbrokenduringdrilling andanearspool(?)brokenduringproduction(Fig.6.35). Theproductionofshell ornamentsandstonebeadsinvolvedthesametechnologyasthatofjadeiteartifacts,and thuswerecraftactivitiesthatthelapidaryartisansofthesesitescouldeasilyperform whenrawmaterialswereavailable,orwhenshellornamentsorstonebeadswereneeded.

Thus,itappearsthatsomeartisanstookadvantageoftheirlapidaryskillsandtoolsto engageinmultipletypesofcraftproductionwhennecessaryorwhenopportunities presentedthemselves.

213 Fig.6.35Fragmentsofworkedshellandstone:brokenshellearspool,Guaytan4 (left),fragmentofworkedshell,Guaytan4(center)andbrokenstonebead(right). Finally,excavationsatGuaytan4yielded920obsidianbladesorbladefragments,

231flakesand249obsidianbladecores.Obsidianbladeproductionissuggestedby

recoveryofbothbladecoresanddebitage,althoughitisuncleariftherepresenceisthe

resultofproductionofobsidianbladesforcuttingshellorforproducingtoolsneededfor

theproductionofcraftgoods.Thesuppositionthatobsidianbladeproductiontookplace

atGuaytan4isstrengthenedbythefactthatWalters(1989:255)recoveredanadditional

5,199obsidianbladecoresinaportionofthepatiogroupthathassincebeendestroyed bytheconstructionofalocalschool.Takentogether,theevidencesuggeststhatobsidian bladeproductionwasforbothinternal and externalconsumption,asthenumberofblades

thatcouldhavebeenproducedwouldhavelikelyfarexceededinternalneeds.

6.6 Discussion

Basedontheevidencepresentedabove,jadeitebeadsappeartohavebeenthe

focusoflapidaryproductionintheMiddleMotaguaValleyduringtheLateClassic period.Evidenceoftheproductionofotherstylesofjadeiteartifactsusingother productiontechniques,suchassawing,wererecoveredatafewsites,andindicatethat

214 artisansatsomesiteswerealsoinvolvedintheproductionofobjectsotherthanbeads.

Nevertheless,surveyandexcavationdidnotrecoverevidenceoftheproductionof

elaboratelycarvedandincisedartifactsatanysitesinthevalley,thoughWalters(1982)

reportedfindingartifactswithsimpleincisedlinesatGuaytan.Thepresenceofmultiple

craftindustriesatsomeMiddleMotaguaValleysitesisanexampleofwhatHirth(2005,

2009a)andShimada(2007)havecalled multicrafting usingoverlappingtechnologies, wheretechnicalknowledgeforthesuccessfulexecutionofonecraftcanbeextendedfor useinthepracticeofdifferent,butrelatedcrafts.

Inthenextchapter(Chapter7),IdiscussMiddleMotaguaValleycraftproduction

activitiesintheirsociopoliticalcontexts.Theevidencepresentedthusfardemonstrate thatduringtheLateClassicPeriodintheMiddleMotaguaValley,jadeitewealthgoods

werebeingproducedbyhouseholdsandpersonswho,accordingtostandardmodelsof

craftproductioningeneralandofancientMayacraftproductioninparticular,shouldnot havebeenproducingjadeiteartifacts.

215 CHAPTER7 ORGANIZATIONOFJADEARTIFACTPRODUCTIONIN THEMIDDLEMOTAGUAVALLEY AsInotedinChapter1,acentraldebateamonghasbeenaboutthe

natureofClassicMayapoliticalorganizationandhowitarticulatedwitheconomic

systemswithinandbetweenpolities.Althoughscholarshaveproposedavarietyof

modelsofClassicMayapoliticalandeconomicorganization,theyhaveconsistently

arguedthatelitescontrolledtheproductionanddistributionofwealthgoodsandusedthis

controltoenhanceorotherwisevalidatetheirpositionwithinsociety(Foias2002,2007;

Rice1987;butseeGraham2002forproblemswithpositing"control").Inparticular,

scholarsnotethatbecauseoftheirhighvalueandtheirsymboliccontent,controllingthe productionanddistributionofwealthgoodswouldhavebeenessentialforthe

maintenanceofpowerbyClassicMayaelites(Aoyama1995;Demarest2004;Emeryand

Aoyama2007:164;Foias2002,2007;Inomata2001,2007;Joyce2000).Basedonthis

lineofreasoning,theysuggestthattheproductionofsuchgoodswouldhavetakenplace

inorneartheresidencesofelites,andmayhavebeenundertakenbyelitesthemselves

(Inomata2001,2007;EmeryandAoyama2007;Widmer2009).

Archaeologicaldatafromthisdissertationfieldresearchandfromotherrecent

studies(Kovacevich2006,2007)suggestthatthiswasnotalwaysthecaseandrequiresa

reassessmentofcurrentmodelsofprehispanicMayawealthgoodsproduction.Inthis

chapter,IcomparecurrentmodelsofClassicMayawealthgoodsproductiontothe

evidencepresentedinChapters46todemonstratethatjadeitewealthgoodswerebeing producedwithinhouseholdsandlikelybypersonswho,accordingtothesemodels,

shouldnothavebeenproducingjadeiteartifacts.Inparticular,Iarguethatourabilityto

216 understandthissystemofjadeiteartifactproductionishinderedifweview all jadeite

artifactsaswealthgoodsthatwereusedinthesamemanner,orhadthesame"value"(see

discussioninChapter3).

Ibeginbysummarizingtheevidencethatisoftenusedtocharacterizewealth

goodsproductionintheMayaarea,includingartifactsofjadeite,pyrite,shell,and paintedpolychromepottery.Ithenevaluatethedatafromthisdissertationfieldresearch

inlightofthesemodels,particularlywithreferencetopossibledifferencesinthe organizationofproductionofdifferentwealthgoods.Iarguethatresearchershavepaid insufficientattentiontovariationinboththeformandcontentofmanywealthgoods, whichhasobscuredourabilitytounderstandClassicMayapoliticalandeconomic organization.Finally,Ipresenttwoalternativepossibilitiestoexplainobserved organizationofjadeiteartifactproductionintheLateClassicMiddleMotaguaValley:

onebasedonadomesticeconomyandonebasedonapoliticaleconomymodel.

7.1 AncientMayaWealthGoodsProduction

Thatavarietyofitemsofpersonaladornmentandotherfinelycraftedwealth

goodswereacentralpartofeliteregaliaandaccoutrement,andlikelyservedasmarkers

ofClassicMayaeliteidentity,isobviousfromthemanydepictionsonpainted polychromevessels,murals,andcarvedmonuments.Itemsidentifiedaswealth,prestige

orstatusgoodsbyMayanistsincludeobjectsandornamentsofjadeite,shellandother

stone,chertandobsidianeccentrics,pyritemirrors,finetextiles,andpaintedpolychrome pottery.Whatisstillunclearhowever,iswhoproducedtheseobjectsandwherethey

wereproduced.Scholarsoftenarguethatbecauseelitesappeartohaveconsumedwealth

217 goodsmoreoftenthannonelites,theydirectlycontrolledtheproductionofthesegoods

eitherbysponsoringtheirproduction(whichsuggeststhepresenceofindependent specialiststhatcanbe“sponsored”)orbyproducingtheseitemsthemselves.Whilethis maycertainlyhavebeentrueforthemostelaborateandfinelycraftedwealthgoods,it failstocapturetherolethat"independent"specialistsmayhaveplayedinwealthgoods production.

ManyargumentsconcerningClassicMayaeconomicorganizationpositthatthe productionofwealthgoodswasorganizedinadifferentmannerthantheproductionof subsistenceorutilitariangoods(e.g.McAnany1993;KingandPotter1994;Potterand

King1995;Inomata2001).ClassicMayawealthgoodsproductionisviewedas:(1) highlyskilled,involvingproductionmethodsthataredifficulttomaster(ReentsBudet

1998:73),(2)ofteninvolvingtheuseofexotic(nonlocal)rawmaterials,and(3) requiringamasteryofesotericknowledgeaboutaestheticandmoralvalues(Inomata

2007:135136).Scholarshavegenerallyreliedononeofthreelinesofevidenceto characterizetheorganizationofClassicMayawealthgoodsproduction:(1)depictionsor referencesfrompictorialorepigraphicsources;(2)indirectevidencefromstylisticand compositionalstudiesofpaintedpolychromepottery;and(3)directevidence,including thepresenceofproductiondebitage,tools,andbrokenorunfinishedwealthgoods.Here,

Isummarizetheevidenceoftenpresentedabouttheproductionofitemsconsidered

"wealth"goodsbyMayascholars.

Mayainscriptionsaregenerallymuteregardingeconomicorganization.

Nevertheless,somescholarspointtoeliteparticipationinwealthgoodsproductionbased

oniconographyandhieroglyphictextsonpaintedceramics.Sometextsonpainted

218 ceramicscontainthenamesoftheartistswhoproducedthem,someofwhomappearto havebeenelitesthemselves(ReentsBudet1994:55,89,132;Stuart1987,1989).For

example,onepainter,AhMaxamof,signedhimself its’aat ,sonofrulerK’ahk’

UkalawChanChaakandLadyShellStar (ReentsBudet1998:74;MartinandGrube

2000:80,81).Somevesselsdepictscribesorartisansperformingartisticworkincourtly settings,suggestingthattheymayhaveengagedinotherformsofcrafting(suchasmask carving),inadditiontopaintinghieroglyphictexts(Coe1973;CoeandKerr1997).

Finally,someindividualsincourtscenesaredepictedwithscribalattiresuchas paintbrushes,leadingsometosuggestthattheyareeitherscribes,orarelinkedtothe creationofthesevesselsthemselves(CoeandKerr1997:71110;ReentsBudet1994:

3667).

Despitethefrequentdepictionsofscribesonthesevessels,identifyingmoredirect evidenceforthelociofpaintedpolychromeceramicsproductionhasprovenmuchmore difficult.Basedonastylisticanalysis,ReentsBudet(1994;1998)arguesthatLate

Classicpaintedpolychromeceramicscanbeclassifiedintoanumberofrecognizable stylesthatsuggesttheywereproducedbyalimitednumberofartisansworkinginso called"palaceschool"contexts.Traceelementanalysisofpaintedpolychromesfromthe siteof Buenavista,Belizeandsurroundingsitessortedintosevengroups,eachofwhich

includedfinelypaintedpolychromesandmoresimplydecorated,lesswellmadevessels

(ReentsBudet etal.2000: 111,116).Theresultsofthesecompositionalanalysesled

ReentsBudetetal.(2000:111,117)tocallthesecompositionalgroupstheproductsof

sevenseparatespecialized"workshops"thatservedawiderangeofconsumersand producedgoodsaccordingtotheneedsoftheirconsumers,which" mostprobablywas

219 associatedwiththerulingeliteofBuenavista."Theysupporttheirargumentforapalace

workshopwithaLateClassicsecondaryrefusedepositrecoveredinassociationwitha palacebuildingatBuenavistathatcontained"literallydozensofwholebutbroken" paintedpolychromevessels,elitedomestictrash(Ball1993:250),and"fragmentsof

ceramiclevigationvatsforacalcareouswhiteslip,avarietyofmodeling,smoothing,

scraping,andburnishingtools,andseveralsmallpaintpotsholdingtracesofred,yellow,

andMayabluepigments"(ReentsBudetetal.2000:111n13).Basedontheproximityof

thisevidencetotheroyalpalaceatBuenavista,Ball(1993:250)arguesthatthebuilding

wasthesiteofa"palacesitedpolychromeproduction"location.

Regardlessoftheproblemsofinferring"workshops"fromchemicalcomposition groupings(Rice2009:133),itisnotsurprisingthatpaintedpolychromeceramicswere createdbyhighlytrainedspecialists.AsMichaelCoe(1973)andothershaveobserved, properexecutionofthesevesselsrequiredthattheartisanbeliterateandintimately

familiarwithMayacosmologyandhistory,whichwouldhavelikelyrequiredlengthy

training(ReentsBudet1998:73).Thesameeruditionwouldhavebeenrequiredfor

scribeswhocraftedtheelaboratelyincisedjade,boneandshellartifactsfoundaselite burialfurniture(CoeandKerr1997).

Nevertheless,todatetheonlydirectarchaeologicalevidencesuggestingthatsuch productiontookplaceinpalacescomesfromtherapidlyabandonedsiteofAguateca

(InomataandTriadan2000;Inomata2001,2007;EmeryandAoyama2007;Aoyama

2007).AtStructureM810(the"HouseoftheScribe"),aLateClassicsubroyalelite

residence,excavationsofthestructureandassociatedmiddensrecoveredmortarsand pestlesbelievedtohavebeenusedtogrindpigmentsaswellashalvedshellslikethose

220 depictedwithscribesinceramicpaintingsthatarearguedtohaveservedaspaintpots

(Inomata2001:326).Inaddition,numerouschertcraftingtoolswithmicrowearpatterns

associatedwithboneandshellworkingwererecoveredalongwithsmallamountsofbone

andshellworkingdebitage(EmeryandAoyama2007:81).Basedontherecoveryof

domesticartifactsintheseexcavations(includinggrindingstones,storagejarsand

cookingvessels),Inomata(2001:327)arguesthatitwastheresidenceofanelitescribe

wholikelyproducedwealthgoodsbothforpersonaluseaswellasforusebytheroyal

eliteresidingintheAguatecapalace(Inomata2001:331).Additionally,theAguateca

datapointtothepracticeofmultiplecrafts(i.e. multicrafting c.f.Hirth2006;Shimada

2007)byeliteorattachedspecialists,asubjectIaddresslaterinthischapter(Inomata

2007).

Furtherevidencefortheparticipationofelitesorattachedspecialistsasproducers ofwealthgoodscomesfromexcavationsattheLate/TerminalClassicsubroyalelite compound9N8atCopan(Webster1989).ExcavationofStructure9N82revealeda carvedhieroglyphicbenchandassociatedsculpturesofscribesandascribalgod, suggestingthattheheadofthecompoundwasanelitescribe(Fash1989).Inaddition, excavationsuncoveredevidenceoftheproductionofshellandlapidaryobjects(including highlycraftedeliteregalia)inbothpublic("secular")andprivate("sacred")areasat

Structure110andPatioH(Webster,EvansandSanders1993:282287;Widmer2009).

Manyofthematerialsworkedwereofnonlocalorigin,includingmarineshell, greenstone,schistandpyrite.Basedontheamountofdebitageandexhaustedtools

(mostlyheavilywornobsidianbladesusedforshellandwoodworking),Widmer(n.d.:

4651)arguesthatproductionwasforbothinternalconsumptionandforexchange

221 (possiblyasgifteditemsortribute)toother,possiblymorehighlyrankedelites.Based onthedomesticnatureofthecontextsofrecoveryofsomeoftheartifacts,Widmer(n.d.:

47)arguesthatthisproductionwaslikelycarriedoutbytheeliteresidentsofthe compound.Takentogether,thedatafrom9N8lendsfurthersupporttotheroleofelites intheproductionofhighlycraftedwealthgoods.AswasthecaseatAguateca, identificationofthisproductionwasaidedbyacatastrophicevent(likelyanearthquake) thatsealedmuchoftheevidence in situ .

Asidefromthesetwowelldefinedexamples,Classicperiodcontextsof productiondebrisofnonceramicwealthgoodselsewhereintheMayaareaaremore variedandequivocal.Forexample,despitethefactthatshellornamentsareoften includedamonglistsofwealthgoodsbyMayanists,fewinstancesofshellornament productionhavebeenreportedfortheClassicperiod.Aoyama(1995)suggeststhata middencontainingchertandobsidiantoolswithmicrotraceevidenceofshellworking wasthebyproductofmarineshellworkingatthesitecenterofCopan.Hisconclusionis doubtfulgiventhepresenceofonlyfinishedartifactsandfreshwater jute shellsinthe

midden,unliketheassemblageofpartiallyworked,unworkedandbrokenshelldebris

recoveredfromashellworkinghouseholdatEjutlainOaxaca(Feinman1999).

Evidenceofshellartifactproductionhasalsobeenreportedfortwostructuresintheelite

acropolisat(DomínguezCarrascoandFolan1999;Folanetal.2001),butitis

difficulttoevaluatethisevidence,asdetailsofthedebitagehavenotbeenreported.In

contrasttotheeliteproductionlocinotedabove,evidenceofLateClassicperiodshell

workingatwasfoundmoreofteninnonelite,ruralhouseholdsthaninelite

contexts(Cobos1994;Pope1994;ChaseandChase2001:132),leadingChaseandChase

222 (1994:10)toconcludethattheproducers"werenotattachedspecialists".Paralleling

thesefindings,cutmarineshellfragments,possiblyfromtheproductionofornaments,

werefoundinaLateClassiccontextataruralnoneliteplazuelagroupintheSan

Lorenzosettlementclusterinthehinterland(YaegerandRobin2004:154).

ThemostextensiveevidenceofLateClassicperiodwealthgoodsproduction

comesfromrecentresearchatCancuen(Kovacevichetal.2001;Kovacevich2003,2006,

2007).ExcavationinstructuresM104andM107yieldedover3,250piecesofjade,

includingaboutonekilogramofmicrodebitageembeddedinearthenpatiofloors

(Kovacevich2007:7677).Whilethegreatmajorityofjadepieceswerepercussion

debitage(91%),cutjadefragments,aswellaseightjadebeads(oneapossibleearflare blankintheprocessofbeingdrilled)werealsorecovered(Kovacevich2007:78).In

additiontojadedebitage,toolsassociatedwithjadeproduction(e.g.chertdrills,

hammerstones,polishingstones,seeChapter6fordetails)wererecoveredfromthe

structuresandassociatedmiddens.Thestructuresarepartofsmallmoundgrouplocated

500mnorthoftheroyalpalace;bothstructuresarerankedinthenexttolowesttierofthe

structuretypologyforCancuen(Kovacevich2007:76).

Despitetheamountofproductionevidencefromthesetwostructures,onlytwo jadeartifactswererecoveredfromthetenexcavatedburialswithinthegroup

(Kovacevich2007:78).Excavationsinelitearchitectureelsewhereatthesiterevealed

higherratesofconsumptionoffinishedartifacts,aswellaspossibleevidenceforthe

finalstagesofjadeartifactproductionintheformofasandstoneearflarepolishercached

inanelitestructure,althoughnootherassociatedproductionevidencewasrecovered

fromelitecontexts(Kovacevich2007:80).Nevertheless,jadebeadswerefoundinall

223 structuretypesatCancuen,thoughtheyweresignificantlylargerinelitestructures,while

earflaresandplaqueswerefoundonlyinelitecontexts.Kovacevich(2007:8286)

concludesthatjadeartifactproductionatCancuenwassegmented,withnonelites performingsimple,butlaborious,tasks(shattering,pecking,sawing)innonelitedomestic

structures,whilethefinalstagesofproductionwereperformedeitherbyelitesthemselves

orbyattachedspecialistsinelitecontexts.

Thecurrentevidence,thoughlimited,providesageneralpictureofthe organizationofClassicMayawealthgoodsproduction.Scholarshaveemphasizedthe highdegreeofartisticandtechnologicalskillthatwasrequiredtoproducemostitems usedaswealthgoods,particularlyforpaintedpolychromevesselsandelaboratelycrafted jadeandshellornaments(ReentsBudet1998;Inomata2001;Rice2009).Indoingso, theyhaveemphasizedthehighlysymbolicaspectsofwealthgoods,arguingthat appropriateproductionofthesegoodswouldhaverequiredeitherwelltrained,highly skilledproducerssupportedbypatrons,orelitesproducinggoodsthemselves.

Nevertheless,thetoolsrequiredforthisproductioningeneraldonotseemtohavebeen highlyspecialized,andinsomecasesparticulartoolsorevenexpedientflakeswereused tocraftobjectsofdifferentrawmaterials(Aldenderferetal.1989;Aldenderfer1991;

EmeryandAoyama2007;Aoyama1995,2007).Evidenceoflargescale,specialized productionunitsseemstogenerallybeabsent,andmostcraftingofwealthgoodsappears tohavetakenplaceinornearresidential,domesticarchitecture.Inthefollowingsections,

Iexaminetheevidenceforjadeartifactproductioncollectedaspartofthisdissertation research,inlightofthesecharacterizationsofwealthgoodsproduction.Indoingdo,I proposesomewaysinwhichmodelsofClassicMayawealthgoodsproductionmightbe

224 fruitfullymodifiedinlightofthesedatatoarriveatamorecompleteunderstandingof

ClassicMayapoliticalanddomesticeconomy.

7.2 MiddleMotaguaValleyWealthGoodsProductioninContext

InChapter2,Idescribedfouraspectsofcraftproductionvariabilitythatare germanetothisdissertationresearch:(1)productionmethodsandtechnology,(2)scale andstructureofproductionunits,(3)thenatureofthegoodsproduced,and(4) sociopoliticalcontextofproduction.ModelsofancientMayawealthgoodsproduction oftenexpectcovariationamongthesedimensions,whichhasledtoanumberof inappropriateexpectationsofparticularformsorsystemsofcraftproduction(c.f.

Feinman1999;Hirth2006,2009b).Inordertofacilitatediscussionandevaluationofthe evidencefromthisdissertationfieldresearch,Idealwitheachofthesetopicsseparately, beforemovingtoamoregeneraldiscussion.

7.2.1 ProductionMethodsandTechnologyintheMiddleMotaguaValley

InChapter6,Isummarizedthetechnologyofjadeiteartifactproductioninthe

MiddleMotaguaValley,includingdescriptionsofproductiontoolsandbyproductsof theproductionprocess.GiventhecharacterizationofClassicMayawealthgoods productiondiscussedabove,weshouldexpecttofindevidenceofmorecomplex productiontechniquesatmorehighlyrankedsitesinthelocalsitehierarchy,with evidenceoflesssophisticatedorskillfulproductionevidenceatlowerranked,nonelite sites.Evidencealongtheselinesmightincludethepresenceofdifferenttools,or

225 differencesintechnologicalsteps(e.g.percussionvs.sawing)athigherversuslower

rankedsites(c.f.Kovacevich2007).

Chertmicrodrillsareoneformaltoolcategoryassociatedwithdrillingofjadeite andshell.DuringtheLateClassicperiodinthePetenLakesregion,Aldenderfer(1991:

210;Aldenderferetal1989)reportsrecoveryofsimilarchertmicrodrillswithmicrotrace evidenceforthedrillingofshellandfinegrainedstonesatthelargestsiteinthesurvey area(),andinassociationwith"scrapsofbrokenandcutjadestone."Elsewherein

Mesoamericahowever,similarchertmicrodrillshavebeenrecoveredinassociationwith jadebeadproductioninaLateFormativeruralnonelitehouseholdatNativitasinPuebla,

Mexico(Hirth2005;Hirthetal.2009),andwithLateClassicperiodmarineshell ornamentproductionatanonelitehouseholdinEjutlaintheValleyofOaxaca(Feinman

1999;FeinmanandNichols2000,2004).

Chertmicrodrillswererecoveredinsurfacecollectionsatallbutninesitesinthe surveyarea(Table7.1).Althoughtheymayhavebeenusedtodrillmaterialsotherthan jade(e.g.shellorotherstone),theirpresenceatmostsitessuggeststhatthesetoolswere widelyavailable.Examiningthefrequencyofsurfacecollectedchertmicrodrillsbysite typefurtherunderscoresthispoint,andshowsthatthetechnologywasnotrestrictedto themosthighlyrankedsitesintheMiddleMotaguaValley(Fig.7.1).Overall,the majorityofchertdrillsfromsurfacecollections(65%,n=68)wererecoveredfromsites inthethreelowesttiersoftheMMVsitehierarchy.

Inaddition,chertbladeswererecoveredfromsurfacecollections(althoughrarely, n=12)fromsitesinalltiersofthesitehierarchy.Prismaticchertbladeslikelyservedas blanksformicrodrills,areductionsequencedocumentedinthePetenLakesregion

226 (Aldenderfer1991b),Nativitas(Hirthetal.2009),aswellastheChannelIslandsin

California(Arnold1987).Althoughthesampleissmallandinconclusive,therecovery ofchertbladesatalltiersofthesitehierarchysuggeststhatthematerial,technologyand skillnecessaryforproducingchertmicrodrillswaswidespread,andnotrestrictedto skilledcraftsmenworkingatelitesites.

SiteName HierarchyType ChertDrills ChertBlades Guaytan4 II 31 3 Guaytan5 II 0 0 Guaytan6 V 9 0 Guaytan7 V 1 0 Guaytan8 IV 3 0 PuenteHato IV 1 0 VargasI V 0 0 VargasIIA V 2 0 VargasIIB III 6 2 VargasIII III 4 1 VargasIIIA II 0 0 VargasIV IV 4 0 MagdalenaI V 16 1 MagdalenaII III 0 0 ElTerronN. V 0 0 ElTerronS. IV 0 0 KM912 IV 1 1 KM913 III 2 1 KM914 III 5 0 KM921 III 0 0 KM922 II 2 0 KM923 III? 8 1 KM931 II 2 1 KM933 I 2 0 KM934 III? 0 0 LosChaguites1 II 6 1 LosChaguites2 III 0 0 TOTALS 105 12 Table7.1Chertdrillsandbladesfromsurfacecollections.

227 Figure7.1Chertdrillsandbladesfromsurfacecollections,bysitetype.This suggeststhatchertdrilltechnologywasavailabletomost(ifnotall)producers,and householdsmayhaveproducedtheirownmicrodrillsfromchertblades. Turningtothetestexcavationdata,chertdrillswererecoveredfromsixofnine sites(Table7.2).Inordertocontrolfordifferencesinthetotalvolumeofexcavationsat differentsites,Icalculatedthenumberofdrillsrecoveredpercubicmeterofsoilateach site(Fig.7.2).Basedonthismeasure,ratesofchertdrillsrecoveredatGuaytan4(Type

II),Guaytan6(TypeV)andMagdalenaI(TypeV)weregenerallysimilar,andfarabove therateofdrillsrecoveredfromthethreeremainingsites.Examiningtheaverage numberofchertdrillsrecoveredpercubicmeterforeachhierarchicalsitetypes,shows thatthehighestnumberwererecoveredfromTypeIIandTypeVsites(Fig.7.3);The lowrateofrecoveryatTypeIIIsitesispartiallyattributabletothefewtestpitsthatwe wereabletoexcavateatthesesites.Nevertheless,thedatashowthatchertdrillswere recoveredinsimilarquantitiesinassociationwithbothnonelite(TypeII)andelite(Type

V)sites,contrarytoexpectationsthattechnologicaldifferenceswouldexistbetweenthem.

228 Hierarchy Chert Chert SiteName Type Drills Blades Guaytan4 II 235 10 Guaytan5 II 0 0 KM931 II 0 0 VargasIIB III 1 0 KM923 III? 0 0 Guaytan8 IV 13 4 Guaytan6 V 23 0 Guaytan7 V 7 0 MagdalenaI V 17 0 TOTALS 296 14 Table7.2Chertdrillsandbladesrecoveredfromtestexcavations.Thetotals forGuaytan4representthesumofallsuboperationsatthesite.

50 47.07 45 42.5 38.33 40 35

30 25 20

15 10 5.11 6.71 2.86 5 0 Guaytan 4 Guaytan 6 Guaytan 7 Guaytan 8 Vargas IIB Magdalena I Figure7.2Chertdrillspercubicmeterfromexcavations.Excavationunitsat Guaytan5,KM931andKM923didnotyieldanydrills.

60

47.07 50

40.42 40

30

20

6.71 10 2.86

0 Type I Type II Type III Type IV Type V Figure7.3Chertdrillspercubicmeterfromexcavations,averagedpersiterank.

229 MoredirectevidenceforthediffusecharacterofdrillingofjadeiteamongMMV sitescomesfromanexaminationofbeadsbrokenorabandonedduringtheprocessof drilling.Atotalof59jadebeadsbrokenduringdrillingwererecoveredfromsurface collectionsandscreeningoflooter'sbackdirtattwelvesites(Table7.3).Themajorityof these(76%)werebuttonbeadsofamicarichjadeitecollectedfromlooter'sbackdirt behindthelargeststructureatVargasIIA;brokenbeadswererecoveredfromonlyone otherTypeVsite(Guaytan7).Comparingthequantitiesofbrokenorabandoneddrilled beadsbysitetypedemonstratesthatdrillingofjadeitebeadstookplaceatallsitetypes, althoughthemajorityofevidencewasrecoveredfromTypeVsites(Fig.7.4).Finally, whileevidenceoftheuseofhollowdrills(i.e.hollowdrillcores)fromsurfacecollections wasrare,theywerecollectedatallsitetypes(Fig.7.5),furtherunderscoringthefactthat hollowtubulardrillingwasawidespreadactivity,andnotonelimitedtohigherlevel, presumablyelitesitetypesbecauseofconstraintsoftechnologyorskill.

BeadsBroken BeadsAbandoned SiteName HierarchyType DuringDrilling DuringDrilling KM93III I 1 1 Guaytan4 II 3 3 Guaytan5 II 1 0 KM93I II 0 1 VargasIIB III 1 3 VargasIII III 1 2 KM91IV III 2 0 LosChaguites02 III 1 0 KM92III III? 1 0 Guaytan8 IV 1 0 VargasIV IV 1 0 KM91II IV 0 1 Guaytan7 V 1 0 VargasIIA V 45 5 TOTALS 59 16 Table7.3Sitesatwhichbeadsbrokenorabandonedduringthe processofdrillingwererecoveredfromsurfacecollections.

230 Figure7.4Surfacecollectedbeadsbrokenorabandonedduringdrilling, quantifiedbysitetype.

Fig.7.5Hollowdrillcoresfromsurfacecollection,quantifiedbysitetype. Walters(1982)arguedthatearlystagesofjadeartifactproduction(i.e.percussion) werecarriedoutatlowerlevel(nonelite)sites,whilefinalstages(i.e.sawing,drilling, polishingandincising)werecarriedoutatelitesites.WhileKovacevich(2006;2007) proposedasimilarsegmentedproductionsystemforCancuen,shearguesthatnonelites undertooktheproductionofstylisticallysimpleformsofjadeiteartifacts,suchasbeads

231 andearflares.Comparisonsofdifferenttechnologicalcategoriesofjadeartifact productionacrossthelocalsitehierarchycanhelptoevaluatethesepropositionsforthe

MiddleMotaguaValley.

AsnotedinChapter6,jadeitepercussiondebitagewasbyfarthemostfrequently

recoveredtechnologicalartifactcategoryinsurfacecollectionsandexcavations.

Comparingthequantityofsmalljadeflakesfromsurfacecollections,thereisevidenceof percussionproductionatallsitetypes,withthehighesttotalsfromTypeII,IIIandVsites

(Fig.7.6).Examiningtheaveragequantityofsmalljadeflakesrecoveredpersitewithin eachsitetyperevealsthesamebasicpattern(Fig.7.7).Theimportantpointisthat percussionflakeswerefoundat all levelsofthesitehierarchy.

Figure7.6–Smalljadeflakesurfacecollectionsbysitetype.Notethatflakeswere recoveredfromallsitetypes.

232 Figure7.7Averagequantityofsmalljadeflakesrecoveredfromsurfacecollections persiteineachsitetype. Jadeflakesrecoveredfromexcavationsprovideaslightlydifferentpictureofjade percussionactivitywhenexaminingthefrequencyofjadeflakesrecoveredpercubic

meterofsoil(Fig.7.8).Thefrequencyofjadeflakeswascalculatedbydividingthetotal

amountofflakesrecoveredineachexcavationunitbythevolumeofsoilexcavatedin

eachexcavationunit.Thefrequencyofjadeflakespersitetypewasthencalculatedby

averagingthefrequenciesofjadeflakesofexcavationunitsateachsitetype.Thehighest

frequenciesarefoundatTypeIIandTypeVsites,whichisareflectionofthelocationof

excavationsintodensesurfacescattersofjadeartifactsatGuaytan4andMagdalenaI.In

fact,theTypeVfrequencyisgreatlyinflatedbytheextremelydensedebitagedepositin

unit8A1,where817jadeflakeswererecoveredinonly0.4m³ofsoil.

233 600

472.92 500

400 330.59

300

200

100 50 0 3.98 0 Type I Type II Type III Type IV Type V Figure7.8Averagequantityofsmalljadeflakespercubicmeterrecoveredfrom excavations,organizedpersitetype. Consideredtogether,theevidencefromexcavationandsurfacecollections

indicatesthatthetechnologyandskillsnecessaryfordrillingjadeartifactswerelargely

redundantacrossdifferentsitetypesintheMiddleMotaguaValley.Furthermore,drilling

and percussionreductionwasperformedatsitesthroughoutthelocalhierarchy.Ifthe

sitehierarchyreflectsdifferencesinthesocialstatus,thenthereisnoevidencefromthe

currentdatatosuggestthatdifferenttasksassociatedwithjadeartifactproductionwere

carriedoutatsitesoccupiedbyelitesversusthoseoccupiedbynonelites.Itshouldbe

notedhowever,thatnoevidenceoftheproductionelaboratelycarvedjadeartifactswas

recoveredatanyoftheMMVsites,norwasanyevidenceofincisingencountered.

Nevertheless,thesedatastillruncountertoexpectationsregardingtheorganizationof

wealthgoodsproductioningeneral,andparticularlytomanymodelsofClassicMaya

wealthgoodsproductiondiscussedearlier.

234 7.2.2 ScaleandStructureofProductionUnits

InChapters4and5andinAppendixA,Idescribedthearchaeologicalsites

surveyedandexcavatedaspartofthisdissertationresearch.Determiningexactlociof production(i.e.inornearwherecraftproductionactuallyoccurred)basedonsurface remainsisdifficult,especiallygiventhetransformationprocessesthathaveaffected archaeologicalsitesintheMiddleMotaguaValley.Manysiteshavebeenheavilylooted orarelocatedonlandthatiscurrentlyundercultivation,usedforcattlepasture,or disturbedbymodernbuildings.Nevertheless,evidenceofjadeartifactproductionwas foundateverysiteinthesurveyregion.Theserangedincompositionfromnonmounded sitesconsistingonlyofsurfaceconcentrationsofartifacts(e.g.KM933),tothose consistingofmultiplestructuresorstructuregroups.Whilestructuresatsomesites servednondomesticfunctions(e.g.vaultedfunerarymonuments,ballcourts),itislikely thatmanyofthestructuresatMMVsitesaretheremainsofdomesticstructuresor structuregroups.Therefore,themostparsimoniousexplanationfortheubiquityofjade productionevidenceatMMVsitesisthatjadeartifactproductionwasnotconcentratedat onlyafewsites,butwasinsteadawidespreadactivitythatwasoftencarriedoutwithinor neardomestichouseholds(representedbystructuregroups).

Wecanexplorethispossibilityabitfurtherbyexaminingcontextswherejade productionevidencewasclearlyassociatedwithparticularportionsofsites.Although jadeproductionevidencewasrecoveredatallMMVsites,inmostinstancesitwasnot

concentratedinparticularportionsofsites,butwasinsteadfounddistributedsporadically

throughoutmanyareasatmanysites.Atonlyafewsitescanweinferthatdebitagewas

associatedwithparticularstructuresorstructuregroups.Wherethiswaspossible,the

235 currentdatasuggestthatthephysicalscaleandstructureofproductionunitsvaried significantly.AtMagdalenaI,adenseconcentrationofjadeitedebitagewasrecovered fromtestexcavationsandsurfacecollectionsontheeasternperimeterofthesite,in associationwithastructuregroupthatincludedStructure3,alarge,multiroomed structurewith2mhighwalls.ThefactthatStructure3containedmultiplerooms suggeststhatitpossiblyservedadormitoryfunction.Productionevidencewasalso collectedinassociationwithcutstonewallsuperstructuresonthewesternedgeof

MagdalenaI,locatednearaseriesoflowmoundsandthelargeStructure7.Althoughthe vesselformsformanyceramicscouldnotbeidentified,excavationunitsinbothareas yieldedfragmentsof comals andstoragejars,furthersuggestingthatdomesticfunctions

werecarriedoutinornearthesestructures.Together,theassociationofproduction

evidenceatMagdalenaI(aTypeVsite)suggeststheproductionofjadeartifactsin

associationwithelite(possiblyresidential)structures.

AtVargasIIA(aTypeVsite),jadeproductionevidenceinthenorthernpartof

thesitewasconcentratedapproximately15mtothenorthofStructure1,alargemound

ofunknownfunctionthathasbeenheavilylooted . Thenextcloseststructureis25mto

theeast.Structure1occupiespartofapossiblealargecivicceremonialgroup,asitis

located30macrossaflatplazaareafromanotherlargemound,whichwewereunableto

examinecloselybecauseitwasonthepropertyofanotherlandowner.Whileitisunclear

whyproductionevidencewasconcentratedinthisarea,itisnotablethatitwasfound

closesttoelitearchitecture.Nevertheless,itappearsthatthestructureservedsome

domesticpurpose,because comal fragmentswererecoverednearthestructure,aswasa

fragmentofabasalt metate ,bothofwhichsuggestprobabledomesticactivity.

236 Incontrast,jadeproductionevidenceatVargasIIIwasfoundmostdensely concentratedinassociationwiththesmallestplatformstructuresatthesite,asmallgroup offourlowstructuresinthesoutheasternportionofthesite,located20mawayfromthe neareststructuregroup.However,aswasthecasewithMagdalenaIandVargasIIA,a possibledomesticfunctionofthegroupissuggestedbythepresenceoffragmentsof cookingandstoragevessels,aswellasabrokenmetatefragment.Asdescribedin

Chapter6,jadeiteproductionevidenceatGuaytan4wasalsoassociatedwithahumble structuregroup,andincludedevidenceofdomesticceramicvesselforms.Inaddition, jadeproductionevidencewasrecoveredatKM931,LosChaguites01andLosChaguites

02,eachofwhichisasmallstructuregroup.Nevertheless,productionevidencewasnot clearlyassociatedwithparticularstructuresatanyofthesethreesites.

Whilethedatadonotprovideconclusiveevidenceofthestructureandscaleof productionunits,theydosuggestthatwealthgoodsproductiontookplacepredominantly withinorneardomesticstructuresintheMiddleMotaguaValley.Manyofthese structuresorstructuregroupslikelyrepresentthephysicalremainsofancienthouseholds.

Thatevidenceofcraftproductionwaslocatedwithinorneardomestichouseholdsisnot surprising,ashouseholdsweretheprimarylociofcraftproductionthroughout prehispanicMesoamerica,apointtowhichIwillreturnlaterinthischapter.

7.2.3 NatureoftheGoodsProduced

AsIdiscussedinChapter2,archaeologicalstudiesofwealthgoodsproduction haveoftenpaidinsufficientattentiontothepossiblegradationsofvalueofthegoods beingproduced,oftencharacterizingwealthgoodsasamonolithiccategoryofnon

237 utilitariangoods.However,inrecentstudiesofClassicMayawealthgoodsproduction,

somescholarshavesuggestedthatnonelitesmayhavebeeninvolvedintheproductionof

wealthgoodsingeneral(McAnany1989)orintheproductionofblankvasesuponwhich paintedpolychromeswereexecuted(Ball1993).Forjadeartifactproduction,some

scholarsarguethatnoneliteparticipationwaslimitedtotheproductionofless“valuable”

artifactssuchasbeads(Kovacevich2007)orthattheyhaveonlyinparticularlylaborious

orunskilledstagesofproductionsuchaspercussion(Walters1982)orgrindingand polishing(MoholyNagy1997).Althoughthepresentdatacannotfullyaddressthese propositions(particularlyinthecaseofunique,highlycraftedorincisedartifacts),they

doallowforsometentativeobservationstobemadeaboutpossibledifferencesinjade

craftingbetweeneliteandnonelitesitesintheMMV.

Almostallsites(n=21,75%)inthesurveyareacontainedevidencelinkedtojade beadproduction,eitherintheformofcompletebeads(alongwiththepresenceofjade

debitage),beadsbrokenorabandonedduringdrilling,performbeadsorthepresenceof

chertdrills(Table7.4).Moreimportantly,evidenceofjadebeadproductioninoneform

oranotherwasfoundatalllevelsofthesitehierarchy.Asexpectedbythemodels

describedearlier,thissuggeststhatstylisticallysimple(i.e.“lessvaluable”)wealthgoods likebeadswerebeingproducedbynonelitesandelitesalike.

Thedistributionofevidenceofnonbeadjadeartifactproductionshowsanumber

ofinterestingpatterns.Whileevidenceofsawingisfoundinfrequently,itisfoundat

everylevelofthelocalsitehierarchy,indicatingthatitwasnotaproductionsteplimited

solelytoelitesitetypes(Fig.7.9).Becauseitwasalaborioustask,craftproducerswould

havebeenunlikelytosawjadeiteintheprocessofproducingbeads.Instead,sawingwas

238 morefrequentlyinvolvedintheproductionofartifactformssuchasplaquesandearflares

(Digby1964;Proskouriakoff1974).Whilejadebeadsarefound(albeitinsmallnumbers)

innonelitecontextsatClassicperiodMayasites(Palka1997;Zeleznik2002;Guderjan

2007),thedistributionofplaquesandearflaresismorerestricted,indicatingthatthese

objectsmayhavehadmore“value”(seeChapter2).Therefore,itispossiblethat

noneliteswereinvolvedintheproductionofsomeofthesemorevaluablegoods,contrary

toexpectationsofsomemodelsofClassicMayawealthgoodsproduction.

SiteName Hierarchy Jade Broken/ JadeBead HollowDrill Chert Type Beads AbandonedJadeBeads Preforms Cores Drills Guaytan3 I ― ― ― ― ― Guaytan4 II X X X X X Guaytan5 II X X ― ― ― Guaytan6 V ― ― ― ― X Guaytan7 V ― X ― ― X Guaytan8 IV ― X ― X X PuenteHato IV ― ― ― ― X VargasI V ― ― ― ― ― VargasIIA V X X X X X VargasIIB III X X X ― X VargasIII III ― X X ― X VargasIIIA II X ― ― ― ― VargasIV IV ― X ― ― X MagdalenaI V X ― X X X MagdalenaII III ― ― ― ― ― ElTerronN. V ― ― ― ― ― ElTerronS. IV ― ― ― ― ― KM912 IV ― X ― ― X KM913 III X ― ― ― X KM914 III ― X ― ― X KM921 III ― ― ― ― X KM922 II ― ― ― ― X KM923 III? ― X X X X KM931 II ― X X X X KM933 I ― X ― X KM934 III? ― ― ― ― ― LosChaguites1 II ― X ― X X LosChaguites2 III ― ― X ― ― Table7.4–Jadebeadproductionevidencefromexcavationsandsurfacecollections.

239 10 9 9 8 7 6 5 5 4 4 3 2 2 1 0

T Type II Ty Typ Type V yp p e e III e I IV

Surface Collection Excavation Figure7.9Jadefragmentsshowingevidenceofsawingbysitetype. Representingthefinalstagesofjadeitebeadandnonbeadartifactproduction,

evidenceofgrindingandpolishingtasks(intheformoffragmentswithgroundor polishedfacets)showasimilarlywidespreaddistributionamongdifferentsitetypes(Fig.

7.10).Theactivitywasnotcarriedoutsolelyineliteornonelitesitestypes,butseemsto

havebeenacraftingactivitycarriedoutatsitesofvaryingstatus.Manyofthese

fragmentswerelikelyfromtheproductionofnonbeadartifactsaswell,andthusadd

furthersupporttotheargumentthatnonelitesintheMiddleMotaguaValleywerenotjust producing“lowvalue”jadebeads,butwerealsoproducingotherartifactformsaswell.

Drillingwasnotatechnologicalstepperformedsolelyfortheproductionofjade beads,butwasalsodonetocreatesuspensionholesforotherartifactforms,suchas plaques,earflaresandpendants.Ifholesintheseitemswerecreatedbytheuseofa

hollowdrill,theresultinghollowdrillcoreswouldlikelyhavedifferentmorphological

characteristicsthanthoseproducedfromdrillingbeads.Forexample,theendsofhollow

drillcoresfromtheperforationofplaqueswouldbeflatfromthegrindingofpolishingof

240 25

20 20

15 13

10 8

5 5

0 Type I Type II Type III Type IV Type V Figure7.10Fragmentswithground/polishedfacetsfromsurfacecollections,bysite type. theplaquepriortodrilling.Thisislikelythecasefortwoofthecoresrecoveredfromthe

Guaytan4excavations,whichappeartohavebeenthebyproductsofplaqueandearflare perforations(Fig.7.11).Ifthisisindeedthecase,thentheirpresenceataTypeIIsite

wouldlendfurthersupporttothenotionthatnonelitesintheMMVwereproducingboth

“low”and“highvalue”jadeartifacts,incontrasttotheexpectationsofpreviousmodels

ofClassicMayawealthgoodsproduction.

Figure7.11HollowdrillcoresrecoveredfromGuaytan4excavations.(a)Likely fromdrillingofaplaque,asthecorewasremovedfromathin,flatobject.(b) Possiblyfromtheproductionofanearflare,asoneendofcoreisfinelygroundflat, whileotherendisonlyroughlypeckedandrounded.

241 Finally,comparingtheinteriordiametersofholesdrilledintobroken,abortedand

completebeadswiththediametersofhollowdrillcoresprovidesanotherpossiblelineof

evidencethatproductionatmanysitesintheMMVwasgearedtowardproducingjade

artifactformsinadditiontosmallbeads.Table7.5summarizesthesemeasurements,

withbutdoesnotincludethetwohollowdrillcoresnotedabove.Becausethehollow

drillcorestapertowardoneorbothends(andarelargerindiameterattheseptumfor biconicaldrillcores),thediameterlistedforthehollowdrillcoresinTable7.5isthe

averageofthosemeasurements.Thediameterlistedforthebroken,abandonedand

completebeadsisthemaximumdiameteroftheholeineachartifact.Therefore,thetable providesaconservativecomparison.Comparingthesemeasurementsshowsthatthe

diametersofthehollowdrillcoresarelargeronaveragethantheholediametersofthe beads,althoughthereissomeoverlapbetweenthem.Becauseitisdifficulttosaywhat

typeofartifactwasbeingdrilledfrommanyofthehollowdrillcores,itisunclearwhat

thisdifferencereflectsintermsofartifactproduction.Nevertheless,thedatasuggestthat

someofthehollowdrillcoreswerelikelythebyproductoftheproductionofartifacts

other thanthetypesofbeadsandbeadfragmentsthatwererecoveredintheMMV.

Complete, Hollow Brokenor Drill Measurement(mm) Abandoned Cores DrilledBeads (n=60) (n=107) AverageDiameter 1.86 4.25 StandardDeviation 0.86 1.13 MaximumDiameter 5.80 8.81 MinimumDiameter 0.57 2.99 Table7.5–Comparisonofaveragediameterofholesincomplete,brokenand abandonedbeadswiththediametersofhollowdrillcores.

242 Ifitisthecasethatthedifferencesobservedbetweentheaveragediametersof

beadsholesandthehollowdrillcoresrepresenttheproductionofdifferenttypesof

artifacts,wecantaketheanalysisastepfurtherandcomparethesemeasurementsacross

differentsitetypes.Table7.6presentsthediametermeasurementsofthebeadholesand

hollowdrillcoresbyhierarchicalsitetype.Onceagain,thedrillholesconsistentlyhave

asmalleraveragediameterthanthehollowdrillcoresforeverysitetypealthoughno

comparisoncouldbemadefortheTypeIIIsites.Thissuggeststhatatthesesitetypes,

someofthehollowdrillcoreswerefromtheproductiononnonbeadartifacts.

Nevertheless,thereissomeoverlapintherangesofthediameters,suggestingthatsome

ofthehollowdrillcoresmayhavebeenfromtheproductionofjadeitebeads.However,

thereisnocleartrendtowardlargerdiameterbeadholesorhollowdrillcoresin

associationwithhigherordersites,whichsuggeststhatlowrankedsitesproduceda

similarrangeofjadeartifactformsasmorehighlyrankedsites.

TypeI TypeII TypeIII TypeIV TypeV

Holes Cores Holes Cores Holes Cores Holes Cores Holes Cores (n=2) (n=0) (n=45) (n=54) (n=11) (n=1) (n=3) (n=2) (n=46) (n=3)

Average 1.46 n/a 1.92 4.13 2.13 7.12 1.53 5.04 1.77 5.01 (mm) Standard Deviation 0.40 n/a 0.98 1.09 1.27 n/a 0.31 0.81 0.63 0.71 (mm)

Max(mm) 1.74 n/a 5.80 7.68 5.25 n/a 1.84 5.61 3.84 5.84

Min(mm) 1.18 n/a 0.71 2.53 0.99 n/a 1.23 4.47 0.57 4.58 Table7.6–Comparisonofdiametersofinteriorholesofbroken,abandonedand completedrilledbeads(“Holes”)andhollowdrillcores(“Cores”),bysitetype.

243 Thegeneralredundancyofsawing,grinding,andpossiblenonbeadproduction

evidenceacrossthelocalsitehierarchyprovidemultiplelinesofevidencetosuggestthat

thetypesofgoodsbeingproducedatlowerranked(nonelite)werethesameasthose beingproducedatmorehighlyranked(elite)sites.Thesedatacontradictmodelsof

ClassicMayawealthgoodsproductionintwoways.First,contrarytotheexpectationsof

thesemodels(e.g.Walters1982;MoholyNagy1997),noneliteswerenotsimply performingtheearlystagesofjadeartifactproduction,butappeartohaveengagedinthe sametypesofproductionactivitiesasthosecarriedoutatelitesites.Second,nonelites wereproducingitemsthatMayanistswouldconsidermorevaluablethansmalljadebeads

(e.g.Ball1993),suchasplaques,earflaresorlargebeads,andwerethereforemorefully involvedintheproductionofwealthgoodsthanpreviouslybelieved.

7.2.4 SociopoliticalContextofProduction

Thesociopoliticalcontextofproductionreferstothelocationofproductionin socialspace(c.f.Costin2001:297),includingthesocialrankorstatusorartisans,andthe relationshipofproducerstoconsumers.Whileitisdifficulttodemonstrate“attachment” fromproductionevidencealone,wecanevaluatetheimplicationsofthedatafromthis dissertationresearchagainsttheexpectationsofattachedproductionmodelsofwealth goods.

Ifthesitehierarchyreflectstosomedegreethesocialstatusofresidentsatthose sites,thenthedataseemtoruncontrarytotheexpectationsofthesemodels.Evidenceof jadeartifactproductionisfoundathigherranking(TypeIVandV)sites,whichfollows theexpectationsofpreviousmodels.Althoughthesociopoliticalstatusoftheindividual

244 artisanscannottypicallybediscernedsolelyfromthelocationofproductiondebris(but

seeInomata2001),itispossiblethatnonelitesmayhaveworkedas“attached

specialists”inthetraditionalsense,asresidentssupportedbypatronsatelitesitesinthe

MMV.Asdescribedearlierhowever,jadeproductionevidencewasrecoveredat all sites

intheMMV,includingatlowrankingsitetypes(TypesI,IIandIII).Iarguethatitis unlikelythateliteswouldhave directly supervisedwealthgoodsproductionatthesesites, butratherthatnoneliteswereengagedinthisproductionasindependentproducers.This

runscontrarytooneofthecentralassumptionsofmodelsofwealthgoodsproduction,

whicharguethatattachedproductionofthesegoodswouldbelocatedwithinornearelite

residencesorsites.Neverthless,itispossiblethatnonelitehouseholdsengagedin

attachedproductionarrangmentsbyproducingjadeitewealthgoodsoncommandforelite patronsoraspartoflocaltributedemands.Iexplorethesepossibilitiesinmoredetail below.

7.2.5 MiddleMotaguaValleyWealthGoodsProductionSummary

Datagatheredaspartofthisdissertationfieldresearchruncontraryto

expectationsderivedfrompreviousmodelsoftheorganizationofwealthgoods production.DuringtheLateClassicperiodintheMiddleMotaguaValley,wealthgoods productionwasawidespreadactivityundertakenatalllevelsofthelocalsitehierarchy,

indicatingthatitwasnotanactivityundertakenonlyatelitesites.Likewise,thereisno

evidencetosupportthenotionthatproductionatelitesiteswaseithermoreskilledor

requireddifferenttechnologiesortoolsthancraftproductionatnonelitesites.The

artifactformsproducedathighrankingandlowrankingsitesweresimilar,suggesting

245 thatproductionofmorevaluableartifactswasnotataskrestrictedtomorehighlyranked

sites.Finally,theevidencesuggeststhatwealthgoodsproductionwasanactivitythat

frequentlyoccurredwithinthecontextofdomesticstructuresorhouseholds,regardlessof

thesociopoliticalstatusofthesite.Thus,thedatasuggestasysteminwhichwealth

goodsproductionwasanactivitycarriedoutbyalllevelsofsociety,gearedtowardsthe productionofavarietyofartifactformsandinvolvingbroadlysimilartechnologiesand skills.Thequestionthen,is why thedatafromtheMiddleMotaguaValleyduringthe

LateClassicperiodappearstobesoanomalousandfailtomatchexpectationsofcurrent modelsoftheorganizationofwealthgoodsproduction.

7.3 AlternativeModelsofMMVWealthGoodsProduction

AsInotedearlier,productionisonlyonecomponentofeconomy,alongwith distributionandconsumption.Unfortunately,thedatapresentlyavailableonlyallowme toaddressproduction,becausefewcontextslinkedtotheconsumptionofjadeitewealth goodswereencounteredaspartofmyexcavations.Thereislimitedevidencefrom previousinvestigations(SmithandKidder1943),however,thatcanhelpinaddressing patternsofconsumptionintheMiddleMotaguaValley.Together,thesedatacanprovide ameanstoevaluatetwotentativemodelsoftheorganizationofwealthgoodsproduction intheMiddleMotaguaValleyduringtheLateClassicperiod,oneinformedbypolitical economyapproaches,andtheotherbydomesticeconomyapproaches.Althoughthe presentdataareinsufficientfordeterminingwhichmodelisabetterfitforthesituationin theMMVduringtheLateClassic,bothhaveexplanatorypower,butascribethe motivationorimpetusforjadeartifactproductiontoelites(politicaleconomyperspective)

246 ortotheeconomicstrategiesofhouseholds,regardlessoftheirsociopoliticalcomposition

(domesticeconomy).Inthesectionsthatfollow,Ibeginbyexaminingthedatafroma domesticeconomyperspective,beforemovingontoevaluatingthedatafromapolitical economyperspective.

7.3.1 DomesticEconomyModel

AsdiscussedinChapter1,thedomesticeconomyreferstothewayshouseholds diversifyproductionstrategiestomeettheirphysicalandsocialneeds(c.f.Hirth2009b:

1).Becausethehouseholdwasthefundamentalunitofadaptationinallpreindustrial agrariansocieties(c.f.Wilk1989;Hirth1993),thedomesticeconomyfocusesattention

onhowhouseholdsfitcraftproductionwithintheiroverallproductionstrategies.

Therefore,itdirectsinterpretationsofarchaeologicalevidenceofcraftproductiontoward

theperspectiveofthehouseholdmembersdoingthework,takinga“bottomup,”rather

than“topdown”viewofthehouseholdlevelproductionofwealthgoods.

Althoughtraditionalmodelsstressthatelitesseektocontroltheproductionof

wealthgoodstoenhancetheirsocialposition(c.f.BrumfielandEarle1987;Blantonetal.

1996),Hirth(2009b.:12)notesthat"thereisnothingtokeepnonelitehouseholdsfrom

makingwealthgoodsiftheresourcesareavailabletodoso."Asnotedearlier,theraw

materials,technologyandskillsnecessaryforjadeiteartifactproductionwerewidespread

intheMiddleMotaguaValley.Justasitistoday,rawjadeitewasanabundantly

availablelocalresourcethatcouldbeeasilyobtainedasriverfloatinthemanytributaries

oftheMotaguaRiverflowingfromthesurroundingmountains(alsoseeChapter3).

Therefore,theavailabledatasuggestthateliteandnonelitehouseholdsalikeengagedin

247 productionofgoodsfromabundantlyavailablerawmaterials,usingskillsaidedby relativelysimpletechnologies.

Thepresenceof multicrafting (seeChapter6)inadditiontojadeartifact productionattheTypeIIsiteofGuaytan4(shellbeadsandotherartifactsandstone beads)andtheTypeIIIsiteofVargasIIB(stonebeads)fitswellwithwhatwouldbe

expectedfromadomesticeconomymodelinwhichhouseholdsusedwhateverresources

wereavailabletothem.Theproductionofshellandstoneartifactsinvolvedtheuseof

thesametechnologyandskillsasjadeartifactproduction,andconstituted“intersecting

technologies”(c.f.Hirth2009b)becauselapidaryproductiontechniquesrelatedtojade

artifactscouldbeextendedtoshellandotherstones.Ifindsuchmulticrafting

inconsistentwithapoliticaleconomymodelinwhichproductionactivitywascontrolled byelites,becausewhenfoundinnonelitehouseholds,itfitsmorereadilywithina

domesticeconomymodelinwhichhouseholdsdiversifybywhatevermeansavailableto

meettheirneeds.Infact,evidenceofmulticraftingof“nonutilitarian”goodshasbeen

foundinanurbanhouseholdcompoundsatTeotihuacan(Widmer1991)andina

householdataruralvillagesiteatEjutlainClassicperiodOaxaca(Feinman1999;

FeinmanandNichols2000,2004),neitherofwhichappeartohavebeencontrolledby

elitesinanydiscernableway.

Inadomesticeconomymodel,theinvolvementofnonelitehouseholdsinthe productionofjadeitewealthgoodsmustbeexplainedintermsofhowitfitintooverall productionstrategies.TherearetwowaystoexplainthisproductionintheMiddle

MotaguaValleyfromadomesticeconomyperspective.First,wealthgoodsproduction

mayhavebeenawayofmitigatingsubsistencerisk,byprovidinghouseholdswitha

248 meanstomeettheirneedsthroughtheexchangeofvaluablegoodsforsubsistence products.Today,theMiddleMotaguaValleyreceivesanaverageannualrainfallof

550mm,anamountatthemarginofwhatisneededtosupportrainfallbasedmaize

agriculture.Thiscouldhavemadeitdifficultforhouseholdswithaccesstoless productiveagriculturallandoutsideoftheLowerLatoRiverValleytoconsistentlymeet

theirsubsistenceneeds.Theexchangeofwealthgoodsforsubsistenceproductsisone possiblewaythatcraftproductionmayhavecomplementedagriculturalactivityamong

nonelitehouseholdstomeettheoverallsubsistenceneedsofthehousehold.However,

asBayman(1999:271)notes,agriculturalproductivityandaccesstoresourcesmustbe

demonstrated,andnotsimplyassumed.Atthispoint,thisisaspeculationthatcannotbe

evaluatedwiththecurrentevidence.

AsecondpossibilityisthatMMVhouseholdsexchangedjadeitewealthgoodsfor

utilitariangoods(e.g.obsidianorobsidiantools,utilitarianceramics)orotherwealth

goods.Althoughhouseholdsaredepictedasindependent,selfsustainingentities(c.f.

Sahlins1972),theyalwaysreliedonextrahouseholdsourcesforthegoodsthattheydid

notpossessthemeansorresourcestoproducethemselves(Wolf1966).DuringtheLate

Classicperiod,distributionmechanismswerecertainlyinplacethatmovedgoodsover

significantdistances.Whilethepresenceofatrue“marketeconomy”duringtheLate

Classicisahighlydebatedtopic,itislikelythatperiodicmarketsexistedwhere

householdscouldexchangegoodsthattheyproducedwithoneanotherandforgoods

fromoutsideofthelocalregion.

ObsidianisonepossiblematerialthatMiddleMotaguaValleyhouseholdsmay

haveacquiredinexchangeforjadewealthgoods.Althoughsourcingofobsidianartifacts

249 recoveredfromsurfacecollectionsandexcavationswasnotundertakenaspartofthis dissertationresearch,theclosestlargeobsidiansourcesisElChayal,locatedover50km southwestoftheMiddleMotaguaValley.UnlikemanyotherpartsoftheMayalowlands,

obsidianwasthepredominanttoolmaterialusedintheMiddleMotaguaValley;other

thanonechertbiface,allotherformaltoolsweremadeofobsidian,andnolargechert

flakeswererecovered.IfinditunlikelythatindividualhouseholdstravelledtoElChayal

toobtaintheirownobsidian,whichleavesopenthepossibilitythattheymanyhave

acquireditinexchangeforjadegoodstheyproducedintheirownhouseholds.AtCeren,

Sheets(2000b)arguesthatmosthouseholdswereengagedintheproductionofvarious

goodsforextrahouseholdexchange,includingfortheacquisitionofexoticitemssuchas

obsidiantoolsandpolychromeservingvessels.Ifthisisindeedthecase,itwouldbe

equallylikelythatMiddleMotaguaValleyhouseholdsexchangedtheirwealthgoodsfor

exoticutilitariangoodsimportedfromelsewhere.

Onedifficultyofapplyingadomesticeconomymodeltotheexistingdataisthat thegoodsproducedbyMMVhouseholdswerewealthgoodsthatservedasmarkersof statusandprestigethroughouttheMayalowlandsandelsewhereinMesoamerica.Ifeel thatthedifficultyinconceptualizingindependent,domesticproductionofwealthgoods stemsfromtwomisconceptions.First,isthemisconceptionthatallwealthgoodshadthe same“value”ormeaningandenduse.Elaborate,highlycraftedanduniquejadeite artifactswithiconographicimagerywerecertainlyitemsthatwererestrictedintheir distributiontoelites,andmayevenhavebeencraftedaspartofsponsoredproduction arrangementsbyelites.Nevertheless,thetypesofjadeiteartifacts(particularlybeads) producedintheMiddleMotaguaValleyappeartohavepredominantlybeen“simple,”

250 “lowvalue”artifactsthatwereusedinbulkbyelitestosignifytheirstatus,butwhichare

alsorecoveredinnonelitecontextsintheMayalowlands(e.g.Zeleznik2002).

Therefore,weshouldnotassumethatalljadeiteartifactswouldhavebeenproducedby elitesorwithinelitecontexts,butratherthattheircontextsofproductionmayhavevaried inthesamemannerastheirvalue.

Secondisthemisconceptionthatjadeartifactshadthesamevalueandmeaningin theMiddleMotaguaValleyastheydidinotherpartsoftheMayalowlands,wherejade wasanexoticandrarerawmaterial.Oneproblemwithevaluatingthispropositionisthe lackofconsumptioncontextsforjadeiteartifacts.Themajorityofevidencerecovered speakstotheproductionofjadeartifacts,butprovidesverylittleevidenceofthe consumptionoffinishedartifacts.Therefore,itisnotknownwhetherproductionwas gearedtowardinternalconsumptionatallhouseholds,orwhetheronlyparticular householdswereconsumingthefinishedartifacts.AsdiscussedinChapter3,jade artifactswereprimarilywealthgoodsthatweredisplayedasornamentation,andareoften foundincludedinburialsandspecialpurposecontexts,suchascachesandtermination rituals.Thesetypesofcontextswerenotuncoveredaspartofthecurrentdissertation research.

7.3.2 PoliticalEconomyModel

Politicaleconomyreferstothewaysinwhichpoliticalelitesmanipulateaspects oftheeconomy(production,distributionorconsumption)totheiradvantage.Ina politicaleconomymodel,productionisseenasbeingdrivenbytherequirementsofelites forwealthgoodsthattheyusetobuildandextendsocialrelationshipswithotherelites

251 andforamassingdurablewealth(Hirth1996:214).Althoughmanymodelsstressthe roleofelitesindirectlycontrollingproductionofwealthgoodsduringtheLateClassic periodasameansofmaintainingexclusiveaccesstothem,theyneednotdirectly

exercisecontrolovertheentireproductionprocess.Instead,elitesmayhaveexercised

lessdirectcontrolovertheproductionofthesegoods,andinsteadreliedonmobilization

strategiessuchastributepaymentstoobtainwealthgoodsfromMMVhouseholds.

Hieroglyphictextsindicatetheroleoftributeformobilizingluxurygoodsata

numberofLateClassicsites,includingcacaoat(Houston1997;2000;Miller

1997),andpossiblyofcottonmantlesatMotuldeSanJose(Foias2002:237).

Ethnohistoricaccountsfrom16thcenturyYucatanlikewiserefertotheroleoftributein

supportingpoliticalelitesatvariouslevels,includingregionalrulers( halach uinic) and

locallords( batabs ),andincludereferencestoluxuryorwealthitems,suchasfeathers andcacao(Roys1943:61).Receivingfinishedorpartiallyfinishedjadeitewealthgoods astributefromnonelitesisonepossiblewaybywhichelitesmighthaveinfluencedthe organizationofwealthgoodsproductionintheMiddleMotaguaValley.

Theproductionofwealthgoodsbynonelitesforuseinthepoliticaleconomyby politicalelitesincontextsthatwerenotdirectlysupervisedbyelitesisdemonstratedin theethnohistoricorarchaeologicalrecordinMesoamerica(OtisCharltonetal.1993;

Berdan1994;Nichols1994;OtisCharlton1994)andelsewhere(Wattenmaker1994,

1998;Sinopoli1998;2003).Inmanyoftheseinstances,theitemsmobilizedastribute weregoodsthatwereeitherlocallyavailable,orthatutilizedskillsalreadyproducedby thosepayingtribute.DuringthePostclassicperiod,Aztectributelistsincludedwealth goods(includingjade,feathers,andfinetextiles)thatweresometimesproducedwithin

252 nonelitecontextsandmobilizedtoelitesat(Berdan1992;Gasco2003).In theMiddleMotaguaValley,jadeitewasabundantandthetypesofgoodsmanufactured likelydidnotrequireagreatdealofskilltoproduce.Thus,itispossiblethatevidenceof nonelitedomesticproductionofjadeitewealthgoodswasaresponsetoelitedemands.

7.3.3 DiscussionofDomesticandPoliticalEconomyModels

Thetwomodelsdiscussedaboveviewthesamephenomena(domesticjadeite

artifactproduction)fromtwodifferentperspectives:onebottomupandonetopdown.

Unfortunately,thepresentdataareinsufficientforfullyevaluatingwhichmodelbetter

fitsthesituationintheMiddleMotaguaValley.Inparticular,wewouldneedbetterdata

regardingtheconsumptionofjadeiteartifactsintheMiddleMotaguaValley,andno

consumptioncontextswererecoveredduringthisdissertationfieldresearch.Thus,itis

unclearhowmuchjadeiteartifactproductionwasgearedtowardinternaluseand

consumptionbyeliteandnonelitehouseholds.

Further,wemightexpectdifferencesinhouseholdassemblagesofforeignimports withinhouseholdsbetweenthetwoalternativeproductionsystemsdiscussedabove.If jadeitewealthgoodswereexchangedbynonelitesthroughindependentexchangeor trade,wemightexpecttoseehighfrequenciesofimportsinnoneliteconsumption contexts.Alternatively,ifjadeitewealthgoodsweretransferredthroughtribute mechanismstolocalelites,wemightexpecttoseesignificantdifferencesinimported wealthgoodsbetweenhouseholdseliteandnonelitehouseholds.Withoutdataon consumption,thesecorrespondingdifferencesinhouseholdartifactassemblagescannot beproperlyevaluated.

253 Ofcourse,thetwomodelsneednotbemutuallyexclusive,andjadeitewealth goodsmayhavebeenproducedaspartofthedomestic and thepoliticaleconomy.With

suchabundantlyavailablerawmaterial,householdscouldhaveproducedsomegoods

independentlyforexchange,yetstillhavebeenrequiredtoprovidesomegoodsastribute

tolocalorregionalelites.Themostcriticalelementinbeadmanufacturewouldhave

thenbeensufficienttimetogrind,drillandpolishbeads,whichwerelaborioustasks.In

thecontextofbothextendedandnuclearfamilyhouseholdshowever,sufficientlaborfor

thesetaskscouldhavebeenharnessedwithinthehousehold.Duringtheagricultural

season,childrenandhouseholdmemberstoooldtoworkinthefieldscouldhavehelped producebeads(Hagstrum2001).Additionally,duringtheagriculturaloffseason,all

householdmemberscouldhavedevotedsometimetotheseactivities(Kenoyeretal.

1991).

ItisinthecontextoftheseactivitiesthatHirth's(2009b)conceptof intermittent

crafting provesusefulforcharacterizingandunderstandingthewaysinwhichMotagua

Valleydomestichouseholdscouldhavefitjadeartifactproductionintotheiragricultural cycles.Ifweviewtheproductionofjadeiteartifactsinthismanner,itprovidesabetter explanationfortheexistingdatathanthetraditionaldichotomiesoffull/parttimeand attached/independentspecialization.Nonelitehouseholdscouldhavefitcraftactivities withintheirnormalproductioncyclesbypracticingthesecraftswhentherewastime availabletodoso.Iftheycouldexchangeorotherwisetransfertheirfinishedorsemi finishedproductstoelitesorothersforagriculturalproducethattheycouldnotproduce

(domesticeconomy),theproductionofjadeartifactsmayhavebeenonewaytomitigate riskintheeventualitythattheirownagriculturalproductionfailed.Thisisahypothesis

254 thatwillrequireagreatdealoffurtherresearch,butprovidesintriguingpossibilitiesfor explainingtheuniquesystemofwealthgoodsproductionintheMiddleMotaguaValley.

Itisalsopossiblethatcontrolofproductionwasnotthekeynodethroughwhich jadeitewealthgoodswerecontrolled.Discussingtheproductionofutilitariangoods,

Foias(2002:236)suggeststhatitwouldhavebeendifficultforelitestocontrol productionifitwasdispersedoutsideofmajorcenters.Basedontheevidencefromthis

dissertationresearch,Isuggestthatasimilardifficultywouldapplytothecontrolofjade

artifactproductionintheMiddleMotaguaValley,whichwaswidelydispersedamong

differentsitetypesinthesurveyarea.Nevertheless,thedispersalofproductionlocidoes

notprecludethepossibilitythatelitescontrolledthe distribution ofwealthgoodsthat wereproducedindependentlybyhouseholds.ArnoldandMunns(1994)arguethatinthe

ChannelIslandsinCalifornia,productionofshellbeadsusedasbothunitsofvalue(i.e. currency)anddisplaygoodswasperformedbynonelite,independentproducersusing locallyavailableresources(e.g.chertformicrodrillsandmarineshell).Whilethe productionofthesewealthgoodswasunlikelytohavebeendirectlycontrolled,elitesstill

exercisedcontroloverthedistributionofshellgoodsthroughtheirownershipofcanoes

necessaryforbringingthemtotheCaliforniamainland,wheretheycouldbeexchanged

forothergoods.Althoughthepresentdataareinsufficientfordeterminingthe

mechanismsofdistributionofjadeitewealthgoodsduringtheLateClassicperiod,itis possiblethatnonelitesproducedgoodsindependently,butdidnotcontroltheultimate

distributionofthesegoods.Despitethefactthatelitescouldhavecontrolledthe

distributionofjadeitewealthgoodsbeyondthelocalsysteminthisscenario,the

motivationforproductionstillfitswithinadomesticeconomymodelbecausehouseholds

255 wouldhaveacted independently inproducingjadeiteartifactsthatbenefitedtheminsome

way,evenifthebenefitthattheyderivedcannotbediscernedatthispoint..

Recently,Wells(2006)andothers(WellsandDavisSalazar2007a)have

introducedtheconceptof"ritualeconomy"(c.f.Spielman1998,2002)asanavenueto

examineandunderstandtheeconomicconsequencesofritualactivityinMesoamerica.

TheyarguethatmanycraftactivitiesinMesoamericansocietiesweregearedtowardthe productionofgoodsneededforritualandsocialpurposes.Inparticular,theystressthe

waythattheneedfortheseitemsdrovecraftproduction,oftenindomestichouseholds.I believethatframingtheproductionofjadeitewealthgoodsintheMiddleMotagua

Valleyintermsofritualeconomyprovidesinsightforunderstandingthestructureofthis productionsystem.AsInotedinChapter3,jadeitewealthgoodsservedavarietyof purposesforClassicMayaelitesandnonelitesalike.Goodsthatsymbolicallyand ideologicallylegitimatedtheauthorityandstatusofelites,suchaslargenecklaces, braceletsandskirtsofjadebeads,wouldhavecreatedanimpetusfortheproductionof thesegoods(seeFoias2007forasimilarargumentregardingceramicvessels).

Additionally,theuseofjadeitebeadsinnonelite,householdlevelritualactivity(e.g. householdterminationritualsortheplacementofjadeitebeadsinthemouthsofburied individuals)wouldhavefurtherincreasedthedemandforthegoods.Thisrecognition allowsustobetteridentifyandunderstandtherolethatnonelitesplayedinancientMaya politicaleconomies,althoughitdoesnothelpindifferentiatingbetweenthemodels presentedabove.

256 7.4 Conclusion

Inthischapter,IpresentedasummaryofpreviousevidenceofLateClassic wealthgoodsproductionintheMayaarea.Previousmodelshavearguedthatwealth goodsproductionwascontrolledbyelites,involveddifficulttomasterskillsor technologies,wouldhavetakenplacewithinornearelitearchitecture,andinvolved attachedspecialists.Incontrast,theevidencecollectedaspartofthisdissertationfield researchsuggeststhatjadeitewealthgoodsproductionintheMiddleMotaguaValleywas awidespreadactivity,involvingwidelyavailabletechnologiesandskills,andwas performedinbotheliteandnonelitesitesthroughoutthesurveyarea.Inrecognitionof theevidence,Isuggestedtwopossibleinterpretationsofthisdata.Adomesticeconomy modelfocusedonthemotivationsofallhouseholdsseekingtotakeadvantageoflocal economicopportunities,andengaginginjadeitewealthgoodsproductionasameansof meetingtheirownsubsistenceneeds.Alternatively,apoliticaleconomyviewswealth goodsproductionasanelitedirectedactivityinwhichnonelitehouseholdswereforced toproducesjadeitewealthgoodsforeliteuse.Althoughthecurrentdataareinsufficient fordifferentiatingbetweenthesetwoalternatives,Iarguethatitislikelythatboththe domesticandpoliticaleconomyinfluencedtheproductionofjadeitewealthgoodsinthe

MiddleMotaguaValleyintheLateClassicperiod.

257 CHAPTER8

CONCLUSIONS

Thedatapresentedinthisdissertationresearchareimportantforseveralreasons.

First,thematerialfromsurfacecollectionsandtestexcavationsrepresentsthelargest collectionofjadeiteproductionevidencerecoveredinMesoamericatodate.Second,the datasetof9,920jadeiteartifactsand435associatedtoolsprovidedtheopportunityfora detailedanalysisofthetechnologicalprocessofjadeiteartifactproduction.Todate,this technologicalanalysisrepresentsthemostcomprehensiveanddetailedanalysisofjade artifactproductioninMesoamerica.Third,thejadeiteproductionevidencewere recoveredfromarangeofeliteandnonelitesites,allowingforanevaluationofcurrent modelsofClassicperiodMayawealthgoodsproductionthatisunavailableatothersites.

Moreover,itconstitutesthemostextensiveevidenceofwealthgoodsproductioninthe

Mayaarea.Inthischapter,Isummarizethemajorfindingsofthisdissertationresearch, andtheimplicationsofthesedataforunderstandingClassicMayaeconomicorganization.

Indoingso,Ialsodiscussthelimitationsofthecurrentdataandsuggestdirectionsfor futureresearchintheMiddleMotaguaValleyandbeyond.

8.1 Technology

Oneoftheprimarygoalsofthisdissertationresearchwasareconstructionofthe technologicalprocessesofjadeiteartifactproduction.Althoughanumberofscholars havediscussedthetechniques,skillsandprocessesinvolvedintheproductionofjadeite artifacts(Kidder,JenningsandShook1946;Foshag1957;Digby1964;Proskouriakoff

1974;Walters1982;Kovacevich2006,2007),thesestudieshavebeenincompleteintwo

258 respects.First,manywerebasedontheexaminationoffinishedartifacts,ratherthanon productiondebitage.Second,thesestudieshavefailedtoexaminejadeartifact productionintechnologicaltermsandhavenotmovedbeyondatypologicaldescription

ofproductiondebitage.Thedatapresentedinthisdissertationaddressesbothofthese

issues.

Althoughsomescholarsemphasizetheskillnecessarytoproducefinelycrafted jadeobjects,theyhaveoftenbeenoverlyimpressedwiththefinishedproducts,andnot consideredthetechnologicalprocessesandstepsinvolvedbeforethefinalstagesoftheir production.AsInotedinChapter6,manyoftheearlystagesofjadeiteartifact productionaretimeconsuming,butdonotrequiremuchspecificskilltoexecute.

Gatheringofrawmaterialforproductionwouldhavebeeneasy,giventheabundanceof jadeiteavailableintheMiddleMotaguaValley.Initialshatteringinvolvedlittlemore thantheknockingoftwojaderockstogethertoproducedebitagesuitableforthe productionofbeads.Productionofotherartifactforms(suchasplaquesandearflare blanks)couldhavebeencarriedoutbyrelatively“unskilled”craftspersons,solongas sufficientrawjade,abrasivesandtoolswereavailable.Basedonthecurrentevidence, thesematerialsappeartohavebeenavailabletoallhouseholds.However,thefactthat evidenceofthefinalstagesofelaborationofmorefinelycraftedjadeiteobjectssuchas incisedartifactswasnotfoundintheMiddleMotaguaValleyissignificant.Their absencefromsurfacecollectionsandexcavationssuggeststhatsomeelaboratejadeite artifactformswerealsocraftedatsitesoutsideoftheregion,possiblyfromblankpieces manufacturedintheMiddleMotaguaValley,animplicationtowhichIreturnina moment.

259 Thetechnologicalanalysispresentedinthisdissertationincludedexaminationof over9,495jadeiteflakesfrompercussionshattering.Iexaminedeachflakeindividually aftersortingthembysizegrades,anddiscoveredthatsomeofthese“flakes”showed evidenceofgrinding,sawing,drillingandpreformingforbeads.Thisdetailedanalysisof percussiondebitageandtheidentificationofevidenceofothertechnologicalprocessin thenominalcategoryof“flakes”ledmetotwoimportantconclusions.Previousanalyses haveviewedjadeitedebitageprimarilyasawasteproductcreatedduringtheprocessof producingartifacts.Forexample,Kovacevich(2006:160)concludesthatthelarge quantityofjadedebitagerecoveredatCancuen“resultsfromthefactthatsomuch materialmustberemovedtoacquiretheperfectpieceofjadetocreateanartifact.”

Basedonmyanalyses,Iarguethatjadeitedebitagewasoften intentionally producedin

ordertoprovidematerialfortheproductionofjadebeads.Whileaseeminglywasteful

useofavaluablerawmaterial(c.f.Hirthetal.2009),percussionshatteringisefficientfor

theproductionofjadebeadsbecause:a)itallowsacraftspersontoidentifyfragmentsof

thehighestqualityintermsofcolorandlackofinclusions,andb)sawingwouldhave beenoverlytimeconsuming,consideringthefactthatjadeiteoftencontainsinternal

flawsnotvisibleonthesurface.Infutureanalysesofjadeorotherlapidaryproduction,it

willbenecessarytoconsiderdebitageasbothawasteproductfrompercussiontoremove

material,aswellas intended rawmaterialfortheproductionofsmallartifacts,including beadsandblanksformosaicinlays.

Second,andfollowingfromtheabovepoint,percussionshatteringforthe productionofjadeitebeadsmayalsohavebeenanefficienttechnologicalprocessfor

distributionofjadeitebeyondtheMiddleMotaguaValley.Iseethisaspotentially

260 workingintwoways.LapidaryartisansintheMiddleMotaguaValleymayhave

exchangednearcompleteorcompletejadeitebeadsthatcouldbeeasilytransported.

BeadsarethemostfrequentlyencounteredjadeiteartifactformintheMayaarea.For

example,ofthealmost19,000jadeiteartifactsrecoveredfromtheCenoteofSacrifice,

thegreatmajoritywerebeads.Prouskouriakoff(1974:18)notesthatmatchedbead

assemblagesarerareatMayasites,suggestingthattheyoftencirculatedsinglyorin

limitedquantitiesandnotalwaysmanufacturedforaspecificuse.Iarguethatone

explanationforthiswasthatproductionofjadebeadsintheMiddleMotaguaValleywas

fordistributiontositesthroughouttheMayaarea.Alternatively,somepercussion

debitageflakessuitableinqualityandcolorcouldhavebeenexchangedpriortopre

forming,withthefinishingofthesebeadstakingplaceatsitestowhichtheywerefinally

distributed.Ineithercase,theconstraintsoftransportingdense,bulkyandheavy bouldersorcobblesofjadeitewouldhaveencouragedtheproductionofsome

stylisticallysimpleartifactssuchasbeadsbyMiddleMotaguaValleyhouseholds.These

transportationconstraintscouldalsohaveencouragedartisanstoproducesimpleplaques

andearflaresasblanksthatcouldbeeasilytransportedandelaboratedintheirfinal

destinations.

Thetechnologicalanalysespresentedinthisdissertationalsodemonstratethe needtoconsidertheroleofmulticraftingwithdifferentrawmaterialsthroughtheuseof intersectingtechnologiesatancientMayasites.Previousstudiesofwealthgoods productionhaveoftenconsideredtheproductionofartifactsfromdifferentmaterialsas

analyticallydistinct,ratherthanexamininghowsomeofthesecraftsmaybelinked

technologically(c.f.Shimada2007:3).Incontrast,althoughthecurrentevidenceis

261 limited,lapidariesatsomesitesintheMiddleMotaguaValleyworkedotherstoneand

shell,inadditiontojadeite.ElsewhereinMesoamerica,Feinmanandcolleagues

(Feinmanetal.1993;Feinman1999)notethelapidaryproductionofshell,onyxand greenstoneornamentsandceramicfigurineswithinthesamehouseholdinClassicperiod

Ejutla,Oaxaca,allofwhichweredoneusingthesametechnology.Futureresearchinthe

MiddleMotaguaValleywillneedtoexaminetheextentofmulticraftingevidenceatsites likeVargasIIA,MagdalenaI,andGuaytan4.

Althoughthetechnologicalanalysisofjadeartifactproductionprovidedanumber ofnewinsights,italsoproducedanumberofnewresearchquestionsandareasthatfuture researchwillneedtoclarify.Onepotentiallyilluminatingavenueforfutureresearchis usewearanalysisofchertdrillsfromtheMiddleMotaguaValley.Althoughformalchert microdrillsareoftenusedtoinferthepresenceofshellworking(Yerkes1983,1991;

Arnold1987;ArnoldandMunns1994;Feinman1999),usewearanalysisbyAldenderfer etal.(1989)suggesttheuseofsomechertmicrodrillsinthePetenLakesregionfor drillingfinegrainedstonesuchasjade,apointthatismadeinthisdissertationresearch.

UsewearanalysesofchertmicrodrillsfromtheMiddleMotaguaValleymayprovide anotherdirectlineofevidenceoftheworkingofshellorjadeiteatparticularsites.

Futureresearchwillalsoneedtoincludeexperimentalreplicationstudiestobetter elucidatethetechnologicalprocessofjadeiteartifactproductionintheMiddleMotagua

Valley.Replicationstudiescouldprovideinformationaboutthetimeneededforvarious technologicalproductionprocesses,suchasgrinding,sawing,anddrilling,thusproviding ameansforevaluatingthe intensity (ameasureofthetimedevotedtoorrequiredfora particularprocess)ofartifactproduction.Experimentalreplicationcouldalsoaidinthe

262 identificationofdiagnostictypesofjadeitefragmentsassociatedwiththeproductionof particularartifactformsandstagesofartifactproduction(e.g.directvs.undirected percussion).

8.2 OrganizationofJadeiteArtifactProduction

Asecondmajorgoalofthisdissertationresearchwastoreconstructthe organizationofjadeiteartifactproductionintheMiddleMotaguaValleyandusethese datatoevaluatecurrentmodelsofwealthgoodsproduction.Followingtraditional modelsofcraftproduction(e.g.BrumfielandEarle1987),anumberofscholarshave proposedafundamentaldichotomybetweentheorganizationofutilitarianandwealth goodsfortheClassicMaya.Inthesemodels,elitesdidnotcontroltheproductionof goodssuchasutilitarianceramics(Rice1987;Ball1993;West2002)andcherttools

(KingandPotter1994;PotterandKing1995),butinsteadcontrolledandadministered theproductionofwealthgoodssuchasfinepolychromeceramics(Foias2002,2007)and itemsofadornment(Inomata2001).Indoingso,Mayanistshavegenerallycharacterized wealthgoodsproductionashighlyskilled,involvingdifficultproductionmethods,using exotic(nonlocal)rawmaterials,requiringamasteryofesotericknowledgeabout aestheticandmoralvalues,andasbeinglocatedinorneareliteresidences.

Theevidencefromthisdissertationfieldresearchdoesnotmatchthese characterizationsofwealthgoodsproductioninanumberofrespects.First,jadeartifact productionwasfocusedonrelativelysimpleartifactforms,suchasbeads,earflareblanks andplaques,ratherthanelaboratelycarvedplaques,beadsandotherornaments.Second, productiondidnotinvolvedifficulttomastertechnologiesorhighlyspecializedtools.

263 Third,productionevidencewaswidespreadandfoundatalllevelsofthelocalsite

hierarchy,suggestingthatelitesdidnotdirectlycontrolorsupervisetheproductionof jadeiteartifactsintheMiddleMotaguaValley.Thus,whilethecontrolofwealthgoods productionmayhavebeenastrategyforthemaintenanceofeliteauthorityelsewherein

theMayaarea,suchastrategydoesnotappeartohavebeenpartofthepoliticaleconomy

intheMiddleMotaguaValley.Thisfindingiscongruentwithrecentresearchthathas

soughttocharacterizethediversityofpoliticaleconomiesintheMayaarea(Massonand

Friedel2002).Futureresearchwillbedirectedtowardelucidatingthepoliticaleconomic

structureoftheMiddleMotaguaValley,includingexaminationofthedistributionof jadeiteandotherwealthgoods.

Thischaracterizationofdiffusewealthgoodsproductionissupportedby

archaeologicalresearchoutsideofMesoamericaaswell.IntheAmericanBottom,

Milner(1990;seealsoMuller1987,1997:342346)pointsoutthatchertmicrodrillsused

intheproductionofwealthgoodssuchasshellbeadsarefoundpredominanlyin

associtionwithdomesticcontexts.Importantly,althoughthereareslighlyhigher

concentrationsofdrillsatelitesites,thedrillsarefoundatalllevelsofthesitehierarchy.

Basedonthisevidence,theyconcludethattheproductionofshellbeadswasanactivity

inwhichhouseholdsatalllevelsofMississippiansocietywereinvolved,andwasnotan

elitedominatedorelitedirectedactivity.Bayman(2002)arguesforasimilarlydiffuse

systemproductionofvariousmarineshellornamentsamongtheinthe

AmericanSouthwest.

Thisresearchhasalsoshownthatjadeiteartifactproductionwasanactivitythat

tookplacewithindomesticcontexts.Regardlessofwhetherthedistributionofjade

264 artifactswascontrolledbythehouseholdsthemselvesorbylocalelites,thissuggeststhat

wealthgoodsproductionwasanactivitythatfitwithinthenormaldomesticcycleof

MiddleMotaguaValleyhouseholds,asitwaselsewhereinMesoamerica(Feinman1999;

FeinmanandNichols2000).Thehouseholdwasthepriomaryunitofcraftproduction

throughoutprehispanicMesoamerica.AsHirth(2009)argues,thepositionofcraft productionasasupplementalandintermittentactivitywithindiversifiedhousehold

economicstrategiesneedsmoreattentioninfutureanalysesofprehispanicMesoamerican economicsystems.Thisisdoublysofortheroleoftheproductionofnonutilitarian goodswithintheMayaarea,whereevidenceofproductionofsuchgoodsinnonelite domesticcontextsisoftenleftunexplained.

Arelatedimplicationofthisdissertationresearchisthatnotalljadewealthgoods were“valued”equally.Amajorobstacletounderstandingtheprehispanicorganization ofwealthgoodsproductionintheMayaareaistheimplicitassumptionthatallwealth goodsservedthesamepurposes,andtherefore,theirpatternsofproduction,distribution andconsumptionweresimilar.AsIdiscussedinChapter3,jadeitewealthgoodswere craftedintoavarietyofartifactforms,andalthoughtheyarefoundpredominantlyinelite contextsduringtheLateClassicperiod,jadeiteartifactsaresometimesrecoveredinnon elitecontexts.AsZeleznik(2002:18)notesforLateClassicperiodCopan,“many individualswereburiedwithonejadebead,butitwastherareindividualwhowasfound withanentirejadenecklace.”Thus,asChaseandChase(1992)note,thereisaneedto distinguishbetweenjadeartifactsthatservedaswealthgoodsmoregenerallyavailableto mostmemberofsociety(i.e.singleorsmallnumbersofbeads)andthosethatmore limitedtoelites.Therefore,scholarsshouldbecarefulwhendiscussingwealthgoodsasa

265 single,monolithicanalyticcategory(seeBayman2002forasimilaragumentat

Hohokamsites).

Another,relatedimplicationofthisdissertationresearchisthatscholarsneedto considertherolethatindependentspecialistsplayedintheproductionofwealthgoodsin theMayaarea.Discussionsoftheproductionofwealthgoodshaveoftenfocusedonthe roleof“palaceartisans”thatwereattachedtotheroyalcourtsatMayacenters(Ball1993;

ReentsBudet1994,1998;Inomata2001;InomataandHouston2001;Folanetal.2001;

McAnany2004).Whilesuchhighlyskilledartisanscertainlyperformedacentralrolein theproductionoftheelaborateregaliaofhighrankingelites,Iarguethattheywere unlikelytohavebeenabletomeetalloftheneedsofelites(bothroyalandsubroyal)in

ClassicMayapolities.Thisisespeciallythecaseif,asInomata(2001)argues,some artisanswereelites.Consider,forexample,theobservationmadebyZelezniknoted above;ifahighrankingeliterequiredalongstrandofjadebeads,wouldthesehavebeen producedbyalimitedcadreofpalaceartisans?Thetimerequiredforgrinding,drilling andpolishingbeadswouldlikelyhavebeenburdensomeifpalaceartisanswereneededto producebothforinternaleliteconsumptionandfordistributiontononelitesaswell.

Moreover,necklacesofjadebeadsarerarelyconsistofmatchedsets;insteadthebeads usuallyvaryinqualityandcraftsmanship.Suchdiversesetsofjadeitebeadsindicatethat multipleartisansproducedsuchitems,andtheyexhibitedvaryingdegreesof

“attachment”toClassicMayaelites.Therefore,IarguethatfuturemodelsofClassic

Mayaeconomicorganizationshouldnotdiscountthepossibleroleofindependent craftspersonsintheproductionofwealthgoods.

266 AsHirth(1996)notes,elitesusewhatevermixofstrategiesavailabletothemto maintainandexpandtheirpositionwithinsociety.Thisdissertationresearch demonstratesthatscholarsneedtoidentifytheparticularmixofstrategiesthatelites employedatparticularClassicMayasites,whichlikelyvariedwithavailableresources.

However,eveninlightofthisvariation,weneedtorecognizethatnotallproductionor distributionwaslikelytohavebeenunderthecontrolofelites.DuringtheColonial period,Spanishconquistadorsusedavarietyoftributeandexchangenetworksto mobilizeresourcesintheMayaareaandthroughoutMesoamerica,manyofwhichwere builtoffpreexistinginstitutuions(Feldman1971).Forexample,intheYucatan,Maya

communitiespaidtaxestotheSpanishintheformofwovencotton mantas ,whichwere producedwithinhouseholdsbywomen(Restall1997:184188).

ItislikelythatClassicperiodelitesalsousedmultipleexchangeanddistribution

networkstomeettheirneeds,asdidotherprehispanicMesoamericanelites.Forexample,

Aztecofficialsmettheirneedsforavarietyofwealthandutilitariangoodsthrough

serviceandmobilizationstrategies(BerdanandAnawalt1992)andthroughmanipuation

ofmarketsthroughouttheempire(Hassig1985).Conqueredprovincesweremadetopay

tributeintheformoflocallyavailableproducts,includingwoventextiles,whichsuggest

thatsystemsforextractionofthesegoodswasalreadyinplacebeforetheimpositionof

tributedemands(Smith1994:334336;Berdan1996:124129).Encouragingcraft productionatthehouseholdandcommunitylevelcouldhavebenefittedprehispanicelites

inanumberofways.Itenabledthemtomoreeasilyextractasurplusofthegoodsthat

specializedhouseholdswerealreadyproducing.Further,byrequiringproductionwithin

thehousehold,rathernthansponsoringitdirectly,thecostsofproductionwereshifted

267 fromeliteandontothehouseholditself(Hassig1985:226227).Understandingthe

varietyofwaysresourcesweremobilizediscrucialifwearetoaccuratelyreconstruct

ClassicMayasystemsofcraftproduction,politicalanddomesticeconomy.This

dissertationresearchdemonstratesthattraditionalmodelsofClassicMayacraft productionareincompleteandhavepaidinsufficientattentiontotheroleofnonelite, independenthouseholdsintheorganziationofwealthgoodsproduction.

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307 APPENDIXA PJ05SURFACESURVEYDATA Thisappendixcontainsdescriptionsofsitesidentifiedaspartofthisdissertation research.Thesitesarelistedherefromeasttowestforeaseofcomparisonbetweenthe descriptionsandthelocationofthesitesinFigureA.1. FigureA.1LowerLatoValleysurveyarea.

308 LosChaguites02 (TypeIII) Thesiteconsistsoffourstructuresaroundasmallplazaontheedgeofaterrace overlookingtheMotaguaRiver,whichislocatedtothesouth.Structure1isalong,two levelstructuremeasuring16mX7m,andisapproximately1mtall.Alooter'strenchhas penetratedandclearedatombonthewesternendofthestructure;therearethreeother looter'sholesinthetopofthestructure,oneofwhichmayalsohavepenetratedatomb. Str.1appearstohavecontainedtwoorthreesuperstructurerooms.Tothewest/southwest ofStr.1isStructure2,anotherstructuremeasuring14mX4mandapproximately1.0m inheight.Alooter'strenchintothewesternendofStr.2alsopenetratedatomb;there aretwoothersmalllooter'sholesinthetopofthesuperstructure.Str.2appearstohave beentoppedbytworooms.TothesoutheastofStr.2isStructure3,asmallrectangular structure(approximately4mX3m)about0.50minheight.Thereisalargelooter'shole inthestructure.TothesoutheastofStr.3isStructure4,asmallrectangularstructure orientedtomagneticnorth,measures5mX3m,andisapproximately1minheight.Str.4 hasthreedifferentsmalllooter'sholes,noneofwhichexposedanysuperstructure. Collectionsofjadeartifactsweremadetothe LosChaguites01 (TypeII) LosChaguites01isasmallsitelocatedtothewest/southwestofLC02.Thesiteconsists ofthreestructuresonthenorthernendofaterraceoverlookingtheMotaguaRiver. Structure1isapproximately1mtallandmeasures5mX5m.TothesouthofStructure1, theriverterracejutsouttoformalarge,flatareathatisapproximately60mx75m,where wesurfacecollectedalargeamountofjadeworkshopdebitage,obsidianartifactsand ceramicsherds.Approximately10meterstothenorthofStructure1areStructures2and 3,bothsmall(height≈0.50m)platformsof3mX3meach.Everystructureatthesite hasatleastonelooter'strench. KM93IV (TypeIII?) WewereonlyabletovisitsiteKM93IVbrieflybeforewewereaskedtoleavebythe landowner.KM93IVislocatedbetweenKM93IIIandLC01,andisseparatedfrom bothsitesbyquebradas.Thesiteconsistsoffourstructuresorientedaroundasmallplaza. ThesiteisalongaterraceoverlookingtheMotaguaRiver.Twostructuresinthenorthern partofthegrouparevaultedfunerarymonumentsmeasuringtwometersinheight;oneof thestructurescontainsalootedtomb.Thesouthernsideofthegroupisboundedbya long,multiroomedstructure,about1minheight.Surfacecollectionsatthissitewere madefromthelevelextensionoftheriverterracetothesouthofthemultiroomed structure.Thegroupisboundedontheeasternsidebyasmall,1mtallplatformstructure. KM93III (TypeI) SiteKM93IIIislocatedtotheeastofKM93II,separatedbyawidequebrada.Thesite spreadsoutacrossawidepartoftheriverterraceoverlookingtheMotaguaRiverandis accessedbyanarrowpartoftheterracefromthenorth.KM93IIIisanonmoundedsite

309 withnosurfaceevidenceofplatformsormounds;surfacecollectionsincludedjadeflakes andotherproductiondebris,obsidian,ceramicsandchertdrills. KM93II (TypeII) SiteKM93IIisseparatedfromKM93IIItothewestandKM93IItotheeastbysmall quebradasandislocatedonanarrowriverterraceoverlookingtheMotagua.Onlythe remainsoftwosmallmoundsoflessthan0.30minheightarestillinevidenceatthesite. ThesiteisunderthesameintensivesabilacultivationasKM93Ianditappearsthatmany ofthestructuresthatwerepartofthissiteweredestroyedintheprocessofpreparingthe fieldforcultivation.Smallcollectionsofjadedebitageandceramicsweremadeatthe site,butwerenotincludedinthecurrentanalysisbecausethebagscontainingthese collectionswerelostduringthecourseofthefieldseason. KM93I“TerzuolaSite” (TypeII) SiteKM93IisbisectedbytheCA9highway,andcontainsstructurestothenorthand southofthehighway.ThesitewasfirstdescribedbyFeldman,etal.(1975)andnamed theTerzuolasite.Currently,thesiteisunderintensesabilacultivation,makingsurface collectionsandaccuratemappingverydifficult.Furthermore,manyofthestructuresin theareaofthesitelocatedtothesouthoftheCA9werecompletelydestroyedwhenthe areawasleveledforcultivationandwhenahouseandpoolwerebuiltonthesouthern edgeofthesite.Currently,thereareonlythreemoundsstillvisibleonthesouthern sectorofthesiteandtwomoundsnorthoftheCA9.Twoofthemoundsinthesouthern sectorare1mtallmoundsthatareapproximately7mX7m. Despitelimitedgroundvisibility,intensivesurfacecollectionsweremadeacrossthe entiresouthernsectorofthesite,althoughnotinassociationwithanystructures. Materialscollectedincludedalargenumberofjadeartifacts,obsidianflakesandblades, andceramics.Themajorityofmaterialwascollectedfromthesouthernandwestern edgesoftheterraceonwhichthesiteislocated.AlthoughWalters(1982)mentionedthe presenceofajadeworkshopinthenortheasternpartofthesouthernsectorofthesite,we foundnosurfaceevidenceofthisworkshopduringoursurvey. KM92III (TypeIII?) Walters(1982)describedsiteKM92IIIasthemostthoroughlydestroyedsitethathe encounteredintheMiddleMotaguaValleysurveyzoneandthisassessmentis unfortunatelycorrect.LocatedonariverterracetothewestofsiteKM93I(thetwoare separatedbyawidequebrada),theentireeasternsectorofthesitewasdestroyedwhen stoneandsoilfromthesitewereremovedtobuildtheroadbedfortheCA9.Onlytwo structuresremainatthesite:partofabasalplatform(6mX1m)atthesouthernedgeof theborrowpit,andasmall,lowplatformstructure(2.5mX4m,orientation:185º)tothe eastoftheborrowpit.Theeasternstructuremaycontainalootedtombchamber,butthis wascoveredwithcollapsedrubbleandthickvegetation.Surfacecollectionsweremade fromtheareastotheeast,southandsoutheastoftheborrowpit.

310 Approximatelytwentymeterstothewest/northwestofthewesternedgeoftheborrowpit, isasmallplatformmound(height=1.5m;area=5mX3m),withpossiblesuperstructure walls.Thestructurehastwolargelooters'trenches.Densevegetationanddisturbance madesurfacecollectiondifficult,butwedidcollectsomeobsidianandjadeflakestothe immediatesouthofthestructure. Anothertwentymeterstothewestisagroupoffivestructures,looselygroupedtogether, situatedclosetotheedgeofaterraceoverlookingtheMotaguaRivertothesouth,20m below.Structure1isavaultedfunerarymonument,measuring5.5mX4m,with1.5m tallstandingwalls.Thewesternandsouthernwallsofthestructurehavebeenexposed bylooters'trenches.Thelooter'strenchonthesouthernfacestructurehasexposedtwo tombchambers,whilealooter'strenchatopthecenterofthestructurealsoappearsto havepenetratedatombchamber.Looter'strenchesarealsoevidentontheeasternand northernfacesofthemound.Tothesouth/southwestofStr.1isStructure2,alarge structurethatwassoovergrownastobeimpossibletofullyexamine.Structure2is approximately10mX10mand2minheight,andhasbeenpenetratedbymultiplelooters' trenches.TothewestofStr.2isStructure3,asmalllootedplatform(lessthan1mhigh), measuringapproximately3mX4m.TothesouthwestofStr.3isStructure4,amultiple roomedstructureorientedtomagneticnorth.Structure4isapproximately8mX6m.A looter'strenchhasexposedaneastfacingentrytooneoftheroomsthatmeasures approximately0.90minwidth.Structure5islocatedimmediatelyeastofStr.2.Itisa long,linearmultiroomedstructuremeasuring10mX5m,withitslongaxisoriented towardsmagneticnorth.Multiplelooters'trenchesshowthestructuretohavelowwalls (approximately0.50mtall)thatlikelysupportedaperishablesuperstructure. Surfacecollectionsweretakenacrosstheentiresite,thoughthegreatestconcentrationsof materialoccurredalongthesouthernandeasternperimetersofthesite. KM92II (TypeII) SiteKM92IImaycorrespondtoWalters'(1982)KM92II,butitisdifficulttotell becauseofthevaguedescriptionofthesite.ThesiteislocatedtothewestofKM92III; thetwositesareseparatedbyasmallquebrada.Thesiteconsistsofagroupof3 structuresarrangedaroundasmallopenarea.Allofthemoundsaresmallplatforms,less that0.50mtallandallmeasuringlessthan3mX3minarea.Eachstructurehadalarge, shallowlooter'sholeinthemiddle.Verylittleculturalmaterialwasobservedin associationwiththesestructures. Immediatelysouthofthisgroup,thenaturalriverterraceextendsapproximately50tothe south.Onthisterracewemadecollectionsofjadedebitage,ceramicsandobsidian acrossthewholearea.Anumberoflooter'strenchesinthesoutheastportionofthe naturalterracerevealedburiedarchitecturenotvisibleonthesurface,includinglowwalls (about0.30mhigh).

311 KM92I (TypeIII) SiteKM92IislocatedtothewestofKM92I.Thetwositesareseparatedbyasmall quebrada.Thesiteincludesanumberofsmallresidentialterraceplatformsrunningeast westalongtheslopesoverlookingtheMotaguaRiver.Weencounteredfourstructures, nonetallerthan2m;allofthesestructureshavebeenseverelylooted.Heavydisturbance bylooters,thickvegetationandtheuseofpartofthesiteasalocalgarbagedump preventedusfrommakingadequatesurfacecollectionsfromthissite.Nevertheless,one ofthestructuresappearstohavemultipleinternalsuperstructurewallsthathavebeen partiallydestroyed,whichisthereasonfordesignatingitasaTypeIIIsite. KM91IV (TypeIII) SiteKM91IVislocateda150meterssouthoftheCA9,alongtheedgeoftheriver terraceoverlookingtheMotaguaRiverandistothewestofKM92I.Thetwositesare separatedbyawidequebrada.TheareanorthofthesitebetweenthesiteandtheCA9 hasbeencompletelyleveledforcultivationandanystructureshavelongsince beendestroyed. SiteKM91IVconsistsofninestructuresarrangedintwogroups.Theeasterngroup, Group1,containsthreestructures:twostructuresonthenorthandoneonthesouth.Itis possiblethatthesestructuresweregroupedaroundacentralplazaarea,butthearea betweenthenorthernandsouthernstructureshasbeenleveledbybulldozerfor cultivation,sothiscannotbesaidwithconfidence.Structure1isa6mX9mstructure, about2minheight.Looter'strenchesintothecoreandsidesofthemoundrevealthatStr. 1isorientedNorthSouthandcontainedlowwalls.Structure2,locatedimmediatelyto thewestofStr.1isasmall6mX5mrectangularstructure,about1minheight,which alsosupportedlowwallswhichappeartohavedividedthesuperstructureintotworooms. ThelongaxisofStr.2isorientedEastWest,anditispossiblethatStructures1and2 bothrestonalong,linearplatformsubstructure,thoughthedestructionfromthefield levelingmakethispossibilitydifficulttoassessfromthesurfaceremains.Approximately 17meterstothesouthofStr.1isStructure3,whichisa5mX4mmultipleroomed structure,about2minheight.Onthesouthernfaceofthestructure,oneofthemultiple looters'trenchesintothestructureappearstohavepenetratedatombchamber. Tothewest/southwestofGroup1isGroup2,agroupofsixstructures(2tothesouth,4 tothenorth)orientedaroundwhatmayhavebeenacentralplaza.Whetheraplaza existedisdifficulttodeterminebecauseoftheuseabulldozertolevelthecentralareafor cultivation.Structure4andStructure6arelocatedonthesouthernsideofthegroup. Structure4appearstobeasmall,vaultedfunerarymonument.Str.4is7mX5mandis approximately2mtall.Thestructurehasbeenheavilylooted.Tombchambersonthe southernandwesternfacesofthestructurehavebeenpenetratedbylooters.Structure6 islocatedtothewest/southwestofStr.4andisalowplatformmound,about0.50min height.TothenorthofStr.4isStructure5,alow(0.50m)5mX3mrectangular platformstructure.Tothenorth/northwestofStr.5isStructure7,alarge,multiroomed

312 structure,about1minheight.Str.7hasbeenextensivelylooted,butportionsofthelow wallsofthesuperstructurearestillevident.TothewestofStr.7isStructure8,alow (0.50mtall)7mX3mrectangularplatform.TothesouthwestofStr.8isStructure9, whichhasbeenverybadlylooted.Str.9appearstohavebeenarectangularstructure, likely2minheight,measuringapproximately6mX6minarea. Anumberoflooter'strenchesintothesurfaceoftheterracetothesouthofGroup2have uncoveredremnantsofburiedarchitecturethatarenotevidentonthesurface.Therefore, noneofthisareacouldbemappedotherthantonotethepresenceofburiedarchitecture. Surfacecollectionsweremadeacrossthewholesiteandincludedjadeitedebitage, ceramics,andobsidian. KM91III (TypeIII) SiteKM91IIIwasbythesamelevelingfortobaccocultivationthatwasdescribedfor KM91IV.Thesiteislocatedonthesouthernedgeoftheriverterraceoverlookingthe Motagua,tothesouthofthelargeleveledfield.Thesiteisdividedintothreesectors, eachseparatedbylevelingassociatedwithfielepreparation. TheeasternmostportionofKM91IIIconsistssolelyofalargescatterofculturalmaterial onthegroundsurface30meterstotheeastofgroupofstructuresatthesite.This moundlesspartofthesiteisseparatedfromthecentralportionofthesitebya5mwide sectionofearth0.50cmdeeperthatwascreatedwhentheareawasleveledforcultivation. Noartifactswereobservedinthisdeepersection. Thecentralportionofsiteisasmallgroupofstructuresthathavebeenveryextensively looted.Thesiteconsistsofsevenstructuresintwoparallelrows,runningroughlyeastto west.Thecentralportionofthesitehasanumberofdeepfurrowsthatwerelikely excavatedbythelandownersforinstallingwaterpipes.Thewesternperipheryofthe centralportionofthesitewasdestroyedtoconstructafeedcorralforcattle.Onthe easternendofthecentralgroupisalow(0.50mtall)rectangularstructure,measuring about2mX3m.Alooterstrenchintothisstructurehaspenetratedatombchamber.The largeststructureinthegroupisthecentralstructureonthenorthernsideofthegroup. Thestructureisa2mtallstructurewithwallsconstructedofschistslabs.Oneofthe numerouslooters'trenchesinthisstructurepenetratedatombchamberonthewestern sideofthestructure.Theentirecentralportionofthestructurehasbeendestroyedbya 1mwidelooter'strench.Theotherfourstructuresallappeartobelowplatformsmounds. Stillfurthertothewestisthewesterngroupofthesite,locatedapproximately70kmto thewestofthecentralportionofSiteKM91III;despitethisdistance,jade,obsidianand ceramiccollectionsweremadecontinuouslybetweenthetwoportionsofthesiteandthus itwasdesignatedasbeingpartofKM91III.Currently,thewesterngroupsiteisbeing usedforgrazinggoatsandanumberofsmallditcheshavebeenexcavatedthroughoutthe sitefortheinstallationofwaterpipes.Thewesterngroupconsistoffivestructureshave beenheavilylooted.Two1mtallvaultedfunerarystructurescontainlooter'strenches

313 thathavepenetratedtombchambers.Surfacecollectionsincludingjadedebitage, obsidianandceramicsweremadeacrossthesite. KM91II (TypeIV) SiteKM91IIisseparatedfromKM91IIIbyasmallquebrada,andislocatedtothesouth ofasoccerfield;partofthesitewasdestroyedtoconstructthesoccerfield.Thesitehas beenheavilylootedanddisturbedbytrashdumping.Thereareatotalof15structuresin all.Almostallofthestructuresareplatformsoflessthat1minheight.Thereisone largemoundonthesouthernperimeterofthesitethatisover4mtallandcontainsa lootedtombatthebaseofitswesternside.Threetombchamberswereobservedinsome ofthelooters'trenchesintheotherstructures.Looter'strenchesinthelevelareaofthe terracetothesouthofthesurfacearchitecturerevealedthepresenceofsomedeeply buriedarchitecturethatwasnotvisibleonthesurface.Surfacecollectionsofjade, ceramicsandobsidianweretakenacrosstheentiresite. VargasI (TypeV) ThesiteofVargasIconsistsoftwostructuregroupsandaballcourt.Thewestern structuregrouphasbeenbadlydestroyedbylootingandcoconutcultivation;becauseof thisdestructionwecouldnottakemeasurementsofthestructures.Inall,itappearsthat therewerethreestructuresinthegroup.Theeasterngroupislocatedjusttothesouthof theroadcutfortheCA9andmuchofthesitewaslikelydestroyedduringthe constructionofthehighway.Smallcollectionsofceramics,jadedebitageandobsidian weremadeatthesite. Totheeastofthewesternstructuregroupisaballcourt,orientedNorthSouth;duetothe densevegetationinthearea,noprecisemeasurementsoftheballcourtweretaken. Approximatelyonehundredmeterstotheeastoftheballcourtisanotherstructuregroup thatislocatedonthefloodplainoftheRioLato.Thegroupconsistsofthreestructures, allover2mtall.Allhavebeenheavilydestroyedbylootersandappeartohavebeen multiroomedstructures.Thepartialremainsofanumberofstructuresdestroyedby cultivationwerenotedbetweentheeasternandwesterngroups.Nosurfacecollections fromthewesterngrouportheinterveningareaweretakenbecauseofpoorvisibilityfrom therecentcultivation. VargasIIA (TypeV) VargasIIAislocatedonaseriesofriverterracesoverlookingtheRioLatototheeast andtheRioMotaguatothesouth/southeast.Becauseoftheextensivelootingand destructionofthesite,itishardtoestimateitssizeorthenumberofstructures. Nevertheless,thesiteappearstoconsistsofatleasttwostructuregroups,onenorthern andonesouthern.

314 Thenortherngroupconsistsofalargestructureonthesouthernsideofthegroupthatis builtintothenaturallyslopingterrain,aswellasalowplatformmound(0.10minheight) onapossibleartificialterracetothenorth.Thelargesouthernstructurehasbeenalmost completelydestroyedbylooters,whohaveexcavatedalargeLshapedtrenchintothe structurethatisapproximately12mlongX7mwideX6mdeep.Overall,thestructureis approximately17mX10mandisorientedtomagneticnorth.Weobservedpossible steppedterraceretainingwallsontheeasternslopeofthecerroonwhichtheterrace behindthestructuresits.Surfacecollectionsfromthenortherngroupconsistedofagreat dealofjadedebitage(includingfinishedandunfinishedjadebeads),obsidian,and ceramics. Tothesouthofthisgroupisasmalllevelareathatwaslikelyacentralplazaontowhich thenorthernstructurefaced.Approximately50msouthofthenortherngroupisa2mtall moundwhichhasbeenheavilylootedandpartiallydestroyedbyriveractionand construction.Theremainderofthesoutherngrouphasbeensothoroughlydestroyedby lootingandconstructionactivitythatstructurecountsandmeasurementswereimpossible tomake;muchofthedamageappearstohavebeendonebybulldozersandbackhoes. Nevertheless,wedidobservethestratigraphicprofileofapartiallydestroyedplatform thatshowedatleastfourreconstructionepisodes.Artifactcollectionsweremadefrom throughoutthesite,mainlyfromlooter'strenchesandbackdirt. VargasIIB (TypeIII) VargasIIBconsistsoftwelvestructureslooselyorganizedintotwogroupsalongthe easternslopesofacerrooverlookingtheMotaguaRivertothesouthandtheRioLatoto theeast.Group1consistsofsixstructureslocatedonanaturalterracethatjutsout40º eastandisboundedbysteepslopestothenorthandtothesoutheast.Structures1thru4 arelow(lessthan0.50mtall),smallsquareplatformstructuresorganizedaroundasmall centralpatio.Allofthestructuresareofapproximatelyequalsize(5mX5m)andhave beenbadlydisturbedbymultiplelooters'pits.Structure1isonthewestsideofgroup, Structure2isonthenorth,Structure3isontheeastandStructure4isonthesouth.Only Str.2showsanyevidenceinthelooter'strenchesofhavingcontainedlowwalls. ApproximatelytenmeterstothesouthofStr.4isStructure5,a0.50mhighsquare(5mX 5m)platformstructurewithalargelooter'shole.Structure6islocatedtothetwenty meterstothesouthofStr.5andappearstobearectangular(10mX5m)structure.Str.6 hasbeenheavilylootedandiscurrentlycoveredbyalargetreewhichhasfallendirectly overthestructure.Collectionsofjadedebitage,obsidianandceramicsweremadefrom acrossthegroupanddowntheeasternslopesofGroup1. GroupIIconsistsofaseriesof6platformstructuresalongaroughlynorthsouthline,all builtintotheeasternslopesofthecerro.Allofthestructureshavebeenlootedand thoroughlydestroyed.Allofthestructuresexceptoneappeartohavecontainedtomb chambersthatwerelooted.Thetwosouthernmoststructurescontaintombsthatappearto havebeenlootedwithinthelastyear.

315 VargasIII (TypeIII) ThesiteofVargasIII(Fig.4.7)containstwogroupsofstructures.Inthenorthernportion ofthesite,12structuresrungenerallyeastwestalonggentleslopes;onlyonegroupof fivestructuresformedpartofatypicalMayaplazagroup.Themajorityofthestructures inthenorthernsectorare1mtallplatformterracesbuiltintogentlyslopingterrain;there arealsotwovaultedfunerarymonumentslessthan2mtall(bothwithlootedtombs). Threeadditionalgroupsoflowplatformstructures(twotothreestructurespergroup, ninestructuresinall)arelocated20metersfurthersouthwest,closertotheriver;nomap wasmadeofthesitebecauseoftimeconstraints. Littlejadeiteproductionevidencewasfoundwithinthecentralportionornorthern perimeterofthenorthernportionofthesite.Themajorityofproductiondebitageand associatedproductiontools(i.e.chertdrills)werefoundscatteredaroundthesmallest platformstructuresatthesite.Thesestructuresarelocatedonthewesternand southwesternperimeterofthenorthernportionofthesite;theirfunctionisdifficultto assesscurrently,butthestructuresformasmallpatiogroupoffourstructureslocated 20mawayfromtheneareststructuregroup. VargasIIIA (TypeII) VargasIIIAislocatedtothesouthwestofVargasIII;thetwositesareseparatedbya smallquebrada.Thesiteconsistsofthreesmall,low(lessthan0.50mtall)square platformstructures.Smallamountsofjade,obsidianandceramicswerecollectedatthe site. VargasIV (TypeIV) VargasIVislocatedtothesouth/southwestofVargasIIIA;thesitesareseparatedbya smallquebrada.TheeasternportionofVargasIVconsistsofagroupoffourstructures organizedaroundasmallpatio,situatedonasmallbluffbetweentwosmallquebradas. Allfourstructuresinthegrouphavebeenlooted.Theeasternstructureinthegroup,a small(lessthan1mtall)squarestructurecontainsalootedtombchamber.Theremaining threestructuresaresmallsquareplatformmounds.Extendingtowestofthiseastern groupareseriesofabout20structuresorganizedintofourtofivegroups.Themajorityof themoundsatthesitearelowmounds,butthereareatleastfourlarger,2mtallmounds. Verylittleculturalmaterialwasevidentacrossthesite,andthemajorityofjadedebitage wascollectedfromareasthatwerenotindirectassociationwithmounds,especially alongthewesternedgeofthesite. MagdalenaI (TypeV) ThesiteofMagdalenaIisthenorthernmostgroupofelitestructuresthatform partofthesiteofMagdalena.Walters(1982)describedthreeportionsofthe Magdalenasite:MagdalenaIII(south),MagdalenaII(central)andMagdalenaI

316 (north).MagdalenaIIIhasbeendestroyedasthetownofMagdalenahasexpanded;the othertwositesarestillrelativelyintact. MagdalenaIislocatedtothewestoftheMagdalenaSanAgustínAcasaguastlán road,onanaturalbluff10metersabovetheroadsurface.Overall,thesiteconsistsof morethan25structuressituatedbetweentheroadandtheRíoLato,boundedtothesouth byasmallquebrada.Allofthestructureshavebeenheavilylooted,someasrecentlyas thelasttwoyearsaccordingtolocalresidentsandlandowners.Wewereunableto exploretheentiresiteindepthbecauseitislocatedonthepropertyofmorethanone landowner.Theeasternportionofthesiteconsistsofeightstructures,someofwhichare situatedonalargeartificialplatformbuiltintothenaturallyslopingterrain. Structure1isalowplatformstructure,measuring5mx4m,orientedEW. Structure2,tothesouthofStr.1isanotherlow,small(3mx3m)platformstructure.A looter'strenchintothecenterofStr.2revealedwhatappearstobeanarrow,cutstone linedchultún.DirectlybehindandtothewestofStr.2isStructure3,thelargeststructure intheeasterngroup,isa2mtall,rectangular(8mx6m)multiroomedstructurewith 1.5mtallstandingwallsrevealedbylooters'trenches.TothenortheastofStr.3is Structure4,aheavilylootedrectangularstructure,approximately4mx6m.Structure5is located11mtothesouthanddownslopeofStr.2.Structure5isalow(lessthan1mtall) square(5mx5m)structurewhichalooter'strenchhasrevealedcontainedaslablined tombchamber.ImmediatelytothesouthwestofStr.5isStructure6,arectangular(5mx 7m)structurewhichalooter'strenchhasrevealedtocontaincurvinginteriorwalls. ConcentrationsofjadedebitagewerefoundinassociationwithStructures1,2and 3.TothenorthwestofStructure4isaseriesoflowplatformstructuresorganizedinto smalltwotothreestructuregroups.Thelargeststructureinthisareaofthesiteisa2m tallvaultedfunerarymonument,measuring9mx8m.Themoundhasbeenverybadly looted.AspartofOperation5D,wescreenedtenbucketsofbackdirtfromthelooters' trenches;thematerialincludedhumanteethexhibitingdentalmutilationandjadeinlays, indicatingthatthelootershadlikelypenetratedatombwithinthestructure.Tothewest oftheeasternareaofthesiteisanopenplazaboundedtothewestandeastbytwolong multiroomedstructures. Furthertothewestofthesestructuresisasmallgroupoftwotothreestructures, allheavilylooted.Thewesternmoststructureinthisgroup,whichissituatedattheedge ofthenaturalriverterrace,containsalooter'strenchwhichrevealedthatitisconstructed ofcutstoneblocks,withapproximately0.90mtallwalls.Heavyconcentrationsofjade debitageandassociatedtoolswerefoundassociatedwiththewesternportionofthis groupandfurtherdownslope.Anumberofotherstructuregroupswereobservedduring abriefspotcheckaroundtherestofthesite,includingtwogroupsthatcontained2mtall vaultedfunerarymonuments;thesestructureswereinareasthatwerenotgiven permissiontoenter MagdalenaII (TypeIII) MagdalenaIIislocatedtothesouthofMagdalenaI;thetwositesareseparatedbya quebrada.LikeMagdalenaI,MagdalenaIIissituatedbetweentheMagdalenaSan AgustínAcasaguastlánroadontheeastandtheRíoLatotothewest.Thesouthernmost portionofthesitehasbeendestroyedbyrecentconstruction.

317 MagdalenaIIconsistsoflow,multiroomedstructures,vaultedfunerarymonumentsless than2mtallandanumberof1mtallmounds.Inall,thereareapproximately15structures atMagdalenaII,althoughthismaybeanunderestimatebecausewewerenotallowed ontothelandthatcontainsthesouthernmostpartofthesite.Thestructuresarearranged insmallformalgroups,thoughlootingthroughoutthesitemakesitdifficulttodetermine thedimensionsandorientationsofmanyofthestructures.Walters(1982)notedthe presenceofajadeworkshoponthewesternperimeterofthesite.Athorough examinationofthisareayieldedverylittlejadeproductiondebitage;itislikelythatthis evidencewaseitherlocatedinasincedestroyedpartofthesiteorwasnotasabundantas Waltersnoted. ElTerronSouth (TypeIV) ThesiteofElTerroniseffectivelydividedintonorthernandsouthernsectorsbyadeep quebradathatseparatesthem.ElTerronSouthissituatedonboththeeasternandwestern sidesoftheMagdalenaSanAgustínAcasaguastlánroad.Totheeastoftheroadare approximatelytenlowplatformstructuresthatstretchfromtheroadtothebaseofatall, steepslopedcerrototheeast.Allofthestructuresinthisareaappeartohavebeenlow residentialmoundsandhavebeenthoroughlylooted.ThemodernvillageofLasVueltas coversmuchofthewesternportionofElTerronSouth.Allofthestructures,scattered throughoutthevillage,havebeenthoroughlylooted.Structuretypesincludevaulted funerarymonuments,multiroomedstructures,andlowplatformstructures.Surface collectionsfromthewesternportionofthesiteincludedjadedebitage,obsidianand ceramics. ElTerronNorth (TypeV) ElTerronNorthisaverylargeeliteresidentialandceremonialsitethatissituatedona seriesofriverterracesoverlookingtheRíoLato,tothewestoftheMagdalenaSan AgustínAcasaguastlánroad.Thesitestretchesoutforalmostahalfkilometerfromsouth tonorthandconsistsofover60mounds.Manyofthestructuresareorganizedintosmall, tightplazagroups.Structuretypesatthesiteincludevaultedfunerarymonuments(some astallasfourmeters),aballcourt,multiroomedstructures,lowplatformsstructures, terraceplatformsandplatformssupportingthinsuperstructurewalls. Surfacecollectionwasmadedifficultacrossthesitebecauseofsábilacultivationinsome areasandthickfoliagethroughouttherestofthesite.Nevertheless,wedidlocatetwo areaswithconcentrationsofjadedebitage.Oneconcentrationwaslocatedinanopen spacebetweentwosmallstructuregroupsandconsistedalmostentirelyofsmalljade flakes.Apieceofcutjadeandsomesmallflakeswerealsofoundinassociationwitha smallstructurethatboundsthesouthernendoftheballcourt.Allstructuresatthesite appeartohavebeenlooted;someoftheselooters'trencheshavepenetratedtomb chambers.

318 PuenteHato (TypeIV) PuenteHatoislocatedtothenorthwestoftheintersectionoftheRíoLatoandthe CA9ontheriverterracesoverlookingtheRíoLato.Thesiteisheavilydamagedby cultivationandconstructionandmuchofthesiteisunderdensevegetation.Overall,there areover20structures,somegroupedintosmallplazagroups.Someofthestructures appeartobesmallvaultedfunerarymonuments(someover2mtall);otherstructuretypes includemultiroomedplatformstructures,anumberoflowplatformsandmoundsless than2mtall.Theonlysurfacecollectionswewereabletomakeatthesitewerefroma barranca tothenorthofthesite. Guaytan3 (TypeI) ThesiteofGuaytan3islocatedtothenorthofGuaytan4onanarrowbluffatthe confluenceoftwosmallquebradas;therearenostructuralremainsatthesite.Theareais definedbyanisolatedsurfacescatterofjadeitedebitage Guaytan4 (TypeIV) Guaytan4iscomprisedoftwogroupsoflowstructureslaidoutoveraseriesofsmall platformsbuiltintogentlyslopingterrain.Inthenorthernportionofthesitearefour structures,allofwhichhavebeenextensivelylooted.Structure1islocatedimmediately adjacenttothemodernroadtoSanAgustinAcasaguastlan,andis12mx8m,oriented roughlynorthsouth.Structure2isa5mx5msquaremound,approximately.5mtall. Structure3islocatedninemeterstothesouthofStructure2,andisanother5mx5m squaremound,approximately.5mtall.Structure4islocatedonthewesternedgeofthe northerngroup,andisasmall(1mtall)mound,locatedatthebaseofasteepslopetothe west.Alooter'strenchdugintothecenterandsidesofthestructurerevealedthe presenceofalootedslablinedtomb.Verylittlejadeevidenceofjadeartifactproduction wassurfacecollectedinthisarea.Approximately25meterstothesouthwestofStructure 4aretheedgesoflowterracewalls(lessthan25cm)builtintothegentlyslopingterrain (Platforms1and2,Fig.5.12). InJuly2004,archaeologicalreconnaissanceidentifieddenseconcentrationsof jadeitedebitagethissouthernportionofGuaytan4(Fig.5.12,5.14).Allsurface collectedandexcavatedevidenceofjadeiteartifactproductionwasrecoveredin associationwiththesouthwesterncornersofPlatforms1and2(Operations1Aand1B) andthenorthernandwesternperimeterofasunkenpatioareabuiltinthelowpointof twoslopes(areaofOperations1D,1E,1F;seeFig.5.5forcontourmapofsouthern portionofGuaytan4).ThesunkenpatioisboundedonthenorthbyPlatform3andon thewestbyasimilarplatformwallidentifiedbyWalters(1980b)inhisexcavationsof thearea(Fig.5.6).BecauseofdensevegetationinthewesternportionofGuaytan4,we wereunabletodefinethelimitsofthewesternedgeofthesunkenpatio.Structure6sits justatoptheplatformwall,althoughIamcouldnotdiscernthisisthesamestructure identifiedandpartiallyexcavatedbyWalters(1980b).Asnotedabove,thesouthern portionofthesunkenpatiowasdestroyedintheprocessofbuildingthelocalelementary school,althoughWalters(1980b)excavatedthisarea,asdescribedearlierinSection

319 5.1.2).InthecenterofthesunkenpatioaretheremainsofStructure5,anextensively lootedmoundbuiltoveraslablinedtomb. Guaytan5 (TypeII) Guaytan5islocatedacrossaquebradatothesouthwestofGuaytan4andacrossa quebradatothesouthofGuaytan6;thesiteiscomprisedofagroupofthreelow platforms(lessthan25cminheight). Guaytan6 (TypeV) Guaytan6isseparatedbyquebradasfromGuaytan4totheeastandGuaytan5tothe south.ThesitewasdescribedbySmithandKidder(1943)andWalters(1982)asbeingan elitecivicceremonialsite.Thesite,asitcurrentlystands,wasanelitesiteofsomesort thatincludedaballcourt,butmuchofthesitehasbeenthoroughlylootedanddisturbed. Overall,thesitecontainsaseriesofplatforms(someofwhichareover3mtall),funerary structuresandmonuments,andmultiroomedstructures. Guaytan7 (TypeV) Guaytan7istotheeastoftheroadtothevillageofGuaytanandsouthofaquebrada. ThisareawasdesignatedbyWalters(1980)as"Area8",howeveritisdefinedas Guaytan7basedontheorderbywhichweencounteredthesesites.Thegroupismade upofapproximately15structures,consistingoflowplatforms,smallfunerarystructures andpossiblemultiresidentialstructureswhichhavebeenheavilydisturbedbylooting, constructionandagriculture.TheareaincludesMound24,excavatedin1930bySmith andKidder(1943)anddescribedinChapter5ofthisdissertation. Guaytan8 (TypeIV) Guaytan8iseastoftheroadtothevillageandsouthofGuaytan7versusGuaytan4, equivalenttothe"Area5"Walters(1980).Thisisanareawithlowplatformsthatrun fromeasttowest,alongahighnaturalterrace,boundedonthesouthbyseveralsmall structuresthatwereleveled;becauseoftheamountofsitedisturbance,itwasnotpossible tomakestructurecounts.Nevertheless,someofthestructureslikelyservedasfunerary monumentsandsomeasmultiroomedstructures,basedonsmallportionsofstructures thatwerestillinevidence.

320 AppendixB PJ05ExcavationDescriptions Acriticalpartofthisdissertationresearchinvolvedexcavationinareasidentified inJuly2004aspossiblejadeiteworkshopsbasedonthepresenceofhighconcentrations ofsurfacedebitage.Thegoalsoftheseexcavationsweretwofold:(1)todetermine whetherthesurfaceevidencewasindicativeof in situ jadeiteworkshops;and(2)to collectevidenceregardingthesocialcontextofthisjadeiteartifactproduction(i.e. specializedvs.domesticcontexts).Nineoperationsoftestexcavationwereundertakenas partofthisdissertationresearch.,withatotalof35excavationunits(TableB.1).

ExcavationsbeganonOctober17,2005andfocusedonthreeofthesepreviously identifiedareas:Guaytan3,Guaytan4andMagdalenaI.Inaddition,eighttestpitswere excavatedatGuaytan5(3testpits),Guaytan7(2testpits),Guaytan8(2testpits)and

KM93I(1testpit).ExcavationmethodsweredescribedinChapter5.Thisappendix presentssummaryinformationabouttheseunits.

Operation Site 1 Guaytan4 2 Guaytan5 3 Guaytan7 4 Guaytan8 6 Guaytan6 7 VargasIIB MagdalenaI 8 9 KM93I 10 KM92III TableB.1Excavationoperationsandcorrespondingsitesfrom2005fieldseason.

321 Operation1 Operation1consistedof5suboperationsinGuaytan4(1A,1B,1D,1E,and1F) andonesuboperationinGuaytan3(1C)( FigureB.1).

FigureB.1.SouthernportionofGuaytan4,showinglocationofexcavationunits. Operation1A Unit1A1 Unit1A1waslocatedinsquareN6/E12ofthesitegridestablishedatGuaytan4. Theunitwas1.00mx1.00msquareandwasexcavatedin10cmarbitrarylevels,savefor threeartificallevelsdefinedbypackedearthfloors,andwasexcavatedtoadepthof 0.80m(FigureB.2).

322 Level Depth Context Comments 001 0.0–0.10m Soiltexture:fineandloose Color: 5/310YRBrown 002 0.0–0.20m Soiltexture:fineandloose Color:5/310YRBrown 003 0.0–0.30m Soiltexture:fine,somewhatcompacted Color:3/210YRBrown 004 0.00.44m Soiltexture:fineandloose Color:3/210YRBrown 005 0.0–0.53m Soiltexture:finewithcompactzones Color:6/2YR Description:Erodedportionsofcompactburnedclayfloor. 006 0.0–0.65m Soiltexture:fineandloose Color:3/210YRBrown 007 0.0–0.72m Soiltexture:fine,somewhatcompacted Color:6/310YRbrown Description:Thislevelwasstoppedat7cmdepthwhenthetopof ared,burnedclayfloorwasencountered. 008 0.0 –0.83m Soiltexture:Looseandsandy Colorofburnedclarfloor:5/47.5YR Coloroffilloffirepit:6/310YR Thislevelonlyinvolvedexcavationofthecontentsofthefirepit (30cmwideX40cmlong&approx.11cmindepth).SeeFigures B.3,B.4

FigureB.2Excavationprofileofunit1A1.

323 FigureB.3.Planof1A1008withhearthtorightofscale..

FigureB.4.Detailofhearthin1A1008. Unit1A2 Unit1A2islocatedingridsquareN7/E12oftheGuaytan4sitegrid.Almostall ofthelevelswere10cmarbitrarylevels.Twolevelsareposiblefloorsthatmatchthose foundinunit1A1,whichisimmedeatelytothesouthof1A2(FigureB.5). Level Depth Context 001 0.00.20m Soiltexture:fine,smoothandloose Color:5/310YR–Brown. Description:Somelargestones,possiblyfromstucturetonorth. 002 0.00.30m Soiltexture:fine,smoothandloose Color:5/310YR–Brown.

324 003 0.00.40m Soiltexture:fine,smoothandloose Color:5/310YR–Brown 004 0.00.50m Soiltexture:fine,smoothandloose Color:5/310YR–Brown Description:Compactflooratthebottomoflevel. 005 0.00.60m Soiltexture:Alittleclayey,smoothandfine Color:5/310YR–Brown Description:SamefloorasencounteredinUnit1A1. 006 0.00.70m Soiltexture:smoothandfine Color:5/310YR–Brown 007 0.00.80m Soiltexture:smoothandfine Color:6/310YR–palebrown 008 0.00.90m Soiltexture:Compat,somewhatclaelyandSandy Color:6/62.5YR–oliveyellow Description:Darkinvariouspatches,andexhibitingsomeerodedportionsofa redclayfloor. 009 0.01.00m Soiltexture:Sandy,looseandfine Color:7/310YRverypalebrown;.95m1m:6/410YRlightreddishbrown Description:Soilwascompactinsomeplaces,withevidenceofaburntclay floor,thoughthiswasnotcontinuousthroughouttheunit. 010 0.01.15m Soiltexture:Sandyandfine Color:8/210YR–white Description:bedrockwithnoculturalmaterial

FigureB.5PofileofPJ051A2 PJ051B Operation1Bwasinitiatedtothenortheastof1A,onthesamegrid,withthe intentionofexcavavtingatestunitimmedeatelyadjacenttothelowplatformsofGuaytan 4.Oneunitwasexcavated,butterminatedbreforereachingbedrockbecausewedidnot havepermissiontoexcavatethrougharchitecturalfeatures,whichbecameapparentafter adepthof0.28mbelowthesurface.

325 PJ051B1 Unit1B1waslocatedingridsquareN9/E19andmeasured1.00mX1.00m. Level Depth Context Comments 001 0.0–0.10m Soiltexture:finaandsemicompact Color: 4/310YR–DarkBrown 002 0.0–0.18m Soiltexture:clayish,semicompact Color:4/310YR–DarkBrown 003 0.0–0.28m Soiltexture:clayley,compact Color:5/310YRbrown Description:Manyflatriverstonesappearingalongwitheroded remainsoffloor. 004 0.00.40m Soiltexture:compact Color:5/310YRbrown Description:Hardandcompactsoilwithabundant,vertucally placedstones 005 0.0–0.50m Soiltexture:clayley,compact Color:5/310YRbrown Description:Cleaninginsouthwesternareaofunittoavoid archictecture(Fig.B.6) 006 0.0–0.64m Soiltexture:clayleyandcompact Color:6/310YR–palebrown Description:Smallextensiónofpreviouslevelbeforeendingsoas nottopenétratearchiotecture.

FigureB.6.Planphotoof1B1005. PJ051C Operation1CwascarriedoutinGuaytan3toexaminethenatureofsurfacejade debitage.Three0.50mX0.50munitswereexcavatedtobedrock.Noneofthe excavationsturnedupmuchinformation.

326 PJ051C1 Unit1C1wasonthenorthernperipheryofthehillthatdefinedGuaytan3.The unitcontained2levelsof20cmindepth. Level Depth Context Comments 001 0.0–0.20m Soiltexture:sandyandfine Color: 5/210YR 002 0.0–0.40m Soiltexture:fine Color:8/210YR PJ051C2 Unit1C2waslocatedtothesoutheastofUnit1C1andwasterminatedat60cm uponmeetingbedrock. Level Depth Context Comments 001 0.0–0.20m Soiltexture:sandyandfine Color: 6/210YR 002 0.0–0.40m Soiltexture:fine Color:6/210YR 003 0.0–0.60m Soiltexture:fine Color:6/210YR PJ051C3 Unit1C3waslocatedtothewestof1C2andwasterminatedat60cmupon meetingbedrock. Level Depth Context Comments 001 0.0–0.20m Soiltexture:sandyandfine Color: 6/210YR 002 0.0–0.40m Soiltexture:fine Color:6/210YR 003 0.0–0.60m Soiltexture:fine Color:8/35YR PJ051D Operation1Dconsistsofsixunitswereselectedforexcavationinanareaof heavyjadesurfacedebitagetodeterminethenatureofthesurfacescatters(1D1thru1D 6).Theunitswerelocatedattheedgeofthequebradathatmarksthewesternedgeof Guaytan4(Fig.5.13,B.6a).Allunitswereexcavatedtobedrock,whichrangedfrom 40cmto1mbelowthenaturalsurface.Intwooftheexcavationunits,alevelofcompact soilwasnotedthatappearedtobetheremainsofanerodedplazafloor,butthiscouldnot beconfirmedacrossalltestunits.

327 FigureB.6a.SchematicdiagramofUnits1D1to1D4(DrawingbyErikaGomez). PJ051D1 Level Depth Context Comments 001 0.0–0.20m Soiltexture:sandyandfine Color: 6/310YR–palebrown 002 0.0–0.40m Soiltexture:fine Color:6/310YR–palebrown PJ051D2 Level Depth Context Comments 001 0.00.20m Soiltexture:looseandsemiclayly Color:5/410YR–yellowishbrown Description:Soilmorecompactatbottomoflevel. 002 0.00.40m Soiltexture:compact,likeapackedearthfloor Color:5/410YR–yellowishbrown 003 0.00.60m Soiltexture:sandybutcompactinplaces Color:5/410YR–yellowishbrown Compactareas:6/410YR PJO51D3(Fig.B.7) Level Depth Context Comments 001 0.00.20m Soiltexture:smooth,compactanduntantosandy Color:5/310YR–brown 002 0.00.40m Soiltexture:generallysmooth,butwithcompact portions Color:6/310YR–palebrown 003 0.00.45m Soiltexture:loose,clayleyandfina Color:6/410YR–lightyellowishbrown 004 0.00.80m Soiltexture:muycompact. Color:5/410YR–yellowishbrown 005 0.01.00m Soiltexture:sandyandfina Color:7/410YR–verypalebrown

328 FigureB.7ProfiledeunidadPJ051D3 PJ051D4(Fig.B.8) Level Depth Context Comments 001 0.00.20m Soiltexture:smoothandsandy Color:5/310YR–brown 002 0.00.40m Soiltexture:smoothperoquesevuelveunpocomáscompactal findelLevel Color:5/410YR 003 0.00.60m Soiltexture:loose Color:5/310YR Bottomofleveliscompact,possiblyfromafloor. 004 0.00.80m Soiltexture:compactinsomeplaces,looseinothers Color:Loosesoil:10YR5/3brown Compactsoil:5/410YR–yellowishbrown 005 0.00.87m Soiltexture:Compact&fineinplaces,sandyinothers Color:Compactsoil:5/310YRBrown Sand:7/110YRLightGray Talpetate5/610YRYellowishBrown Steriletalpetateappearsatbottomoflevel.

FigureB.8ProfileofPJ051D04.

329 PJ051D05 (Fig.B.9) Level Depth Context Comments 001 0.00.20m Soiltexture:semicompactandsandy Color:10YR6/4YellowishBrown 002 0.00.40m Soiltexture:Semicompact Color:10YR5/4,YellowishBrown 003 0.00.60m Soiltexture:semicompact Color:10YR5/3,Brown 004 0.00.80m Soiltexture:Smooth Color:10YR5/4,YellowishBrown;10YR6/4,LightYellowish Brown 005 0.01.00m Soiltexture:looseandsandy Color:10YR6/4,LightYellowishBrown

FigureB.9–ProfiledeUnidad1D05 PJ051D6(Fig.B.9a) Level Depth Context Comments 001 0.00.20m Soiltexture:loose Color:5/310YR–Brown 002 0.00.40m Soiltexture:loose Color:5/310YRBrown 003 0.0 0.55m Soiltexture:loose,withsemicompactareas Color:6/410YRLightYellowishBrown 004 0.00.75m Soiltexture:hard&compact,containingsomefine,loosesoil Color:5/410YRYellowishBrown 005 0.00.95m Soiltexture:fineandsandy Color:7/310YR–VeryPaleBrown

330 FigureB.9a–North profileofUnit1D06. PJ051Eand1F Fiveunits(Operation1Eand1F)wereexcavatedfromeasttowestalong Platform3,along,platformretainingwallthatformsthenorthernedgeofthesunken patiointhesouthernportionofGuaytan4.Excavationwasinitiatedtoobtainastratified sampleofproductiondebitage,basedonthepresenceofhighsurfaceconcentrationsof jadeitedebitagelocatedatopandbelowtheplatformwall.Theareaisthenorthern portionofthegroupexcavatedbyWalters(1980,1989),inwhichhereportedfinding densedepositsofjadeitedebitage.Fouroftheunits(1E1thru1E4)wereplacedbelow (southof)theplatformwall.,Anadditionalunit(1F1)wasplacedontheplatformitself, approximately1mnorthoftheplatformwall.Allunitswereexcavatedtobedrock, whichrangedfrom84cm(1F1)to1.8m(1E3)belowthenaturalsurface.After excavation,itwasobservedthatunits1E3and1E4werebothnorthoftheplatform retainingwall. PJ051E1(Fig.B.10) Level Depth Context Comments 001 0.00.23m Soiltexture:smooth,loose,slightlysandy Color:5/42.5Y–lightolivebrown 002 0.00.43m Soiltexture:smoothandloose Color:5/42.5Y–lightolivebrown Description:Asmallareaofhardednedsoilwasencountered

331 at.33m,whichwasyellowishbrown(5/510YR). 003 0.00.63m Soiltexture:1)compact,probablyanerodedfloor;;2)looseand fine;3)compact Color:1)6/510YR–brownishyellow;2)5/510YR–yellowish brown;3)6/42.5Y–lightyellowishbrown 004 0.00.83m Soiltexture:smoothandloose,compactinsomeareas Color:5/510YR–yellowishbrown 001 0.00.23m Soiltexture:1)looseandsandy;2)compact Southern Color:1)5/42.5Y–lightolivebrown;2)6/42.5Y–light extension yellowishbrown 002 0.00.43m Soiltexture:smooth,loose,somewhatsandy Southern Color:5/42.5Y–lightolivebrown extension 003 0.00.63m Soiltexture:1)looseandsmooth;2)clayley Southern Color:1)5/510YR–yellowishbrown;2)6/42.5Y–light extensión yellowishbrown 004 0.00.83m Soiltexture:1)smooth&loose;2)clayley&compact Southern Color:1)5/510YR–yellowishbrown;2)6/42.5Y–light extensión yellowishbrown 005 0.00.89m Soiltexture:fineandloose,withvariousclayleyandcompactspots Color:5/510YR–yellowishbrown 006 0.00.93m Soiltexture:powdery Color:6/510YR–brownishyellow Description:Thin,erodedportionoffloor(5cmthick)appearsin northeastsectorofunit(7/410YR–verypalebrown) 007 001.03m Soiltexture:smoothandlooseunderfloor Color:6/510YR–brownishyellow Description:Thinportionoffloor(5cmthick)appearsinnortheast sectorofunit. 008 0.01.25m Soiltexture:compact,looseandsandy Color:6/410YR–lightyellowishbrown

FigureB.10–ProfileofPJ051E1

332 PJ051E2(FigureB.11) Level Depth Context Comments 001 0.00.20m Soiltexture:compact Color:10YR4/3,DarkBrown/Brown 001 0.00.20m Soiltexture:compact Southernextensionof Color:10YR4/3,DarkBrown/Brown unit2 001 0.00.20m Soiltexture:compact Extension2b Color:10YR5/3,Brown Southernextensionof unit2a 002 0.00.40m Soiltexture:Semicompact Color:10YR5/3,Brown 002 0.00.40m Soiltexture:Semicompact Southernextensionof Color:10YR5/3,Brown unit Description:Inthislevelwasencounteredthe beginingoftheobsidianbladecorecache 002 0.00.40m Soiltexture:Semicompact Extension2b Color:10YR5/3,Brown Southernextensionof unit2a 003 0.00.50m Soiltexture:semicompact Color:10YR5/4,YellowishBrown 003 0.00.48m Soiltexture:semicompact Southernextensionof Color:10YR5/4,YellowishBrown. unit 003 0.00.60m Soiltexture:semicompact Extension2b Color:10YR5/3,Brown Southernextensionof unit2a. 004 0.00.70m Soiltexture:loose Color:5/410YR–yellowishbrown 005 0.00.80m Soiltexture:semicompact Color:10YR5/4,YellowishBrownand10YR5/3, Brown 006 0.01.00m Soiltexture:smoothandsemicompact Color:10YR5/4,YellowishBrownand10YR5/3, Brown 007 0.01.20m Soiltexture:compact Color:10YR5/4,YellowishBrown 008 0.01.30m Soiltexture:semicompact Color:sand10YR7/3,VeryPaleBrown Tierracafé10YR5/4,YellowishBrown

333 FigureB.11Northandeastprofileof1E02(1E2a,1E2b). PJ051E3(Fig.B.12) Thisunitwasinitiatedasa50cmx50cmunit,butwaseventuallyexpandedto 1mx1mtoenableexcavationtostreiledeposits. Level Depth Context Comments 001 0.00.20m Soiltexture:compact Color:10YR5/3Brown 001 0.00.20m Soiltexture:compact Extension3aeastern Color:10YR5/3Brown. extensionofuint1E3. 001 0.00.20m Soiltexture:compact Extension3b Color:10YR5/3,Brown southern1mx.5m extensionofuint1E 3/3a. 002 0.00.31m Soiltexture:semiclayishandcompact máximo Color:10YR5/3Brown

334 002 0.00.28m Soiltexture:semicompactandfino Extension3aeastern máximo Color:10YR6/4–LightYellowishBrown extensionofuint1E3. 002 0.00.28m Soiltexture:Semicompact Extension3b máximo Color:10YR5/3Brown southern1mx.5m Piso:10YR6/4LightYellowishBrown extensionofuint1E 3/3a. 003 0.00.50m Soiltexture:compact Color:10YR5/4YellowishBrown 003 0.00.50m Soiltexture:semicompact Extension3b Color:10YR5/4,YellowishBrown southern1mx.5m extensionofuint1E 3/3a. 003 0.00.50m Soiltexture:semicompact Extension3b Color:10YR5/3Brown southern1mx.5m extensionofuint1E 3/3a. 004 0.00.70m Soiltexture:loose Color:5/410YR–yellowishbrown Arena:10YR7/2LightGray 005 0.00.90m Soiltexture:loose Color:10YR5/3–Brownand10YR5/4Yellowish Brown Arena:10YR7/2,LightGray 006 0.01.10m Soiltexture:smoothandloose Color:10YR5/4YellowishBrown 007 0.01.30m Soiltexture:looseandsandy Color:10YR5/3and10YR5/4–BrownandYellowish Brown 008 0.01.50m Soiltexture:fine Color:sand10YR7/3VeryPaleBrownand10YR7/1 LightGray Tierracafé:10YR5/4YellowishBrownand10YR5/3 Brown 009 0.01.70m Soiltexture:semicompactandfine Color:10YR7/1,LightGray 010 0.01.80m Soiltexture:fine Color:10YR7/3,VeryPaleBrown

335 FigureB.12–ProfilesofPJ051E3 PJ051E4(B.13) Level Depth Context Comments 001 0.00.20m Soiltexture:1)looseandslightlysandy;2)looseand sandy Color:1)6/27.5YR–pinkishgray;2)6/310YR–pale brown 002 0.00.40m Soiltexture:clayleyandcompact Color:6/410YR–lightyellowishbrown 003 0.00.60m Soiltexture:clayleycompact Color:6/410YR–lightyellowishbrown 004 0.00.80m Soiltexture:clayleyandcompact Color:6/410YR–lightyellowishbrown 001a 0.00.20m Soiltexture:1)loose&slightlysandy;2)loose&sandy Northernextension. Color:1)6/27.5YR–pinkishgray;2)6/310YR–pale brown 002a 0.00.40m Soiltexture:alittlecompact Northernextension.

336 Color:6/410YR–lightyellowishbrown 003a 0.00.60m Soiltexture:1)clayley&compact;2)abitsandy Northernextension. Color:1)6/410YR–lightyellowishbrown;2)5/510 YR–yellowishbrown 004a 0.00.80m Soiltexture:compact Northernextension. Color:6/410YR–lightyellowishbrown 005 0.01.00m Soiltexture:loose,finaandsmooth Color:5/510YR–yellowishbrown 006 0.01.20m Soiltexture:1)powdery;2)smoothandloose;3)sandy Color:1)5/310YR–brown;2)6/410YR–light yellowishbrown;3)7/42.5Y–paleyellow 007 0.01.40m Soiltexture:sandyandfine Color:7/42.5Y–paleyellow 008 0.01.60m Soiltexture:sandyandloose Color:8/27.5YR–pinkishwhite

FigureB.13–ProfiledePJ051E4 PJ051F1 Unite1F1islocatedapproximately5meterstothenortheastofunit1E3. Level Depth Context Comments 001 0.00.20m Soiltexture:sandyandfine Color:6/310YR–PaleBrown 002 0.00.25m Soiltexture:looseandfine Color:6/310YRPaleBrown 003 0.00.31m Soiltexture:compact Color:5/310YR(Brown)andwithdarkareas:4/6 7.5YR(StrongBrown)and3/15YR(VeryDark Grey) 004 0.00.41m Soiltexture:loose

337 Color:10YR5/3Brown 005 0.00.48m Soiltexture:fineandsmooth Color:5/410YR–YellowishBrown 006 0.00.60m Soiltexture:fine Color:5/410YR–YellowishBrown 007 0.00.74m Soiltexture:compact Color:5/410YR–YellowishBrown 008 0.00.84m Soiltexture:fine Color:Threesoilcolorsappearinthislevel,butthey couldnotbedefinedbecauseofthefinetextureofthe soil:10YR5/4(caféamarillento);7.5YRN8/0 (blanco);10YR6/3(caféclaro).. Operation2 TestexcavationsatGuaytan5(aType2site)wereintendedtoassessthenature ofsurfacescattersofjadeiteandobsidiandebitage.Thesiteislocatedacrossaquebrada tothesouthwestofGuaytan4andacrossaquebradatothesouthofGuaytan6;thesiteis comprisedofagroupofthreelowplatforms(lessthan25cminheight)(Fig.5.21). Unfortunately,allthreeofourexcavations(Operation2,Units2A1,2A2,and2A3) wereterminatedatamaximaldepthof20cmuponreachingbedrock.Nosubsurface ceramicsorevidenceofjadeiteartifactproductionwasrecoveredfromanyofthe excavations;twoobsidianbladeswererecoveredfromoneunit.

PJ0521 Unit2A1waslocatedinthewesternportionofthesite. Level Depth Context Comments 001 0.00.10m Soiltexture:clayley,compactandhard Color:7.5YR3/3. PJ0522 Unit2A2waslocatedinthesouthernportionofthesite. Level Depth Context Comments 001 0.00.20m Soiltexture:clayley,compactandhard Color:3/37.5YR 002 0.00.25m Soiltexture:clayley,compactandhard Color:3/37.5YR PJ0523 Unit2A2waslocatedsouthUnit2A2. Level Depth Context Comments 001 0.00.20m Soiltexture:clayley,compactandhard Color:3/37.5YR Operation3 Guaytan7isasectorofthesouthernportionofGuaytanthatcontainsacoreof eliteresidentialstructuresthatwerestudiedandexcavatedbybothSmithandKidder (1943)andWalters(1980)(Fig.5.11);itisaTypeVsiteinthelocalsitehierarchy..

338 Duringsurveyofthissectorofthesite,asmall,widelyscatteredcollectionofjadeite debitagewasobservedinasmallplazaontheeasternedgeofthesitesector,whichhas partiallydestroyedonitswesternedgebytheroadtoSanAgustinAcasaguastlan.Two small50cmX50cmunits(Op.3A1and3A2)wereexcavatedtorapidlyassessthe significanceofthissurfacematerial.Anerodedplasterfloorwasuncoveredatadepthof approximately50cmbelowthesurfaceintheeasternmostofthetwoexcavationunits; jadedebitagewasrecoveredfrombelowthisplasterfloor.Bothunitsyieldedsignificant amountsofjadeitedebitageflakes,butfewcategoriesofevidenceofothertypesofjade artifactproduction.CeramicsdatedtotheClassicperiodgenerally,withthemajority fromtheLateClassicperiod.Bedrockwasreachedatapproximately1.3metersbelow surfaceinbothunits. PJ053A1(Fig.B.14) UnitlocatedinthesouthwesternpartofGuaytán7,initiatedasa0.50mX0.50m unitandsubsequentlyextenstendedtotheeastby0.50m.Unitwasexcavatedin20cm arbitaraylevels,exceptwhenfloorswereclearlyencountered. Level Depth Context Comments 001 0.00.20m Soiltexture:smoothandloose Abundant Color:5/32.5Y–lightolivebrown ceramicsand jadeflakes. 002 0.00.40m Soiltexture:smoothandloose Color:5/32.5Y–lightolivebrown 003 0.00.60m Soiltexture:1)smooth;2)clayley;3)compact Color:1)5/32.5Y–lightolivebrown;2)5/52.5Y–yellowish brown;3)6/210YR–lightbrownishgray Description:possibleerodedportionsofanunevenfloor. 004 0.00.70m Soiltexture:1)compact;2)slightlysandy Color:)6/210YR–lightbrownishgray;2)7/310YR–very palebrown Description:Near70cm,soilbecomesbeginsnotablymore compact,likeafloor. 001a 0.020m Soiltexture:compact Eastern Color:5/32.5Y–lightolivebrown. extensionof unit. 002a 0.00.40m Soiltexture:1)smoothandloose;2)compact Eastern Color:1)5/32.5Y–lightolivebrown;2)6/210YR–light extensionof brownishgray unit. 003a 0.00.60m Soiltexture:1)smooth;2)clayley;3)compact Eastern Color:1)5/32.5Y–lightolivebrown;2)5/52.5Y–yellowish extensionof brown;3)6/210YR–lightbrownishgray unit. Description:largerocks(1020cmlong)wereencounteredin thislayer. 004a 0.00.70m Soiltexture:slightlysandy Eastern Color:7/310YR–verypalebrown extensionof Description:largequantityofsmallrocks. unit.. 005 0.00.74m Soiltexture:1)slightlysandy,looseandfine Thislot Color:1)6/410YR–lightyellowishbrown comversonly Description:Soilissandyto74cmindepth,whewrethefloor thematerial beginstoappearinthisextensiónoftheunit. from.70.74m. Characteristicsofthefloor(Fig.B.15):compactclay(color7/2 10YR–ligthgray),withsmallstones(3mmto1cm)inclusions.

339 Thesurfaceiscoarseanderoded,theapproximatethicknessis3 6cm.Thefloorismadeuneven,sinceinthewesternportionit isfoundto6870cmindepth,whileintheextremeitis80cm. 005a 0.00.90m Soiltexture:1)slightlysandy;2)sandy;3)floor(described Thefloorends above) atadepth Color:1)7/310YR–verypalebrown;2)7/210YR–light maximumof gray 86cm. Description:Intheeastextensiónoftheunitthereisslightly sandyyellowishsoilslightlyandininthewesternhalfunderthe floorthereisaverylooseyellowishsand. 006 0.01.10m Soiltexture:1)sandyandfine;2)sandy Color:1)7/27.5YR–pinkishgray;2)8/110YR–white 007 0.01.30m Soiltexture:sandy,sandfina1/161/8mm Color:8/110YR–white 008 0.01.40m Soiltexture:sandy Color:8/110YR–white Description:Whitesandwithnoculturalmaterial.

B.14Northandeastprofilesof3A1(DrawnbyErikaGomez).

340 FigureB.15Planoffloorinlevel3A1005. PJ053A2(Fig.B.16) Theunitwaslocated5.0mtotheeastoftheunit3A1,andwasinitiallya.50 x.50munit,butwassubsequentlyextededby.50mtotheeast.Weexpectedfindingthe samefloowasinUnit3A1,butwedidnotfinditintheexcavation. Level Depth Context Comments 001 0.00.20m Soiltexture:1)looseandsmooth;2)loose Color:1)4/42.5Y–olivebrown;2)3/22.5Y–verydark grayishbrown Description:somelargerockswereencounteredinthislevel. 002 0.00.40m Soiltexture:1)smoothandloose;2)compact Color:1)3/22.5Y–verydarkgrayishbrown;2)6/32.5Y– lightyellowishbrown 003 0.00.60m Soiltexture:1)smoothandloose,slightlycompact;2)smooth andloose. Color:1)6/32.5Y–lightyellowishbrown;2)5/210YR– darkgrayishbrown 004 0.00.80m Soiltexture:1)smoothandloose;2)smooth Color:1)6/32.5Y–lightyellowishbrown;2)4/210YR– darkgrayishbrown 001ª 0.00.20m Soiltexture:1)looseandsmooth;2)loose Eastern Color:1)4/42.5Y–olivebrown;2)3/22.5Y–verydark extensionof grayishbrown unit. 002ª 0.00.40m Soiltexture:1)smoothandloose;2)compact Eastern Color:1)3/22.5Y–verydarkgrayishbrown;2)6/32.5Y– extensionof lightyellowishbrown unit. 003ª 0.00.60m Soiltexture:1)smoothandloose,slightlycompact;2)smooth Eastern andloose. extensionof Color:1)6/32.5Y–lightyellowishbrown;2)5/210YR– unit. darkgrayishbrown 004a 0.00.80m Soiltexture:1)smoothandloose;2)smooth Eastern Color:1)6/32.5Y–lightyellowishbrown;2)4/210YR– extensionof darkgrayishbrown unit. 005 0.01.00m Soiltexture:1)compact;2)slightlysandyandloose;3)smooth andloose Color:1)6/32.5Y–lightyellowishbrown;2)6/42.5Y–light yellowishbrown;5/310YR–brown

341 006 0.01.20m Soiltexture:1)sandyandloose;2)sandyandloose Color:1)7/32.5Y–paleyellow;8/22.5Y–white Description:Beginingsofthewhitesandthatliesabovethe naturaltalpetatewereencounteredatthebottomofthelevel. 007 0.01.30m Soiltexture:Sandy Color:8/22.5Y–white Description:Whitesandwthnotculturalmaterial.

FigureB.16Easternandnorthernprofilesof3A2(DrawnbyErikaGomez). Operation4 Guaytan8(aTypeIVsite)isasectorofthesiteofGuaytanlocatedatthefar southernperimeterofGuaytanCiudadela,approximately150meterstotheeastof Guaytan4and50meterstothesouthoftheGuaytan7testexcavations(Fig.5.11). Althoughnoarchitecturalremainsarevisibleonthesurfaceofthissector,itshouldbe notedthatthesectorliesdirectlytothesouthofaheavilylootedareaofeliteresidential architecturethatsitsonasmallnaturalplateauabovethefield.Duringsurvey,35pieces ofworkedjadeitewerecollectedinthefield,whichhadbeenusedformaizecultivation asrecentlyas2002.Aftertalkingwiththelocallandowneranddeterminingthatthefield hadonlybeenplowedbyhorsedrawnplows,Idecidedtoexcavatetwosmalltestunitsto assessthecharacterofdepositslocatedbelowtheplowzone(Operation4,units4A1, 4A2).Unfortunately,excavationshadtobeabandonedbeforecompletionwhenthe landowner’ssonschangedtheirmindsaboutgrantinguspermissionandaskedustoleave. Noundistrurbed,stratifiedcontextswereencounteredineitherunit,although fragmentsofburntclay,possiblyfromtheexteriorofawaddleanddaubstructure,were recoveredinunit4A1.

342 PJ054A01(Fig.B.17) UnitlocatedinGuaytan8,measuring1.00mx0.50m.Excavationwascarriedout in20cmarbitrarylevelstoadepthof1.80. Level Depth Context Comments 001 0.00.20m Soiltexture:compact Color:10YR5/3,Brown Description:PrimerCompacthummiclayerwithrocksandhighly disturbedculturalmaterial. 002 0.00.40m Soiltexture:looseandsemicompact Color:10YR5/3,Brown Description:Thislevelwassimilarlevel1inthefirstfewcentimeters. Anumberofburnedredclayfragments(2,5YR4/8,Red)werenoted. Inthelastcentimetersthesoilbegantoappearadifferentcolor:10YR 6/4,LightYellowishBrown. 003 0.00.60m Soiltexture:looseandsemicompact Color:6/410YR–lightyellowishbrownand10YR7/1,LightGray Description:Itconformedatfirstbyclearyellowishcoffeecolorland loose,thenbegantoappearsandcolorveryclearcoffeeinthesideThis ofthewellandsubsequentlytotheWestto0,52mofDepth,withtiny blackparticlesasinclusions,thesameonewasaverythinlayer. Amongthe0,50mandthe0,52manotherchangeinthelandwas given,thesameonewasmorelooseandslightlymoreclear, neverthelessintheSouthwesterncorner,landwasfoundyellowish coffee(10YR5/4,YellowishBrown),semicompactofwhichsome potswereobtained.ToaDepthof0,55malastchangeinthisLevel wasgiven,wasobservedsandclearcoffee(10YR6/3,VeryEven Brown).InsidetheLevelpumicewasfoundalso. 004 0.00.80m Soiltexture:semicompactandfine Color:10YR6/4,LightYellowishBrown Description:Levelcomposedbylandyellowishcoffeeinalmostallthe excavation.IntheSouthwesterncornerwaspresentedofdifferentway, sincewasmorebrilliant(bythequantityofmicathatcontained), besideswasnotloosebutinlumpsandwithsomefragmentsofcoal. Inherahammerofjadeto0,69wasfoundmofDepth.Inthe Northeasterncorner,thelandwassemicompactandofcoloryellowish coffee.Subsequently,intheSouthwesterncorner,coffeecolorland wasobserved(10YR5/3,Brown),surroundedbylandclearcoffee(10 YR6/3,EvenBrown)andlandclearyellowishcoffee(10YR6/4, LightYellowishBrown).Alreadyintheendoflot,almostallwasland fine,alwayswithfragmentsofcoalandsmallstones. 005 0.01.00m Soiltexture:smoothandloose Color:10YR6/4,LightYellowishBrown Description:Levelconformedbylandyellowishcoffeespace,smooth andloosethatoccupiesallthelot.To0,95mdarkerlandwasfound (10YR6/2,LightBrownishGray),probablybyburns,thatcontinued totheend.Alsoitcontainedaseriesofrocks,thatpresentedsignsofto havebeenburned,thereforeitscolorwasalmostblackandsomethey wereblackcompletely.Hadbesidessomepots,enlargingthequantity ofceramicsrecoveredofthisLevelincomparisonwiththeprevious one.

343 006 0.01.20m Soiltexture:looseandsandy Color:10YR6/4,LightYellowishBrown Description:Levelinwhichlandwasfoundyellowishclearcoffee, looseandofconsistencysandy.Approximatelyto1.10mofDepth,a crossstripeoflandwasfoundsemicompactthatwentofthe NortheasterncornertotheSouthwest.Itwasofthesamecolorofthe previouslymentionedanduponextractingitreturnedloose,gavethe onlythickimpressionofbeing.IntheNorthwestcornersand Southeastern,landwasfoundloosecoffee(10YR5/3,Brown),thatin theenddominatedinthelot. 007 0.01.40m Soiltexture:looseandsandy Color:10YR5/3,Brown Description:Thisitconformedbylandcoffeelooseandsandy,thatin someparts(NortheasterncornersandSoutheastern)werepresentedin lumpsandevenshowedsomefragmentsofcoalandsmallstonesas inclusions.Ingeneral,itsprofileesaremorecompactsthanthecenter ofthelot,whileintheendoftheLevel,thelandwasalittleclearer. 008 0.01.60m Soiltexture:looseandcompactensectores Color:10YR5/3,Brown Description:Levellandcomprisingcoffee,loose0.10minthefirst, changingtoalightershadeinthelastcentimeters(10YR6/4Light yellowishBrown).Between1.50mand1.55m,changesitstexture, beingmorecompactandinlumps.Attheendofthelotappearedvery finesand,whosesizewasgreaterthan1/16mm.Wholebatchwas smallrocksasinclusions. 009 0.01.80m Soiltexture:sandy Color:10YR6/4,LightYellowishBrown Description:Thislevelwasatestofthewesternhalfoftheunitto excludethepresenceofmoreculturalmaterial,asthelevelabove whichlittlewasrecovered.Wascomposedofloosesandsmoothand clear,yellowishbrown,whichlaterchangedtolightgray(10YR7/2, LightGray).Inclusionswasquitesmallstonesorgrit.

344 FigureB.17Northandeastprofilesnorteof4A1. PJ054A2(Fig.B.18) Theunitwas1.00mx1.00mandatthesamecharacteristicswereslightly differentfromthewellsdescribedsofar.Atthehigherlevelswereinclusionsoftalpetate clodsandrocksredlightthathadbeenpoorlypresentedinotheroperations,whichwere frequentfromthesecondtothefourthlevel.Italsofound"cascahuín"whichisamaterial usedtodayasdegreasing,intheclaythatisusedforthemanufactureofpotteryinSan AgustínAcasguastlán.Itispossiblethattheevidenceofthismaterialintheindustry,was associatedwithitsuseforsimilarpurposes. Level Depth Context Comments 001 0.000.20m Soiltexture:compact Color:5/42.5Y–lightolivebrown Description:Earthasacompactclodswhopresented regularquantityofpottery. 002 0.000.40m Soiltexture:1)compact;2)clayley;3)talpetate Color:1)5/42.5Y–ligtholivebrown;2)6/42.5Y –lightyellowishbrown;3)5/32.5Y–lightolive brown Description:Thislevelalsocompactthesoil,is abundantandfewlumpsofgraveltalpetate,aswell asareaswithlandclayleyyellowish.Apartfromthis, andpresentedsomereddishlumpscafesverylight weight,similartothepumice,whichweresmalland mediumsized(about10cm). 003 0.000.60m Soiltexture:1)compact;2)clayley;3)talpetate Cascahuínismaterial

345 Color:1)5/42.5Y–lightolivebrown;2)6/42.5Y thatisanaturalreddish –lightyellowishbrown;3)5/32.5Y–lightolive andgreenish,which brown hasasoapy Description:Leveltocontinuetotalpetateandclods consistencyasliketalc. ofearthcompactdaclayleysectors.Interspersedwith Thismaterialisusedin abundantpebblesandsmalllumpsofstoneand theproductionof reddishlightbrownabove.Itwasalsoobservedwith ceramicsinthearea relativeabundanceofsmallstones"cascahuín", today. amongwhicharesomecompleteandsomeareas whereitlookslikereddishmaterialdisintegrated. 004 0.000.80m Soiltexture:1)compactandlooseenalgunos sectores Color:6/410YR–lightyellowishbrown Description:Thefirst12cmofsoilhadLevelclayley compactandthenstartstobecomeloosewhilethe coloristhesame.Thepotteryisrelativelyabundant 005 0.001.00m Soiltexture:1)slightlysandy;2)sandy Color:1)6/410YR–lightyellowishbrown;2)8/2 7.5YR–pinkishwhite Description:Thefirstfewcentimetersofsoilhada littlesandy,thenappearscompletelyintermingled withsandysoil. 006 0.001.20m Soiltexture:sandy Color:8/15YR–white Description:Presentsyellowishsandysoil interspersedwithsandwhiter. 007 0.001.30m Soiltexture:sandy Color:8/15YR–white Description:Whitesandinwhichtherewasno culturalmaterial.

FigureB.18Northandsouthprofilesof4A2(DrawnbyErikaGomez).

346 Operation6 Operation6waslocatedintheareaknownasGuaytan6.Theonlyunit,6A1, waslocatedbetweenasmall,levelplatform,andthequebradathatseparatesGuaytan6 fromGuaytan4.levelingplatformborderingacreektotheeast,whilewestofitare severalstructures. PJ056A1(Fig.B.19) Theunitwas1.00mx1.00mandwasplacedinanareawherechertdrillsandjade debitagewereevdentonthesurface.Wehopedtoencounteramidden,astheareawas locatedbehindtheneareststructure,butdidnotencounteranymiddendepositsinthe area. Level Depth Context Comments 001 0.00.20m Soiltexture:compact Color:6/310YR–palebrown Description:Manystoneinclusions5cminlengthand smaller. 002 0.00.40m Soiltexture:compactandclayley Color:5/52.5Y–lightolivebrown Description:soilcontinuestobecompactandbeginsto beslightlyclayleywithsimilarsmallstoneinclusionsto previouslevel. 003 0.00.60m Soiltexture:compact Noculturalmaterial Color:5/52.5–lightolivebrown wasrecoveredanyof Description:excavationendedwiththislevelbecauseof thislotsowedecided theappearanceofmanylargerrocks,(36cminsize, tocompletethe whichmaybefromfillforanartificalplatform. excavationofthispit.

FigureB.19Northandeastprofilesof6A1.DrawnbyErikaGomez.

347 Operation7 Operation7waslocatedatthesiteofVargasIIB,ontheeasternfaceeasthill uponwhichthesiterests. PJ057A01(Fig.B.20) Unit7A01waslocatedontheeastsideofoneofthelootedstructuresthatispart oftheseriesthatrunsnorthsouthalongtheeasternfaceofthehill.Theunitdimensions were0.50mx1.00mandtheunitwasexcavatedinarbitrarylevelsof0.20meach,toa maximumdepthof0.70m.Almostallthematerialencounteredwasfromtheforthe lootingandcollapseofthestructure(Fig.40). Level Depth Context Comments 001 0.00.20m Soiltexture:fine Color:10YR5/3Brown Description:darkhumuslayerwithschist,boulders,roots,and smallstoneinclusions. Halwaythroughthelevelwasobservedasoilcolorchangetoa darkerbrown(10YR4/2,DarkGrayishBrown),whichis perhapsthenaturalhumus. 002 0.00.40m Soiltexture:fine Color:10YR4/2DarkGrayishBrown Description:loosedarkbrownsoil,withboulders,shale,stones andasmallbitofrootsasinclusions. 003 0.00.60m Soiltexture:loose Color:10YR4/2DarkGrayishBrown Description:loosedarkbrownsoilwithlargeroots(which hamperedtheworkofexcavation),boulders,smallstonesand shaleinclusions. 004 0.00.70m Soiltexture:loose Color:10YR4/2DarkGrayishBrown Description:samecolor,darkbrownwithfineandlargeroots, shale,pebblesandsmallstonesaspreviou,butwithverylittle artifacts,soexcavationwasabandoned.

348 FigureB.20Westprofileof7A1. Operation8 Operation8wascarriedoutatMagdalenaI(Fig.B.21).Seventestpitswere excavated:onetestpitintheeasternperimeterofthesite(8A1),onetestpitinthe centralplazaarea(8A3),andfivetestpitsinthewesternportionofthesite(8A2,8A4, 8A5,8A6,and8A7).8A1locatedatthesoutheastendofthesite,justwhereitends elevationwasdividedbytheroadtoSanAgustínAcasaguastlán.8A2waslocatedatthe northwestcornerofthesite,afewmetersfromtheRioLato.8A3unitislocatedinthe centerofasmallopensquare,while8A4islocatedsoutheastofthewesterngroupof structures.8A5unitislocatedwestofthegroup,atabout1.50mfromthewallvisible fromalooter’spitintoastructurethatflanksthissiteanddirectlyadjacenttothearea overlookingtheRioLato.8A6unitislocatedtothewestofunit5atalowerendandthe nearestriver.8A7islocatedjustbehindthelootedstructureonthewesternedgeofthe site,inthehopesoffindingundisturbedmaterialadjacenttothestructure.

349 Fig.B.21MapofsouthernportionofMagdalenaI PJ058A1(Fig.B.22) Unitwasplacedbetweentwostructures:arectangularstructureandanother structureinwhichacentrallylocatedpossiblewaslocated.Theunitwas1.00m longx0.50mwideanddugin0.20marbitrarylevels,toadepthof0.80m. Level Depth Context Comments 001 0.00.30m Soiltexture:compact Color:10YR5/3Brown Description:compactandverymuddy.Halfwayindepththrough thelevelweregrayspotsthroughoutthelevelandespeciallyinthe west,andalsoincludedwereseveralrocksofschistwhich hamperedtheworkofexcavation,sothelevelhadathicknessof 0.30m.Betweenthe0.20mand0.30m,wasrecoveredalarge amountofpotteryandjadeflakesmixedwithsoilandsmall carbonizedpiece;thefinal10cmpossiblyincludedanerodedfloor andsubfloor. 002 0.00.40m Soiltexture:semicompact Color:10YR5/3–Brownand10YR5/4YellowishBrown Description:startedoutwiththesamesemicompactsoilaslevel one,thenchangedtoamoreyellowishbrown,smoothersoil;the twosoilcolorsweremixedbetween0.35mand0.40m. 003 0.00.60m Soiltexture:semicompactandcompact Color:10YR5/4YellowishBrownand10YR6/4Light

350 YellowishBrown Description:yellowishbrown,semicompactandmicaceoussoilat thebeginningoflayer,butsoilbecamemorecompactedatabout 0.45mindepth,withmoreroots.Alightersoilcolowithbrown micaceousappearancewasencounteredbeginningat0.50min depth. 004 0.00.80m Soiltexture:smoothandsandy Color:10YR5/4YellowishBrown Description:afterafewcentimeters,thesoilthatwasfoundwasa slightlydarkerbrowntone,whichwascontainedbrownspots(10 YR5/3,Brown).Onlyoneceramicfragmentwasrecoveredinthe upperportionofthislevel.

FigureB.22Northandeastprofileof8A1. PJ058A2(FigB.23) Theunitislocatedtowardsthenorthwestedgeofsite,inanareanearmodern quartzandshalequarrying,afewmetersfromtheRioLato,whichwasnearandwestof thissector.Theunitis1.00mlongx0.50mwide,andliesbetweentwostructures,which flankthenorthpatio. Level Depth Context Comments 001 0.000.20m Soiltexture:1)compact;2)clayley,loose,slightlycompact Color:1)5/310YR–brown;2)5/510YR–yellowishbrown Description: compactatthebeginning,butthenmore looseandfine.Approximately13cmindepthintheeast portionoftheunit,thesoilbeginstoappearmore yellowandclayley. 002 0.000.40m Soiltexture:compact Color:5/510YR–yellowishbrown Description:Abitc ompact,clayleyandyellowish. 003 0.000.60m Soiltexture:slightlycompact,clayley,slightlysandy Color:5/510YR–yellowishbrown Description:Yellowishsoilwithsmallrockinclusions. 004 0.000.80m Soiltexture:compact,slightlysandy Color:5/510YR–yellowishbrown Description:y ellowsoilwithonlytwoverysmall fragmentsofpottery

351

FigureB.23Northandeastprofilesof8A2(DrawnbyErikaGomez). PJ058A3(Fig.B.24) Theunitwasplacedonaplatformwithasmallsquareatthecenterintheeastern MagdalenaI.Unitwas1.00mx0.50mandexcavatedin0.20cmnaturallevels. Level Depth Context Comments 001 0.000.20m Soiltexture:muycompact Color:5/310YR–brown Description:Compactsoilwithfewartifacts. 002 0.000.40m Soiltexture:1)compact;2)compact,clayley Color:1)5/310YR–brown;2)6/410YR–lightyellowishbrown Description:levelbeganasafairlycompactlumps.Thereafterthe soilismoreyellowish,smoothandsomewhatpasty,likewetclay. withfewsmallfragmentsofpottery.

FigureB.24Westandnorthprofilesof8A3(DrawnbyErikaGomez). PJ058A04(Fig.B.25) UnitlocatedsoutheastStructure7,measuring1.00mlongx0.50mwide, excavatedtoadepthof0.40minarbitrarylevelsof0.20meach. Level Depth Context Comments 001 0.000.20m Soiltexture:compact Color:10YR4/2DarkGrayishBrownand10YR5/3Brown Description:levelismostlyhumusandwallcollapsematerial.A pieceofgreenstoneaxwasrecoveredinthecollapseinthenorth portionoftheunit.Below0.07m,humicsoilgavewaytolighter

352 brown,compactsoilhorizon. 002 0.000.40m Soiltexture:semicompact Color:5/310YR–brownand6/410YR–lightyellowishbrown Description:semicompactwithrocksandrootsinclusions.Inhalf ofthelot,thelandchangedtoalighterbrowntexture,moresmooth andsandy,butwithfewerstoneswithenoughroots.

FigureB.25Northandeastprofilesof8A4. PJ058A5(Fig.B.26) UnitwaslocatedtothewestanddownslopeofStructure7.Theunitwas1.00m longx0.50mwide. Level Depth Context Comments 001 0.000.39m Soiltexture:1)compactcafé;2)compactamarillenta Color:1)6/410YR–lightyellowishbrown;2)5/410YR– yellowishbrown Description:soilwithabundantpebbles.Afterafewcentimeters, aseriesoflargerstoneswereencountered,probablyfrom collapseofthestonewallbehindStructure7.Whentheserocks wereremoved,otherrockscontinued,denselypackedand withoutapparentorderandexcavtionwashalted.

FigureB.26Northandeastprofilesof8A5(DrawnbyErikaGomez). PJ058A6(Fig.B.27) Theunitislocatedafewmeterswestanddownslopeofunit8A5.Itsdimensions were1.00mlongx0.50mwideandwasexcavatedin0.20marbitrarylevels.

353 Level Depth Context Comments 001 0.000.20m Soiltexture:1)smoothandloose;2)compact Color:1)5/310YR–brown;2)7/410YR–verypalebrown Description:brownsoilwithpebbles,andschistinclusions. Approximately6cmindepth,therewasayellowishsoil(talpetate). 002 0.000.40m Soiltexture:1)compact;2)smoothandloose Color:1)7/410YR–verypalebrown;2)5/310YR–brown Description:Mostofthelevelwastalpetate,butalsocontained brownsoilinsectors.

FigureB.27Profilesof8A6(DrawnbyErikaGomez). PJ058A07 UnitlocatedwestoftheWestofMagdalenaGroupI,specificallytoalootingof0.30min oneofitsstructures. Thisisawellborehole0.50mwidex1.00mlong,withaDepthofabout0.08m. Level Depth Context Comments 001 0.000.08m Soiltexture:compactandsemicompact Color:10YR6/3PaleBrown Description:LevelGroundcolorlightbrown,compactatfirstand thensemicompact.Asinclusionshadsmallstonesandroots. After0.05M,wasaseriesofslabsneatlyplaced,thatmightbepart ofthewallexposedbythelooting.Thelandthatwaspossibly coveredwiththemixturewhichjoined. Operation9 TheoperationislocatedsouthwestofthesitecalledTerzuolaonthe93kmroute oftheCA9,intheareacalledKM93I.Weconductedasingleunitcalled9A1of1.00m longx0.50mwide,butthesurfaceshowedfragmentsofworkedstoneandsomegreen flakes,excavationsdidnotprovidemuchmaterial,however,itispossiblethattheeastern Excavationisastructuredestroyedbysowingenoughaloeinthesector. PJ059A1(Fig.B.28) TheunitwaslocatedSWofthesiteandafewmetersnorthofasmallmodern building.Onthesurfaceoftheareachosenforexcavationwereslicesofgreenstone,a greenstonework,andothermaterials.Theunitwas1.00mx0.50mandpresented evidenceofapossiblestructuretotheeastofthewell,buttoodestroyed.Therewasvery littlematerialassociatedwiththeworkofjade .

354 Level Depth Context Comments 1 0.00.20m Soiltexture:1)tierracompactcafé;2)tierracompactamarillenta Color:1)4/310YR–darkbrown;6/42.5Y–lightyellowish brown Description:inthislottherewasconsiderableamountofpottery. Therewereseveralslicesofgreenstoneandasmallportioninthe formofatruncatedcone,alsorecoveredfragmentsofobsidian. 2 0.00.40m Soiltexture:compact Color:6/42.5Y–lightyellowishbrown Description:thereweresomesmallstonesandearthclodsin leaves,butcanbeundone.Thefirst10cmnoevindencióany material,whiletherestofthelotwereonly4smallpotsandany othermaterial.

FigureB.28Northandeastprofilesof9A1(DrawnbyErikaGomez). Operation10 TheoperationislocatedsouthwestoftheareaknownasKMIII92,immediately westofTerzuola.Weperformedonlyone,10a1,justinasectorwhichpresenteda concentrationofchips,butapparentlythereisnostructureinit.TheXunitwas1.00m and0.50mwiththeexceptionofthesurfacedoesnotpresentfurtherevidenceofgreen stone. PJ0510A1(Fig.B.29) ItislocatedintheareaidentifiedasSOKM92III,locatedimmediatelywestof Terzuola.Theunitwasexcavatedto1.00mlongx0.50mwide.Thiswellmadelittle materialassociatedwiththeworkofjadeandotherculturalmaterialFigure49). Level Depth Context Comments 001 0.00.20m Soiltexture:1)smooth;2)talpetate Color:1)5/410YR–yellowishbrown;2)5/42.5Y–lightolive brown Description:inthissectorwasseentalpetate,whichspreadtothe surface,toreachthe20cmdepth.Theculturalmaterialwasvery lowandtherewaslittleslicesofgreenstone,andafewfragments ofpottery,obsidianandquartz.

355 FigureB.29Northandeastprofilesof10A1.

356 APPENDIXC LITHICARTIFACTANALYSES Thisappendixprovidesdetailsofthetypesofmeasurementstakenaspartofthe lithicartifactanalysesundertakenaspartofthisdissertationresearch.Inthesectionsthat follow,Iprovidesummarydescriptionsoftheartifactcategoriesexaminedaspartofthis dissertation.Therawdataderivedfromtheselithicanalyseseareavailableuponrequest fromtheauthorat [email protected] . C.1JadeCobbleorChunk(n=29) Artifactsinthiscategorywereidentifiedaspiecesofjadeitelargerthan5cm,but thatdonotresembleflakes,eitherbecausetheywere"blockyfragments"withroughly similarlength,widthandthicknessmeasurements,orbecausetheywereunworked nodulesofjadeite.Measurementsincludedmaximumlength,width,andthickness,as wellasweight.Othercharacteristicsnotedwerethepresenceofcortexfromnatural weathering,indicationsthatthecobblewaswaterword(indicatedbysmoothedexterior surfacesthatwerenotflatortheresultfromgrinding),andthenumberofpossibleflake removalscarspresentonthecobbleorchunk.Themajority(n=21,72%)ofthecobbles orchunkscontainedoneormoreflakescars,butwereincludedinthesamecategoryas cobbleswithoutflakescarsbecauseofthedifficultyofdifferentiatingbetweenscars producedbynaturalfracturingversusthoseproducedbyintentionalpercussion. C.2LargeJadeFlakes(n=54) Jadeflakesmeasuringlongerthan5cminlengthandcontainingeitherastriking platformorventralbulbofpercussionweredefinedaslargejadeflakesandwere individuallymeasured,weighedandexamined.Inadditiontothemaximumdimensions andweightofeachflake,notesweremadeaboutthepresenceofcortexonanyportionof theflake,aswellasevidenceofwaterwornsurfacesandofthepresenceofscarsfrom thepreviousremovalofflakes. C.3SmallJadeFlakes Inthisanalysis,anyangularorirregularpieceofjadeitedebitagewascategorized asasmallflakeifwaslessthan5cminlength.Becausejadeitefracturesinanirregular andlargelyunpredictablemannerowingtoitsdensecrystallinestructure,analysisof individualflakesdoesnotprovidereliableinformationaboutthereductionsequenceused inproducingjadeiteartifacts.Therefore,alldebitageflakeswerepassedthroughaseries ofnestedwirescreensof1/2",1/4"and1/8"meshsize;flakesfromeachsizegradewere thencountedandweighedinaggregate.Thiswasdonetoobtainasmuchdetailabout debitagevariationaspossible,andinthehopethatitmightprovideinformationabout variationinthemanufacturingsequenceofjadeiteartifacts. C.4Hammerstones(n=8) Hammerstonesarestonesusedaspercussorstoremoveflakesorfragments throughtheuseofpercussiontechniques.Theywereidentifiedbasedontheirroughly sphericalshape(createdbypecking)andonevidenceofbatteringontheirsurface. Maximumlength,widthandthicknessofeachhammerstonewasrecorded,alongwiththe

357 weight.Allhammerstonesweremadeofjadeite.Detaileddatafortwoofthe hammerstonesaremissingbecauseofacorruptfileinwhichtheoriginalinformationhad beenentered. C.5JadeBeadPreform(n=34) Jadebeadpreformswereidentifiedashavingbeenroughlyshapedbygrindingor percussionintotheformofoneofthebeadshapesdescribedaboveinSection6.2.8,but uponwhichdrillinghadnotbeenattempted.Measurementsincludeddiameter,length, width,thickness,andweightofeachbeadpreform.Manybeadpreformsretainedscars frominitialshattering,despiteinitialgrindingofsomeofthebeadpreforms,andthiswas notedaswell. C.6Broken/UnfinishedJadeBead(n=111) Artifactsinthiscategoryweredefinedasbeadseitherbrokenorabandoned duringtheprocessofdrilling.Measurementsincludeddiameter,length,width,thickness, andweightofeachfragmentarybead;ifthebeadwasroughlycircular,onlydiameterwas measured,becausethelengthandwidthmeasurementswouldhavebeensimilar,ifnot identical.Ifthefragmentarybeadwasdrilled,themaximuminteriordiameterofthehole wasmeasured;itwasalsonotedwhetherthefragmentarybeadwasdrilledbiconicallyor uniconically.Inaddition,itwasnotedwhetherthebeadwasroughlyormorefinely groundintoshapeononeormoresidesofthebead,asubjectivedeterminationthatwas madebasedonthecomparativesmoothnessoftheexteriorsurfacesofthefragmentary bead.Asidewasdefinedassimplythesurfaceonwhichdrillingwasinitiated,which enabledtheother“side”tobeidentifiedasthesurfaceoppositewhichdrillingbegan. Theshapeofeachfragmentarybeadwasalsonotedusingthecategoriesdescribedin Section6.2.8. C.7JadeHollowDrillCores(n=62) Artifactsincludedinthiscategoryaredefinedasthebyproductoftheuseof hollowdrillstomakeholesinjadeiteartifacts.Measurementsofallhollowdrillcores included:maximumlength,diameterattopofcore,diameteratbottomofcore,weight; thediameteratthecenterpointofthecorewastakenforbiconicaldrillcores.Inaddition, observationsweremadeofthepresenceofabsenceofgrindingexhibitedonbothendsof thehollowdrillcores,whichwasidentifiedbasedonthepresenceofaflatsurfaceonthe endofthehollowdrillcore. C.8CompleteJadeBead(n=18) Artifactsassignedtothiscategoryincludedonlybeadsthatweredrilled completely.Measurementsforeachbeadincludedmaximumdiameterandthicknessof thebeaditself,maximuminteriordiameterofthedrilledhole,andweightofthebead. Allbeadswereexaminedtodetermineiftheyweredrilleduniconicallyorbiconically. Fourtypesofbeadswereobserved:button,donut,sphericalandtubular.Buttonbeads arecircular,butflatandthin.Donutbeadsarethickerthanbuttonbeads,andnot completelyflatontheirends.Sphericalbeadswereroughlyspherical.Tubularbeadsare cylindricalinshape,andgreaterthicknessthandiameter.

358 C.9CutJadeFragment(n=20) Artifactsassignedtothiscategorycontainatleastoneflatsurface,representing thesurfacealongwhichasawwaspassedtoremoveafragmentofjadeite.Identification ofcutorsawedfragmentswasmadebasedonthepresenceofalipatoneendoftheflat (cut)facesofanartifact,whichdistinguishtheseartifacttypesfromthosethatwere groundononesurfaceorfacet.Allcutjadefragmentsrecoveredinthisdissertationfield researchwerefragmentsthatwereremovedfromlargerartifactsbysawing. Measurementsincludedthemaximumlength,widthandthickness,andtheweightofthe artifact.Measurementsweretakenforalldimensionsoftheartifactitself,aswellasfor thecutsurface(s)(listedintheCommentscolumn).Observationsabouttheshape(in crosssection)atthebottomofthecutwerealsonotedwherepossible.Additional observationsabouttheartifactarenotedinthecomments. C.10JadeFragmentwithGroundFacet(n=97) Artifactsinthiscategoryincludealljadeartifactsthatcontainedatleastone groundfacet,butdidnotcontainvisiblesignsofhavingbeenremovedbysawing. Determinationofwhetherafragmenthadagroundfacetrestedonthepresenceofatleast onesmoothedsurfacewithvisiblestriationsfromthegrindingprocess,andnotfrom naturalsmoothing.Inmanycases,evidenceofgrindingisnotpresentonallsurfacesof theartifact,butrestrictedonlytoaportionofthesurface.Inthesecases,themaximal dimensionsoftheground,flatsurfacewasrecorded;wheremultiplesurfacesshowed evidenceofgrinding,eachfacetwasmeasuredindividuallyandrecorded.Some fragmentswithevidenceofgrindinglookedsimilartoartifactsassignedtothevarious beadcategoriesdescribedabove,andmayhavebeengroundartifacts,suchasplaques, thatwereintentionallysmashedinordertoproducerecycledfragmentsforbread production.Nevertheless,unlessareasonablycleardeterminationcouldbemadethatthe groundfragmentwasintendedtobeabead,itwascategorizedasaJadeFragmentwith GroundFacet. C.11ChertBladeFragments(n=26) Chertbladesweredefinedaslong,thinchertartifactswithparallellateraledges, andflatventralsurfacesanddorsalsurfaceswithoneormoreridges.Measurements includedmaximumlength,width,thicknessandweightofeachblade,aswellasnoteson thenumberofridgesonthedorsalsurfaceofthefragment.Incaseswhereonlythe medialsectionofachertartifactwasrecovered,itwascategorizedasablade,forlackof evidenceofflakingtoproduceadrilloneitherend. C.12ChertDrills(n=401) Chertdrillsweredefinedaslong,thinchertartifactswithparallellateraledges, flatventralsurfaces,dorsalsurfaceswithoneormoreridgesandwithtapereddistalor proximalendsproducedbytheremovalofmicroflakes.Measurementsincludedthe weightandmaximumlengthofthedrill,aswellasthemaximumwidthandthickness acrossthemedialportionofthedrill.Inaddition,width,lengthandthickness measurementsofthedrillbitweretakenifthebitwaspresent.Noteswerealsotaken regardingthesubjectivedegreeofwearexhibitedonthedistalportionofthedrill(e.g. blunt,sharp,semisharp),aswellasthenumberofridgesonthedorsalsurfaceofthedrill.

359 C.13WorkedShell(n=39) Allworkedshellartifactsareincludedinthisgeneralcategory.Measurementsfor allartifactsincludedweight,maximumlength,widthandthickness.Observationsabout theformofparticularshellartifactsarenotedinthe“Comments”column. C.14NonjadeStoneBeads(n=22) Thiscategoryincludesallnonjadestonebeads,regardlessofwhethertheywere completeorbroken;allbeadsweredrilledeithercompletelyorpartially.Measurements includedweight,maximumlength,minimumandmaximumdiameters,maximum diameterofdrillhole.Commentsincludedthecolorandtypeofstone(when identifiable),andotherobservations. C.15ObsidianBladesandBladeFragments(n=1936) Measurementsonobsidianbladeandbladefragmentsincludedweight,maximum length,maximumwidth,maximumthicknessandnumberofridesonthedorsalsurface oftheblade(Fig.C.1).Allbladeswereobservedregardingthetypeoffragment:whole, proximal,medialordistal.Theshapeincrosssectionofallbladeswasalsonote: triangular(onlyoneridgeondorsalsurface),trapezoidal(2ormoreridgesondorsal surface),ormultiple(fragmentswithsectionsofdorsalsurfacewithoneridge,andother sectionswith2ormoreridges).Forproximalandwholebladefragments,thewidth, depth(thickness)andangleoftheplatformandthewidthanddepthofthebulbof percussionbelowtheplatformweremeasuredwherepossible.Thesubjectivedegreeof “nicking”onthelateraledgesofbladeswasnotedaswell:none,light,some,andheavy. Finally,themorphologyoftheterminationofdistalbladefragmentswasnoted. FigureC.1 Diagramshowingobsidian blademeasurementstakenas partoftheanalyses(drawing byPeterKelterborne). Measurementstakenare circled(parenthesesindicate columnheadingindatabase): L (Length); Wm (Width), D(Thickness); W(PlatformWidth); Wp (ProximalWidth); ~Wp (ProximalDepth); α(PlatformAngle); PlatformThicknessnot shown,butisperpendicularto “W”ondrawing.

360 C.16ObsidianFlakes(n=1044) Nosystematiceffortwasmadetoidentifyobsidianflakesaccordingto technologicalcategories.Instead,allflakeswerecategorizedaccordingtosize,by placingthemincircleswithdiametersof.5cm,1cm,2cm,3cm,4cm,5cm,6cmand7cm. Flakeswereassignedtoeachcategorywhentheentiretyoftheflakefitwithinthecircle. Flakesineachsizecategorywerethencountedandweighedinaggregate. C.17ObsidianBladeCores(n=251) Obsidianbladecoresareartifactsfromwhichobsidianbladeshavebeenremoved throughtheapplicationofpressuredetachment.Becauseoftheuniquecharacterofthe obsidianbladecorecache(n=245)fromGuaytan4excavationunit1E2,anextensive numberofmeasurementsweretakenforallcoresinthecache;thesearepresentedinthe “ObsidianCoreCache”tabofthe“NonJadeArtifactData.xls”.Allotherobsidianblade coreswerefragmentary,andonlybasicmeasurementsandobservationweretakenon theseartifacts;thesearepresentedinthe“MiscellaneousArtifacts”tab.Measurements takenonthecoresfromthecachearenotedinFigureC.2. FigureC.2Drawing(Source: PeterKelterborne)ofobsidian bladecore,indicatingwhere measur ementslistedincolumn headingsin“ObsidianCore Cache”databaseweretaken oneachcore.Descriptionsof themeasurementsandakeyof abbreviationsusedarealso foundinthesamedatabase worksheet.

361 C.18MiscellaneousArtifacts(n=12) Allartifactsthatdidnotfitinoneofthecategoriesnotedabovearelistedinthis category;observationsaboutthetypeofartifactarenotedinthe“Comments”column. Measurementsincludedmaximumlength,widthandthickness,andweight.

362 APPENDIXD MiddleMotaguaValleyCeramics (writtenbyErickRochette,SelketCallejasandMónicaPellecer) ThisappendixpresentsdescriptionsoftheceramicanalysesperformedbyLic. SelketCallejasaspartofthisdissertationfieldresearch.Lic.Callejashasworkedasa ceramicistintheMiddleMotaguaValleywithvariousprojectsdirectedbyLic.Hector ParedesandLic.LuisRomero.Belowisthechapterabouttheceramicssubmittedto IDAEHaspartofthePJ05informe. ComopartedelasinvestigacionesrealizadasporelProyectodeInvestigación sobrelaProduccióndeJadeeneláreadelRíoLato,serealizóelanálisispreliminarde losmaterialescerámicosrecuperadosdelasexcavacionescondosobjetivosprincipales: a) Determinarsecuenciascronológicas b) Seleccionar el material diagnóstico y desechar el material no diagnóstico (depositándolo debidamente identificado nuevamente en algunas áreas de excavación) Lametodologíaaplicadaparalarealizacióndedichoanálisisincluyóel lavadoymarcadodelmaterial,laclasificaciónytomademuestras,dibujo, fotografíayporúltimoladescripciónporvajillas.Enlamuestraseincluyeron tantolosmaterialesrecuperadosmediantelarecoleccióndesuperficie,comoel delasexcavacionesllevadasacabodurantelatemporadadecamporealizadade octubreadiciembre. Laclasificacióncerámicaserealizóconformealatipologíadefinida previamenteparalaregióndelMotaguaporJoséHéctorParedesyLuisAlberto Romero,aplicandoelSistemadeAnálisisdelAtributoConsistente,una combinacióndelosSistemasTipoVariedadyVajilla(planteadospor…),que sebasaenlarigurosidadelsistemaVajilla,peroqueagrupatipos,quese clasificansegúnlavariabilidaddeladecoración,pasta,formaoacabadode superficie,mediantecaracterísticasquepermanecenatributoconsistenteyque nospermitenidentificarlosmaterialesdecadavajilla(Martínez,2005citandoa Paredes2004;Martínez2005). Procedenciadelosmateriales Losmaterialesprocedendeexcavacionescontroladas,limpiezadesaqueosy recoleccióndesuperficiedediferentesGruposdelossitiosdeGuaytan,Vargas, Magdalena,TerzuolayLosChagüites.Lasoperacionesdelascualesprocedenlos materialessonlassiguientes:

363 Descripcióndelosmateriales Ladescripcióndelosmaterialesrecuperadosenlarecoleccióndesuperficie, limpiezadesaqueosyexcavacionescontroladasseclasificóporvajillaslascualesson descritasacontinuacióntomandocomoatributosfundamentales:lapasta,laforma,la decoraciónyelacabadodesuperficie. VAJILLAJÍCAROINCISO Fase: HuisajoaMagdalena Pasta Elcolordelapastaescafénaranja(5YR6/8),detexturamedia,másomenosporosay defracturairregular.Eldesgrasanteestáformadoporpequeñosfragmentosdepiedra pómezmolida.Lamayorpartedelamuestrapresentamalacocciónounacocciónno uniformeyaqueseobservaunafranjagrisáceaalcentrodelafractura. Forma Laformamáscaracterísticasonloscuencos,perotambiénseobservancántarospequeños yvasijasdebocarestringida.Losbordessongeneralmenteredondos,algunos ligeramentebiseladosenelexterior,otrosligeramenteplanos.Lasparedesdeloscuencos puedensercurvas,ligeramenterectodivergentes,ligeramentecurvodivergentes.Enla muestraseobservóunfragmentodecántarodecuerpoligeramentecomprimido.Las basesporlogeneralsoncóncavas.Nohayejemplaresqueindiquenlapresenciade soportes,asasocualquierotroaditamentoenlasvasijasdelavajilladeJícaroIncisopara elClásicoTemprano.OtracaracterísticadeéstavajillaesqueparalafaseHuisajo,existe mayordiversidaddeformasqueparalamismavajilladurantelaFaseMagdalena.Las dimensionesdelasvasijassonporlogeneralpequeñas,conungrosordebordequevade los3alos8mm. Decoración Ladecoracióncaracterísticaeselinciso,éstepuedeserfino,medioyalgunasvecesmuy fino.Losdiseñossonexclusivamentegeométricos,desdesimpleslíneasconcéntricasen lapartemediadetodalaparedexternadelavasija,hastadiseñosdepetatillos,espiraleso grecas.Porlogenerallosdiseñossonsimétricossobretodalabandaincisaqueseubica enlapartemediadelaparedexterior.Ademásdelinciso,éstavajillapresentacomo atributoconsistenteunabandadepinturarojayaseaúnicamenteenelbordeoextendida medioouncentímetrosobrelaparedexternaeinterna. Acabadodesuperficie: OtroatributodelavajillaJícaroInciso,quepermitesuclaraidentificacióneselengobe naranjaqueseobservaperfectamenteenlosejemplaresdelaFaseHuisajo.Elengobe cubretodalapiezaygeneralmentevaalisadoyenbajopulido,aunquealgunostienenun pulidomayor. Temporalidad

364 Lasvasijasdelavajillasediferencianentemporalidadporvariosatributos,siendoelmás importanteeldeterminadoporlabandadecolorrojoqueseubicaenelborde.Parala faseHuisajo,estaessimplementedecolorrojoygeneralmenteselocalizaúnicamenteen ellabioyenmínimaextensiónsobrelapared,mientrasqueparalafaseMagdalenase utilizóelcolorrojohematitaespecularylabandaseextiendedesdeelbordehastaunoo doscentímetrostantoenlaparedinternacomoexterna..Otroatributoquepuedeayudara identificarlatemporalidadsonlasformasdelasvasijas,queparalafaseHuisajosonmás variadas,mientrasqueparaMagdalena,sereducecasiexclusivamenteacuencos.El engobetambiénconstituyeelementodiagnósticoimportante,debidoaqueenlafase Huisajo,elcolordeestéesdeunnaranjamásintensoquerecubretodalapiezayparala faseMagdalena,eláreacubiertaporengobesevareduciendoenlaparedexterna. Mientrasmástardíoeselmaterial,algunosejemplaresyanoconservanelengobenaranja, sinoquepresentanunasuperficiemásburda.

Fig.1 JícaroInciso Fig.2V.JícaroInciso VAJILLACARRIZOINCISO Fase: HuisajoaMagdalena Pasta Lapastaesdecolorcafénaranja(7.5YR6/6),puedevariartambiéndependiendodela cocciónalaquehayasidosometida,decaféclaroaunatonalidadrosa(7.5YR7/4, 7.5YR).Elcolordelapastaencuantoalacocciónesregular,algunosconuncolor uniforme,otrosconunafranjagrisáceaqueseobservaalcentrodelafractura.Latextura esmásomenosfina,defracturaregularyunpococompacta.Comoantiplásticocontiene cristalesdecuarzomuypequeñoyfino. Forma

365 EnlamuestradematerialcerámicodelProyectodeJade2005,sóloseobservaron fragmentosdecuencos,queeslaformamásgeneral,peropuedenencontrarseaunque muyescasamentecántarospequeñosyposiblementeotrasformasbásicas.Losbordes sonredondosoligeramentebiseladosenelexterior.Lasparedesporlogeneralson curvodivergentes,peropuedensertambiéncurvoconvergentesylasbasessoncóncavas. Lasdimensionessonbásicamentedecuencospequeñosconbordescuyogrosorvaría entrelos4ylos7mm. Decoración Ladecoracióneselincisoporlogeneralmedioygrueso.Losdiseñossongeométricos conlíneasentrelazadasoformandorectángulos,líneasinclinadas,líneasenformadeZo lazos.Esteincisotambiénseubicaenunabandaquegeneralmenteocupalapartemedia delaparedexternadelcuencooinclusopuedeextendersehastalaparteproximaldela base,dependiendogeneralmentedelaformadelavasija.Otroatributoimportantedela vajillaeslabandarojaqueseubicaenellabioybordedelasvasijas.Estapuede encontrasesólosobreellabioopuedeextenderseunoodoscentímetroshacialapared internayexternadelapieza. Acabadodesuperficie Elacabadodesuperficieesmuyimportanteparaidentificarestavajilla,puesconstituye unodesusprincipalesatributosyconsisteenunbañodepinturacremaquecubretodala vasija.EstacaracterísticapermitediferenciarlodeotrasvajillasincisascomoelJícaro Inciso.Porlogenerallapiezapresentaunalisadoybajopulido. Temporalidad AligualqueenlavajillaJícaroInciso,elatributomásimportanteparaidentificarla temporalidadeslabandarojaenelborde,queparaelClásicoTardíosepresentaenrojo hematitaespecular. Fig.3 CarrizoInciso Fig.4V.CarrizoInciso

366 VAJILLAMAPACHEESTRIADO Fase: Huisajo Pasta Lapastaesdecolorcafénaranja(7.5YR6/6),latexturaesmedia,másomenosporosa queserompeconciertafacilidadlocualquieredecirquesetieneunapastarelativamente suaveofrágilynoduracomoenotrasvajillas,ademásfracturaesbastanteirregular.El desgrasanteestácompuestodepiedrapómezyenmenorescalaporfragmentosde cristalesdecuarzo,posiblementearenaderío.Lacocciónengranpartedelamuestraes buena,porlauniformidadenelcolordelapasta,enotrasocasionesseobservaenla fracturaunatonalidadgrisácea.Estauniformidadenelcolordelapastaposiblementese debaaquelapastanoesmuycompacta,loquepermitequeelcalorsedistribuya uniformementeportodaslasseccionesdelapieza,apesardeexistirzonasbastante gruesascomolosbordesengrosadosyelgollete. Forma Laformabásicasonloscántarosgrandesynoselocalizóenlamuestraotrotipode forma.Losbordessonredondosyevertidosodivergentes,generalmenteengrosadosenel interior.Loscuellossoncurvodivergentes,loscuerposprobablementesubglobulareso achatadosylasbasesporlogeneralsoncóncavas.Ningunodelosejemplarespresenta asasosoportesnialgúnotroaditamento.Cómosemencionóaliniciodeéstepárrafo,los cántarossongrandesconundiámetroaproximadodelabocadelavasijaquevadelos25 alos40centímetros.Elgrosordelosbordesesdeaproximadamentede10mm.yporlo generalvaengrosándosehastallegaralcuello. Decoración ElelementomásimportanteparalaidentificacióndelavajillaMapacheEstriadoessu decoracióndeunestriadogruesoquepuedeencontrarseenelcuelloycuerpodelcántaro. Porlogenerallavasijaestádecoradadelasiguienteforma:Enelbordepresentapintura rojaonaranjaqueseextiendehastaunosdoscentímetrosaproximadamenteporlaparte internadelbordedelavasijaestodependiendodeltamañodelcántaro,posteriormente enelcuellopuedellevarunacombinacióndediseñosydedecoración,talycomoel punzonadogruesoqueporlogeneralformalíneasinclinadasenelcuello,luegoalapar delpunzonadounincisomedioqueformalíneascruzadasounadecoracióndepetatillo,y tambiénpuedeencontrarseenelcuelloelestriadoenlíneasverticales.Lapartedel cuerpoporlogeneralestátotalmenteestriadoconlíneashorizontaleseinclinadasque lleganhastalaparteenlacualdainiciolabasedelavasija. Acabadodesuperficie: Algunasmuestraspresentanrestosdeengobenaranjaenelcuello,porloqueelengobe podríaserzonal.Elrestopresentaúnicamenteunburdoalisadoenelcuelloycuerpoyun bajopulidoaproximadamenteapartirdelabase.

367 Fig.5V.MapacheEstriado Fig.6V.MapacheEstriado VAJILLAHUITEINCISO Fase: HuisajoaMagdalena Pasta Lapastaesdecolorcafénaranja(5YR6/6),sutexturamedia,yaquepresentaalgunos porosynoesmuyhomogénea,lafracturaesmásomenosregular.Eldesgrasante constituyentedelapastasonfragmentosdepiedrapómezmolidaqueseobservanen abundanciaynosedetectaotrotipodeantiplástico.Encuantoalacocción,lamayoríade ejemplarespresentalatonalidadgrisáceaalcentrodelafractura,porloquela uniformidadenelcolordelapastasóloseobservaenalgunassecciones. Forma Laformamáscomúnsonloscuencosaunqueposiblementetambiénvasospequeños.Los bordesentodalamuestrasonredondos,laparedesdeloscuencospuedensercurvoso ligeramentecurvodivergentesaunqueenmenorescala.Lasbasespuedensercóncavaso planasynopresentanningúnaditamentocomosoportes,asas,enteotros.Eldiámetro aproximadodeloscuencosvadelos14alos24centímetros,siendomáscomuneslosde menoresdimensiones.Elgrosordelbordevadelos4alos6mm.,elgrosordepared varíadelos5alos7mm. Decoración Ladecoraciónprincipalenéstavajillaeselincisoqueporlogeneralesmedioylos diseñossonmuysimples:líneasconcéntricasa¾delaparedexternayproximaldel borde.Tambiénseobservanenlasparedesexternasincisosdelíneasverticalesycurvas. Algunasvasijasnollevanincisoyconstituyenunavariedaddelavajilla.Otroelemento

368 deladecoraciónquepuedenonollevarlasvasijasdelavajillaHuitéIncisoesunabanda rojaenelborde,queadiferenciadelJícaroInciso,elCarrizoIncisoyotrasvajillas,es casisiempremuypequeña,esdecirquenoseextiendemásalládelbordeolabiodela vasija. Acabadodesuperficie ElacabadodesuperficiedelavajillaHuitéIncisoconstituyetambiénelprincipalatributo quepermitesurápidaidentificación,elcualconsisteenunbañodepinturacremasobrela superficieexternaysóloseencuentraalisadaynopulida.Elinteriordelavasijaporlo generalllevaunengobedecolornaranjapálidoquesiseencuentraalisadoypulido. Temporalidad ComoenlasvajillasJícaroyCarrizoInciso,elelementodiagnósticomásimportantees labandarojahematitaespecularparalafaseMagdalena.Sinembargo,enéstavajillaes muchomásdifícildeestablecerlatemporalidad,debidoaquemuchasvasijasno presentanladecoracióndelabandarojaenelborde. Fig.7 V.Huité Inciso Fig.8V.HuitéInciso VAJILLACANTORAL Fase: Huisajo Pasta Elcolordelapastaescafénaranja(5YR6/6),latexturaesmediabastanteuniformey homogéneadefracturamásomenosregular.Elprincipalelementonoplásticodelapasta

369 eslapiedrapómezmolidamuyfinaqueseobservaenaltoporcentaje.Lacocciónes regularaligualquelamayoríadelasvajillasdelaregión,puesseobservalatonalidad grisáceaalcentrodelafractura,aunqueparalavajillaCantoralesmínima,porlogeneral sóloenlaszonasengrosadasdelapieza. Forma Enestavajillaseincluyenexclusivamentelosplatos,cuyosbordessonredondos,la mayoríaligeramenteengrosadosenelinterior.Lasparedessonrectodivergentes,yen muypocoscasosmuyligeramentecurvodivergentes,yaqueestoconstituyeunatributo consistentedelavajillaCantoral.Lasbasessoncomúnmenteplanas.Losplatospueden serdediferentestamaños,aunqueporlogeneralsondeuntamañoregular.Elgrosorde losbordesvadelos6alos8mm.yeldelasparedesdelos5alos10mm.Estosplatos puedenonollevarsoportescónicososoporteanular,cuandosoncónicoslosplatosson tetrápodes. Decoración LaúnicadecoraciónquepresentanlosplatosdelavajillaCantoraleslapinturarojaque vaenlaparedexternadesdeelbordeolabiohastadondeexactamentecomienzalabasey constituyeelatributoconsistentedelavajilla. Acabadodesuperficie Laparteinteriordelosplatosllevacasisiempreunengobecafénegro,aunquepuedeser tambiéndecolornaranja,ésteseencuentraalisadoypulido.Laparteexternallevala pinturarojaquellevaunpulidomediopuesnoesdemasiadobrillante. Fig.10 V.Cantoral Fig.9.V.Cantoral

370 VAJILLAGUAYABALROJO Fase: Huisajo Pasta Elcolordelapastaescafénaranja(5YR6/6),sutexturaesfina,bastantecompacta,de fracturamásomenosregular.Eldesgrasanteestácompuestoporfinosfragmentosde piedrapómezmolidayelcolorenlafracturaesregularmenteuniformeaexcepciónde algunaszonasendondeseobservaunatonalidadgrisácea.Porlogenerallaspartesmás delgadaspresentanmayoruniformidadymejorcocción,mientrasquelaszonasmás gruesascomoelbordeyelgolletepresentanlatonalidadgrisalcentrodelafractura. Forma Laformacaracterísticadeestavajillasonloscántarosynosehaencontradootraforma básica.Entrelosbordespredominanlosredondosysolamenteseobservaronalgunos ligeramenteplanos,otrosligeramenteagudosyenmenorcantidadengrosadosenel interior.Elcuelloescomúnmentedemedioaaltoysiemprecurvodivergente,elcuerpo posiblementeessemiglobularylasbasespuedenserplanasycóncavas.Estetipode cántarosnollevanasa,soportes,vertederanialgúnotroaditamento.Loscántarossonde untamañointermedio,conundiámetroaproximadodelcuellodelos12alos18cm.El grosordelbordevaríadelos5alos15mm.dependiendodeltamañodelcántaro,el grosordelasparedesdelcuellovadelos7alos13mm.yelgrosordelasparedesdel cuerpodelos3alos6mm. Decoración Estavajillatienedostiposdedecoracióncaracterística:Lapinturarojayladecoración aplicada.Lapinturarojaescasisiemprezonalyselocalizacomúnmenteenunabanda rojaenelborde,enelcuello,casisiempresóloenseccionesverticalesaunquepuede cubrirlatotalidaddelbordeyenelhombro.Lasaplicacionesformancaras antropomorfas,algunasvecesmásprominentesqueotrasyporlogeneralformanojos, narizyboca.Enalgunasocasioneslaaplicaciónsólotieneformadeespigayseaplican muyescasamente(1ó2espigasentodoelcántaro),éstastambiénpuedenestar punzonadas.Seobservóenlamuestraquelapinturarojarecubrelaaplicación.Otrotipo dedecoraciónquellevanalgunoscántarosdelGuayabalRojoesunaespeciede impresiónconlauñaenelborde. Acabadodesuperficie Lasuperficiedeloscántarosseencuentraenlapartedelcuelloúnicamenteconunburdo alisado,sólolasecciónquevapintadatieneunpulidomayor.Elcuerpodeloscántarosse encuentracubiertoconunengobecafénaranjaqueseencuentraalisadoypulido,yal igualqueenelcuellolapartedelhombroquellevapinturapresentaunmayorpulimento.

371 Fig.12V.GuayabalRojo Fig.11V.GuayabalRojo VAJILLAFLAMBOYAN Fase: Huisajo Pasta Lapastaesdecolorcafénaranja(5YR6/6),latexturaesmedia,lafracturaesmáso menosregularyesregularmentecompacta.Elelementonoplásticodelapastasonlos fragmentosdepiedrapómezmolida,generalmentemuypequeños.Todoslosejemplares presentanunatonalidadnouniforme,principalmentelosplatosgrandes. Forma Lasformasmáscomunessonlosplatosycuencosconbordesredondos,bordes compuestosquellevanunaodosacanaladurasenlaparteinternaylosbordesplanos.Las paredesdelosplatossonsumayoríacurvodivergentes,siluetacompuestaocurvadas. Entreloscuencosexistemayorvariedad,encontrándosecuencosdeparedescurvas,de paredligeramentecurva,deparedesrectodivergentesydeparedescurvoconvergentes. Lasbasesdelosplatosycuencossongeneralmenteplanasoligeramentecóncavas.Los platospuedenllevarsoportesyporlogeneralsontetrápodos.Lossoportessuelenser redondosyvaciados,algunosconsonaja,éstostambiénpuedenestardecoradosconuna simpleformazoomorfa.Otrotipodesoportesenlosplatossonlossoportescónicospero untantocurvosquetambiénseencuentranvaciadosconagujerosparalacirculacióndel

372 oxígeno.Entreloscuencoslossoportesmáscomunessonlosanulares,especialmentelos pequeñoscuencosconparedescurvas. Lasdimensionesdelosplatosdeparedcurvodivergentevandelos26alos28cm.Entre loscuencoslamuestraindicaqueeldiámetroaproximadovadelos16alos24cm., mientrasqueenloscuencosdeparedescurvasesde13y14cm.Sólosedetectóunplato quenopresentaparedesycuyodiámetroaproximadoesde33cm.Elgrosordelos bordesdependedelaformayvaríadelos5alos10mm.yelgrosordelasparedesvade los3alos10mm.Laalturaaproximadadeloscuencosdeparedcurvaesde5y5.5cm. Decoración Ladecoraciónqueconstituyeelatributoconsistentedeestavajillaeslapinturarojasobre elengobenaranjaqueseubicadentroofueradelavasija.Losdiseñospintadosson simples,generalmentebandasrojasqueseextiendendesdeelbordehasta1ó2 centímetrossobrelaparedinternaoexterna,círculosdepinturarojaenlaparedexterna, puntos,manchas,manchasonduladas,líneasonduladas,osimplementesecciones verticalesquellevanpinturaroja. Acabadodesuperficie Unodelosatributosmásimportantesenlaidentificacióndelosmaterialesdelavajilla Flamboyaneselacabadodesuperficiequeestáconstituidoporunengobenaranjaque comúnmenterecubrelavasijapordentroyporfuera,aunqueestepuedeserzonal,sobre todoenlaparedexterior.Elengobeseencuentraalisadoypulidomedioysobreéstese aplicaladecoracióndepinturaroja. Fig.13V.Flamboyan Fig.14 V.Flamboyan

373 VAJILLATRIUNFOESTRIADO Fase: Huisajo Pasta Lapastaesdeuncolorcafénaranja(7.5YR6/6),casisiempredetexturamediayde fracturairregularyunpocoporosa.Elelementonoplásticodelapastaeslapiedra pómez,queseobservaenunaltoporcentaje,losfragmentosnosonmuyfinosyvarianen tamañodemenosde1mm.alos3ymm.Estoindicaquepresentanfragmentosbastante grandesqueindicanlatexturadelapasta.Enalgunasocasionesseobservancristalesde cuarzoyenmenorcantidadpartículasdemica.Lacocciónengranpartedelamuestraes buena,indicandounauniformidadalaexposicióndelcalorysóloenalgunassecciones sepresentalatonalidadgrisácea. Forma Laformabásicadelavajillasonloscuencosdegrandesdimensionesyenlamuestrase observaronmuypocosbordesdecántaros.Losbordesdeloscuencossuelenserredondos, algunosligeramenteplanos,otrosplanosenellabioyengrosadosenelinterior,otros redondosengrosadostambiénenelinterior.Enelcasodelosbordesdecántaroséstos sonredondosyunodeellosengrosadoenelinterior.Loscuellossoncurvodivergentes enloscántarosylasparedesdeloscuencossoncurvoconvergentesosimplemente curvadas.Enloscántarosesdifícildeestablecereltipodecuerpos,peroposiblemente seansubglobulares.Lasbasesenambasformasparecensercóncavas.Ningunadelas formasquecomponenestavajillapresentaasasoalgunaotraañadidura.Noseencontró estematerialenelmaterialcerámicodelProyectodeJade2005. Decoración Másqueunadecoraciónelestriadoenestavajillaconstituyeelacabadodesuperficie, debidoaqueésteesmínimo.Porlotanto,únicadecoraciónquepuedeonopresentarsees lapinturarojaonaranjasobreellabiooborde,principalmenteenloscuencos. Acabadodesuperficie LasvasijasdelavajillaTriunfoEstriadonopresentanengobeyúnicamenteelestriado finoquenoalteraengranmedidalasuperficie.Elestriadopudorealizarseconun instrumentosencillo,talvezunatuza,unfragmentodetelauotroobjetoquenoalterara engranmedidalasuperficiedelapieza. VAJILLAPETÓN Fase: Huisajo Pasta Lapastaescafénaranja(5YR6/6),detexturafina,compactaydefracturaregular.El principaldesgrasanteeslapiedrapómez,enmuyfinosfragmentos.Lacocciónquese observaesbuenaenalgunaszonas,perodetonalidadvariadaenotras.

374 Forma Laformacaracterísticasonloscántarosdebordeplanooredondo,decuelloligeramente divergenteocurvodivergente.Loscuerposposiblementesonglobulares,achatadoso subglobulares.Lasbasesseguramentesonplanasoligeramentecóncavas. Decoración Estoscántarosnopresentanalgunadecoraciónespecíficaaunqueesmuydifícilde determinardebidoalacasitotalausenciadebordesdeéstavajilla. Acabadodesuperficie Losmaterialespuedenpresentardostiposdeacabadodesuperficie,unengobecaféoun engobecorintoorojizo.Esteporlogeneralseencuentraalisadoypulidomedioyestos permitenidentificaralavajillaPetónquepuedesercaféorojizo. Fig.15.V.Petón VAJILLAGUARANJA Fase: ManzanalyMagdalena Pasta Lapastaessiemprecafénaranja(5YR6/6),detexturamedia,unpocoporosayde fracturairregular.EldesgrasantesecomponedurantelafaseManzanaldefragmentosde piedrapómezyapartirdelafaseMagdalenapredominaelusodemicaqueva aumentandoencantidadconformellegaalafasePalmilla.Éstasvasijastambién presentanunauniformidadenelcolordelaspastas,casisiemprenaranja. Forma Lasformasmáscomunessonloscántarosperopuedenobservarsetambiénalgunos cuencosgrandes.Losbordessonredondos,engrosadosenelinterior,algunosdivergentes yenmenormedidaplanos,generalmenteenloscuencos.Loscuerpodeloscántarosson globularesyenloscuencoslasparedessoncurvadasoligeramentecurvoconvergentes. Lasbasesporlogeneralsoncóncavasoplanas.Estoscántarospuedenonopresentar asasdegrantamañazo.

375 Decoración Nopresentanmayordecoraciónmásquepinturarojaonaranjaenelbordeylaaplicación característicaqueconsisteenunaespeciedetresagujerosimpresosconlosdedosqueva generalmenteenelcuerpodeloscántarosyqueesmuycomúnentrelosmaterialesde otrossitiosdelaregión.Enéstamuestrasóloseobtuvounfragmentoconéstaaplicación. Acabadodesuperficie: Lasuperficienopresentaengobeyúnicamenteseencuentraalisadaburdamente,tantoen loscántaroscomoenloscuencos.

Fig16.V.Guaranja Fig.17V.Guaranja VAJILLAMAIZAL Fase: Manzanal Pasta Decolorcafénaranja(5YR6/6y7.5YR6/6),la pastaposeeunatexturamedia,muyhomogéneaymásomenoscompactaydefractura regular.Eldesgrasanteestácompuestodefragmentosmuyfinosdepiedrapómezenmuy pocacantidadylapastaademáspresentaunabuenacocciónporlauniformidadenel color.

376 Forma Únicamentesehanincluidoenlavajillacuencosdegrantamaño,cuyosbordes constituyenunodelosatributosconsistentes,porserdivergentedelabioredondoyde biselplanointerior.Lasparedesdeloscuencossonligeramentecurvoconvergentesylas basessoncóncavasoplanas.Porlogeneral,estoscuencospresentanasasredondasy horizontales. Decoración LaúnicadecoraciónquepodemosobservarenloscuencosdelavajillaMaizalesqueel bordedebellevarpinturaroja,constituyendootrodelosatributosdelavajilla. Acabadodesuperficie Generalmenteelúnicoacabadoqueseobservaenlasuperficiedelaparedexternaesun alisadodeburdoamedio,mientrasqueeninteriorseobservaunalisadomedioyunbajo pulido,siendotambiénunacaracterísticaimportanteparasuidentificación.

Fig.18V.Maizal Fig.19 V.Maizal VAJILLAYAJEINCISO Fase: Manzanal Pasta Elcolordelapastaescafénaranja(5YR3/2,5YR6/6),latexturaesvademediaafina, defracturageneralmenteirregular,muypocoporosaperonoextremadamentecompacta.

377 Eldesgrasanteestácompuestoporpiedrapómezmolidamuyfinayenmuypocoscasos sepresentalamicacomoelementoantiplástico,aunquecuandosepresentaesenmuy pocacantidad.Enalgunosejemplaresdelamuestraseobservanpequeñoscristalesde cuarzoquetambiénpuedenactuarcomoelementosantiplásticosdelapasta.Lacocción quepresentanesmuypocouniforme,debidoaqueseobservaclaramenteenlafracturael contrastedelastonalidadescafénaranjadelapastaconunatonalidadgrisácea.Muy pocostiestostienenunacoloraciónuniforme. Forma Laformabásicasonloscuencospequeños,aunqueenmaterialesdeotrossitiosdela regióntambiénselocalizancántarospequeños.Losbordessonredondos,lasparedes ligeramentecurvadasoligeramenteconvergentes,lasbasesporlogeneralsonplanaso ligeramentecóncavas.Lasdimensionesdeloscuencossonbásicamentepequeñosde entre10y15cm.dediámetroyelgrosordelosbordesvaríadelos4alos7mm. Decoración Unodelosatributosconsistentesdelavajillaeselinciso,quecasisiempreesfinoya vecesmuyfino.Losdiseñossongeométricos,porlogeneralsimpleslíneasconcéntricas enlapartemediadelapared,tambiénsuelenencontrarsedecoracionesdepatatilloo algunasgrecasperomuysimples,estotambiénenunabandaenlapartemediadela paredexterna.Otrotipodediseñosonlaslíneassonlasonduladasymientraseldiseñoes máscomplicado,elincisoesmásfino. Acabadodesuperficie Elsiguienteatributoimportantedelavajillaeselacabadodesuperficiequeconsisteenel engobenegroquecubrelapieza.Estesepresentaunalisadoypulidoaltoenlaparte externadelavasija,mientrasqueenelinteriorpuedepresentarunalisadoypulidomedio obajo. Fig.20V.YajeInciso

378 Fig.21V.YajeInciso VAJILLAENCINALNEGRO Fase: Manzanal Pasta Lapastapresentauncolorcafénaranja(5YR6/6),latexturaesmedia,untantoporosay defracturairregular.Elcomponenteantiplásticomásimportanteyabundanteeslapiedra pómez,perotambiénseobservanalgunoscristalesfinosdecuarzosemilechoso.Enla fracturaseobservadiferenciaenelcolordelapastadebidoseguramente,alapoca uniformidaddelatemperaturaalaquefueexpuestoyalasdiferenciasenelgrosordela pieza,yaqueenlaszonasmásgruesasseobservaunatonalidaddegrisanegra. Forma Laformamáscaracterísticasonloplatos,perotambiénselocalizancuencosyalgunos cántaros.Losplatossoncasisiempredeparedescurvodivergentesyloscuencosde paredescurvasoligeramentecurvoconvergentes.Lasbasesenlosplatossonplanas debidocomúnmenteaquellevansoportes,yenloscuencospuedenserligeramente cóncavasoplanas.Lossoportesenlosplatospuedenserdetablero,quepuedenestar decorados,algunossoncalados,esdecir,conunaespeciedepunzonadogrueso;otros soportessonredondosyvaciadosdebaseplana,aunqueposiblementetambiénlleven soportescónicosalgocurvados.Lasdimensionesenlasvasijasdeestavajillapueden variaraunqueporlogenerallosplatossongrandes,mientrasqueloscuencosylos cántarossonpequeños.Eldiámetroaproximadoentrelosplatosvaríadelos22alos35 cm.,elgrosordelosbordesenestosvadelos5alos10mm.yelgrosordelasparedes

379 delos4alos9mm.Entreloscuencoseldiámetroaproximadovadelos10alos16cm. yelgrosordelosbordesdelos3alos6mm.,elgrosordelasparedespuedevariardelos 5alos9mm.Enloscántaroselgrosordelbordeesaproximadamentede4mm.yel grosordeparedesesde5y6mm. Decoración LavajillaEncinalNegropuedetenerpordecoraciónalgunasaplicacionesdecaras antropomorfas,pequeñasaplicacionesdebandascolocadasenposiciónverticalyenmuy pocasocasionesdecoracióndepastillaje.Todaséstasaplicacionesseubicanenlaparte proximaldelabase,enlaparedexterior.Otroelementoquepuedetomarsecomo decoraciónseobservaenelbordedelosplatos,elcualpuedeserondulado. AcabadodeSuperficie Cómoenotrasvajillasdelaregión,elacabadodesuperficieconstituyeunodelos atributosconsistentesmásimportantes.Lavajillapresentaunengobequepresentaun acabadoenalisadoypulidoalto,generalmenteenlaparteexterior,aunquetambiénel interiordelavasijapuedepresentaréstascaracterísticas. Fig.22 V.Encinal Negro

380 VAJILLANARANJALMANCHADO Fase: Manzanal Pasta Lapastaesdetexturamedia,untantoporosaydefracturairregularenlasmásgruesasy demayorregularidadenlaszonasmásfinasodelgadas.Elcolorescafénaranja(5YR 6/6)yelcomponentenoplásticomásabundanteeslapiedrapómezmolidamuyfina, aunqueseobservanalgunosfragmentosquepuedenllegaralos3mm.dediámetro.Otras inclusionesquepuedecontenerlapastaaunqueenmenorcantidadestánformadaspor finoscristalesdecuarzosemilechoso.Porlogenerallamuestrapresentaunabuena cocciónysóloenlaszonasmásgruesasseobservapocauniformidadenelcolordela pasta. Forma Lasformassonvariadas,perolamáscaracterísticasonlosplatosgrandes,aunque tambiénseobservanalgunoscuencosycántarospequeños.Losbordesenlosplatosson generalmenteredondosenellabioycompuestosconunaodosacanaladuras.Otras formaspresentanbordesplanosoligeramentebiseladosenelexterior.Lasparedesdelos platossoncasisiempredesiluetacompuestaobastantecurvodivergentes,enloscuencos éstaspuedensercurvadas,ligeramenterectodivergentes,curvodivergentesy ligeramentecurvoconvergentes.Lasbasessoncasisiempreplanasoligeramente cóncavas.Losplatosdesiluetacompuestaodeparedescurvodivergenesenlamayoría deloscasossontetrápodes,consoportesredondosdebaseplanaoamorfos,siempre vaciadosperoconagujerospordondecorreeloxígeno,otrossoncónicosperocurvados. Lasdimensionesdelosplatossondeaproximadamentedelos20alos38cm.de diámetro,conungrosordebordequevadelos4alos7mm.yungrosordeparedesque varíatambiéndelos4alos7mm.Loscuencosquesonmuchomáspequeñosquelos platos,puedentenerunaalguradeentre4.5cm.,5.5cm.ymás,ungrosordebordesde entre4y7mm.aproximadamenteyungrosordeparedesde4a7mm.Elgrosordelas paredesenunejemplarcuyaformaesuncántaro,esde6mm.aproximadamente. Decoración Ladecoraciónnoconstituyeunatributoconsistentedelavajilla,yaqueéstapuede presentardistintostiposdedecoraciónosimplementenopresentarninguna.Algunasde lasobservadasenlamuestrasonlosincisos,generalmenteenloscántaros,algunas aplicaciones,acanaladuras,punzonados,etc.Esdecir,noexisteuntipodedecoración específicaqueidentifiquealavajillaNaranjalManchado. Acabadodesuperficie Porotraparte,elacabadodesuperficiesiconstituyeunatributoconsistentedelavajilla, yaqueelengobecafénaranjaquerecubreenlamayoríadeloscasoslatotalidaddela vasija,siconstituyeunelementoprácticoparasuidentificación.Enlosplatoselengobe puedeestarsóloenelexteriorauqueporlogeneraltambiénpresentaelmismoengobeen elinterior.Enloscántarossóloseobservaenlaparteexternayalgunasvecesenlas paredesinternasdelcuello.Entreloscuencospuedeestartambiénenelinterioryexterior oserzonal,puesalgunasvecessólocubrelamitadounasecciónmáspequeñadela

381 paredexterna.Elengobegeneralmentepresentaunalisadoypulidoquevademedioa alto. Fig23 V.Nara njalManchado VAJILLAFLORIPINACANALADO Fase: Manzanal Pasta Elcolordelapastaescafénaranja(7.5YR6/6),detexturamediaafina,bastante compactayuniformeydefracturaregular.Elúnicocomponenteantiplásticoobservado eslapiedrapómezmolidamuyfinayenmuypocacantidad.Seobservamuypoca uniformidadenlatonalidaddelapasta,ypredominalatonalidadgrisáceaalcentrodela fractura. Forma Lasformasmáscaracterísticasapesardeunagranausenciadebordessonlosvasosy cuencosnomuygrandes.Losbordessonredondos,lasparedesrectasomuyligeramente curvasylasbasessonplanasoligeramentecóncavas.Lacasitotalausenciadebordes

382 impidedeterminarundiámetroaproximadodelasvasijas,peroseconsideranomayores 16cm.dediámetro. Decoración Ladecoraciónconstituyeunodelosdosatributosmásimportantesdelavajillayconsiste enladecoraciónacanaladaquepuedesersuave,mediaoprofunda.Porlogeneralel acanaladoesvertical,aunquetambiénhayacanaladosenposiciónhorizontal generalmenteubicadoenlaparteproximalalbordedelaparedexterna.Cuandoel acanaladoesvertical,casisiemprecubretodalavasija,mientrasquecuandoeshorizontal, sóloseobservanunaodosacanaladuras.Tambiénseincluyóenlamuestrauntipode decoraciónqueformaunaespeciedeimpresionesenlaparedexterna,yaqueésta decoraciónnodañalasuperficie,seguramenteporqueerarealizadaantesdelsecadoy coccióndelapieza.Estetipodeacanaladurassoncirculares.Encuantoaltamaño,las acanaladuraspuedenserfinas,mediasogruesas. Acabadodesuperficie Otroelementoimportantequeconstituyeunatributoconsistenteenlavajillaeselengobe cafénaranjaquecubrelapieza.Esteporlogeneralpresentaunalisadoypulidodemedio aalto,casisiempresóloenelexteriordelosvasos,mientrasqueenloscuencospuede encontrarseconéstascaracterísticasinternayexternamente. VAJILLAPUJÓNACANALADO Fase: Manzanal Pasta Lapastaesdecolorcafénaranja(7.5YR6/6,7.5YR3/2),latexturaesmedia,muy homogéneayregularmentecompacta,lafracturaesregular.Eldesgrasanteestá compuestofragmentosmuyfinosdepiedrapómezyalgunoscristalesdecuarzomuy finos.Elcolordelapastaenlafracturaseobservamuyuniforme. Forma Lasformasmáscomunessonloscuencosyplatos,aunquetambiénhayvasosycántaros pequeños.Losbordessonredondos,unosmásgruesosqueotrosdependiendodelaforma. Lasparedesdelosplatosporlogeneralsoncurvodivergentesodesiluetacompuesta.,en loscuencospuedenligeramentecurvodivergentesodesiluetacompuesta.Losvasos tienenparedesrectasoligeramentecurvas.Lasbasessoncasisiempreplanasenlos platos,vasosycántarosyplanasyligeramentecóncavasenloscuencos.Losplatos puedenonollevarsoportes,redondos,amorfosocónicos.Losplatosporlogeneralson grandes,loscuencosycántarosycántarossonmáspequeños.Losbordespuedentenerun grosorquevadelos5alos8mm.ylasparedesdelos6alos9mm.,dependiendodela formadelavasijaydeltamañodelamisma. Decoración

383 Unadelascaracterísticasmásimportantesdelavajillaesladecoraciónacanalada,yasea enlasparedesexternasocercadelbordeinterno.Lasacanaladurasexternassonmás característicasenlosvasos,cántarosycuencos,mientrasquelaslocalizadascercadel bordecorrespondenmásconlosplatos.Lasacanaladurastambiénpuedenserverticalesy encontrarseenlaparteproximaldelabaseenlosplatos.Otroelementodecorativoenlos platospuedeserelbordeonduladoquealgunospresentan.Otrotipodedecoraciónque algunosejemplarespresentansonlasaplicacionesdecarasantropomorfasopastillaje. Decoración Elotroatributoconsistenteloconstituyeelengobenegropulidoquecubrelapieza.En losplatosycuencosselocalizaalisadoypulidoaltotantoexternacomointernamente,en losvasospuedeirtambiénalinteriorperonoconlamismacalidaddepulimentoyenlos cántarosseencuentrasóloenlaparteexterna. Fig.24V.PujónAcanalado VAJILLACHILANGA Fase: ManzanalyMagalena Pasta Elcolordelapastavaríadeblanco,cremayrosado(7.5YR7/4,10YR8/2), predominandoenlamuestrafragmentosdepastacolorcrema.Latexturaesporosa, aunqueesunapastabastantehomogénea,compactaydefracturaregular.Eldesgrasante principalsonloscristalesmuyfinosdecuarzoquenosonmuyabundantes.Presentanuna excelenteuniformidadenelcolordelapasta.

384 Forma Lasformasmáscomunessonloscuencoscuyosbordessoncomúnmenteredondos, aunquetambiénseobservanalgunosplanosoligeramentebiseladosyagudos.Las paredessoncurvodivergentes,curvadas,rectodivergentesodesiluetacompuesta.Las basesporlogeneralsoncóncavasoplanasconalgúntipodesoporte.Elgrosordelos bordesnovaríademasiado,teniendolosmismosentre3y5mm.Lasparedestienenun grosorquevadelos4alos7mm.yeldiámetroaproximadodelasvasijasvadelos15a los25cm.aunqueéstasdimensionespuedenvariar. Decoración LadecoraciónconstituyeelprincipalatributodelavajillaChilangayconsisteenel engobeUsulutánsobreelcualseaplicalapinturaroja(MartínezandMonterroso,2005). Losdiseñosobservadosenlamuestrasongeométricosespecialmentebandasrojasenla parteproximalalbordeenlaparedexterioraligualqueenlaparteproximalalabase. Tambiénseubicandentrodeéstasbandaspuntosrojosounaespeciederombosyotras decoraciones.Tambiénsonmuycomuneslasdecoracionesdefiguraszoomorfas. Acabadodesuperficie Comosemencionóantes,elengobeUsulutánesunodelosatributosconsistentesenesta vajilla,cuyasuperficiesepresentageneralmenteconunalisadoypulidoalto,loqueleda unbrilloespecialalapiezacomosucedeenlasvajillasCopadoryGualpopa. Fig.25V.Chilanga

385 VAJILLAGUALPOPA Fase: Manzanal Pasta Elcolordelapastaesbeige(10YR8/2),latexturafina,homogéneaycompactayde fracturaregular.Loselementosantiplásticosquecomponenlapastasonpequeños fragmentosmuyfinosdepómezycristalesdecuarzo,aunqueenmuypocacantidad, ademáséstoscomponentessondifícilesdeobservarporelcolordelaarcilla.Elcolores uniformeynoseobservancambiostanbruscosenlatonalidadqueseobservaenla fracturadelosfragmentosdeotrasvajillasconpastascafénaranja. Forma Lasformasmáscomunessonloscuencos,aunquetambiénformanpartedelavajillalos vasosyenmuchamenorescalaloscántaros.Losbordessonporlogeneralredondos, aunquetambiénhaybordesligeramenteplanos,otrosderedondosdebiselinterior.Porlo generaldeparedescurvadas,paredescurvoconvergentes,paredesdivergentesycurvo divergentes.Lasbasespuedensercóncavas,redondasyplanas.Lasdimensionesvarían segúnlasformas,peroeldiámetroaproximadodeloscuencosvadelos15alos25cm. aunqueestasdimensionespuedensermayoresomenores.Elgrosordelosbordesenla muestravadelos4alos6mm.Elgrosordelasparedespuedevariardependiendodela formadelavasijaaunqueungrosoraproximadovaríadelos4alos7mm. Decoración Ladecoraciónenestavajillaesvariadapredominandoelusodeloscoloresnaranja,rojo ynegro.Losdiseñosporlogeneralsongeométricos,aunquetambiénhaydecoraciones dezoomorfosypseudoglifos.Porlogenerallasvasijasllevanalgunasbandasdecolor rojoonegroylasfiguraszoomorfasestándelineadasencolornegroalternandoconotros diseñosencolorrojo.Entrelasfiguraszoomorfaspredominanlosmonosylasaves.La vajillaGualpopapuedepresentarúnicamentediseñosgeométricoselaboradosconpintura rojaqueseaplicasobreelengobenaranja.Ladecoraciónpuedeirtantoenelexterior comoenelinteriordelavasijaosolamenteenelexterior. Acabadodesuperficie Constituyeunatributoconsistenteysetratadeunengobecremanaranjaquerecubreen sumayoríalatotalidaddelapieza.Esteseencuentraalisadoypulidoalto,loqueledaun brillomuyaltoalavasija.Ladecoracióndepinturarojaonegraseaplicasobreelengobe.

386 Fig.26V.Gualpopa Fig.27V.Gualpopa VAJILLAJUMUZNALROJO Fase: ManzanalyMagdalena Pasta Elcolordelapastaescafénaranja(5YR6/6),detexturaquevademediaafinay bastantecompacta,muypocoporosaydefracturamásomenosregular.Loselementos noplásticossonlosfragmentosdepiedrapómezbastantefina.Elcolorqueseobservaen alafracturadealgunosfragmentosnoesmuyuniforme,yaquepresentalatonalidad grisáceaalcentrodelamisma,enotrocasossiseobservaciertauniformidad. Forma Laformabásicasonlosplatos,aunquesepuedenencontrartambiéncuencoscon característicassimilares.Losbordessonredondosymenorcantidadligeramentedebisel redondoenelinterior.Lasparedesconstituyenunodelosatributosconsistentesyaque enlosplatossonligeramentecurvoconvergentes,mientrasqueenloscuencospueden sersolamentecurvadas,portantonoexisteenestavajillaotrotipodeparedes.Lasbases porlogeneralsonplanasocóncavasycasisiemprellevansoporteanular.Algunos fragmentossondifícilesdeubicar,yaquetiendenaconfundirseconlavajillaCantoral, estosegúnRomero(comunicaciónpersonal,2005)debidoaquelosplatosdelavajilla JumuznalRojoevolucionanparafinalesdelClásicoTempranoeiniciosdelClásico MediodelavajillaCantoral,siendoesosmaterialesunexcelenteindicadortantodela temporalidadcomodelacontinuidad,cambioseimportanciadelacerámicacomo indicadorparaelestudiodeunasociedad.Encuandoalasdimensionesdelasvasijas, éstastienenungrosordebordedeaproximadamenteentre4y9mm.,ungrosorde paredesde5a9mm.quetiendeasermásgruesoenlaparteproximalelbordeymás delgadaconformellegaalabase.Eldiámetroaproximadoenloscuencosesde13a24

387 cm.mientrasqueenlosplatosesde22a30cm.Laalturaaproximadadeunplatocon todoysoporteanularesde5cm. Decoración Laúnicacaracterísticadecorativaquepresentaestavajillaeslabandadepinturarojaque vadesdeelbordehastaunoodoscentímetrosdelaparedexterna.Enalgunoscasos puedelabandarojaserunpocomásextensaytambiénenalgunoscasoséstapuede extendersesobrelaparedinterna. Acabadodesuperficie Enelexterior,lasvasijaspresentanúnicamenteunalisadoypulidomediosinpresentar engobe.Enelinteriorgeneralmentellevanengobecafénegroquevaalisadoypulidode medioaalto.Enotrasocasioneselengobeinteriorescafénaranjaquetambiénse presentaalisadoypulido.Labasesólosepresentaconunburdoalisado. Fig.28V.JumuznalRojo VAJILLACOPADOR Fase: Magdalena Pasta Lapastaesdecolorbeige(10YR8/2),latexturaesfina,homogénea,duraycompactay lafracturaesregular.Elelementoantiplásticodelapastasonloscristalesdecuarzomuy muyfinos,quenosonmuyabundantes.Enlafracturaseobservaunaexcelentecocción,

388 puesseobservaunauniformidadenelcolor.Lasvariantesdepastacafénaranjaseha justificadocomounaproducciónlocal,imitandolasvariedadesdecopadorelaboradasen HondurasyElSalvador(MartínezandMonterroso,2005). Forma Lasformasbásicassonloscuencosyvasos,conbordesredondos,ligeramentedebisel redondoenelinteriorobordesplanos.Lasparedesenloscuencospuedensercurvo divergentes,desiluetacompuestaparedescurvadas.Enlosvasosporlogenerallas paredessonrectasoligeramenterectodivergentes.Lasbasessoncomúnmenteplanaso cóncavas.Lasdimensionessonvariadas,desdecuencospequeñosaotrosdemayor diámetro.Elgrosordelosbordesvadelos5alos7mm.ylasparedestienen aproximadamentelamismadimensión. Decoración Ladecoracióndelavajillaespolicroma,conpredominiodeloscoloresnegroyrojo, aunquetambiénseencuentrandecoracionesennaranja,blancoyrojohematitaespecular. Losmotivosdecorativossonvariados,desdediseñosgeométricoshastafiguras antropomorfas,zoomorfas,pseudoglifos,entreotros.Loscuencospuedenpresentar decoracióntantoenlasparedesexternascomoexternasdelavasija,mientrasquelos vasosúnicamenteestándecoradosenelexterior.Elatributoprincipalparadefinirlas distintasvariedadesdeCopadoresladecoración. Acabadodesuperficie Otracaracterísticadelavajillaeselengobequepresentanlaspiezas,quegeneralmente vadelcolorcremaalnaranja.Generalmenteestesepresentaconunpulidoalto,aunque tampocosonextrañaslassuperficiesmates(MartínezandMonterroso,2005;citandoa Viel,1993). VAJILLAJARALROJO Fase: Magdalena Pasta Lapastaescafénaranja(5YR6/6),detexturamediaafina,bastantehomogéneay compacta,defracturamuyregular.Eldesgrasanteestácompuestodepiedrapómez molidamuyfina,yenalgunoscasosalgunaspartículasdemicayfinoscristalesde cuarzo.Lapiedrapómezeselelementoantiplásticomásimportanteenlapasta,aunque noesmuyabundantecomoenotrasvajillas.Lacocciónquepresentanlosejemplaresde lamuestraesbastanteuniforme,auquecontendenciaalcolorcaféqueseobservaenla fractura. Forma Laformabásicadelavajillasonlosplatosgrandes,aunqueenestamuestrasehan incluidoalgunoscuencosquepresentancaracterísticassimilares.Losbordesson

389 redondos,algunoscompuestos,especialmenteenlosplatos,otrosligeramenteplanosen ellabioyenmenorcantidaddebiselplanoenelinterior.Lasparedesdelosplatos constituyenunodelosatributosconsistentesmásimportantesdelavajillaaunquelos cuencosqueseincluyeronenestavajillanopresentanéstacaracterística,yconsisteen paredescurvodivergentesodesiluetacompuesta,loquelodiferenciadelosplatosdelas vajillasCantoralyJumuznalRojo.enloscuencossepuedenencontrarparedesrecto divergentes,perotambiéncurvodivergentes.Lasbasessonporlogeneralplanaso ligeramentecóncavas.Losplatoscasisiempresontetrápodes,consoportesredondos, amorfosocónicosperosiemprevaciados.Enlosplatoslasdimensionesdelosbordes varíandelos5alos9mm.,elgrosordelasparedesdelos5alos5mm.yeldiámetro aproximadoesde17a30cm. Decoración Ladecoraciónprincipalquepresentalavajillaeslapinturarojaqueconstituyeotrodelos atributosconsistentes.Dichapinturaseubicaporlogeneralsóloenlasparedesexternas deloscuencosyplatos.Losplatospuedenllevartambiénaplicaciones,generalmentede carasantropomorfasopequeñasbandasaplicadasenformaverticalubicados generalmenteenlapartepróximaalabase. Acabadodesuperficie Lasuperficieexternadelasparedesestácubiertaconpinturarojacasisiempresólo presentabajopulido.Laparteinternacomúnmentepresentaunengobecafénegroo puedeencontrarseúnicamenteconunalisadoybajopulido. Fig.29 V.JaralRojo

390 VAJILLAESPUMUYAPLICADO Fase: Magdalena Pasta Lapastaescafénaranja(5YR6/6),latexturaesmediaunpocoporosa,homogéneay compactaydefracturamásomenosregular.Elelementonoplásticoeslapiedrapómez muyfina,conalgunosfragmentosdemayortamaño.Sinembargolacantidaddepómez noesmuyabundanteyenalgunoscasosseobservantambiénalgunoscristalesdecuarzo muyfinosyenotros,mayorabundanciademica.Adiferenciadeotrasvajillas,lavajilla EspumuyAplicadosipresentaunauniformidadcasitotalenelcolordelapasta, indicandoposiblementeunaexposicióncontroladayuniformedurantelacoccióndelas piezas. Forma Laformaquecaracterizaéstavajillasonlosincensariosbicónicos.Losbordesdelcuenco superiorsonredondosylosbordesdelsoportedepedestalporlogeneralsondelabio plano.Lasparedesdelcuencosuperiorsuelensercurvodivergentesoligeramentecurvo divergentes.Lasbasesentreelcuencoyelsoportedepedestalesplana.Elsoporteque sostienealcuencoessiempredepedestaldeunaalturaaproximadaalos8cm.Encuanto alasdimensiones,generalmenteelcuencosuperiortieneaproximadamentelasmismas dimensionesqueeldiámetrodelsoportedepedestal.Elgrosordelosbordesdelcuenco varíadelos5alos8mm.ylaparedungrosoraproximadodeentre6y11mm.El soportetieneungrosorquevadelos5ylos10mm.ylasparedesdelsoportedeentre6y 12mm.Eldiámetroaproximadodelcuencosuperioresdeentre26a32cm.Elsoporte poseetieneentre18y25cm.dediámetro. Decoración Ladecoraciónqueseobservaenlosincensariossonlasaplicacionesdeespiga,elemento queademásdelaforma,tambiénconstituyeelatributoconsistentedelavajilla.Las espigaspuedenircolocadasenlíneaverticalyencontrarseensoloenunodelosladosde laparedexternadelcuencosuperior.Enotroscasospuedellevarlasaplicaciones alrededordetodalaparedexternayeltamañoycantidaddelasmismasvaríaencada muestra.Elsoportegeneralmentenollevaningunadecoración,salvoenalgunoscasos dondepresentanrestosdepinturablanca,posiblementefugitiva,sobrelaparedexterna delsoportedepedestal. Acabadodesuperficie Tantolasuperficiedelcuencocomodelpedestal,únicamentepresentanunburdoalisado ynopresentanengobeoalgúngradodepulimento.

391 VAJILLAZACATALALISADO Fase: Magdalena Pasta Lapastaescafénaranja(5YR6/6),detexturamedia,defracturairregular.Eldesgrasante predominanteeslapiedrapómezenfragmentosfinos,aunquealgunosdemayortamaño. Otroelementoqueapareceenalgunosejemplareseslamica,quesecombinacon fragmentosdepiedrapómez.Elcolorqueseobservaenlapastaesregularmente uniformeenlaszonasmásdelgadasyconlafranjagrisáceaalcentro. Forma Estavajillaestácompuestaexclusivamenteporcántarosdegrantamaño,cuyosbordes sontotalmenteevertidosydelabioredondo.Elcuelloesporlogeneralcurvodivergente yelcuerposeguramenteesglobularosubglobular.Lasbasespuedensercóncavaso ligeramenteplanas.Nopresentanasasovertedera. Decoración Estoscántaroscarecendedecoraciónalguna. Acabadodesuperficie Ademásdelbordeevertido,elsiguienteatributoconsistenteeslasuperficiealisadamedia quepresentan,sinlapresenciadeengobeopintura. VAJILLAPAJARAL Fase: Magdalena Pasta Elcolordelapastaescafénaranja(5YR6/6),latexturaesmedia,defracturairregular conalgunosporos,perobastantehomogénea.Elcomponenteantiplásticopredominante eslapiedrapómezenfragmentosmuyfinos,aunquealgunosdemayortamañomiden entre0.1y0.3milímetrosdediámetro.Engranpartedelamuestraseobservóabundante micacomoelementoantiplástico.Esposiblequeseaestavajillalaquemáspresenta fragmentosdemicacomodesgrasante.Ademáslapastapresentaunabuenacoccióncon uniformidadenelcolordelapasta. Forma LasformascaracterísticasdelavajillaPajaralsonformasespeciales,entreellaslos comalesylossahumerios,aunquetambiénsehanincluidodentrodeéstamuestra fragmentosdeotrasvasijasespecialescomournas.Losbordesenloscomalesson redondos,algunosengrosadosenambaslados,otrosredondosengrosadosenelinterior. Enlossahumerioslosbordestambiénsonredondos,algunosligeramenteplanos.Las paredesdeloscomalespuedenserrectodivergentes,desiluetacompuesta,rectas, curvadasosinpared.Enlossahumeriossongeneralmentecurvadasoligeramentecurvo divergentes.Lasbasesporlogeneralsonplanasenloscomalesyligeramentecóncavas

392 enlossahumeriosyéstosúltimosllevanmangosquepuedenvariardeforma.Las dimensionesdeloscomalesvaríanelgrosordelosbordes,quevandesdelos8alos18 mm.elgrosordelasparedesde11a17mm.yundiámetroaproximadodemásde40cm. Lossahumeriostienenungrosordebordesdeentre6y11mm.ungrosordeparedque vadelos7alos13mm.yundiámetrode14a16cm.aproximadamente. Decoración Enloscomalesladecoraciónprincipaleslapinturaroja,yaseaúnicamentesobreel borde,paredeseinclusoenlasuperficiedelcomal.Algunasparedesexternasdelos comalestambiénpresentandecoraciónconpinturaroja.Algunossahumeriostambién presentanpinturarojaonaranja,especialmentesobreelmango.Además,laprincipal característicaenladecoracióndelossahumeriossonlasfigurillaszoomorfasquese encuentranporlogeneralenlapartesuperiordelmango,queporlogeneralsonaves, lagartos,perros,monos,jaguares,entreotros. Acabadodesuperficie Generalmente,lossahumeriossolamentepresentanunalisadoburdoynollevanengobey tampocoseencuentranpulidos.Loscomalessolamenteestánalisadosenlapartesuperior, yalgunospresentanunaespeciedeengoberojomuyfino,casisiempreconabundante mica. VAJILLAARIPÍNINCISO Fase: Magdalena Pasta Lapastaesdecolorcafénaranja(7.5YR6/6),detexturamedia,conalgunosporos aunqueavecesbastantefinaydefracturamásomenosregular.Eldesgrasanteprincipal eslapiedrapómezmolidaybastantefina,algunosfragmentosdemica,peronoagran escalayalgunoscristalesdecuarzo.Lacocciónqueseobservaenlafracturaesbastante buena,aunquealgunosfragmentospresentandostonalidadesenelcolor. Forma Lasformasbásicassonlosvasosyloscuencospequeños.Predominanlosbordes redondos,otrossonligeramenteagudosytambiénhayalgunosplanos.Lasparedesde losvasossonporlogeneralrectasyligeramentecurvasenloscuencos.Lasbasesson planasoligeramentecóncavas.Loscuencosaligualquelosvasostienenbordesque varíanentrelos4ylos7mm. Decoración Losincisossonvariados,desdesimpleslíneasonduladasuhorizontales,másomenos ubicadasenlapartemediadelapared,hastaotrosmáselaboradosquepresentangrecas, posiblespseudoglifosybolutas.Tambiénsepuedenobservarabundantesdiseños geométricos,líneas,petatillos,triángulos,círculos,etc.

393 Acabadodesuperficie Unodelosatributosmásimportantesdelavajilla,ademásdelincisoeselengobecafé naranjaqueposee.EstepuedefácilmenteconfundirseconlavajillaPinalIncisoquelleva unengobecafénegro,conlavajillaJícaroIncisoqueposeeunengobenaranja.Sin embargo,lavajillaAripínIncisonopresentalabandarojaenelbordeylosincisosson másfinosydiversos.Elengobecafénaranjaporlogeneralpresentaunalisadoypulido quevademedioaalto. Fig.3 0V.AripínInciso VAJILLACHISPANROJO Fase: Magdalena Pasta Estematerialnoesmuyabundanteenlamuestraycomúnmentepresentaunapastacafé naranja(5YR6/6)ysólounfragmentoqueseincluyóenestegrupoporsus característicasposeeunapastaroja(2.5YR4/6).Latexturaesmedia,pocoirregularenla fracturaymásomenoscompactaynomuyhomogénea.Eldesgrasanteenlaspastas cafénaranjaesunamezcladecristalesdecuarzolechosoconfragmentosdepiedra pómezmolida,mientrasqueenlapastarojaseobservancristalesdecuarzoy posiblementeferruginosos.Otrofragmentoposiblementeposeearenaderíocomo elementonoplásticodelapasta.Encuantoalacocción,unapartedelamuestrapresenta uniformidadenelcolor,mientrasqueenelrestoseobservaunatonalidadgrisácea. Forma Laescasezdelamuestrapresentaúnicamentefragmentosdecuencospequeñosy posiblementevasos.Losbordesengeneralsonredondosysólounoesplano.Lasparedes soncurvasoligeramentecurvodivergentes.Nohaymuestradebases,perose seguramenteseanplanasycóncavascomoenlamayoríadevajillas.Loscuencos posiblementetienenundiámetroaproximadode12cm.yelgrosordelosbordesdela muestravadelos5alos8mm.muysimilaraldelasparedesquevaríamuypoco,entre los4alos8mm.

394 Decoración Lacaracterísticamásimportanteeslapinturarojahematitaespecularquecubrelapieza, aunquetambiénpuedenpresentaracanaladurasoincisosquenoconstituyenunatributo fundamentalparasuidentificación. Acabadodesuperficie Lapinturarojoespecularquecubrelapiezadebetomarsecomoelprincipalacabadode superficie,yaqueporlogeneralestotalycuandoesparcialsóloelinteriorpuede presentaralgúntipodeengobeoscuroounodecolorcrema,otambiénpresentarrojo especularenelinterior.Estapinturaledaunabrillantezexcepcionalalasvasijasque conformanestavajilla. VAJILLACASACAESTRIADO Fase: Magdalena Pasta Elcolordelapastaescafénaranja(5YR6/6),latexturaesmedia,enalgunoscasosse fracturaconciertafacilidad,tambiénesunpocoporosa.Lapiedrapómezesel desgrasantemásimportanteenlacomposicióndelapasta,aunquealgunosfragmentos tambiéncontenganarenaderío.Lacocciónesregular,yaquealgunasmuestraspresentan enlafracturalatonalidadgrisácea,especialmenteenlaszonasgruesascomolosbordesy elgollete. Forma Predominanloscuencos,aunquetambiénhaycántarosgrandes.Losbordessonredondos, enloscántarosengrosadosenelinterior,enloscuencossontambiénredondos,redondos engrosadosenelexterior,planosengrosadosenelexterioryplanosdebiselinterior.Los cuellosdeloscántarossoncurvodivergentesyelcuerpoposiblementesubglobular.En loscuencoslasparedessonligeramentecurvoconvergentesylasbasescóncavas.No presentanasas,vertederasosoportes.Elgrosordelosbordesenloscántarosvadelos6a los10mm.,enloscuencosdelos5alos13mm.Eldiámetroaproximadoenloscántaros varíadelos28alos42cm.,entreloscuencosvaríadelos17alos42cm. Decoración Generalmenteposeenunabandarojaonaranjaenelborde,loscántarosextendida aproximadamentedoscentímetroshaciaelinterior;enloscuencos,sóloenelbordeo labio.Ladecoracióneselestriadomedio,generalmenteorientadohorizontalmentesobre elcuerpodeloscuencosycántaros.Laorientaciónprácticamentenovaríaysalvoenlos cuellosdeloscántaros,dondeladecoraciónpuedeserunacombinacióndelestriadocon punzonadoaligualqueenlavajillaMapacheEstriado.

395 Acabadodesupeficie Elacabadodesuperficieprevioaefectuarelestriadoseguramentefueúnicamenteun burdoalisado,yaqueniloscántarosniloscuencospresentanengobe.Enelcasodelos cuencoslaparteinternaseencuentratambiénsolamenteenunaalisadoburdoomedio. Fig.31 V.Casaca Estriado VAJILLAENCANTOESTRIADO Fase: Magdalena Pasta Decolorcafénaranja(5YR6/6),latexturaesmedia,enalgunoscasosunpocoporosay enotrosmáscompacta,lafracturaesirregular.Eldesgrasanteeslapiedrapómezaunque enalgunoscasostambiénseobservaarenaderío.Otroelementoutilizadoenalgunos ejemplaresdelavajillasonlosfragmentosdemica.Comoenlamayoríadevajillas, algunosfragmentospresentanunauniformidadenelcolordelapasta,mientrasqueotros no. Forma Lavajillasecomponecasiexclusivamentedecuencos,aunquetambiénexistenalgunos bordesdecántarosyenmenorcantidadaúndevasijasconbocarestringida.Enlos cántaroslosbordessonensumayoríaredondos,algunosengrosadosenelinteriory generalmentesonbordesevertidosodivergentes.Entreloscuencoshaybordesredondos yplanos,predominandolosprimerosqueseencuentranlevementeengrosadosenel interior,mientrasquelosplanospuedenestarengrosadosenelexterioroserligeramente biselados.Elcuellodeloscántarosescurvodivergente,decuerposubglobularydebase cóncava.Loscuencostienenparedesligeramentecurvodivergentesocurvas,no presentanasasnialgúnotroaditamento.Elgrosordelosbordedeloscántarosvaríade los7alos12mm.,conundiámetroaproximadode24a30cm.Entreloscuencosel grosordelbordevade10a16mm.,eldelasparedesde5a12mm.conundiámetro aproximadode27a38cm.

396 Decoración Ladecoraciónescasinula,yaquealgunossólopresentanunabandarojaenelbordeyel estriadomásquedecoraciónpareceserelacabadodesuperficie,puesnopresentanun diseñoopatrónespecífico.Tampocoseobservaunadecoracióndistintaparaloscuellos deloscántaroscomoenlasvajillasCasacayMapacheEstriado. Acabadodesuperficie Nopresentanengobe,yelestriadopuedeconstituirelacabadodelasuperficieyaquees muyfinoysinunpatrónespecífico.Elinteriorpuedepresentarunalisadoburdoomedio entreloscuencos. Fig.32 EncantoEstriado VAJILLACOCALLISO Fase: Magdalena Pasta Lapastaestambiéncafénaranja(/.5YR6/6),detexturamedia,fracturaregulary bastantehomogéneaycompacta.Elprincipalelementonoplásticoaligualqueenelresto delasvajilladelaregióndelMotaguaestácompuestoporpiedrapómezmolida,aunque enestecasotambiénseobservaabundantesfragmentosdemicaquevasustituyendocada vezmásalapiedrapómezcomodesgrasante.Latonalidadqueseobservaenlafractura esbastanteuniforme,loqueindicaríaunacocciónbastantebuena. Forma Lavajillasecaracterizaporestarcompuestaúnicamentedevasijasconbocarestringida, lamayoríadeellosconborderedondo,algunosdeellosengrosadosenelinterior,otros ligeramenteplanos.Elatributoconsistentedelavajillaestáenlasparedesquesoncurvo convergentes,peroretorcidasacausadelaformadelavasija.Nopresentanasaoalgún

397 otroaditamentoylasbasesseguramentesonplanasoligeramentecóncavas.Elgrosorde losbordesvaríadelos6alos10mm.ylasparedesdelos5alos12mm. Decoración Estasvasijasporlogeneralnopresentanningúntipodedecoración. Acabadodesuperficie Otroelementoimportanteperonomuyexaltadoparaidentificarlasvasijascocalliso,es precisamenteelalisadoburdoqueéstaspresentanenlaparedexterior,yaqueno presentanningúntipodeengobeopintura. VAJILLAYAJALROJO Fase: Magdalena Pasta Lapastaesdecolorcafénaranja(7.5YR6/6),latexturaesdemediaagruesa,de composiciónmásbienheterogéneaydefracturairregular,lapastatambiénposeealgunos poros.Lacomposiciónheterogéneadelapastasedebeaquecontieneunamezclade elementosnoplásticos,conpredominiodelapiedrapómezyposiblementearenaderío, mezcladaconcristalesdecuarzo.Losfragmentosdepiedrapómezquesonlosmás abundantesyfácilesdeobservarsepresentandesdepartículasmuyfinashasta fragmentosqueoscilanentre0.1y0.4mm.dediámetro.Casitodoslosfragmentos presentanlacaracterísticatonalidadgrisáceaalcentrodelafractura. Forma Lamuestrasecomponeexclusivamentedecántaroscuyosbordesporlogeneralson evertidosodivergentes,aunquealgunossonmuchomásdirectosqueotros.Estossoncasi siempreredondosengrosadosenelexterior.Loscuellossoncurvodivergentes,algunos másaltosqueotros.Lapartedelcuerpoesmuydifícildeestablecerconexactitudla forma,peroposiblementeporeltamañoseansubglobularesoglobulares.Lasbases seguramentesonplanasocóncavas.Comoenotrasvajillasdecántaros,estosno presentanasas,soportes,vertederasnialgúnotroaditamento.Elgrosordelosbordesva delos7alos14mm.yeldiámetroaproximadodelos29aunpocomásde40cm. Decoración Laúnicadecoraciónquepresentaneslabandarojonaranjaenelbordeyenalgunos casosseobservantambiénlíneasmuyescasasydispersasenelcuello. Acabadodesuperficie Elacabadodesuperficieconstituyeposiblementeelprincipalatributoconsistenteyse tratadeunbañoposiblementedepinturacremaquelodiferenciadelrestodecántaros. Lasuperficienopresentaengobeyúnicamentesetieneunalisadomedioaburdo.

398 VAJILLAPIÑALACANALADO Fase: Manzanal Pasta Pastacafénaranja(7.5YR6/6),detexturafina,másomenoscompactaydefractura regular.Eldesgrasanteestácompuestodepiedrapómezyenalgunoscasossemezcalcon finoscristalesdecuarzo.Lapastatambiénpuedecontenerenmenorcantidadfragmentos demica.Seobservalatonalidadgrisáceaenlafracturadealgunosdelosejemplares. Forma Existenenlavajillaplatosquesonlosmáscomunes,perotambiénhaycuencosovasos. EnlamuestradelProyectodeJade2005,estavajillaespocorepresentativa.Losbordes sonredondosocompuestoséstosúltimosporlogeneralenlosplatos,lasparedes puedensercurvodivergentesenplatos,ligeramentecurvasencuencosyrectasenlos vasos.Losplatossonbastanteabiertosconbordesevertidos.Lasbasessongeneralmente planasylosplatospuedenllevaralgúntipodesoporte.Sinembargoestonosedetectóen lamuestra. Decoración Ladecoracióncaracterísticaelacanalado,queenlosplatosseubicageneralmenteenla paredinternaoexternayenloscuencosyvasosenlapartemediadelapared.Noseha observadootrotipodedecoración,aexcepcióndequelosplatospuedentenerunborde ondulado. Acabadodesuperficie Otrodelosatributosconsistenteseselengoberojoquedebenpresentarlasvasijasdela vajillaPiñalAcanalado,elcualsepresentacasisiempreconunaltopulidoy comúnmentecubrelaparteinternayexternadelavasija. VAJILLAARENALINCISO Fase: Manzanal Pasta Lapastatieneuncolorcafénaranja(5YR6/6,10YR8/3),latexturaesfina,compactade fracturaregular.Loscomponentesnoplásticossonvariados,peroenmuypocas cantidades,observándosealgunoscristalesmuyfinosdecuarzo,fragmentosmuyfinosde pómezmolidayfragmentosdemica.Seenestavajillaunauniformidadenlacocción, posiblementeporlafinezaydelgadezdelasparedes. Forma Porlogenerallasformasbásicasonloscuencosyvasosconbordesredondos,deparedes curvadas,ligeramentecurvodivergentesorectas.Lasbasessonplanasoligeramente cóncavas.Lasdimensionesdelasvasijassonpequeñas,conungrosordebordesqueva delos3alos5mm.

399 Decoración Unodelosatributosdelavajillaeselinciso,generalmentefino,sobrelasparedes externasdeloscuencosyvasos,Losmotivospuedenvariar,perocomúnmenteson geométricos,conlíneasfinas,petatillos,ofigurassimplesderostros,espirales,grecas, cuadros,triángulos,uotrasformas. Acabadodesuperficie Esteesunodelosatributosconsistentesimportantesdentrodelaramadelosincisos,ya queelArenalIncisodebellevarunengobequevadeblancoacrema,casisiempre internayexternamente,aunqueenelinteriorpudellevarunengobecolornaranja.La superficieporlogeneralllevaalisadoypulidoalto. VAJILLAZARZAL Fase: Magdalena Pasta Lapastaesdecolorcafénaranja,detexturamediaafina,defracturaregular.Presentael desgrasantedepómezaunquetambiénseobservanenalgunoscasosfragmetosdemicay cristalesdecuarzo.Lacocciónesbastanteuniformeaunqueseobservaenalgunos fragmentoscambiosenlatonalidad. Forma Lasformasmáscomunessonloscuencosconbordesredondos,deparedesrecto divergentesoligeramentecurvadasocurvoconvergentes.Lasdimensionesnosonmuy grandesylamuestraesmuyescasaparadeterminartodassuscaracterísticas. Decoración Ladecoracióneselincisomedioygruesoformandoalgunosdiseñosmuycomplejosyno tansimplescomoelrestodelamuestraqueconformanlosincisos.Ademáspuede presentarlabandaroja,aunqueestonoseobservóenlamuestraporlaescasezdebordes. Algunospresentanapersonajesyotrasformasmáscomplejas. Acabadodesuperficie Lasuperficiepresentaunabañodepinturablancayenlasáreasquenoestánincisasun alisadomedio. Resultadospreliminareseinterpretación EnelanexoNo.1sepuedenobservarlacantidaddematerialesporoperacionesypor vajillas,paratenerunavisiónrápidadelatemporalidadporoperacióny

400 VAJILLAGUARANJAROJO Fase: MagdalenaaPalmilla Pasta Elcolordelapastaescafénaranja(7.5YR6/6y5YR6/6),detexturamedia,fractura irregular.Elprincipaldesgrasanteeslamica,locuallodiferenciadealgunosejemplares condesgrasantedepómez.Elcolorqueseobservaenlafracturadelostiestosesmuy regular. Forma Loscántarosgrandesylastapaderassonlasformasmáscomunes,perotambiénexistan algunoscuencos.Losbordesredondosoligeramenteplanos,casisiempreengrosadosen elexterior.Loscuerposposiblementeseanglobularesosubglobularesconbases cóncavas.Loscuencosposeenparedesligeramentecurvoconvergentes.Loscántarose inclusoloscuencospuedenpresentarasasgrandes.Lasdimensionessondecántarosmuy grandes,conundiámetroqueinclusorebasalos40cm. Decoración Ladecoraciónmásimportanteeslapinturarojaquepuedeencontrarseenelborde,cuello, cuerpoyasas,condiseñosnomuyvariados,algunasvecespuntosrojos,líneas,manchas círculos,entreotros.Lastapaderasquepresentanasa,llevanporlogeneralpinturaroja formandocírculos. Acabadodesuperficie Solamentepresentanunburdoalisadoqueavecespuedellegaramedio.Nopresentan engobenipulimento. OtrasVajillas Porsupresenciaenmenorescala,sunuevaintroducciónalatipologíapropuestaparala regióndelMotaguaosuproducciónforánea,sedescribenbrevementeacontinuación otrasvajillaspresentesenlamuestradelProyectodeJade2005: VAJILLAPLOMIZO Fase: Palmilla LavajillaPlomizopresentaunapastadecolorcrema(2.5Y8/3,8/4),latexturaesmuy finaycompactaydura,defracturaregular.Nosehapodidoidentificareltipode desgrasante,porselapastademasiadofina.Lafracturapresentalafranjagrisalcentro. Lasformassondifícilesdedeterminarporlaausenciadebordes,peroloscuerpos posiblementeindicanvasosycántaros.Elúnicobordequesepresentaenlamuestraes redondoyunadelasbasesesplana.Lasdimensionesindicanquesonvasijaspequeñas, conungrosordebordede6mm.yelrestodecuerpotienenungrosordepareddeentre los3ylos5mm.Laúnicadecoraciónqueseobservaeselacanaladovertical.Encuanto

401 alacabadodesuperficie,ésteconstituyeelatributoprincipalporquepresentaunengobe naranjaquefuecubiertoconunacapadeplomoqueledaunbrillocaracterístico. VAJILLATIQUISATE Fase: Magdalena Lamuestracuentasolamentecondosposiblesfragmentos,unodeengobenaranjayel otrocrema,porloqueesdifícildescribirtodassuscaracterísticas. VAJILLAMANDARINDALINCISO Fase: Magdalena Losmaterialesdeestegrupoconformanunanuevavajillaenlatipologíadelaregióndel MotaguaMedio.Elcolordelaspastaenéstavajillaesporlogeneralcafénaranja (7.5YR6/6,5YR5/6,5YR5/8,7.5YR5/8),latexturadeesfina,compactaydefractura regular.Eldesgrasantesecomponedeinclusionesdepómezmuyfina,ademásde pequeñoscristalesdecuarzolechoso,tambiénmuyfinos.Lacocciónquepresentaes muybuenaporlauniformidadenelcolordelapasta. Entrelasformasobservadasseencuentranloscuencosytalvezvasos,losbordesson redondosoligeramentedebiselplanoenelinterior.Lasparedessonligeramentecurvo divergentes,ligeramentecurvadasyrectasylasbasessonplanas.Lasdimensionesdelos cuencossonpequeñasyelgrosordelosbordesvadelos4alos5mm.Ladecoraciónes elincisofino,generalmentesólolíneashorizontales,verticalesoinclinadas,sinpresentar algúnpatrónespecífico.Elacabadodesuperficieconstituyetambiénunatributo consistentealigualqueladecoracióndeincisofino,pueslasuperficiepresentaengobe naranjainternayexternamente.Otrospresentanenelinteriorunengobedecolordistinto, avecesbeigeonaranjapálido. VAJILLAMANZANOTAL Fase: Magdalena? Lapastaescafénaranja,lasformassonbásicamentecuencosdeparedescurvadaso ligeramentecurvoconvergentes,presentanlacaracterísticadequeenlaparteexternade laparedposeenunalisadoyunpulidomedio,mientrasquelaparteinteriorllevanpintura roja.Losbordestambiénsoncaracterísticos,puessiempresonengrosadosenelinterior. Puedenonollevarasasverticales,ylamuestraenestematerialeramuypequeña.

402 VAJILLATUNAL Fase: Magdalena? Seincluyóenestegrupocasisólocuerposdealgunasvasijasquepresentanunabanda impresacomoelementodecorativo,peronosepudoestableceraquevasijapertenecían, esdecirnosecuentaconbordesquenosayudenaidentificarlasformas,aunqueporlo generalparecensercuerposdecántaros.Lapastaescafénaranja,lamayoríacon abundantemicacomoelementodesgrasantedelapasta. VAJILLATERRONAL Fase: MagdalenaaPalmilla Elcolordelapastaescafénaranja(5YR6/6),detexturaburdaensumayoría,defractura irregularmuyporosayheterogénea.Comodesgrasantepresentaabundantemica,en algunoscasosfragmentosdepiedra,talvezesquistoogreenstone,peroenfragmentosde grantamañoentre2y3mm.Enalgunoscasoslapastatambiéncontienefragmentosde pómezycristalesdecuarzo.Lacocciónsepresentauniforme.Encuantoalasformas, predominanloscántarosdecuellopequeñoyloscuencos.Losbordesporlogeneralson muyredondos,engrosadosgeneralmenteenelexterioryotrosenelinterior.Loscuerpos sonposiblementesemiglobularesyloscuencosconparedesligeramentecurvo divergentes.Lasbasesseguramenteeranplanasocóncavas.Lasdimensionesdelas vasijas,especialmenteenloscántaros,losbordeslleganhastalos20mm.ylasparedesde los4alos15mm.Lavajillanopresentaningúntipodedecoraciónyelacabadode superficieesmuyburdo,posiblementesólounburdoalisado.Loscántarospuedenllevar asasverticales. VAJILLAPAPAYAL Fase: ? Estavajillasehaclasificadocomonueva,porcarecerenlatipologíaungrupoque contengamaterialesconunengobenaranjapálidocomoelqueseincluyóenlavajilla Papayal.Laspastassoncafénaranja,nopresentanmayordecoración,aunqueunodelos fragmentos–alparecerunvasollevadecoraciónacanalada.Elatributoconsistenteen estecasofueelengobenaranjapálido,ylasformasqueseobservaronfueroncuencos, cántarosyvasos.Encuantoalatemporalidadmuydifícildedeterminar,debidoala muestratanpequeña,perovariosdelosejemplaresprocedendelosnivelesmás tempranos.

403 VAJILLAJOCOTAL Seformóestavajillaconfragmentosdeloqueparecensertapaderascondistintos engobesperoconcaracterísticassimilarestalescomoagujerosenlapartesuperior, decoraciónpunzonadaypequeñasaplicacionescomodebotóndondeseencuentranlos agujeros.Lastapaderasoformaespecialsondecolorrojoycafé. VAJILLAUSULUTÁN Fase: Motagua Elcolordelapastavadeblancoacrema(10YR8/2,2.5Y8/3,8/4),aunquetambiénse incluyeronaquíposiblesFalsoUsulután,sobretodoporqueenalgunasdecoraciones negativastambiénhaypastascafénaranja(5YR6/6),queseguramentesonlocales.La texturaesmuyfina,siendodifícildeobservarelcomponenteantiplásticodelapasta.Se observaenelbordeoáreamásgruesalatonalidadgrisácea,peroelrestopresentanuna buenacocción.Entrelasformasqueseobservaronenlamuestraseencuentranlosplatos yloscuencosdebordesredondos,planosconacanaladura,redondosengrosadosenel interioryalgunosligeramenteagudos.Lasparedessoncurvodivergentesodesilueta compuesta,paredescurvas,entreotras.Lasbasessonplanasoconvexas.Elgrosordelos bordesvaríadelos6alos12mm.yeldelasparedesdelos5alos7mm. Ladecoraciónesnegativaconcolorescremaymarrónocafécorinto,yelrestoen colorescremaynaranja,algunasenrojo.Porlogeneralsonbandasolíneasyelplato llevaladecoraciónmáscaracterísticaeimpresionanteenlamuestradeladecoración usulután.Algunosllevanelnegativosóloalinterior,mientrasqueotrosentodoelcuerpo. Elacabadodesuperficieesdeunaltopulidoporelbrilloquepresentanlosfragmentos. CERÁMICAPOLICROMA Fase: ? Laspastassondecolorrojoybeige(2.5YR6/8,2.5Y6/3,2.5Y7/4),latexturaesfina, compactayhomogéneaenlostresejemplares,dondeesdifícilobservarloselementosno plásticos.Unodelostiestosposeedesgrasantedepómezmuyfina,otrodelostiestos poseefragmentosferruginososrojizos,otropresentafragmentosferruginososnegrosy pómez.Todospresentanuniformidaddecolorenlafracturayportantounaexcelente cocción. Lasformassondeunplatoconpestañabasal,ydoscuencos.Losbordessonredondosy planos.Lasparedesdelplatosoncurvodivergentes,ydeloscuencossonrecto divergentesydelotrorectasoligeramentecurvas.Elgrosordelosbordesesdeaprox.4 y5mm.Ladecoraciónespolicroma,enelplatolaparteinteriordelasparedestiene pintadoslospiesypiernasloquepodríanseralgunospersonajes;enlasparedesexternas presentaunadecoraciónconmotivosgeométricos,aligualquelabasequetambiénestá decoradajuntoconelfondodelplato.Unodeloscuencosposeelíneasnegras,blancasy

404 unabandaroja,grecasytambiénlabaseestádecorada.Elotrocuencoovaso,presenta enpinturarojaloquepareceseruntocadoconplumas,ademásdeotroscolorescomoel crema,naranjaynegro.Loscuencostienenacabadodesuperficiequeseencuentra alisadoypulidofinoporelbrilloquepresenta,mientrasqueelplatounalisadoypulido medio. CERÁMICAPRECLÁSICA Fase: Motagua¿? Enestegruposeintegraronvariosmaterialesrecuperadosmediantelarecolecciónde superficie,quepresentabancaracterísticaspreclásicascomograndespestañaslabialesy mediales,monocromía,bordesengrosados,bordesconacanaladuras,entreotras características,porlafaltadeunatipologíaparadichoperíodoenlaregión. CERÁMICAESTUCADA Fase: Magdalena Aquíseincluyeronlossietefragmentosdecerámicaestucadaqueserecuperaronen excavacionescontroladas,algunosconcolorescelestes,verdes,rojoentreotros.Esta cerámicacorrespondealperíodoClásicoTardío. Fig.33 CerámicaEstucada CERÁMICACOLONIAL Únicamenteseencontrarondosfragmentosdeposiblecerámicacolonial,peroéstosson muypequeñosyprocedenderecoleccionesdesuperficie.

405 MISCELANEOS1 Enelpresentegruposeincluyóelmaterialquepordistintosmotivosnopudoser clasificadoenningunadelasvajillasestablecidas,algunasvecesporquesólosepresentó unejemplaryéstenocorrespondíaalascaracterísticasdeningunodelosgruposcreados durantelaclasificacióndelosmaterialescerámicos. MISCELANEOS2 Enestegruposeincluyerontodasaquellasformasespecialescomopelotitasdecerámica, fragmentosdefigurilla,fragmentosdesilbatos,sellosyotrasformasespecialesqueson dignasdeunestudioaparteporquenospermitenindagaracercadelasactividadesde sociedadesantiguas. TIESTOSREUTILIZADOS Enestegruposeincluyóatodosaquellosfragmentosdecerámicaquepresentabanrasgos dehabersidoreutilizadosparadiversasformas,posiblementeparautilizarloscomo adornosocomoinstrumentosparaciertasactividades,juegos,pesca,entreotras;después desufrirunaseriedetransformaciones.Aquísepuedenencontrarcírculosperforados, tiestosdedistintasformas:triángulos,rombos,óvalos,círculos,etc.yqueensumayoría presentanevidenciadehabersidolimadosparadarleslaformadeseada.

406 VITA ErickThomasRochette EDUCATION MasteroftheArtsinAnthropology,2002,ThePennsylvaniaStateUniversity BacheloroftheArtsinArchaeology,1999,BostonUniversity EMPLOYMENTHISTORY TeachingAssistant,DepartmentofAnthropology,ThePennsylvaniaState University,Fall2000Spring2002,Spring2004,Spring2006,Spring2007, Fall2007 Lecturer,DepartmentofAnthropology,ThePennsylvaniaStateUniversity, Summer2002,Summer2003,Summer2004,Summer2007,Spring2008 Lectuer,DepartmentofAnthropology,IndianaUniversityofPennsylvania, Fall2008Spring2009 FIELDANDLABORATORYRESEARCH ProjectDirector(9/05Present), Lower Rio Lato Archaeological Jade Project, Guatemala (E.Rochette,PSU,P.I.) FieldDirector(6/027/02), Centre County Rock Shelter and Fox Hollow Sites (D. Snow,PSU,P.I.) FieldAssistant(1/984/98;3/004/00), Archaeological Project, Belize (N.Hammond,BostonUniv.,P.I.) FieldAssistant(1/003/00), Cuello Archaeological Project , Belize (N.Hammond, BostonUniv.,P.I.) PUBLICATIONS "JadeinFull:DomesticProductionofJadeiteWealthGoodsintheMiddle MotaguaValley,Guatemala."In Housework: Specialization, Household Economy and Domestic Craft Production in Mesoamerica ,K.Hirth,ed. ArcheologicalPapersoftheAmericanAnthropologicalAssociation. WashingtonD.C.:AmericanAnthropologicalAssociation,2009 “¿Aquiénestáasociado?:Laproducciónartesanaldomésticadebienesdeestatus enlacuencamediadelríoMotagua"(2ndauthor:MónicaPellecer,Lic.). In XXI Simposio de Investigaciones Arqueológicas en Guatemala, 2007 , J.P.Laporte,B.ArroyoandH.Mejía,eds.MuseoNacionalde ArqueologíayEtnología,Guatemala,2008 BookReview:Salt: White Gold of the Ancient Maya ,H.McKillop(MayaStudies Series,UniversityofFloridaPress),in Latin American Antiquity, Vol.14 Num.4,2003

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