Geology of the York Tin Deposits Alaska
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Pamphlet to Accompany Scientific Investigations Map 3131
Bedrock Geologic Map of the Seward Peninsula, Alaska, and Accompanying Conodont Data By Alison B. Till, Julie A. Dumoulin, Melanie B. Werdon, and Heather A. Bleick Pamphlet to accompany Scientific Investigations Map 3131 View of Salmon Lake and the eastern Kigluaik Mountains, central Seward Peninsula 2011 U.S. Department of the Interior U.S. Geological Survey Contents Introduction ....................................................................................................................................................1 Sources of data ....................................................................................................................................1 Components of the map and accompanying materials .................................................................1 Geologic Summary ........................................................................................................................................1 Major geologic components ..............................................................................................................1 York terrane ..................................................................................................................................2 Grantley Harbor Fault Zone and contact between the York terrane and the Nome Complex ..........................................................................................................................3 Nome Complex ............................................................................................................................3 -
A (Sixth) List of New Mineral Names
352 A (sixth) list of new mineral names: By L. J. Srv.Nc~a, M.A., F.G.S. Assistant in the Mineral Department of the British Museum. [Communicated March 11, 1918.] Achla,~ite. (R. Koechlin, l~iineralogisches Taschenbuch der Wiener Mineralogischen Gesellschaft, 1911, pp. 12, 62 ; Min. Petr. Mitt., 1912, vol. xxxi, p. 91 (Achiardit).) Synonym of Dachiardite (G. D'Achiardi, 1906; 4th list). Aohlusite. W.F. Petterd, 1910. Catalogue of the Minerals of Tasmania, 8rd edit., Hobart, 1910, p. 191; Papers Roy. Soc. Tasmania, 1910, p. 191. A green alteration product of topaz resembling steatite in appearance, but near soda-mica in composition. Derivation not stated, but no doubt from ~X~.J~, mist, alluding to the cloudy alteration of the clear topaz. Aomite-augite. F. Zambonini, 1910. Mineralogia Vesuviana. Mere. Accad. Sci. Fis. Mat. Napoli, vol. xiv, pp. 158, 155 (acmlteaugite). The same as aegirine-augite (H. Rosenbusch, 1902 ; 2nd List), but brown in colour. Aegerite. (~Jineral Resources U.S. Geol. Survey, for 1910, 1911, part ii, p. 886.) Trade-name for a bitumen allied to elaterite. Aconite. (Mineral Resources U.S. Geol. Survey, for 1909, 1911, part ii, p. 738.) Trade-name for a bitumen very similar to elaterite. Albanite. C. I. Istrati and M. A. Mihailescu, 1912. Bul. Soc. Rem~ne ,Sti., vol. xx, p. 626. A bituminous material from Alt~nia. Alleharite. B. Je~.ek, 1912. Zeits. Kryst. Min., vol. li, p. 275 (Alleharit). Small, acicular, orthorhombic crystals, resembling stibnite in appearance, found with vrbaite (q.v.) on specimens of realgar and i Previous lists of this series have been given at the ends of vols. -
Introduction of Domestic Reindeer Into Alaska
M * Vice-President Stevenson. Mrs. Stevenson. Governor and Mrs. Sheakley. Teachers and Pupils, Presbyterian Mission School, Sitka, Alaska. 54th Congress, SENATE. f Document 1st Session. \ No. 111. IN THE SENATE OF THE UNITED STATES. REPO R T ON WITH MAPS AND ILLUSTRATIONS, MY SHELDON JACKSON, GENERAL AGENT OF EDUCATION IN ALASKA. WASHINGTON: GOVERNMENT PRINTING OFFICE. 1896. CONTENTS. Page. Action of the Senate of the United States. 5 Letter of the Secretary of the Interior to the President of the Senate. 7 Report of Dr. Sheldon Jackson, United States general agent of education in Alaska, to the Commissioner of Education, on the introduction of domestic reindeer i nto A1 aska for 1895. 9 Private benefactions. 11 Appropriations of Congress. 13 Importation of Lapps. 14 Distribution of reindeer. 15 Possibilities of the future. 16 Effect upon the development of Alaska. 16 Disbursements. 18 APPENDIXES. Report of William Hamilton on the itinerary of 1895. 21 Annual report of William A. Kjellmann. 42 Trip to Lapland. 43 Arrival at Teller Reindeer Station. 54 Statistics of the herd.. 55 Fining a reindeer thief. 57 Breaking in deer. 60 The birth of fawns. 61 Milking. 63 Eskimo dogs. 63 Herders and apprentices. 65 Rations. 72 Reindeer dogs. 73 Harness. 75 The Lapps. 77 Sealing. 78 Fishing. 79 Eskimo herd. 80 Sickness. 82 School. 82 Buildings. 83 Police. 84 Christmas. 85 Skees. 85 Physician. 88 Fuel. 89 Annual report of W. T. Lopp, Cape Prince of Wales, herd... 91 Letter of J. C. Widstead to Dr. Sheldon Jackson. 93 Letter of Dr. Sheldon Jackson to Hon. W. -
Festivals and Ceremonies of the Alaskan Eskimos: Historical and Ethnographic Sources, 1814-1940
Festivals and Ceremonies of the Alaskan Eskimos: Historical and Ethnographic Sources, 1814-1940 Jesús SALIUS GUMÀ Department of Prehistory, Universitat Autònoma de Barcelona AGREST Research Group [email protected] Recibido: 15 de octubre de 2012 Aceptado: 16 de enero de 2013 ABSTRACT The main objective of this article is to shed light on the festive and ceremonial events of some of the Eskimo cultures of Alaska through a review of the ethnohistorical documents at our disposal. The study centers on the ancient societies of the Alutiiq, Yup’ik and a part of the Inupiat, communities that share a series of com- mon features, and sees their festive and ceremonial activities as components of the strategies implemented to maintain control over social reproduction. This review of the historical and ethnographic sources identifies the authors and the studies that provide the most pertinent data on the subject. Key words: Ethnohistory, social reproduction, musical behaviors, Alaska Eskimo. Festivales y ceremonias de los esquimales de Alaska: fuentes históricas y etnográficas, 1814-1940 RESUMEN El objeto de este artículo es arrojar luz sobre las fiestas y ceremonias de algunas culturas esquimales de Alaska a través de la revisión de documentos etnohistóricos a nuestra disposición. La investigación se centra sobre las antiguas sociedades de los alutiiq, yup’ik y parte de los inupiat, comunidades que tienen una serie de rasgos comunes y contemplan sus actividades festivas y ceremoniales como parte de estrategias para mantener el control sobre la reproducción social. Esta revisión de fuentes históricas y etnográficas identifica a los autores y a los estudios que proporcionan los datos más significativos sobre el tema. -
Optical Properties of Common Rock-Forming Minerals
AppendixA __________ Optical Properties of Common Rock-Forming Minerals 325 Optical Properties of Common Rock-Forming Minerals J. B. Lyons, S. A. Morse, and R. E. Stoiber Distinguishing Characteristics Chemical XI. System and Indices Birefringence "Characteristically parallel, but Mineral Composition Best Cleavage Sign,2V and Relief and Color see Fig. 13-3. A. High Positive Relief Zircon ZrSiO. Tet. (+) 111=1.940 High biref. Small euhedral grains show (.055) parallel" extinction; may cause pleochroic haloes if enclosed in other minerals Sphene CaTiSiOs Mon. (110) (+) 30-50 13=1.895 High biref. Wedge-shaped grains; may (Titanite) to 1.935 (0.108-.135) show (110) cleavage or (100) Often or (221) parting; ZI\c=51 0; brownish in very high relief; r>v extreme. color CtJI\) 0) Gamet AsB2(SiO.la where Iso. High Grandite often Very pale pink commonest A = R2+ and B = RS + 1.7-1.9 weakly color; inclusions common. birefracting. Indices vary widely with composition. Crystals often euhedraL Uvarovite green, very rare. Staurolite H2FeAI.Si2O'2 Orth. (010) (+) 2V = 87 13=1.750 Low biref. Pleochroic colorless to golden (approximately) (.012) yellow; one good cleavage; twins cruciform or oblique; metamorphic. Olivine Series Mg2SiO. Orth. (+) 2V=85 13=1.651 High biref. Colorless (Fo) to yellow or pale to to (.035) brown (Fa); high relief. Fe2SiO. Orth. (-) 2V=47 13=1.865 High biref. Shagreen (mottled) surface; (.051) often cracked and altered to %II - serpentine. Poor (010) and (100) cleavages. Extinction par- ~ ~ alleL" l~4~ Tourmaline Na(Mg,Fe,Mn,Li,Alk Hex. (-) 111=1.636 Mod. biref. -
Annual Report Noaa Ocseap Ecological Studies Of
ANNUAL REPORT NOAA OCSEAP Contract No. 03-6-022-35210 Research Unit No. 460 ECOLOGICAL STUDIES OF COLONIAL SEABIRDS AT CAPE THOMPSON AND CAPE LISBURNE, ALASKA Principal Investigators Alan M. Springer David G. Roseneau Renewable Resources Consulting Services, Ltd. 3529 College Road Fairbanks, Alaska 99701 839 i CONTENTS I. Summary of objectives, conclusions and implications with respect to OCS oil and gas development 1 II. Introduction -> A. General nature and scope of study 3 B. Specific objectives 3 c. Relevance to problems of petroleum development 3 III. Current state of knowledge 9 Iv. Study area 9 v. Sources, methods and rationale of data collection A. Census 16 B. Phenology of breedirrgacttvities 18 c. Food habits 18 VI. Results A. Murres 19 B. Black-legged Kittiwakes 66 c. Horned Puffins 84 D. Glaucous Gulls 89 E. Pelagic Cormorants 94 F. Tufted Puffins 94 G. Guillemots 96 H. Raptors and Ravens 98 I. Cape Lewis 99 J. Other areas utilized by seabirds 101 K. Other observations 104 840 ii VII and VIII. Discussion and Conclusions 105 Ix. Summary of 4th quarter operations 111 x. Acknowledgements 113 XI. Literature cited 114 841 LIST OF TABLES TABLE PAGE 1. Murre census summary, Cape Thompson. 19 2. Murre census, Colony 1; Cape Thompson, 1977. 20 3. Murre census, Colony 2; Cape Thompson, 1977. 21 4. Murre census, Colony 3; Cape Thompson, 1977, 22 5. Murre census, Colony 4; Cape Thompson, 1977. 23 6. Murre census, Colony 5; Cape Thompson, 1977. 24 7. Score totals, Colonies 1-4. 25 8. Compensation counts of murres; Cape Thompson, 1977. -
HEAVY MINERAL CONCENTRATION in a MARINE SEDIMENT TRANSPORT CONDUIT, BERING STRAIT, ALASKA by James C
Alaska Division of Geological & Geophysical Surveys PRELIMINARY INTERPRETIVE REPORT 2016-4 HEAVY MINERAL CONCENTRATION IN A MARINE SEDIMENT TRANSPORT CONDUIT, BERING STRAIT, ALASKA by James C. Barker, John J. Kelley, and Sathy Naidu June 2016 Released by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES Division of Geological & Geophysical Surveys 3354 College Rd., Fairbanks, Alaska 99709-3707 Phone: (907) 451-5010 Fax (907) 451-5050 [email protected] www.dggs.alaska.gov $3.00 Contents INTRODUCTION .................................................................................................................................................. 1 REGIONAL SETTING ............................................................................................................................................ 2 MATERIALS AND METHODS ................................................................................................................................ 3 RESULTS .............................................................................................................................................................. 5 Heavy Mineral Deposition in the Bering Strait Area .................................................................................... 5 Heavy Mineral Composition ......................................................................................................................... 8 Mineralogy .................................................................................................................................................. -
Geology and Ore Deposits of the Central York Mountains, Western Seward Peninsula, Alaska
Geology and Ore Deposits of p50 the Central York Mountains, I Western Seward Peninsula, S3 Alaska GEOLOGICAL SURVEY BULLETIN 1287 O GC oc O es ^ HI » <=; HI i i QC GO eea 00 Geology and Ore Deposits of the Central York Mountains, Western Seward Peninsula, Alaska By C. L. SAINSBURY GEOLOGICAL SURVEY BULLETIN 1287 Description of the geologic structure, stratigraphy, petrology, and ore deposits of an area containing tin deposits and a new type of beryllium deposit UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library, of Congress catalog-card No, 78-602244 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $3.00 (paper cover) CONTENTS Page Abstract_ _______________________________________________________ l Introduction__________-__-_-______--__---------____________--_--__ 2 Location_ ___________________________________________________ 2 Purpose and scope of report_._--___-----_--____-________-_-_-_ 3 Methods of study__________-_---___--_--_-_.________._----___ 4 Acknowledgments __________-_-__----___---_______l______--____ 4 Previous work_____-__-__-----_-________--___________---____- 5 Sedimentary rocks._________-____-_-_____-___-_-___________----_-__ 6 Pre-Ordovician rocks___________________________________________ 7 Slate of the York region-____________________________________ 7 Argillaceous and dolomitic limestone.___--___-_______-----___ 9 Undifferentiated limestone and argillaceous and dolomitic lime stone_ ________________________________________________ 10 Summary of pre-Ordovician rocks_______-_-__________------_ 11 Lower Ordovician rocks.____-___-_--_____---__________-___--_-_ 12 Argillaceous limestone and limestone (shallow-water facies) _ _ _. -
The Occurrence of Zeunerite at Brooks Mountain Seward Peninsula Alaska
GEOLOGICAL SURVEY CIRCULAR 214 THE OCCURRENCE OF ZEUNERITE AT BROOKS MOUNTAIN SEWARD PENINSULA ALASKA By WalterS. West and Max G. White UNITED STATES DEPARTMENT OFT Oscar L. Chapman, Secret GEOLOGICAL SURV W. E. Wrathe;r, Direct r THE OCCURRENCE OF ZEUNERITE ~ BROOKS MOUNTAIN SEWARD PENINSULA, SKA By Walter S. West and Max G. This report concerns work done o behalf of the U. S. Atomic Ener CoDllllis$ion and is .published with the permission of the Commission. Washington, D. C.,l952 Free on application to the Geological Survey, Washington 25, D. C. THE OCCURRENCE OF ZEUNERITE AT BROOKS MOUNTAIN SEWARD PENINSULA, ALASKA CONTENTS Page Page Abstract.................................... 1 Mineral Deposits and Introduction .. ; . 1 radioactivity studies.. 3 Geology . 2 E'oggy Day prospect. 3 Description of rock types . 2 Tourmaline No. 2 claim. 6 Slate . 2 Minor occurrences Limestone . 2 of zeunerite. 6 Granite . 2 Radioactivity of the granite. 7 Dikes............................. 3 Conclusions. 7 Structure . .. 3 Recommendation for Hydrothermal alteration of sedimen- prospecting. 7 tary rocks and granite ............ , . 3 R.eferences cited . • . 7 ILLUSTRATIONS Page Plate 1. Geologic map of the Brooks Mountain area, Teller quadrangle, Seward Peninsula, Alaska .. .. .. • . • . • Inside back cover Figure 1. Index map of the Seward Peninsula, Alaska, showing the location of the Brooks Mountain area . • . • . 2 TABLE Pa"ge Table 1. Analyses of selected samples from the Brooks Mountain area, Seward Peninsula. • . 4 ABSTRACT mineral zone may occur below the zone of oxidation at the Foggy Day prospect. Zeunerite occurs near the surface of a granite stock on the southwest flank of Brooks Mountain, INTRODUCTION Alaska. The largest deposit is at the Foggy Day prospect. -
List of Abbreviations
List of Abbreviations Ab albite Cbz chabazite Fa fayalite Acm acmite Cc chalcocite Fac ferroactinolite Act actinolite Ccl chrysocolla Fcp ferrocarpholite Adr andradite Ccn cancrinite Fed ferroedenite Agt aegirine-augite Ccp chalcopyrite Flt fluorite Ak akermanite Cel celadonite Fo forsterite Alm almandine Cen clinoenstatite Fpa ferropargasite Aln allanite Cfs clinoferrosilite Fs ferrosilite ( ortho) Als aluminosilicate Chl chlorite Fst fassite Am amphibole Chn chondrodite Fts ferrotscher- An anorthite Chr chromite makite And andalusite Chu clinohumite Gbs gibbsite Anh anhydrite Cld chloritoid Ged gedrite Ank ankerite Cls celestite Gh gehlenite Anl analcite Cp carpholite Gln glaucophane Ann annite Cpx Ca clinopyroxene Glt glauconite Ant anatase Crd cordierite Gn galena Ap apatite ern carnegieite Gp gypsum Apo apophyllite Crn corundum Gr graphite Apy arsenopyrite Crs cristroballite Grs grossular Arf arfvedsonite Cs coesite Grt garnet Arg aragonite Cst cassiterite Gru grunerite Atg antigorite Ctl chrysotile Gt goethite Ath anthophyllite Cum cummingtonite Hbl hornblende Aug augite Cv covellite He hercynite Ax axinite Czo clinozoisite Hd hedenbergite Bhm boehmite Dg diginite Hem hematite Bn bornite Di diopside Hl halite Brc brucite Dia diamond Hs hastingsite Brk brookite Dol dolomite Hu humite Brl beryl Drv dravite Hul heulandite Brt barite Dsp diaspore Hyn haiiyne Bst bustamite Eck eckermannite Ill illite Bt biotite Ed edenite Ilm ilmenite Cal calcite Elb elbaite Jd jadeite Cam Ca clinoamphi- En enstatite ( ortho) Jh johannsenite bole Ep epidote -
Clintonite-Bearing Assemblages in Chondrodite Marbles from the Contact Aureole of the Tøebíè Pluton, Moldanubian Zone, Bohemian Massif
Journal of the Czech Geological Society 51/34(2006) 249 Clintonite-bearing assemblages in chondrodite marbles from the contact aureole of the Tøebíè Pluton, Moldanubian Zone, Bohemian Massif Asociace obsahující clintonit v chondroditových mramorech moldanubika z kontaktní aureoly tøebíèského plutonu, Èeský masiv (6 figs, 4 tabs) STANISLAV HOUZAR1 MILAN NOVÁK2 1 Department of Mineralogy and Petrography, Moravian Museum, Zelný trh 6, CZ-659 37 Brno, Czech Republic; [email protected] 2 Institute of Geological Sciences, Masaryk University, Kotláøská 2, CZ-611 37 Brno, Czech Republic; [email protected] Clintonite is a minor to accessory mineral in chondrodite marbles. They represent a rare type of metacarbonate rocks in the Varied Unit of the Moldanubian Zone, forming thin bodies enclosed in migmatites. Clintonite occurs exclusively in marbles from contact aureole of melanocratic ultrapotassic granites (durbachites) of the Tøebíè Pluton. Chondrodite marbles consist of dominant calcite, less abundant dolomite; amounts of silicates vary from ~ 5 to 30 vol. %. The early mineral assemblage Dol+Cal+Prg ±Phl is replaced by the assemblage Chn+Cli+Cal ±Chl I ±Spl. Accessory minerals include fluorapatite, diopside, tremolite, pyrrhotite, and rare zircon and baddeleyite. Violet fluorite occurs on late fissures. Clintonite forms colourless to pale green flakes and sheaf-like aggregates, up to 2 mm in size. It has extraordinary high Si (2.7392.986 apfu) and Si/Al ratio (0.520.60). The contents of Fe (0.0410.128 apfu), Na (0.0350.134 apfu), tot Ti (0.0040.024 apfu) and K (≤ 0.005 apfu) are low. High concentrations of F (0.4371.022 apfu) corresponding up to 26 % of the F-component are the highest ever-recorded in clintonite. -
SIDEROPHYLLITE from BROOKS MOUNTAIN, ALASKA" Rosbnr R
SIDEROPHYLLITE FROM BROOKS MOUNTAIN, ALASKA" RosBnr R. Coars aNl Josnrn J. Fenev ABsrRAcr A brittle, dark green mica (siderophyllite) from Brooks Mountain, Alaska, unusually high in divalentiron (30.16/6 FeO) and with almost no magnesia is described. The indices of refractionare:a:1.590, F:1.640 and "y:1.640. A specimen of mica from a granite pegmatite on Brooks Mountain, Seward Peninsula, Alaska, proved upon analysis to be siderophyllite, the rare high-ferrous member of the biotite group. The name siderophyllite was given by Lewis,l in allusion to the large percentage of iron which it contains, "to a hard black mica" with "laminae very brittle" found in the neighborhood of Pike's Peak, Colorado. As the feature that distinguishes his mica from previously described micas of high iron content is its large percentageof ferrous oxide (25.50%) and minor percentagesonly of ferric oxide (I.55%) and magnesia (l.I47o), it can be inferred that Lewis intended to restrict the application of the name siderophyllite to micas having a similar composition. This restriction is here made explicit. The mica from Alaska describedin this paper is therefore siderophyllite. LocerroN AND MoDE ol OccURRENCE Brooks Mountain is in the central part of the York Mountains' in the northwestern part of the Seward Peninsula, Alaska. The siderophyllite occurs in a pegmatite sill which is associated with a stock of coarse- grained porphyritic alaskite about 2 miles in diameter, forming the southern part of Brooks Mountain. The pegmatite sill, intrusive into fine grained marble, is exposed in one of two small pits about 500 feet northwest of a small ruined cabin on the saddle between the headwaters of Mint River and those of Crystal Creek, a tributary of Lost River.