Nevada Archaeologist Volume 9 1991

Total Page:16

File Type:pdf, Size:1020Kb

Nevada Archaeologist Volume 9 1991 1::i::iN 1041-4479 NEVADA ARCHAEOLOGIST VOLUME 9 1991 A SPECIAL PRINTING IN CONJUNCTION WITH ADVENTURES IN THE PAST, A GREAT BASIN TRIBUTE NEVADA ARCHAEOLOGICAL ASSOCIATION NEVADA 80AAd of DiR£OOflS ARCHAEOLOGICAL ASSOCIATION ThE BoARd 01 DiREcrORS 01 mE NEVAdA AAclwolo<;icAl AssociAliON is ,IrCTEd ANNuAlly by m, ", .. bE..J.ip. BoARd MEMbERS "RIlE ONE \'fAR IfRMS. ThE Bo.Ad 01 DiRECTORS EIECrs "" Aw,,:iAlioN's ThE dESiGN foR m. NAA Ioqo WAS ildAplId by Robmr EIsrON roo.. AGAAfidd FIAT P£TROGlypk oIfiaRS roo.. ""'" ",MbE", ,I£wd 10 mE BoAAd. ThE BoAAd of DiRECrORS Also AppOiNTS mE Ediroo of "" NEVAdA ARcOOoIoqisr foR A TERM NOt TO EXCEEd mE Yf~ ThE BoARd of DiRECTORS Mffl"'i THREE: liMfS ... YEAR, 0NCf ~ M SOI..I1k:RN pARJ of rlif STAIF ir.. NovEMbER, 0NCf iN m, NORmERN pART 01 "" SrAII .. MARCh ANd ONU .. OcrobER iowEdiAlIly pRioR TO "" ANNUAl MmiN<;. ThE NEVAdA ARcl...okx;icAI AssociAriON is AN iNcoRpoI.md, NON­ poofir OR<;ANiwiON REGismlEd iN rhE SrArE 01 NEv.w., ANd HAs NO pAid MEMbER PAT IlARkER 'MJ>I<¥'''' M,MbE..J.ip is opEN ro ANY pER<ON 'iiGr<iNG rilE NAA coo. NEVAd.. ARcOOoIo<;icAl AssociAriON 01 Emics '"'" is iNTIREsrrd .. ARCI.uol<x;y ANd ir; AlliEd sciENCB, ANd iN m, COI'NJlVATiON 01 ARCiwolo<;ic.t RE'iOUlCf'i. RR,Usr; foR MEMbER DAUINA !'fARis MFMbE..J.ip ANd d .... shoold bE """ ro rhE TRfA'iURfR '""'" AddRf'" LKoIN ColMy o,ApIH!, N.AA is showN bElow. MAkE AD c1ifds ANd ""''l' ORdERS pAyAhl£ ro m. NEV.d. AIlcIwoolo<;ic.tA'iSOCiArioN. M,,",,,..J.ip CARds wiU bE is'iUEd MEMbER Bob EIsrON ON mE pAyMENT 01 dues ANd mE REaipT 01 AsiGN,d CodE 01 Emics. NE"Ad.. Andwolo<;icAl AssociAriON AcrivF MEMbERS REaM AsthsaIipriON TO rhE NEV.d. ARdwoloqisT ANd m. NAA NEWS!mER. SthicRipriON is by ME"bE..J.ip ONly; MEMbER DiANE JE .... i"", """""R, r.dividuAl OR Iw::k is5UEs MAy bE pt>IICi<ASFd "pARAlIly. o,....cliill eo....ry o,ApIFR, N.AA MEMbER DAvid JohNsON NEvAd.. ARcOOoIoqicAl AssociAriON HtIEN Mom'NSON 876-6944 ~9 m EI CAM"" Ro.o<l MEMbER DAN K.o.ffm lAs VEGA', NEv.d. 8910 ~ o,....cliill ColMy o,AplfR, N.A.A. RAMONA RENO 847-0H4 MEMbER HElEN MORTENSON P.O. Box 10~ ARcOOo-NEVAdA SociffY SiMI< Chy, NEVAdA 89428 MEMbER SusAN MlIllpIry TR£ASURER DiANE JENNiNGs 747-4808 And..""NEVMA SociEry 2 n ~ PtnN.w [)oM RENO, NEVAdA 89 ~m fuTuRE !w.<s Ediroo DR. G..oy HAYNES 784.-6704 MANUSCllip" srn..irfEd foR publiCATioN iN "" NEvAdA ARc!..fO/oq5T DEpARTM'NT 01 ANThROpOloqy shoold follow mE sryIE GUid, 01 "" JANUARY 1979 isSUE 01 UNMRShy 01 NEVAdA, RENO AorERiCAN ANri9viry. MANUSCRip" should bE rypEd ANd doulli RENO, NEVAdA 89~~7 SpAUd ~, iNcludiNG NOlES ANd biblioq<Aphy, ANd iUusmAriONs shoold bE CAME ....REAdy wim A CApTioN rypEd ON A DuES "pARAlI shEET 01 pApER, Also dotlrk"I"'CEd. su"" issiONs roo.. A\OCArioNAl AS UlEU AS pROfBsiON.ts _ ENCO<JRAGHI. SrudENT ................................................. $ ~.OO AcrM ...................................................... 10.00 MAN=Rip" should bE srn..rn ro NEVAliA ARclwolo<;i>f, do AcrivF FAMily ............................................. 12.00 DAvid S. JoIr.soo, Posr OfflU Box 704, CARSON Chy, NEVAdA SuppoRTiNG .•••••••.•••••.•.....••••••.•••••...•..•..••.•• 2 ~.OO 89702"()704. SpoNsoR •....•..••.•••••••••••.••..•..•••..•.••••••....•.• ~O.OO PATRON .................................................. 100.00 All ",,",,,..J.ip CAII<jORiES RECfM AsOOsrnipTiON ro rhE NEVAliA ARc!..,okx;isr, rhE jouRNAl of "" AssociATioN. Nevada Archaeologist Volume 9 1991 EDITOR'S CORNER This issue of the Nevada Archaeologist was printed by the U. S. Bureau of Land Management, Nevada State Office in Reno, Nevada. Our thanks to Dr. Pat Barker for arranging this. This issue provides another varied set of offerings that we hope prove of interest to the members of the Nevada Archaeological Association. Four articles deal with prehistoric sites, material culture, and paleoenvironments; two other articles discuss historic-period sites in Nevada. The final paper in this issue is a valuable bibliography of all articles published over the years in the Nevada Archaeologist. We have Mona Reno to thank for this compendium, which is arranged alphabetically by author. CONTENTS Amateur Archaeologists Speak: A Crescentic Hypothesis P. W. Hutchinson. 1 Charcoal Production Sites in the Pine Nut Mountains, Douglas County, Nevada Margaret Herleman. 3 Investigations at Serendipity Cave, Eureka Cave, Nevada Ronald F. King 7 Quartz Crystal Flakes and Artifacts from Western Nevada Donald R. Tuohy 11 Archaeology in the Oilpatch: A Research and Management Agenda for Trap Spring Barry A. Price 1 7 Historic Aboriginal Use of Pahute Mesa Ronald L. Reno and Gregory H. Henton. 26 Bibliography of Articles in the Nevada Archaeologist Volumes 1-8 Ramona L. Reno 38 II AMATEURARcHAEOLOGISfS SPEAK: A CRESCENTIC HYPOTHESIS P. W. Hutchinson Reno, Nevada Nevada Archaeologist Volume 9 1991 The Sunshine Well site in eastern Nevada has about human development from the most yielded one of the largest and most diverse primitive stages to modern times. One of collections of crescents found in the Great Mumford's objectives is an exploration of the Basin. Fortunately most were photographed in role played by ritual,language and social situ (Fig. I), and documented as to provenience, organization in the course of human events. typology, and metric attributes. The study of According to Mumford's thesis, human these objects (all found on the surface) spans a development was influenced more by ritual period of more than 15 years (see Hutchinson and social processes than by tool-making or the 1988). conquest of nature. Crescents are distinctive artifacts, and are usually Of relevance here is the use that humans may considered to date to the Paleo-Indian period. have given crescentic tools in some form of Archeologists most often find them on the fossil ritual behavior. In Mumford's book (1966: 150 shorelines of dried Pleistocene lakes. Some Fig. 4), a photograph shows a European people believe they were fastened to wooden Paleolithic figure of a nude woman carved in spears-shafts and thrown at waterfowl. stone, with a caption that includes this passage: "the woman of Laussel, carved in the rock, Recent backhoe trenching at Sunshine Wells holds a bison's horn, itself a sexual symbol long has revealed an ancient marsh buried under in use in Italy as a taunt of cuckoldry. The approximately 4 feet of deltaic sediments. Also combination of crescent horn and female form exposed in the trenching were Pleistocene bones recurs in the Egyptian Moon Goddess, Hather; in a braided streambed about 10 feet below the and may indicate an early astronomical interest." surface of the present lakebed. A carbon-14 date from burned twi gs at the bone level is In some respects, the "Venus of Laussel" seems 10,690 B.P. Lithic flakes have also been found to embody mystery and fascination. The in the lowest level. crescent -shaped bison horn is held aloft for all to see, and this stance may represent a ritual. It POSSlBLEFuNCTIONS OF CRESCENTS: is possible that the Sunshine Well crescents and ECONOMIC AcnvmES crescents from other sites were once used to Crescents were constructed with care from perform rituals. high-quality raw materials, and they seem almost gemlike and ornamental. They are never While we know that Great Basin crescents are especially abundant in site inventories; this almost always found in areas that once had fact, plus their locations near lakeshores, abundant water, we also know that they are suggests to me that they were used by women. lunar-shaped and that they were fashioned by If functional, they could have served to harvest humans. Crescents are generally delicately tules, herbs, and roots, or have been used to cut shaped and rather small to be comfortably held willows for basketry and net-manufacture. They by a man's larger fingers; it seems that larger may also have been used to clean fish, fowl, crescents could have been made to fit men's and hares (Hattori, Newman, and Tuohy 1990). hands, like lithic scythes, yet the specimens that we know of are relatively small (Figure I). ANoTIIEl!. Possmu: FuNCIlON OFCIlli."iCENTS: L" RnuAL Lewis Mumford mentions the crescentic form Throughout the history of the human race, in The Myth of the Machine (1966), a book women have been symbolically associated with which offers readers a cornucopia of ideas lunar phases. Some women believe their menstrual cycles are controlled by phases of the moon. I propose that crescents were possibly used by women at Great Basin lakeshores to Hattori, E. M., M. Newman, and D. Tuohy. 1990. Blood perform some sort of ritual. residue analysis of flaked stone crescents from the northern Great Basin. Paper presented at the 22nd Great Basin Anthropological Conference, Reno. More scientific evidence is required to demonstrate the manner in which crescents Hutchinson, P. W. 1988. The prehistoric dwellers at were used, and their true age, but these thoughts Lake Hubbs. In Early human occupation in far western may be of some interest in our search for North America: the Clo vis-Archaic interface (J.A. WiUig, C. M. Aikens, and J.L. Pagan, eds.), pp. 303-318. Nevada insights about the prehistoric life of Great Basin State Museum Anthropological Papers Number 21. peoples. Mumford, Lewis. 1966. The Myth of the Machine: Techniques and Human Development. Harcourt, Brace and World, N.Y. Fig. 1: Crescent found at Sunshine Well, site SW-1. 2 CHARCOAL PRODUCTION SITES IN THE PINE NUT MOUNTAINS, DOUGLAS COUNTY, NEVADA Margaret Herleman , Carson City, Nevada Nevada Archaeologist Volume 9 1991 INTRODUCTION topped with two to five inches of wet clay soil. In this paper I describe several charcoal Care must be taken to make the soil layer as production sites in western Nevada, located on airtight as possible.
Recommended publications
  • The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology
    EXHIBIT 89 The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology Dr. Saxon E. Sharpe, Dr. Mary E. Cablk, and Dr. James M. Thomas Desert Research Institute May 2007 Revision 01 May 2008 Publication No. 41231 DESERT RESEARCH INSTITUTE DOCUMENT CHANGE NOTICE DRI Publication Number: 41231 Initial Issue Date: May 2007 Document Title: The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology Author(s): Dr. Saxon E. Sharpe, Dr. Mary E. Cablk, and Dr. James M. Thomas Revision History Revision # Date Page, Paragraph Description of Revision 0 5/2007 N/A Initial Issue 1.1 5/2008 Title page Added revision number 1.2 “ ii Inserted Document Change Notice 1.3 “ iv Added date to cover photo caption 1.4 “ vi Clarified listed species definition 1.5 “ viii Clarified mg/L definition and added WRPT acronym Updated lake and TDS levels to Dec. 12, 2007 values here 1.6 “ 1 and throughout text 1.7 “ 1, P4 Clarified/corrected tui chub statement; references added 1.8 “ 2, P2 Edited for clarification 1.9 “ 4, P2 Updated paragraph 1.10 “ 8, Figure 2 Updated Fig. 2007; corrected tui chub spawning statement 1.11 “ 10, P3 & P6 Edited for clarification 1.12 “ 11, P1 Added Yardas (2007) reference 1.13 “ 14, P2 Updated paragraph 1.14 “ 15, Figure 3 & P3 Updated Fig. to 2007; edited for clarification 1.15 “ 19, P5 Edited for clarification 1.16 “ 21, P 1 Updated paragraph 1.17 “ 22, P 2 Deleted comma 1.18 “ 26, P1 Edited for clarification 1.19 “ 31-32 Clarified/corrected/rearranged/updated Walker Lake section 1.20
    [Show full text]
  • Fall / Winter 2018
    Fall/Winter 2018-19 Communities connected “Nearing the bottom of the trail in winter near the end of the day.” to nature Photo: Chris McNamara through a system The Pinyon Trail of trails An East Valley destination in cool seasons When you're looking for a change in perspective and a pleasant, non-strenuous hike, mountain bike, or equestrian trail ride with beautiful views in all directions, the Pinyon Trail in the Pine Nut Mountains east of Carson Valley is your destination. Named for Nevada’s state tree, the single-leaf pinyon pine, the Pinyon Trail is open to hikers, mountain bikers, equestrians, and dogs. The shoulder seasons, April to June and September to December, are the best times to hike this trail, which gets too hot in mid-summer. But you may be able to hike or ride there all winter, because when our Sierra Nevada trails are covered with snow, there's a good chance that the Pinyon Trail will be snow-free, or close to it. The Pinyon trail is a non-motorized three-mile loop which crowns a large hill with continuous views of the Pine Nut and Carson Ranges. From the trailhead, a one-mile "spur" gently climbs through the pinyon forest, crossing twice with a motorized off-road track, to arrive at the trail junction where trail users can go either direction on the loop. The return trip back to the trailhead from the junction results in a round-trip trail distance of about 5.2 miles. Taking the loop twice, which mountain bikers and trail runners often do, extends the length to about 8.2 miles.
    [Show full text]
  • Water Budget and Salinity of Walker Lake,Western Nevada
    ENT OF T TM H R E A IN P E T E D U.S. Geological Survey Water Budget and Salinity of R I O S. Fact Sheet FS-115-95 R U. G Walker Lake,Western Nevada E Y O E L V O R GICAL SU Walker Lake (fig. 1) is one of the rare although this site does not have the In some valleys, local streams also perennial, terminal lakes in the Great longest streamflow record, no upstream contribute surface-water flow. Thus, Basin of the western United States. The reservoirs or irrigation diversions exist and estimates of surface-water consumption in lake is the terminus for all surface-water streamflow has been measured contin- table 2 are minimum values, because local and ground-water flow in the Walker uously at the site since 1939. Long-term streamflow in valleys may not have been River Basin Hydrographic Region (fig. 2) average annual flows were estimated by measured. In Smith Valley, 8,700 acre- that is not consumed by evaporation, comparing the average annual flow at a ft/yr of Desert Creek flow has been in- sublimation, or transpiration. stream-gaging station with the average cluded in the water budget. In Antelope annual flow at site 4 for years of concur- Valley, the contribution from Mill and The concentration of dissolved solids rent record. Then, this partial record was Slinkard Creeks is unknown, so the difference of 15,000 acre-ft between (salts) in the lake and the lake-surface adjusted to a long-term average using the average inflow and outflow underesti- altitude fluctuate primarily in response 55-year average at site 4.
    [Show full text]
  • HISTORY of WASHOE COUNTY Introduction
    HISTORY OF WASHOE COUNTY Introduction Lying in the northwest portion of the State of Nevada, named for a tribe of American Indians and containing a land area in excess of 6,000 square miles, Washoe County today consists of two of the nine original counties -- Washoe and Lake (later renamed Roop) Counties -- into which the Territory of Nevada was divided by the first territorial legislature in 1861. The country, "a land of contrasts, extremes, and apparent contradictions, of mingled barrenness and fertility, beauty and desolation, aridity and storm,"1 was claimed by the Spanish Empire until 1822 when it became a part of Mexican territory resulting from Mexico's successful war of independence from Spain. Mexico ceded the area to the United States in 1848 following the Mexican War, and the ceded lands remained part of the "unorganized territory" of the United States until 1850. Spanish and Mexican constructive possession probably had little effect on the life styles of the Northern Paiutes and the Washos -- the two American Indian tribes which inhabited the area. The Northern Paiutes ranged over most of Washoe County2 save the series of valleys lying along the eastern foothills of the Sierra Nevada. These valleys were the domain of the Washos, a small, nomadic tribe whose members spoke an alien tongue and from which the name of the county is derived3. The 1840's During the 1840's Washoe County was traversed by a number of trappers and explorers, as well as several well-defined emigrant trails leading to California and Oregon. In 1843 mountain man "Old Bill" Williams4 led his trappers from the Klamath Lake region of California to Pyramid Lake and the Truckee River.
    [Show full text]
  • UNIVERSITY of NEVADA-RENO Nevada Bureau of Mines and Geology Un~Vrrsiryof Nevada-8.Eno Reno, Nevada 89557-0088 (702) 784-6691 FAX: (7G2j 784-1709
    UNIVERSITY OF NEVADA-RENO Nevada Bureau of Mines and Geology Un~vrrsiryof Nevada-8.eno Reno, Nevada 89557-0088 (702) 784-6691 FAX: (7G2j 784-1709 NBMG OPEN-FILE REPORT 90-1 MINERAL RESOURCE INVENTORY BUREAU OF LAND MANAGEMENT, CARSON CITY DISTRICT, NEVADA Joseph V. Tingley This information should be considered preliminary. It has not been edited or checked for completeness or accuracy. Mineral Resource Inventory Bureau of Land Management, Carson City District, Nevada Prepared by: Joseph V. Tingley Prepared for: UNITED STATES DEPARTMENT OF E INTERIOR '\\ !\ BUREAU OF LAND MANAGEMENT Carson City Office Carson City, Nevada Under Cooperative Agreement 14-08-0001-A-0586 with the U.S. GEOLOGICAL SURVEY NEVADA BUREAU OF MINES AND GEOLOGY UNIVERSITY OF NEVADA, RENO January 1990 TABLE OF CONTENTS INTRODUCTION ........................ 3 LOCATION .......................... 4 MINERAL RESOURCES ...................... 4 MINING DISTRICTS AND AREAS .................. 6 ALLEN HOT SPRINGS AREA ................. 6 ALPINE DISTRICT .................... 7 AURORA DISTRICT .................... 10 BELL DISTRICT ..................... 13 BELLMOUNTAIN DISTRICT ................. 16 BENWAY DISTRICT .................... 19 BERNICE DISTRICT .................... 21 BOVARDDISTRICT .............23 BROKENHILLS DISTRICT ................. 27 BRUNERDISTRICT .................. 30 BUCKLEYDISTRICT ................. 32 BUCKSKINDISTRICT ............... 35 CALICO HILLS AREA ................... 39 CANDELARIA DISTRICT ................. 41 CARSON CITY DISTRICT .................. 44
    [Show full text]
  • Chapter 7 Land Use and Agriculture
    Chapter 7 Land Use and Agriculture Chapter 7 Land Use and Agriculture Introduction This chapter describes the affected environment for land use and agriculture in the study area and the potential impacts on land use and agriculture that would result from the acquisition alternatives and No Action Alternative. Sources of Information The key sources of data and information used in the preparation of this chapter are listed below. Full references can be found in Chapter 17, References. ICF Jones & Stokes interpretation of USGS land use information (ICF Jones & Stokes 2008) . Carson City Field Office Consolidated Resource Management Plan (Bureau of Land Management 2001) . Lyon County Master Plan (Lyon County 1990)1 . Mineral County Master Plan (Mineral County Regional Planning Commission 2006) . The University and DRI analysis of GIS data related to agriculture (Bonnenfant et al. 2009) The USGS land use dataset was the foundation for this section because it provides the greatest amount of information in a single dataset, and most study area acreages were calculated from this dataset. For local descriptions, such as agricultural land in Mason Valley, newer and more detailed data were used when available. As a result, total acreages are not consistent. This is particularly true in the case of irrigated land—the USGS data include more land under this category than the newer and more detailed University and DRI data. Data sources are noted throughout this report. It is important to note that land use is a dynamic resource and therefore it is not possible to present absolute current information; the best information available is presented in the Revised DEIS.
    [Show full text]
  • Geology and Mineral Resources of the Reno 1 O by 2° Quadrangle, Nevada and California
    Geology and Mineral Resources of the Reno 1 o by 2° Quadrangle, Nevada and California U.S. GEOLOGICAL SURVEY BULLETIN 2019 Geology and Mineral Resources of the Reno 1 o by 2° Quadrangle, Nevada and California By DAVID A. JOHN, JOHN H. STEWART, JAMES E. KILBURN, NORMAN J. SILBERLING, and LARRY C. ROWAN U.S. GEOLOGICAL SURVEY BULLETIN 2019 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Geology and mineral resources of the Reno 1 o by 2° quadrangle, Nevada and California I by David A. John ... [et al.]. p. cm.-(U.S. Geological Survey bulletin; 2019) Includes bibliographical references. Supt. of Docs. no.: I 19.3:2019 1. Mines and mineral resources-Nevada-Reno Region. 2. Mines and mineral resources-California. 3. Geology-Nevada-Reno Region. 4. Geology-California. I. John, David A. II. Series. QE75.89 [TN24.NJ 557.3 s-dc20 [553'.09793'55] 92-32554 CIP CONTENTS Abstract 1 Introduction 2 Acknowledgments 2 Background studies 2 Geologic mapping 2 Gravity data 4 Aeromagnetic data 4 Isotopic-dating studies 4 Paleomagnetic data 4 Geochemical data 5 Mines and prospects data 6 Remote-sensing data 7 Area description 7 Geology 8 Pre-Tertiary
    [Show full text]
  • Geology and Water Resources of Smith Valley, Lyon and Douglas Counties Nevada
    Geology and Water Resources of Smith Valley, Lyon and Douglas Counties Nevada By O. J. LOELTZ and T. E. EAKIN GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1228 Prepared in cooperation with the Office of the State Engineer State of Nevada UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1953 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Abstract_ _ _ _____________________________________________________ 1 Introduction. ______________________________________________________ 2 Purpose and scope of the investigation. .___-_______---__---_--___ 2 Acknowledgments. ____________________________________________ 3 Geographical sketch-__________________________________________ 3 Historical sketch-______________________________________________ 5 Climate---_----------------_---_-__---------_---_---------------_ 7 Precipitation _ _______________________________________________ 7 Temperature_ _______________________________________________ 10 Physiography and drainage_________________________________________ 11 General features-___--_-_-_--__-_________________________.._-___ 11 Mountains_ _________________________________________________ 11 Alluvial fans and valley floor-___________________________________ 13 Streams._____________________________________________________ 14 Geology._________________________________________________________ 17 General- __.-_---___-----------_-______-_____-________________
    [Show full text]
  • Late Quaternary Deformation and Seismic Risk Vl in the Northern Sierra Nevada-Great Basin Boundary Zone Near the Sweetwater Mountains, California and Nevada
    University of Nevada Reno !Late Quaternary deformation and seismic risk vl in the northern Sierra Nevada-Great Basin Boundary Zone near the Sweetwater Mountains, California and Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by Garry Fallis Hayes W\ April 1985 i MINIS 1 LIBRARY University of Nevada Reno April 1985 ii ABSTRACT Remote-sensing, seismic and field studies indi­ cate three major zones of Quaternary deformation near the Sweetwater Mountains. Holocene fault scarps are present in the Antelope, Little Ante­ lope, Smith and Bridgeport Valleys, and in the Sonora Basin. Two other vaguely defined zones, between Carson and Antelope valleys, and from the Bridgeport Valley east to Bald Mountain, may repre­ sent Mio-Pliocene zones of faulting which more recently have acted as conjugate shears releasing stress between fault basins in the Western Great Basin between the Sierra Nevada and Walker Lane shear zone. The northern portion of the Sierra Nevada-Great Basin Boundary Zone is less active than the south­ ern part in Owens Valley, as shown by lower slip rates, shorter fault lengths and lower levels of historical seismicity. Maximum Credible Earthquake magnitudes for the fault basins range from 6.3 to 7.2, with expected displacements of 3 meters or more. iii ACKNOWLEDGEMENTS The author would like to thank Dr. D.B. Slemmons, Craig DePolo and J.O. Davis for helpful discussions during the course of this study. Special thanks to Craig DePolo, Susan Hciyss and Ron Smith, who assisted with the field studies, and to Glenn Hayes who assisted with the manuscript preparation.
    [Show full text]
  • Yerington Dist Rict, Nevada
    ,._ ·_/ DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY · GEORGE OTIS SMITH, Director Professional Paper 114 GEOLOGY AND ORE DE_POSITS OF THE YERINGTON DIST_RICT, NEVADA BY • ADOLPH KNOPF WASHINGTON GOVERNMENT PRINTING OFFICE 1918 ._,., .. .,... ... '· _.! ~ 1 • ~ :. •• ~ .... \, :'. ·CONTENTS. Page .. Pago. Preface, by F. L. Ransome ...................... :. 5 Part I. General features-Continued. Outline of report ................................ 7 Gener;,tl geology-Continued. Pttrt I. General features .................•....•.. 9 Epitome of the. geologic history of the Geography ........................ ·......... 9 district .....•......................... 29 Field work .................................. 9 Part II. The ore bodies ......................... 31 Bibliography ............................... 9 General features ............................ 31 . History of mining .......................... 11 Minerals of the ore deposits .................. 31 Production .................................. 12 Primary ·minerals ....................... 31 General geology ............................ 12 Secon'dary minerals .......... ~ .......... 33 'l'riassic rocks . ............ : ........... 12 Contact-metamorphic ore deposits ........... 34 Character ........................... 12 Geologic environment ................... 34 Age ............................... 12 Composition of the rocks inclosing the Volcanic rocks ...................... 13 ore deposits ....................... 34 Andesites .....................
    [Show full text]
  • A Management-Oriented Classification of Pinyon-Juniper Woodlands of the Great Basin
    Utah State University DigitalCommons@USU All U.S. Government Documents (Utah Regional U.S. Government Documents (Utah Regional Depository) Depository) 6-1998 A Management-Oriented Classification of Pinyon-Juniper Woodlands of the Great Basin Neil E. West Robin J. Tausch Paul T. Tueller United States Department of Agriculture Forest Service Rocky Mountain Research Station Follow this and additional works at: https://digitalcommons.usu.edu/govdocs Part of the Environmental Indicators and Impact Assessment Commons Recommended Citation West, Neil E.; Tausch, Robin J.; Tueller, Paul T.; United States Department of Agriculture; Forest Service; and Rocky Mountain Research Station, "A Management-Oriented Classification of Pinyon-Juniper Woodlands of the Great Basin" (1998). All U.S. Government Documents (Utah Regional Depository). Paper 495. https://digitalcommons.usu.edu/govdocs/495 This Report is brought to you for free and open access by the U.S. Government Documents (Utah Regional Depository) at DigitalCommons@USU. It has been accepted for inclusion in All U.S. Government Documents (Utah Regional Depository) by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. ". '.'" . '. -.. USDA United States ~ Department of Agriculture . A Management-Oriented Forest Service Rocky Mountain Classification of Pinyon- . Research Station General Technical Juniper Woodland~_ of the" Report RMRS-GTR-12 June 1998 . Great Basin· .. ..... (11'11111~!~I!I!ll!lllj~l"IlI···) . , ~~ Neil E. West Robin J. Tausch Paul T. Tueller REPRODUCED BY: ~ u.s. Department of Commerce . --­ National Technical Information Service Springfield, Virginia 22161 , . ~ . The Authors We used the already delineated National Hierarchical Framework of Ecological Units (ECOMAP 1993) down to Neil E.
    [Show full text]
  • Pine Nut Land Health Project
    Sierra Front Sierra Pine Nut Field Office, Nevada Office, Field Land Health Project FINAL ENVIRONMENTAL ASSESSMENT DOI-BLM-NV-C020-2013-0017-EA U.S. Department of the Interior Bureau of Land Management Carson City District Sierra Front Field Office 5665 Morgan Mill Road Carson City, NV 89701 775-885-6000 April 2014 It is the mission of the Bureau of Land Management to sustain the health, diversity, and productivity of the public lands for the use and enjoyment of present and future generations. DOI-BLM-NV-C020-2013-0017-EA ii Table of Contents 1.0 INTRODUCTION ......................................................................................... 1 1.1 Background ...................................................................................................................... 1 1.2 Purpose and Need ............................................................................................................. 2 1.3 Scoping and Issues Identification ..................................................................................... 3 1.4 Decision to be Made ......................................................................................................... 3 1.5 Land Use Plan Conformance Statement........................................................................... 3 1.6 Relationships to Statutes, Regulations, and Other Plans .................................................. 4 2.0 ALTERNATIVES .......................................................................................... 6 2.1 Description of Alternatives .............................................................................................
    [Show full text]