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Josie Pearl, Prospector on Nevada's Black Rock Desert
JUNE, 1962 40c • • • • . Author's car crossing the playa of Black Rock Desert in northwestern Nevada. On Black Rock Desert Trails When Dora Tucker and Nell Murbarger first began exploring the Black Rock country in northwestern Nevada they did not realize what a high, wide and wild country it was. On the Black Rock a hundred miles doesn't mean a thing. In the 10,000 square miles of this desert wasteland there isn't a foot of pavement nor a mile of railroad— neither gasoline station nor postoffice. Antelopes out-number human beings fifty to one. There's plenty of room here for exploring. By NELL MURBARGER Photographs by the author Map by Norton Allen S AN illustration of what the want to! Ain't nothin' there!" is known as "the Black Rock country," Black Rock country affords Thanking him, we accepted his re- the desert from which it derives its in the way of variety and con- port as a favorable omen and headed name actually is a stark white alkali trast, we made a J 50-mile loop trip out into the desert. Almost invariably playa, averaging a dozen miles in out of Gerlach last June. Our previous we find our best prowling in places width and stretching for 100 miles exploring of the region had been mostly where folks have told us there "ain't from Gerlach to Kings River. Merging in the northern and eastern sections, nothin'." imperceptibly with the Black Rock on so we hadn't the slightest idea of what Rising precipitously from the dead the southwest is the section known as we might find in the southern part. -
Tectonic Evolution of the Northern Sierra Nevada
TECTONIC EVOLUTION OF THE NORTHERN SIERRA NEVADA BATHOLITH A DISSERTATION SUBMITTED TO THE DEPARTMENT OF GEOLOGICAL AND ENVIRONMENTAL SCIENCES AND THE COMMITTEE ON GRADUATE STUDIES OF STANFORD UNIVERSITY IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY Nicholas James Van Buer December 2011 © 2011 by Nicholas James Van Buer. All Rights Reserved. Re-distributed by Stanford University under license with the author. This work is licensed under a Creative Commons Attribution- Noncommercial 3.0 United States License. http://creativecommons.org/licenses/by-nc/3.0/us/ This dissertation is online at: http://purl.stanford.edu/xb187vq0064 Includes supplemental files: 1. Plate 1. Geologic Map of the Jayhawk Well 7.5' Quadrangle, Pershing County, Nevada (jayhawkwell.pdf) 2. Plate 2. Geologic Map of the Juniper Pass 7.5' Quadrangle, Pershing County, Nevada (Juniperpass.pdf) 3. Plate 3. Geologic Map of the Tohakum Peak NE 7.5' Quadrangle, Pershing County, Nevada (TohakumpkNE.pdf) 4. Plate 4. Geologic Map of the Tunnel Spring 7.5' Quadrangle, Pershing County, Nevada (tunnelspr.pdf) 5. Plate 5. Geologic Map of the Bob Spring 7.5' Quadrangle, Pershing County, Nevada (bobspring.pdf) 6. Plate 6. Geologic Map of the Tohakum Peak SE 7.5' Quadrangle, Pershing County, Nevada (TohakumpkSE.pdf) 7. Plate 7. Geologic Map of the Sage Hen Spring 7.5' Quadrangle, Pershing County, Nevada (SageHenSpr.pdf) 8. Plate 8. Geologic Map of the Bluewing Spring 7.5' Quadrangle, Pershing County, Nevada (BluewingSpr.pdf) ii I certify that I have read this dissertation and that, in my opinion, it is fully adequate in scope and quality as a dissertation for the degree of Doctor of Philosophy. -
Brxs R43.Pdf
MINERAL RESOURCES OF THE KUMlVA PEAK 38-BV 60"OUADRANGLE INTRODUCTION Parallel Survey. Descriptions of mines and prospects within the auadranale were made bv HI! 11 91 51. Lincoln 11 9231. The Kumiva Peak 30' by 60' Quadrangle lies about 40 ~anderburg-(1936). ~vertdn11947). onh ham i1969); miles north of Reno in western Nevada. The southern and Johnson (1977). Descriptions of the geology of the boundary is the 40th parallel and the western boundary, Washoe County portion of the quadrangle were included in the 120th meridian, lies about % mile west of the Nevada- the work by Bonham (1969); Johnson (I9771 described California state line. Portions of Washoe and Pershing the geology of the Pershing County part of the quadrangle. Counties, the northern half of Pyramid Lake, and a large During 1984-85, the Nevada Bureau of Mines and part of the Pyramid Lake Indian Reservation ail lie within Geology conducted a mineral inventory of the Sonoma- this quadrangle. Gerlach Resource Area for the Bureau of Land Management The John Fremont end Kit Carson party traveled through and, as part of that project,many mines andprospects in the central portion of this area in early January 1844. The the Kumiva Peak 30' by 60' Quadrangle were examined Fremont party discovered and named Pyramid Lake and and sampled. Field data were collected by Jack Quade, passed along its eastern shore on their way south. The J. V. Tingley, R: B. Jones, and L. J. Garside. In 1986, earliest mining activity, gold and silver prospecting, began T. L. T. Grose reported on several prospects in the about 1670 in Cottonwood Canyon in the northern Fox southern part of the quadrangle and, in 1967, J. -
Winnemucca District Proposed Resource Management Plan and Final Environmental Impact Statement DOI-BLM-NV-W000-2010-0001-EIS
BLM Winnemucca District Proposed Resource Management Plan and Final Environmental Impact Statement DOI-BLM-NV-W000-2010-0001-EIS Volume 2: Chapters 3, 4 Winnemucca District, Nevada District, Winnemucca August 2013 Winnemucca MISSION STATEMENT To sustain the health, diversity, and productivity of the public lands for the use and enjoyment of present and future generations. BLM/NV/WN/ES/13-11+1793 Volume 2 of 4 TABLE OF CONTENTS Section Page 3. AFFECTED ENVIRONMENT ............................................................................................. 3-1 3.1 Introduction ...................................................................................................... 3-1 3.2 Resources ....................................................................................................... 3-1 3.2.1 Air Quality ............................................................................................ 3-2 3.2.2 Geology ............................................................................................. 3-14 3.2.3 Soil Resources .................................................................................. 3-18 3.2.4 Water Resources ............................................................................... 3-22 3.2.5 Vegetation – General ......................................................................... 3-36 3.2.6 Vegetation – Forest/Woodland Products ........................................... 3-41 3.2.7 Vegetation – Invasive and Noxious Species ...................................... 3-42 3.2.8 Vegetation -
STATE of NEVADA Brian Sandoval, Governor
STATE OF NEVADA Brian Sandoval, Governor DEPARTMENT OF WILDLIFE Tony Wasley, Director GAME DIVISION Brian F. Wakeling, Chief Mike Cox, Big Game Staff Biologist Pat Jackson, Carnivore Staff Biologist Cody McKee, Elk Staff Biologist Cody Schroeder, Mule Deer Staff Biologist Peregrine Wolff, Wildlife Health Specialist Western Region Southern Region Eastern Region Regional Supervisors Mike Scott Steve Kimble Tom Donham Big Game Biologists Chris Hampson Joe Bennett Travis Allen Carl Lackey Pat Cummings Clint Garrett Kyle Neill Cooper Munson Matt Jeffress Ed Partee Kari Huebner Jason Salisbury Jeremy Lutz Kody Menghini Tyler Nall Scott Roberts Cover photo credit: Mike Cox This publication will be made available in an alternative format upon request. Nevada Department of Wildlife receives funding through the Federal Aid in Wildlife Restoration. Federal Laws prohibit discrimination on the basis of race, color, national origin, age, sex, or disability. If you believe you’ve been discriminated against in any NDOW program, activity, or facility, please write to the following: Diversity Program Manager or Director U.S. Fish and Wildlife Service Nevada Department of Wildlife 4401 North Fairfax Drive, Mailstop: 7072-43 6980 Sierra Center Parkway, Suite 120 Arlington, VA 22203 Reno, Nevada 8911-2237 Individuals with hearing impairments may contact the Department via telecommunications device at our Headquarters at 775-688-1500 via a text telephone (TTY) telecommunications device by first calling the State of Nevada Relay Operator at 1-800-326-6868. NEVADA DEPARTMENT OF WILDLIFE 2017-2018 BIG GAME STATUS This program is supported by Federal financial assistance titled “Statewide Game Management” submitted to the U.S. -
Mining Districts of Nevada
NEVADA BUREAU OF MINES AND GEOLOGY REPORT 47 Second Edition MINING DISTRICTS OF NEVADA Joseph V. Tingley MACKAY SCHOOL OF MINES 1998 UNIVERSITY OF NEVADA RENO CONTENTS Historical background Development of mining districts in Nevada Previous work Organization of report Acknowledgments District descriptions References Appendix A List of Nevada mining district names Appendix B Nevada mining districts listed by county Appendix C Nevada mining districts listed by commodity Figure 1. Record of proceedings of miners’ meeting at Gold Hill, 1859 Figure 2. Mining laws of the Reese River mining district Figure 3. DeGroot’s map of Nevada Territory, 1863 Figure 4. Menardi’s map of Nevada, 1908 Plate 1 Mining districts of Nevada Note: Hyperlinks are denoted by underlined blue text. PREFACE TO THE SECOND EDITION Most of the major changes included in the second edition of Mining Districts of Nevada resulted from mineral assessment work carried out in south central Nevada between 1992 and 1996 (Tingley and others, 1993, 1997). Six new mining districts, Cedar Spring, Gold Range, Jamestown, Pocopah, Rainstorm, and Trappmans, have been added in Nye County and two districts, Joe May Canyon and White Caps, have been added in Clark County. Six Nye County districts, Antelope Springs, Cactus Springs, Clarkdale, Kawich, Wellington, and Wilsons, and three districts in Lincoln County, Don Dale, Groom, and Papoose, have boundary modifications and new material has been added to their descriptions in the text. In the northern part of the state, the boundary of the Argenta district, Lander County, has been modified to reflect the development of a major gold mine; gold has now surpassed barite as the major commodity produced from this district. -
Geochemical Data for Environmental Studies of Mercury Mines in Nevada
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geochemical Data for Environmental Studies of Mercury Mines in Nevada by John E. Gray, Monique G. Adams, James G. Crock, and Peter M. Theodorakos Open-File Report 99-576 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Government. U.S. Geological Survey, P.O. Box 25046, MS 973, Federal Center, Denver, CO 80225-0046 ISBN 0-607-93726-2 1999 U.S. DEPARTMENT OF THE INTERIOR Bruce Babbitt, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director ________________________________________________________________________ For additional information Copies of this report can write to: be purchased from: Chief Scientist, Central Region Books and Open-File Reports Mineral Resources Program U.S. Geological Survey U.S. Geological Survey Federal Center Box 25046, Federal Center Box 25046 Denver, CO 80225-0046 Denver, CO 80225-0046 2 TABLE OF CONTENTS Introduction………………………………….……………………………………………………….. 4 General Geology and Mineralogy…………………………....…………………………….………… 5 Sample Collection and Preparation………………………………………………………………….. 5 Analytical Methods……………….……………..…………………………………………………… 6 Solid Sample Analysis………………………...………………………………………………… 6 Inductively Coupled Plasma-Atomic Emission Spectrometry……………...………...……. 6 Atomic Absorption Spectrometry………..……………………………...………………….. 7 Water Sample Analysis…..……...……………...…..…………………………………………… 7 Inductively -
Prospecting for a Blind Geothermal System Utilizing Geologic and Geophysical Data, Seven Troughs Range, Northwestern Nevada
GRC Transactions, Vol. 38, 2014 Prospecting for a Blind Geothermal System Utilizing Geologic and Geophysical Data, Seven Troughs Range, Northwestern Nevada Corina Forson1, James E. Faulds1, and Phil Wannamaker2 1Nevada Bureau of Mines and Geology, University of Nevada, Reno NV 2Energy and Geoscience Institute, University of Utah, Salt Lake City UT Keywords resources. Researchers estimate that only ~20% of the accessible Nevada, Basin and Range, structural controls, Seven Troughs geothermal resources in the Great Basin have been discovered, Range, blind geothermal system, exploration, geologic map- suggesting that opportunities abound for discovering blind or ping, Magnetotelluric, two-meter survey hidden geothermal systems (Brook et al., 1979; Richards and Blackwell, 2002). If prospecting for a truly blind geothermal system, it becomes Abstract important to distinguish between a blind, hidden, and conventional geothermal resource. All geothermal systems have three main The Seven Troughs Range in Pershing County, Nevada, has elements: heat source (magmatic or high geothermal gradient in been identified as an area with high potential for hosting a blind amagmatic settings), reservoir (to hold and sustain the hot water), geothermal system. A reconnaissance 2D magnetotelluric (MT) and fluid, which is the medium that transfers the heat. Conven- survey across the western U.S. has shown a possible correlation tional geothermal systems exhibit fluid surface manifestations, between broad low resistivity anomalies, extending from the up- such as fumaroles or hot springs. Hidden geothermal systems per to deep crust, and loci of high enthalpy geothermal systems. lack fluid features on the surface but contain more subtle features Where MT surveys have been conducted across the Basin and (or paleo manifestations), such as siliceous sinter, travertine, tufa Range, anomalous zones of high conductivity strongly correlate deposits, and/or hydrothermally altered rocks. -
Notes on Some Mining Districts in Humboldt County, Neyada
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOE 4:14: NOTES ON SOME MINING DISTRICTS IN HUMBOLDT COUNTY, NEYADA BY FREDERICK LESLIE RANSOME WASHINGTON GOVERNMENT PRINTING OFFICE 1909 CONTENTS. Page. Introduction.............................................................. 7 Itinerary.................................................................. 9 General history of mining development..................................... 10 Literature................................................................. 13 Seven Troughs district..................................................... 14 Introduction.......................................................... 14 General geology........................................................ 15 Topography....................................................... 15 Early exploration................................................. 16 Pre-Tertiary rocks.................................................. 16 Tertiary volcanic rocks............................................. 18 Distribution and development of the mines............................. 20 Character of the deposits.............................................. 22 Outlook for the district................................................. 25 Rosebud district.......................................................... 25 Situation and history.......................... ; ........................ 25 General geology........................................................ 26 Ore deposits......................................................... -
Hycroft Mine Expansion Project B
BLM Black Rock FINAL ENVIRONMENTAL IMPACT STATEMENT Field Office/Winnemucca, Nevada DOI-BLM-NV-W030-2011-0001-EIS Hycroft Mine Expansion Project July 2012 Ne / Office District Winnemucca U.S. Bureau of Land Management Winnemucca District Office Black Rock Field Office 5100 E. Winnemucca Blvd. Winnemucca NV 89445-2921 vada 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. BLM/NV/WN/ES/12-2+1793 DOI-BLM-NV-W030-2011-0001-EIS HYCROFT MINE EXPANSION PROJECT FINAL ENVIRONMENTAL IMPACT STATEMENT TABLE OF CONTENTS ABBREVIATIONS AND ACRONYMS................................................................................XIII EXECUTIVE SUMMARY .................................................................................................... ES1 1 INTRODUCTION................................................................................................................ 11 1.1 Introduction ............................................................................................................... 11 1.2 Organization of Document ....................................................................................... 12 1.3 Purpose of and Need for Action ............................................................................... 17 1.4 Land Use Plan Conformance.................................................................................... 18 1.4.1 Sonoma Gerlach Management Framework Plan...................................... -
Alodaibi's Dissertation-Thesis Office Convert to PDF 2
TECTONIC VERSUS VOLCANIC ORIGIN OF THE SUMMIT DEPRESSION AT MEDICINE LAKE VOLCANO, CALIFORNIA by Mark Leon Gwynn A thesis submitted to the faculty of The University of Utah in partial fulfillment of the requirements for the degree of Master of Science in Geology Department of Geology and Geophysics The University of Utah May 2013 Copyright © Mark Leon Gwynn 2013 All Rights Reserved The University of Utah Graduate School STATEMENT OF THESIS APPROVAL The thesis of ________________________ Mark Leon Gwynn_______________________ has been approved by the following supervisory committee members: John M. Bartley , Chair January 8, 2013 Date Approved Michal Nemcok , Member January 15, 2013 Date Approved Richard D. Jarrard , Member January 10, 2013 Date Approved and by ______________________D. Kip Solomon______________________ , Chair of the Department of ___________________ Geology and Geophysics__________________ and by Donna M. White, Interim Dean of The Graduate School. ABSTRACT Medicine Lake Volcano is a Quaternary shield volcano located in a tectonically complex and active zone at the transition between the Basin and Range Province and the Cascade Range of the Pacific Province. The volcano is topped by a 7x12 km elliptical depression surrounded by a discontinuous constructional ring of basaltic to rhyolitic lava flows. This thesis explores the possibility that the depression may have formed due to regional extension (rift basin) or dextral shear (pull-apart basin) rather than through caldera collapse and examines the relationship between regional tectonics and localized volcanism. Existing data consisting of temperature and magnetotelluric surveys, alteration mineral studies, and core logging were compiled and supplemented with additional core logging, field observations, and fault striae studies in paleomagnetically oriented core samples. -
United States
CONTACT-METAMORPHIC TUNGSTEN DEPOSITS OF THE UNITED STATES. By FRANK L. HESS and ESPER S. LARSEN. INTRODUCTION. Production of tungsten ores in the United States. For years the United States has been not only one of the largest producers of tung sten concentrates but the largest producer of scheelite and ferberite, and in 1918 it was by far the largest producer of tungsten concen trates from contact-metamorphic deposits. Of the 5,061 short tons of concentrates carrying 60 per cent of tungsten trioxide (WO3) produced in this country in 1918, 2,734 tons was scheelite, and of this scheelite 1,427 tons was obtained from contact-metamorphic de- posits, a quantity equaled by the total output of only a few other countries. The quantity would probably have been increased ma terially had not the price of tungsten fallen after the signing of the armistice. Our total output of tungsten in 1918 was, however, less than half the output of wolframite from the Chinese placers (including a small quantity from veins), probably equivalent to more than 11,200 tons of concentrates carrying 60 per cent of tungsten trioxide. Definition. Contact-metamorphic tungsten deposits have been formed through the combined action of the heat and solutions ema nating from a cooling intrusive granitic magma on limestones and the other intruded rocks and to a less extent on the granitic rock itself, by which the rocks are altered to or replaced by an aggregate of garnet, epidote, diopside, quartz, calcite, scheelite, and other minerals. Most deposits of this class are at or very near the contacts, and they clearly represent replacement of the limestones and other rocks.