Humboldt County Elk Management Sub-Plan
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Chapter 2 Management Plan
Chapter 2 Management Plan Mahogany Canyon in the High Rock Canyon Wilderness 2.1 INTRODUCTION This chapter contains objectives and decisions for managing the natural, physical and cultural resources described in the Act and those located in parts of the planning area not included in the National Conservation Area or designated Wilderness Areas. Background information is provided for each of these resources to establish points of reference for the decisions that follow. 2.2 PROGRAM-SPECIFIC OBJECTIVES AND DECISIONS 2.2.1 LAND HEALTH STANDARDS Land Health Standards are expressions of physical and biological condition or degree of function required for sustainable environmental health. These standards engender measurements that describe on- the-ground conditions in relation to the four fundamentals of healthy, properly functioning ecosystems that are identified at 43 CFR § 4180. These fundamentals are: • Watersheds in properly functioning physical condition; soil and plant conditions support infiltration, soil moisture storage, and the release of water that is in balance with climate and landform and maintain or improve water quality, water quantity, and timing and duration of flow. Ecological processes, including the hydrologic cycle, nutrient cycle, and energy flow, are maintained in order to support healthy biotic populations and communities. • Water quality complies with State water quality standards and achieves BLM management objectives. • Habitats are restored or maintained for listed, proposed, candidate and other special status species. BLACK ROCK-HIGH ROCK RMP 2-1 JULY 2004 Chapter 2 –Management Plan Standards are achieved through the use of guidelines developed for specific programs and uses. Because the Standards were originally applied to livestock grazing, guidelines for livestock grazing (Appendix B) will continue to apply to that use. -
Mule Deer and Antelope Staff Specialist Peregrine Wolff, Wildlife Health Specialist
STATE OF NEVADA Steve Sisolak, Governor DEPARTMENT OF WILDLIFE Tony Wasley, Director GAME DIVISION Brian F. Wakeling, Chief Mike Cox, Bighorn Sheep and Mountain Goat Staff Specialist Pat Jackson, Predator Management Staff Specialist Cody McKee, Elk Staff Biologist Cody Schroeder, Mule Deer and Antelope Staff Specialist 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 Sarah Hale Ed Partee Kari Huebner Jason Salisbury Matt Jeffress Kody Menghini Tyler Nall Scott Roberts 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 2018-2019 BIG GAME STATUS This program is supported by Federal financial assistance titled “Statewide Game Management” submitted to the U.S. -
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. -
Burning Man Geology Black Rock Desert.Pdf
GEOLOGY OF THE BLACK ROCK DESERT By Cathy Busby Professor of Geology University of California Santa Barbara http://www.geol.ucsb.edu/faculty/busby BURNING MAN EARTH GUARDIANS PAVILION 2012 LEAVE NO TRACE Please come find me and Iʼll give you a personal tour of the posters! You are here! In one of the most amazing geologic wonderlands in the world! Fantastic rock exposure, spectacular geomorphic features, and a long history, including: 1. PreCambrian loss of our Australian neighbors by continental rifting, * 2. Paleozoic accretion of island volcanic chains like Japan (twice!), 3. Mesozoic compression and emplacement of a batholith, 4. Cenozoic stretching and volcanism, plus a mantle plume torching the base of the continent! Let’s start with what you can see on the playa and from the playa: the Neogene to Recent geology, which is the past ~23 million years (= Ma). Note: Recent = past 15,000 years http://www.terragalleria.com Then we’ll “build” the terrane you are standing on, beginning with a BILLION years ago, moving through the Paleozoic (old life, ~540-253 Ma), Mesozoic (age of dinosaurs, ~253-65 Ma)) and Cenozoic (age of mammals, ~65 -0 Ma). Neogene to Recent geology Black Rock Playa extends 100 miles, from Gerlach to the Jackson Mountains. The Black Rock Desert is divided into two arms by the Black Rock Range, and covers 1,000 square miles. Empire (south of Gerlach)has the U.S. Gypsum mine and drywall factory (brand name “Sheetrock”), and thereʼs an opal mine at base of Calico Mtns. Neogene to Recent geology BRP = The largest playa in North America “Playa” = a flat-bottomed depression, usually a dry lake bed 3,500ʼ asl in SW, 4,000ʼ asl in N Land speed record: 1997 - supersonic car, 766 MPH Runoff mainly from the Quinn River, which heads in Oregon ~150 miles north. -
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. -
United States Department of the Interior U.S. Geological Survey
UNITED STATES DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY RESOURCE ASSESSMENT OF THE BUREAU OF LAND MANAGEMENT'S WINNEMUCCA DISTRICT AND SURPRISE RESOURCE AREA, NORTHWEST NEVADA AND NORTHEAST CALIFORNIA An Interim Project Status Report by Jeff L. Doebrich \ George V. Albino 2, Charles E. Barker 3, Wendell A. Duffield 4, Victor C. Dunn s, Willam F. Hanna 6, Joseph P. McFarlan 7, Dawn J. McGuire 8, Michael S. Miller 9, Stephen G. Peters \ Donald Plouff 10, Gary L. Raines \ Don L. Sawatzky1, and Gregory T. Spanski " United States Geological Survey Open-File Report 94-712 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North America Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1994 'USGS, MS 176, Reno Field Office, Mackay School of Mines, University of Nevada, Reno, NV 89557-0047 2U.S. Geological Survey, Unit 62101, APO AE 09811-2101 3USGS, MS 971, Box 25046, Denver Federal Center, Denver, CO 80225-0046 4USGS, Bldg. 3, 2255 North Gemini Dr., Flagstaff, AZ 86001-1698 5Bureau of Land Management, 705 E. 4th St., Winnemucca, NV 89445 6USGS, National Center, MS 927, 12201 Sunrise Valley Dr., Reston, VA 22092-0001 7Bureau of Land Management, P.O. Box 460, Cedarville, CA 96104 8USGS, MS 973, Box 25046, Denver Federal Center, Denver, CO 80225-0046 'Western Field Operations Center, U.S. Bureau of Mines, E. 360 Third Ave., Spokane, WA 99202 10USGS, MS 989, Bldg. -
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. -
University of Nevada Reno (Jreeology of Paleozoic Basinal Rocks in The
i \ University of Nevada Reno (jreeology of Paleozoic Basinal Rocks in the Northern Fox Range; Washoe County, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology. by Mark F. Thiesse V i August 1988 11 MINES LIBRARY The thesis of Mark F. Thiesse is approved: 2H03 Thesis Advisor Department Chairman Dean, Graduate School University of Nevada Reno August 1988 iii ACKNOWLEDGEMENTS I would like to thank Dr. R .A. Schweickert for his help, encouragement and patience throughout this project. Dr. Bruce Wardlaw provided the conodont identification which suggested the Carboniferous (?) age of the metamorphic rocks. Other thanks go to Andy Markos and Bob Strobel for help with the thin sections and interesting discussions. And finally, thanks to Carol for typing and for funding this project. iv ABSTRACT The Fox Range in Northwestern Nevada is a typical Basin and Range fault block mountain range which has been tilted about 30° to the east, accelerating the erosion of Tertiary volcanic rocks along the steep western flanks, and exposing Paleozoic metamorphic rocks. The Paleozoic rocks consist of a very fine grained, siliceous mudstone which was regionally metamorphosed from mid-greenschist to mid-amphibolite facies producing argillite, schist, limestone, quartzite, and gneiss. These Paleozoic rocks exhibit three generations of structures. Di created the schistose and gneissic layering common throughout the range, along with abundant tight to isoclinal folds. D2 structures are dominated by two large, map-scale antiforms and occasional smaller, open to tight, east to northeast trending folds and assorted lineations. D3 structures are limited to a few north-south trending, open to gentle folds which affect all pre-Tertiary lithologies. -
University of Nevada, Reno Geology, Alteration, Paragenesis, And
University of Nevada, Reno Geology, Alteration, Paragenesis, and Geochemistry of the Vortex Zone of the Hycroft Gold-Silver Deposit, Humboldt County, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Masters of Science in Geology by Karl Lowry Dr. Tommy Thompson/Thesis Advisor December, 2013 THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by KARL LOWRY entitled Geology, Alteration, Paragenesis, And Geochemistry Of The Vortex Zone Of The Hycroft Gold-Silver Deposit, Humboldt County, Nevada be accepted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Tommy Thompson, Ph. D., Advisor Christopher Henry, Ph. D., Committee Member Thom Seal, Ph. D, Graduate School Representative Marsha H. Read, Ph. D., Dean, Graduate School December, 2013 i Abstract The Hycroft gold-silver mine is a low sulfidation epithermal hot spring deposit located 55 miles west of Winnemucca, NV near the Blackrock desert. It is located in the historic Sulphur district, which has had mining on and off since the late 1800’s. Sulphur was the main commodity initially, with the later discovery and mining of silver, alunite, and mercury through the first half of the 20th century. Gold was discovered in the district in 1974 by the Duvall Corporation. The first gold mining and recovery by heap leach was conducted in 1983 by Standard Slag. Allied Nevada acquired the property in 2008 and discovered the Vortex zone through induced polarization and resistivity surveys. The oldest rocks in the region are the Permian Happy Creek Volcanic Series. These are overlain by the Auld Lang Syne Group of metamorphosed argillaceous to sandy sedimentary rock. -
Mineral Resources of the Black Rock Desert Wilderness Study Area, Humboldt County, Nevada
Mineral Resources of the Black Rock Desert Wilderness Study Area, Humboldt County, Nevada U.S. GEOLOGICAL SURVEY BULLETIN 1726-E Chapter E Mineral Resources of the Black Rock Desert Wilderness Study Area, Humboldt County, Nevada By J.P. CALZIA, W.A. LAWSON, J.C. DOHRENWEND, DONALD PLOUFF, and ROBERT TURNER U.S. Geological Survey J.E. OLSON U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1726 MINERAL RESOURCES OF WILDERNESS STUDY AREAS: HUMBOLDT AND PERSHING COUNTIES, NEVADA DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1987 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center, Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Mineral resources of the Black Rock Desert Wilderness Study Area, Humboldt County, Nevada. U.S. Geological Survey Bulletin 1726-E (Mineral resources of wilderness study areas Humboldt and Pershing counties, Nevada ; ch. E) Bibliography Supt. of Docs. No.: I 19.3:1726-E 1. Mines and mineral resources Nevada Black Rock Desert Wilderness. 2. Black Rock Desert Wilderness (Nev.) I. Calzia, J.P. II. Series. III. Series: U.S. Geological Survey Bulletin 1726. QE75.B9 No. 1726-E 557.3s 87-600346 [TN24.N3] [553'.09793'54] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine the mineral values, if any, that may be present. -
Mesozoic Geology of the Jackson Mountains, Northwestern Nevada
Mesozoic geology of the Jackson Mountains, northwestern Nevada BRANCH J. RUSSELL* Department of Geological Sciences, Northwestern University, Evanston, Illinois 60201 ABSTRACT morphism and the development of only modest generally regions of oceanic and/or magmatic foliation, except near thrust faults, suggest that arc volcanism and sedimentation prior to mid- The Jackson Mountains Unit, a tectono- thrusting in the Jackson Mountains was thin Cretaceous time. The Paleozoic continental stratigraphic unit in the Jackson Mountains, skinned. margin of North America, recognized by Burch- northwestern Nevada, includes the Upper Trias- fiel and Davis (1972), apparently strikes north- sic pelagic, carbonate, and volcanogenic sedi- INTRODUCTION east through west-central and north-central mentary rocks of the Boulder Creek beds, the Nevada. Until now, regional tectonic models Upper Triassic to Middle Jurassic volcanic and The Black Rock Desert region in north- have considered the Black Rock Desert region volcanogenic sedimentary rocks of the Happy western Nevada is one of the least understood to be underlain by a late Paleozoic magmatic arc Creek complex, and the Lower Cretaceous provinces of pre-Tertiary rocks in the western (Moores, 1970; Silberling, 1973; Burchfiel and sedimentary rocks of the King Lear Formation. Cordillera. Considerably more is known of the Davis, 1972; Speed, 1977, 1979; and Stevens, The lower Mesozoic rocks of the Jackson pre-Tertiary paleogeography and tectonic his- 1977). Speed (1978a) proposed that cooling and Mountains Unit record a transition from sedi- tory of adjacent provinces (Fig. 1). The northern subsidence of a late Paleozoic magmatic arc in mentation on a starved lower slope-basinal Sierra (D'Allura and others, 1977; Schweikert, northwestern Nevada during early Mesozoic margin, locally interrupted by prograding depo- 1978), eastern Klamath (Irwin, 1977; Davis and time promoted the formation of a marine sition from shoaled Mesozoic and possibly Pa- others, 1978; Hamilton, 1978), and eastern basinal province.