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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. -
Wilderness Study Areas
I ___- .-ll..l .“..l..““l.--..- I. _.^.___” _^.__.._._ - ._____.-.-.. ------ FEDERAL LAND M.ANAGEMENT Status and Uses of Wilderness Study Areas I 150156 RESTRICTED--Not to be released outside the General Accounting Wice unless specifically approved by the Office of Congressional Relations. ssBO4’8 RELEASED ---- ---. - (;Ao/li:( ‘I:I)-!L~-l~~lL - United States General Accounting OfTice GAO Washington, D.C. 20548 Resources, Community, and Economic Development Division B-262989 September 23,1993 The Honorable Bruce F. Vento Chairman, Subcommittee on National Parks, Forests, and Public Lands Committee on Natural Resources House of Representatives Dear Mr. Chairman: Concerned about alleged degradation of areas being considered for possible inclusion in the National Wilderness Preservation System (wilderness study areas), you requested that we provide you with information on the types and effects of activities in these study areas. As agreed with your office, we gathered information on areas managed by two agencies: the Department of the Interior’s Bureau of Land Management (BLN) and the Department of Agriculture’s Forest Service. Specifically, this report provides information on (1) legislative guidance and the agency policies governing wilderness study area management, (2) the various activities and uses occurring in the agencies’ study areas, (3) the ways these activities and uses affect the areas, and (4) agency actions to monitor and restrict these uses and to repair damage resulting from them. Appendixes I and II provide data on the number, acreage, and locations of wilderness study areas managed by BLM and the Forest Service, as well as data on the types of uses occurring in the areas. -
Rose-Marcella-Thesis-2020.Pdf
CALIFORNIA STATE UNIVERSITY, NORTHRIDGE Nebkha Morphology, Distribution and Stability Black Rock Playa, Nevada A thesis submitted in partial fulfillment of the requirements For the degree of Master of Arts in Geography By Marcella Rose December 2019 The thesis of Marcella Rose is approved: _______________________________________ _____________ Dr. Julie Laity Date _______________________________________ _____________ Dr. Thomas Farr Date _______________________________________ _____________ Dr. Amalie Orme, Chair Date California State University, Northridge ii Acknowledgements Dr. Orme, I really don’t think that there is a sufficient combination of words that exist to properly express the immense amount of gratitude I feel for everything that you have done for me. This college education changed my life for the better and I hope you realize what a significant role you were within that experience. I am thankful that not only did I get a great professor, but also a friend. Dr. Laity, thank you so much for having faith in me and for taking me on as one of your last students to advise. But most of all, thank you for pushing me to be better – I needed that. Dr. Farr, I was so excited during DEVELOP that you accepted to be a part of my committee. It was a pleasure to work with you within the Black Rock Playa research team but then to also take our research a step further for this graduate thesis. I would also like to thank the staff at the Bureau of Land Management, Winnemucca: Dr. Mark E. Hall, Field Manager of the Black Rock Field Office; Shane Garside, Black Rock Station Manager/ Outdoor Recreation Planner; Brian McMillan, Rangeland Management Technician; and Braydon Gaard, Interim Outdoor Recreation Planner. -
Ground-Water Resources-Reconnaissance Series Report 20
- STATE OF NEVADA ~~~..._.....,.,.~.:RVA=rl~ AND NA.I...U~ a:~~::~...... _ __,_ Carson City_ GROUND-WATER RESOURCES-RECONNAISSANCE SERIES REPORT 20 GROUND- WATER APPRAISAL OF THE BLACK ROCK DESERT AREA NORTHWESTERN NEVADA By WILLIAM C. SINCLAIR Geologist Price $1.00 PLEASE DO NOT REMO V~ f ROM T. ':'I S OFFICE ;:: '· '. ~- GROUND-WATER RESOURCES--RECONNAISSANCE SERIES .... Report 20 =· ... GROUND-WATER APPRAISAL OF THE BLACK ROCK OESER T AREA NORTHWESTERN NEVADA by William C. Sinclair Geologist ~··· ··. Prepared cooperatively by the Geological SUrvey, U. S. Department of Interior October, 1963 FOREWORD This reconnaissance apprais;;l of the ground~water resources of the Black Rock Desert area in northwestern Nevada is the ZOth in this series of reports. Under this program, which was initiated following legislative action • in 1960, reports on the ground-water resources of some 23 Nevada valleys have been made. The present report, entitled, "Ground-Water Appraisal of the Black Rock Desert Area, Northwe$tern Nevada", was prepared by William C. Sinclair, Geologist, U. s. Geological Survey. The Black Rock Desert area, as defined in this report, differs some~ what from the valleys discussed in previous reports. The area is very large with some 9 tributary basins adjoining the extensive playa of Black Rock Desert. The estimated combined annual recharge of all the tributary basins amounts to nearly 44,000 acre-feet, but recovery of much of this total may be difficult. Water which enters into the ground water under the central playa probably will be of poor quality for irrigation. The development of good produci1>g wells in the old lake sediments underlying the central playa appears doubtful. -
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. -
Humboldt County Elk Management Sub-Plan
HUMBOLDT COUNTY ELK MANAGEMENT SUB-PLAN TABLE OF CONTENTS INTRODUCTION 2 BACKGROUND 3 PLAN GOAL 5 SCOPE OF THE PLAN 5 HUMBOLDT COUNTY PLAN PROCESS 6 POTENTIAL ELK CARRYING CAPACITY ASSESSMENT 7 STEERING COMMITTEE PROCESS 9 PLANNING UNIT SPECIFICS 10 UNITS 031 11 UNITS 032 13 UNITS 033 15 UNIT 034 17 UNIT 035 20 UNIT 051 22 MANAGEMENT ACTIONS 25 NDOW 25 BLM 27 USFS 27 USFWS 28 APPENDIX 30 1 INTRODUCTION Low densities of elk have been reported in many portions of Humboldt County with the bulk of the sightings occurring recently in unit 051. Based on observations that started as early as 1990 to 2014, it appears a small group of elk established a home range within the Santa Rosa Range. This small herd has continued to increase throughout the last two decades. In January of 2013, two cow elk were collared to track movement and use areas. Since the start of that project, to date, one collar has been recovered with data of known use areas. The second collar is due to fall off in August of 2015. In January 2014, the first elk survey flight was conducted. During this survey, a total of 21 elk were observed. All 21 animals were bulls with no cows being located. Prior to this survey, animals have been observed from the air on several occasions, incidentally during other specie surveys. Another follow-up survey was conducted in March 2015 to try to determine the number of elk existing in the Santa Rosa Range. During this flight no elk were observed. -
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. -
Gravity and Magnetic Data Along a Seismic Refraction-Reflection Line in Northwest Nevada and Northeast California
Gravity and Magnetic Data Along a Seismic Refraction-Reflection Line in Northwest Nevada and Northeast California By Janet E. Tilden, David A. Ponce, Jonathan M.G. Glen, and Kathleen D. Gans Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government Report Series 2005-1446 U.S. Department of the Interior U.S. Geological Survey Contents Introduction ...................................................................................................................................1 Acknowledgments .........................................................................................................................1 Gravity and Magnetic Data............................................................................................................1 Gravity Methods .........................................................................................................................2 Magnetic Methods......................................................................................................................3 General Discussion .......................................................................................................................3 References Cited ..........................................................................................................................5 Appendix .....................................................................................................................................11 Figures Figure 1. Shaded relief -
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.