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MULE DEER Unit 032
Nevada Hunter Information Sheet MULE DEER Unit 032 LOCATION: Unit 032 is located northwest of the town of Winnemucca. The unit is bounded on the north by the Oregon state line, on the east by State Route 140/291, on the south by Unit 034 and on the west by the Sheldon NWR boundary. ELEVATION: The elevations range from a high of 9,458 feet at Duffer Peak in the Pine Forest Range to 4,000 feet along the Black Rock Desert or the base of the Pine Forest Range. TERRAIN: The Pine Forest Range runs north and south with steep canyons draining into the flats. The valley floors have some agricultural development. VEGETATION: The majority of the basins and slopes up to 6,500-foot elevation. Above this elevation, sites are typically characterized by aspens in the drainages, mahogany groves and dense stands of brush and grass. There are some limber pine stands at the higher elevations around Duffer Peak. LAND STATUS: Approximately 85% of the unit is public-owned. Private land is mostly associated with agriculture or mining. HUNTER ACCESS: From Winnemucca drive north on Highway 95 and west on Highway 140. Primary and secondary road access is relatively good. Four-wheel drive (high clearance) vehicles are recommended to access most of the unit for hunting purposes. The Blue Lakes Wilderness Study Area covers 24,000 acres the Duffer Peak area and is closed to all motorized travel. Access on some roads may be restricted by private landowners in the Leonard Creek drainage. Ask permission before accessing private parcels in this area. -
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. -
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. -
Quaternary Fault and Fold Database of the United States
Jump to Navigation Quaternary Fault and Fold Database of the United States As of January 12, 2017, the USGS maintains a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. For the most up-to-date information, please refer to the interactive fault map. Lake Range fault zone (Class A) No. 1607 Last Review Date: 2016-03-03 citation for this record: Sawyer, T.L., Haller, K.M., and Adams, K., compilers, 2016, Fault number 1607, Lake Range fault zone, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, https://earthquakes.usgs.gov/hazards/qfaults, accessed 12/14/2020 02:29 PM. Synopsis This discontinuous zone of normal faults bounds the west front of the Fox Range and Lake Range from Buckbrush Spring southward along and apparently beneath Pyramid Lake to east of Anaho Island, and locally traverses piedmont slope along the east side of the Pyramid Lake basin. Both the Lake Range and Fox Range are east-tilted blocks that border sedimentary basins on their west sides. The range-front faults are expressed as abrupt west-facing range fronts and juxtapose late Quaternary piedmont- slope deposits against bedrock. Short piedmont faults are marked by scarps on late Quaternary piedmont-slope deposits east of Sheep Pass in the Lake Range and at mouth of Hell's Kitchen Canyon, where the fault projects southward beneath Pyramid Lake. Regional geologic mapping and reconnaissance photogeologic mapping are the sources of data. Trench investigations and detailed studies of scarp morphology have not been conducted. -
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. -
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. -
The Timing and Evolution of Cenozoic Extensional Normal Faulting in The
AN ABSTRACT OF THE THESIS OF Zachary J. Gonsior for the degree of Master of Science in Geology presented on March 13, 2006. Title: The Timing and Evolution of Cenozoic Extensional Normal Faulting in the Southern Tobin Range, Pershing County, Nevada. Abstract approved:______________________________________________________ John H. Dilles The Tobin Range of central Nevada lies in the Basin and Range extensional province near the transition between more extended terrane (>50%) to the south and east, and generally less extended terrane to the north and west. Geologic mapping, 40Ar/39Ar dating and whole-rock geochemical analysis were employed to establish the Cenozoic stratigraphy, geometry and timing of normal faults, and magnitude of extension in the vicinity of Golconda Canyon in the southern Tobin Range. The Golconda Canyon area lies near the westernmost extent of a major east- west trending paleo-valley that likely predates Basin and Range extension in that region. In-filling and over-topping the paleo-valley are a series of Oligocene to Miocene volcanic rocks. Confined to the paleo-valley is a series of thin basaltic lava flows above which lies the rhyolitic Caetano Tuff (~34 Ma). Units also present in the Golconda Canyon area, but not confined to the paleo-valley include, from bottom to top, a ~700m-thick sequence of andesite lavas, lahars, and ignimbrites (~33 Ma); four late Oligocene-early Miocene rhyolite ignimbrites; a unit of syn-tectonic landslide breccia and sedimentary rock; and a sequence of fluvial and lacustrine tuffaceous sedimentary rocks intercalated in the center of the section with a 60m-thick series of basaltic lavas (~14 Ma). -
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. -
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. -
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