Spring 2020, Volume 39.1
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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. -
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. -
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. -
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. unnamed faults southeast Pine Forest Range (Class A) No. 1492 Last Review Date: 1998-07-19 citation for this record: Sawyer, T.L., compiler, 1998, Fault number 1492, unnamed faults southeast Pine Forest Range, 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 02:50 PM. Synopsis This group of subparallel to left-stepping faults appears to form a zone that has range-bounding normal faults along the southeast front of the southern Pine Forest Range and piedmont faults near Tipperary Mine and southeast of Duffer Peak. A few range-front faults near Battle Creek and north of Tipperary Mine are marked by short scarp on piedmont-slope deposits. Reconnaissance photogeologic mapping of the fault zone is the source of data. Trench investigations and detailed studies of scarp morphology have not been conducted. Name Refers to faults mapped by Willden (1964 #3002), Slemmons comments (1966, unpublished Vya 1? X 2? sheet), and Dohrenwend and Moring (1991 #281) along the southeast front and within the southern Pine Forest Range, from Battle Creek northeast to the southern Pine Forest Range, from Battle Creek northeast to the west flank of Duffer Peak at Big Creek, and faults in the northernmost Black Rock Range. -
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 -
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. -
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 -
Timing of Cenozoic Volcanism and Basin and Range Extension in Northwestern Nevada: New Constraints from the Northern Pine Forest Range
Timing of Cenozoic volcanism and Basin and Range extension in northwestern Nevada: New constraints from the northern Pine Forest Range Joseph P. Colgan† Trevor A. Dumitru Michael McWilliams Elizabeth L. Miller Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, USA ABSTRACT Oligocene and Miocene volcanism, and simi- widespread middle Miocene extension in the lar geologic relationships in nearby ranges center of the province (Colgan et al., 2004). High Eocene–middle Miocene volcanic rocks in suggest that a larger region of northwest- fault-bounded ranges in this region give way the northern Pine Forest Range, Nevada, are ern Nevada was also little extended during northward to the high lava plateaus of southern ideally situated for reconstructing the timing this interval. Basin and Range faulting in Oregon, and the pre-Miocene tectonic history and style of volcanism and extensional fault- northwestern Nevada appears to have begun is obscured in many places by gently dipping ing in the northwesternmost part of the Basin no earlier than 12 Ma, making it distinctly Cenozoic lavas. Previous workers suggested and Range province. A conformable sequence younger than deformation in much of central that older Oligocene–early Miocene rocks in of Cenozoic volcanic and sedimentary strata and southern Nevada, where peak extension northwestern Nevada (Fig. 2) may record early in the northern Pine Forest Range dips occurred in the middle Miocene or earlier. Miocene(?) extensional faulting (Noble et al., ~30°W, and 11 new 40Ar/39Ar ages from this 1970; Graichen, 1972), but the relevant units sequence defi ne 3 major episodes of volcanic Keywords: Basin and Range, Pine Forest have not been studied in suffi cient detail to activity. -
UNIVERSITY of NEVADA RENO PERMIAN-TRIASSIC SOURCE BED ANALYSIS at QUINN RIVER CROSSING, HUMBOLDT COUNTY, NEVADA a Thesis Submitt
UNIVERSITY OF NEVADA RENO PERMIAN-TRIASSIC SOURCE BED ANALYSIS AT QUINN RIVER CROSSING, HUMBOLDT COUNTY, NEVADA A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by Scott Byron McDaniel III January 1982 MINES LIBRARY I ( * 2 .3 © 1982 SCOTT BYRON McDANIEL All Rights Reserved The thesis of Scott Byron McDaniel is approved: University of Nevada Reno January, 1982 11 ACKNOWLEDGMENTS The writer wishes to take this opportunity of expressing his appreciation to the many people who have contributed of their time and energy in the furtherance of this investigation. I wish to acknowledge the help ful discussions with N. J. Silberling, R. C. Speed, B. R. Wardlaw and L. T. Larson. Special appreciation is ex pressed to J. Lintz, Jr. for his continuing advice throughout the project. Advice and assistance in sur veying, mapping and rock sampling were given by T. De Rocher. Special gratitude is also extended to the Reynosa family and Jim Reid of the Ivory Ranch at Quinn River Crossing, Nevada. I wish to thank Sun Exploration Company, Denver, Colorado, who partially financed this project and also gave me great support. Appreciation is expressed for thin section analyses prepared by Michael Wilson of AGAT Consultants, Inc., of Denver, Colorado, under contract to Sun Exploration Company. Ill ABSTRACT The Quinn River Crossing area is located in north west Humboldt County, Nevada„ Measured sections are lo cated at the southeast margin of the Pine Forest Range and southwest area of the Bilk Creek Range. The Permian Lime stone and Triassic units in both areas have yielded faunules.