Paleozoic Tectonic Domains of Nevada: an Interpretive Discussion to Accompany the Geologic Map of Nevada
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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. -
Ecoregions of Nevada Ecoregion 5 Is a Mountainous, Deeply Dissected, and Westerly Tilting Fault Block
5 . S i e r r a N e v a d a Ecoregions of Nevada Ecoregion 5 is a mountainous, deeply dissected, and westerly tilting fault block. It is largely composed of granitic rocks that are lithologically distinct from the sedimentary rocks of the Klamath Mountains (78) and the volcanic rocks of the Cascades (4). A Ecoregions denote areas of general similarity in ecosystems and in the type, quality, Vegas, Reno, and Carson City areas. Most of the state is internally drained and lies Literature Cited: high fault scarp divides the Sierra Nevada (5) from the Northern Basin and Range (80) and Central Basin and Range (13) to the 2 2 . A r i z o n a / N e w M e x i c o P l a t e a u east. Near this eastern fault scarp, the Sierra Nevada (5) reaches its highest elevations. Here, moraines, cirques, and small lakes and quantity of environmental resources. They are designed to serve as a spatial within the Great Basin; rivers in the southeast are part of the Colorado River system Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the Ecoregion 22 is a high dissected plateau underlain by horizontal beds of limestone, sandstone, and shale, cut by canyons, and United States (map): Washington, D.C., USFS, scale 1:7,500,000. are especially common and are products of Pleistocene alpine glaciation. Large areas are above timberline, including Mt. Whitney framework for the research, assessment, management, and monitoring of ecosystems and those in the northeast drain to the Snake River. -
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. -
HISTORY of the TOIYABE NATIONAL FOREST a Compilation
HISTORY OF THE TOIYABE NATIONAL FOREST A Compilation Posting the Toiyabe National Forest Boundary, 1924 Table of Contents Introduction ..................................................................................................................................... 3 Chronology ..................................................................................................................................... 4 Bridgeport and Carson Ranger District Centennial .................................................................... 126 Forest Histories ........................................................................................................................... 127 Toiyabe National Reserve: March 1, 1907 to Present ............................................................ 127 Toquima National Forest: April 15, 1907 – July 2, 1908 ....................................................... 128 Monitor National Forest: April 15, 1907 – July 2, 1908 ........................................................ 128 Vegas National Forest: December 12, 1907 – July 2, 1908 .................................................... 128 Mount Charleston Forest Reserve: November 5, 1906 – July 2, 1908 ................................... 128 Moapa National Forest: July 2, 1908 – 1915 .......................................................................... 128 Nevada National Forest: February 10, 1909 – August 9, 1957 .............................................. 128 Ruby Mountain Forest Reserve: March 3, 1908 – June 19, 1916 .......................................... -
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. -
Preliminary Geologic Map of the Galena Canyon Quadrangle, Lander County, Nevada
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY To accompany the Preliminary Geologic Map of the Galena Canyon Quadrangle, Lander County, Nevada by JeffL.Doebrich1 Open-File Report 94-664 Prepared in cooperation with Santa Fe Pacific Mining Inc. under Cooperative Research and Development Agreement 9300-1-94 1994 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. !U.S. Geological Survey, Reno Field Office, MS-176, Mackay School of Mines, University of Nevada, Reno, Nevada, 89557-0047 DESCRIPTION OF MAP UNITS Qd Mine dump (Holocene) Present around active and abandoned mining operations in the Copper Canyon, Iron Canyon, an Copper Basin areas Qfp Flood plain deposits (Quaternary) Includes sand, silt, and clay deposits in the flood plain of the Reese River in the southeast corner of the quadrangle. Contacts approximately located using large-scale color aerial photographs Qaf Younger alluvium and fanglomerate deposits (Quaternary) Clay, silt, sand, and gravel primarily in active stream channels but also covering outwash fans at the mouth of major drainages emanating from the range. Contacts of outwash fans approximately located using large-scale color aerial photographs Qc Colluvium (Quaternary) Includes talus, slope wash, and other colluvial deposits Qls Landslide deposits (Quaternary) Qoa Older alluvium (Quaternary) Poorly sorted gravel deposits with a silty to sandy matrix. Includes terrace and valley-fill deposits at higher elevations; dissected by stream channels containing younger alluvium (Qaf). -
Lahontan Cutthroat Trout Species Management Plan for the Upper Humboldt River Drainage Basin
STATE OF NEVADA DEPARTMENT OF WILDLIFE LAHONTAN CUTTHROAT TROUT SPECIES MANAGEMENT PLAN FOR THE UPPER HUMBOLDT RIVER DRAINAGE BASIN Prepared by John Elliott SPECIES MANAGEMENT PLAN December 2004 LAHONTAN CUTTHROAT TROUT SPECIES MANAGEMENT PLAN FOR THE UPPER HUMBOLDT RIVER DRAINAGE BASIN SUBMITTED BY: _______________________________________ __________ John Elliott, Supervising Fisheries Biologist Date Nevada Department of Wildlife, Eastern Region APPROVED BY: _______________________________________ __________ Richard L. Haskins II, Fisheries Bureau Chief Date Nevada Department of Wildlife _______________________________________ __________ Kenneth E. Mayer, Director Date Nevada Department of Wildlife REVIEWED BY: _______________________________________ __________ Robert Williams, Field Supervisor Date Nevada Fish and Wildlife Office U.S.D.I. Fish and Wildlife Service _______________________________________ __________ Ron Wenker, State Director Date U.S.D.I. Bureau of Land Management _______________________________________ __________ Edward C. Monnig, Forest Supervisor Date Humboldt-Toiyabe National Forest U.S.D.A. Forest Service TABLE OF CONTENTS Contents EXECUTIVE SUMMARY ……………………………………………………………………..1 INTRODUCTION……………………………………………………………………………….…2 AGENCY RESPONSIBILITIES……………………………………………………………….…4 CURRENT STATUS……………………………………………………………………………..6 RECOVERY OBJECTIVES……………………………………………………………………19 RECOVERY ACTIONS…………………………………………………………………………21 RECOVERY ACTION PRIORITIES BY SUBBASIN………………………………………….33 IMPLEMENTATION SCHEDULE……………………………………………………………..47 -
Central Nevada
University of Nevada Reno LATE CENOZOIC GEOLOGY AND TECTONICS OF STEWART AND MONTE CRISTO VALLEYS, WEST - CENTRAL NEVADA A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science .I by Mark Philip Molinari fit ; December, 1984 ii ABSTRACT Discontinuous right-normal-slip faults comprise the N30 0W trending, 45 kilometer long Stewart - Monte Cristo fault zone (SMCFZ). Initiation of the SMCFZ postdates the 15.5 to 11.0 m.y. Esmeralda Formation. Right-normal-slip >1 meter occurred on the southern segment of the SMCFZ during the 1932 Cedar Mountain earthquake (Ms= 7.2-7.3). Geomor- phic evidence supports at least three and possibly five or six surface faulting events on the southern segment during the latest Pleistocene and Holocene. Gentle folds in the Esmeralda Formation east of and sub-parallel to the SMCFZ are coeval with and genetically related to faulting. Structural development of the SMCFZ is similar to other right-lateral wrench faults and is consistent with labora- tory wrench fault models. The SMCFZ is the youngest and southeasternmost fault of a system of major late Cenozoic, left-stepping, en echelon right-slip faults in the central Walker Lane. - .~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ iii TABLE OF CONTENTS page ABSTRACT .................. S S ii INTRODUCTION . 0 0 1 0 * I Location and Extent of Study Area . S S S S 1 Regional Tectonic and Geologic Setting. S. S a * 0 1 Purpose and Scope ...... a a * a 5 Methodology . 6 Previous Work . 8 Physiography. 10 MESOZOIC STRATIGRAPHY. 13 Sedimentary Rocks . & 13 Mina Formation . 13 Luning Formation . 13 Plutonic Rocks . -
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. -
Eocene–Early Miocene Paleotopography of the Sierra Nevada–Great Basin–Nevadaplano Based on Widespread Ash-Flow Tuffs and P
Origin and Evolution of the Sierra Nevada and Walker Lane themed issue Eocene–Early Miocene paleotopography of the Sierra Nevada–Great Basin–Nevadaplano based on widespread ash-fl ow tuffs and paleovalleys Christopher D. Henry1, Nicholas H. Hinz1, James E. Faulds1, Joseph P. Colgan2, David A. John2, Elwood R. Brooks3, Elizabeth J. Cassel4, Larry J. Garside1, David A. Davis1, and Steven B. Castor1 1Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA 2U.S. Geological Survey, Menlo Park, California 94025, USA 3California State University, Hayward, California 94542, USA 4Department of Earth and Environment, Franklin & Marshall College, Lancaster, Pennsylvania 17604, USA ABSTRACT the great volume of erupted tuff and its erup- eruption fl owed similar distances as the mid- tion after ~3 Ma of nearly continuous, major Cenozoic tuffs at average gradients of ~2.5–8 The distribution of Cenozoic ash-fl ow tuffs pyroclastic eruptions near its caldera that m/km. Extrapolated 200–300 km (pre-exten- in the Great Basin and the Sierra Nevada of probably fi lled in nearby topography. sion) from the Pacifi c Ocean to the central eastern California (United States) demon- Distribution of the tuff of Campbell Creek Nevada caldera belt, the lower gradient strates that the region, commonly referred and other ash-fl ow tuffs and continuity of would require elevations of only 0.5 km for to as the Nevadaplano, was an erosional paleovalleys demonstrates that (1) the Basin valley fl oors and 1.5 km for interfl uves. The highland that was drained by major west- and Range–Sierra Nevada structural and great eastward, upvalley fl ow is consistent and east-trending rivers, with a north-south topographic boundary did not exist before with recent stable isotope data that indicate paleodivide through eastern Nevada. -
Paleozoic Geology of the Dobbin Summit-Clear Creek Area, Monitor
AN ABSTRACT OF THE THESIS OF DIANE CAROL WISE for the degree of MASTER OF SCIENCE in Geology presented on August 13, 1976 Title: PALEOZOIC GEOLOGY OF THE DOBBIN SUMMIT- CLEAR CREEK AREA, MONITOR RANGE, NYiE COUNTY, NEVADA Abstract approved: Redacted for Privacy son Paleozoic limestones, dolomites, quartz arenites, and other clastic rocks were mapped in the vicinity of Dobbin Summit and Clear Creek in the central Monitor Range. Sedimentary rock units present in this area represent the shallow-shelf eastern assemblage and basin and also the basin-slope facies of the traditional limestone- clastic assemblage. The four oldest, Ordovician, units were deposited in shallow shelf environments. The Lower Ordovician Goodwin Formation is composed of about 1200 feet of calcareous shales and thin-bedded limestones. The overlying Antelope Valley Limestone is about 500 feet thick and consists of wackestones, packstones, and rare algal grainstones.The Copenhagen Formation (135 feet thick) is the highest regressive deposit of sandstone, siltstone, and limestone below the transgressive Eureka Quartzite.The Eureka is a quartz arenite 181 feet thick, with an intercalated shallow marine dolomite member. The transition from shallow to deep water conditions can be seen in the change from algal boundstones to laminated lime mud- stones in the Hanson Creek Formation (190 feet thick).The super- jacent Roberts Mountains Formation (285 feet thick) is composed of lime mudstones and allodapic beds deposited in basinal, deep water conditions.During earliest Devonian -
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.