Decision-Support Tools for Conserving Greater Sage-Grouse During Fire and Fuels Management Projects in Pinyon and Juniper Woodla
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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 .......................................... -
Northern Paiute and Western Shoshone Land Use in Northern Nevada: a Class I Ethnographic/Ethnohistoric Overview
U.S. DEPARTMENT OF THE INTERIOR Bureau of Land Management NEVADA NORTHERN PAIUTE AND WESTERN SHOSHONE LAND USE IN NORTHERN NEVADA: A CLASS I ETHNOGRAPHIC/ETHNOHISTORIC OVERVIEW Ginny Bengston CULTURAL RESOURCE SERIES NO. 12 2003 SWCA ENVIROHMENTAL CON..·S:.. .U LTt;NTS . iitew.a,e.El t:ti.r B'i!lt e.a:b ~f l-amd :Nf'arat:1.iern'.~nt N~:¥G~GI Sl$i~-'®'ffl'c~. P,rceP,GJ r.ei l l§y. SWGA.,,En:v,ir.e.m"me'Y-tfol I €on's.wlf.arats NORTHERN PAIUTE AND WESTERN SHOSHONE LAND USE IN NORTHERN NEVADA: A CLASS I ETHNOGRAPHIC/ETHNOHISTORIC OVERVIEW Submitted to BUREAU OF LAND MANAGEMENT Nevada State Office 1340 Financial Boulevard Reno, Nevada 89520-0008 Submitted by SWCA, INC. Environmental Consultants 5370 Kietzke Lane, Suite 205 Reno, Nevada 89511 (775) 826-1700 Prepared by Ginny Bengston SWCA Cultural Resources Report No. 02-551 December 16, 2002 TABLE OF CONTENTS List of Figures ................................................................v List of Tables .................................................................v List of Appendixes ............................................................ vi CHAPTER 1. INTRODUCTION .................................................1 CHAPTER 2. ETHNOGRAPHIC OVERVIEW .....................................4 Northern Paiute ............................................................4 Habitation Patterns .......................................................8 Subsistence .............................................................9 Burial Practices ........................................................11 -
Hydrographic Basins Information
A p p e n d i x A - B a s i n 54 Crescent Valley Page 1 of 6 Basin 54 - Crescent Valley Crescent Valley is a semi-closed basin that is bounded on the west by the Shoshone Range, on the east by the Cortez Mountains, on the south by the Toiyabe Range, and on the north by the Dry Hills. The drainage basin is about 45 miles long, 20 miles wide, and includes an area of approximately 750 square miles. Water enters the basin primarily as precipitation and is discharged primarily through evaporation and transpiration. Relatively small quantities of water enter the basin as surface flow and ground water underflow from the adjacent Carico Lake Valley at Rocky Pass, where Cooks Creek enters the southwestern end of Crescent Valley. Ground water generally flows northeasterly along the axis of the basin. The natural flow of ground water from Crescent Valley discharges into the Humboldt River between Rose Ranch and Beowawe. It is estimated that the average annual net discharge rate is approximately 700 to 750 acre-feet annually. Many of the streams which drain snowmelt of rainfall from the mountains surrounding Crescent Valley do not reach the dry lake beds on the Valley floor: instead, they branch into smaller channels that eventually run dry. Runoff from Crescent Valley does not reach Humboldt River with the exception of Coyote Creek, an intermittent stream that flows north from the Malpais to the Humboldt River and several small ephemeral streams that flow north from the Dry Hills. Surface flow in the Carico Lake Valley coalesces into Cooks Creek, which enters Crescent Valley through Rocky Pass. -
Paleozoic Rocks Antelope Valley Eureka and Nye Counties Nevada
:It k 'I! ' Paleozoic Rocks Antelope Valley Eureka and Nye Counties Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 423 Paleozoic Rocks of Antelope Valley Eureka and Nye Counties Nevada By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 423 P,rinciples of stratigraphy applied in descriptive study of the Central Great Basin Paleozoic column UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page Silurian system ____________________________________ _ Abstract------------------------------------------- 1 36 Introduction. _____________________________________ _ 2 General features-------------------------------- 36 Geologic setting ______________ ------ ___ --------- 2 Roberts Mountains formation ___________________ _ 37 History of investigation ________________________ _ 5 Lone Mountain dolomite ______ ---_-------------- 39 Purpose and scope _____________ -- ______ ------ --- 6 Devonian system ______________ ---- __ - _- ___ - _------- 41 Acknowledgments ______________________________ _ 6 General features _____________ - ___________ -_----- 41 Geologic structure as related to stratigraphy __________ _ 6 Western Helderberg age limestones of the Monitor Paleontologic studies ______ ..:. _______ ~ ________________ _ 9 · Range ______ - _.- ___ --------------------------- 42 The Paleozoic column at Antelope Valley -
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 -
Final Report
FINAL REPORT Decision-support tools for conserving Greater Sage-Grouse during fire and fuels management projects in pinyon and juniper woodlands JFSP 09-1-08-4 Erica Fleishman, University of California, Davis (principal investigator) Jeanne C. Chambers, USDA Forest Service, Rocky Mountain Research Station, Reno, Nevada (co-principal investigator) David S. Dobkin, High Desert Ecological Research Institute, Bend, Oregon (co-principal investigator) Brett G. Dickson, Conservation Science Partners, Truckee, California (co-principal investigator) ABSTRACT Prescribed fire and other fuels management treatments have been suggested as mechanisms to slow expansion of pinyon and juniper woodlands while minimizing potential expansion of cheatgrass (Bromus tectorum) and increasing habitat quality and quantity for Greater Sage- Grouse (Centrocercus urophasianus). These treatments also may reduce the probability of severe wildfires, which can have undesirable effects on social, economic, cultural, and ecological values. However, achieving long-term goals related to fire and fuels may conflict with short-term goals related to survival and viability of native species. Fire can fragment high-quality habitat for species associated with woodlands, including more than 20 native species of breeding birds. Additionally, expansion of pinyon and juniper woodlands may have been patchy but common and natural before European settlement of the Great Basin. Evaluation of spatial and temporal trade-offs of actions to reduce probability of wildfire, maintain sagebrush steppe, and conserve native species, including rare or endangered species, can identify strategies that are either consistent or incompatible with achieving these and other objectives simultaneously. We monitored use by Greater Sage-Grouse of areas treated with fire or proposed for treatment. -
A History of the Tonopah Area and Adjacent Region of Central Nevada, 1827-1941
A History of the Tonopah Area and Adjacent Region of Central Nevada, 1827-1941 A History of the Tonopah Area and Adjacent Region of Central Nevada, 1827-1941 A thesis presented to the Faculty of the Department of History UNIVERSITY OF NEVADA In partial fulfillment of the requirements for the degree MASTER OF ARTS by Lucile Rae Berg MAY 1942 with an introduction by Robert D. McCracken Nye County Press TONOPAH, NEVADA Published in 2011 by Nye County Press P.O. Box 153 Tonopah, Nevada 89049 Copyright © 2011 by Nye County Press All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage or retrieval system, without permission in writing from the publisher. ISBN 978-1-878138-04-0 DESIGN BY JANE RAESE Text set in ii-point Adobe Caslon Pro Frontispiece: Lucile Berg in her twenties, circa 1937. Courtesy Lucile R. Berg. Printed in the United States of America Contents Editor's Introduction Acknowledgments Map of South Central Nevada 1 General Description of Big Smoky, Reese River, Monitor, and Ralston Valleys Special Points of Interest Hot Springs Blue Spring Elephant Rock Diana's Bowl or Devil's Punch Bowl Northumberland Caves 2 Early Expeditions Through the Region Fremont's Third Expedition, 1845 Jedediah Smith, 1827 Captain J. H. Simpson, 1859 3 Early Mining Camps in the Region, 1860-1880: Northern Section Ione Ophir Canyon Last Chance, Hercules, and Summit Canyons Kingston Canyon Santé Fe Northumberland 4 -
Geologic Map of the Tonopah 1° by 2° Quadrangle, Central Nevada
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP MF-1877-A U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE TONOPAH 1° BY 2° QUADRANGLE, CENTRAL NEVADA By Donald H. Whitebread and David A. John INTRODUCTION Qb Basalt of Lunar Crater area This map is part of a folio of maps of the (Quaternary) Lava flows and local Tonopah 1° by 2° quadrangle, Nevada, prepared cinders and dikes under the Conterminous United States Mineral Tba Basalt and andesite flows Assessment Program. (Tertiary) As mapped, probably includes some Quaternary lava flows in DESCRIPTION OF MAP UNITS Pancake Range. Includes trachyandesite of Red Mountain and trachyandesite of Thunder Mountain in San Antonio SURHCIAL DEPOSITS Mountains Qa Alluvial, lacustrine, and eolian Tr4 Rhyolitic rocks (Tertiary) Rhyolitic deposits (Quaternary) A s to dacitic flows, dikes, and small mapped, locally includes Tertiary gravel intrusive bodies. Includes Brougher QTIs Landslide deposits (Quaternary and Rhyolite of Bonham and Garside (1979) Tertiary) and Oddie Rhyolite 734 Andesitic rocks (Tertiary) Andesitic SEDIMENTARY ROCKS AND to latitic flows, volcanic breccia, and UNCONSOLIDATED DEPOSITS dikes Includes Gilbert Andesite, Mizpah Trachyte, and volcanics of Lime Ts4 Sedimentary rocks and bedded tuff Mountain of Bonham and Garside (Tertiary) Tuffaceous siltstone and (1979) sandstone, bedded tuff, and diatomite. Tas Andesitic rocks (Tertiary) Andesitic Includes Esmeralda and Siebert to latitic flows, flow breccias, sills, Formations. K-Ar ages about 11-13 Ma dikes, and plugs (Evernden and James, 1964; Evernden Tfs Rhyolitic rocks (Tertiary) Rhyolitic and others, 1964) for Esmeralda to dacitic flows, dikes, sills, and Formation and 13-17 Ma (Bonham and irregular small intrusive bodies Garside, 1979) for Siebert Formation Ta2 Andesitic rocks (Tertiary) Andesitic Ts3 Sedimentary rocks and bedded tuff to latitic flows, flow breccias, dikes, (Tertiary) Sandstone and siltstone, sills, and minor intrusive bodies commonly tuffaceous. -
STRATIGRAPHY and STRUCTURE of the SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract Approved: U G
AN ABSTRACT OF THE THESES OF Joseph T. Lipka IC for the degree ofMaster of Sciencein Geology presented on April 17, 1987 Title:STRATIGRAPHY AND STRUCTURE OF THE SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract approved: U G. Johnson Early Paleozoic limestones and dolomites of the shallow shelf transitional facies belt were mapped in the southern Sulphur Spring Range, Eureka County, Nevada.The four youngest units in the map area are in fault contact with the Lower Devonian rocks and wereprobably transported westward, along a low-angle normal fault. The minoirlal dolomites of the Hanson Creek Formation, dated as latest Ordovician in the map area, were deposited in a low-energy lagoon.Overlying the Hanson Creek Formation, with a gradational contact, is the lower member ofthe Lone Mountain Dolomite, a probable reef complex.The exposed thickness of the lower Lone Mountain Dolomite is estimated to be 250 feet.The Lower Devonian Old Whalen Member of the Lone Mountain Dolomite is composed of well-bedded, alternating brown and gray dolomites.The repetition of rock types in the Old Whalen Member indicates recurring shallow marine environments on a broad carbonate platform.The Old Whalen is estimated to be 1400 feet thick.Directly overlying the Old Whalen Member, is the Kobeh Member of the Mc Colley Canyon Formation.Rocks of the Mc Colley Canyon Formation were deposited on a shallow shelf under normal marine conditions.The mid-Lower Devonian Kobeh Member is sparsely to abundantly fosciliferous and varies from a peloidal wackestone to a peloidal sandy wackestone to a sandy peloidal packstone.The thickness is 276 feet.Overlying the Kobeh Member are the abundantly fossiliferous beds of the lower part of the Bartine. -
Geology of the Southern Reveille Range, Nye County, Nevada
UNLV Theses, Dissertations, Professional Papers, and Capstones 5-2008 Geology of the southern Reveille Range, Nye County, Nevada Matthew Alan McKelvey University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geology Commons, Stratigraphy Commons, and the Volcanology Commons Repository Citation McKelvey, Matthew Alan, "Geology of the southern Reveille Range, Nye County, Nevada" (2008). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1447. http://dx.doi.org/10.34917/3434676 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. GEOLOGY OF THE SOUTHERN REVEILLE RANGE, NYE COUNTY, NEVADA by Matthew Alan McKelvey Bachelor of Science Austin Peay State University 2001 A thesis submitted in partial fulfillment of the requirements for the Master Degree of Science in Geoscience Department of Geoscience -
An Interview with HOMER HOOPER
An Interview with HOMER HOOPER An Oral History conducted and edited by Robert D. McCracken Nye County Town History Project Nye County, Nevada Tonopah 1990 COPYRIGHT 1991 Nye County Town History Project Nye County Commissioners Tonopah, Nevada 89049 Homer Hooper 1990 CONTENTS Preface Acknowledgments Introduction CHAPTER ONE Information on Homer's family background, including Chief Kawich; Shoshone camps and native plants in the 1920s and 1930s; Art Hooper's cowboying on Monitor Valley ranches; Stewart Indian School; the Hooper family moves to the Reese River Valley; discussion of the Shoshone language. CHAPTER TWO Further discussion of the Shoshone language; wild carrots; Alice Hooper helps begin the Yomba Shoshone Reservation; moving to the reservation; some of the original ranches in the Reese River Valley; travel in the 1930s; early Shoshone families in the valley, and other families moving in. CHAPTER THREE Haying in the Reese River Valley; ranchers leaving the valley during the Depression; some ranchers who stayed, and working for some of those ranchers; working with horses; renting horses to deer hunters in the 1940s; further discussion of ranch, work; working for mines in Grantsville and Ophir Canyon; working for Basic Magnesium at Gabbs and for the Mercury Mine at Ione. CHAPTER FOUR A return to work at Gabbs; an accident and subsequent health problems; some of the present- day residents of the Yomba Shoshone Reservation; diversion dams in the Reese River Valley; area health care and schooling; Western Shoshone land rights; running over the mountains and running down deer INDEX PREFACE The Nye County TOwn History Project (NCTHP) engages in interviewing people who can provide firsthand descriptions of the individuals, events, and places that give history its substance.