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												  STRATIGRAPHY and STRUCTURE of the SOUTHERN SULPHUR SPRING RANGE, EUREKA COUNTY, NEVADA Redacted for Privacy Abstract Approved: U GAN 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.
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												  University of Nevada Reno Ge.Ology of the Northern Part of TheUniversity of Nevada Reno Ge.ology of the Northern Part of the Diamond Range, Eureka and White Pine Counties, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by William D. Haworth December 1979 1 mines' USSUinr i V i e s / s The thesis of William D. Haworth is approved: / y o 5 University of Nevada Reno December 1979 V Figure 1 View of the western side of the northern part of the Diamond Range; the a lk a li fla t of Diamond Valley is at far left. ABSTRACT Upper Paleozoic rocks of the post-orogenic overlap assemblage are exposed throughout the northern part of the Diamond Range. The limestones, si Itstones, sandstones, shales, and conglomerates are characterized by abundant chert and quartz that was reworked from eugeosynclinal rocks exposed in the source area to the west. Continental sediments of the Newark Canyon Formation were deposited during the Early Cretaceous on an erosional surface above the Carbon Ridge Formation of Permian age. North-trending anticlines and syncl'ines are the dominant structures in the area. The major portion of the range is an asymmetrical syncline that plunges gently to the south. Several small scale folds on the east side of the area have been overturned to the east. The rocks were de formed both prior to and following the deposition of the Newark Canyon Formation. Numerous normal fa u lts, many of which are transverse to the trend of the folds, and a reverse fault have displaced the folded rocks.
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												  Affected Environment and Environmental ConsequencesBLM U.S. Department of the Interior Bureau of Land Management Land Speed Record Challenger North American Eagle, Inc. Diamond Valley, Eureka County, Nevada Final Environmental Assessment DOI-BLM-NV-B010-2016-0018-EA Preparing Office Battle Mountain District Office 50 Bastian Road Battle Mountain, NV 89820 December 2017 This page intentionally left blank. TABLE OF CONTENTS i Table of Contents Chapter One: Purpose and Need for Action ............................................................... 1 1.0 Introduction ......................................................................................................... 3 Purpose and Need for Action .............................................................................. 3 1.2 Decision to be Made ........................................................................................... 6 1.3 Public Scoping Issues Identified .......................................................................... 6 1.3.1 Relevant Issues....................................................................................................... 6 1.4 BLM Responsibilities and Relationship to Planning ............................................. 7 1.4.1 Conformance to Plans, Statutes, and Regulations ................................................. 7 Chapter Two: Management Alternatives ................................................................... 11 2.0 Introduction ........................................................................................................13 2.1 Proposed Action: Land
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												  Overall Economic Development Plan; 2001 Eureka County Comprehensive Economic Development Strategy and 2011 Eureka County Master PlanEUREKA COUNTY, NEVADA COMPREHENSIVE ECONOMIC DEVELOPMENT STRATEGY (CEDS) Preparation of this Plan Overseen By: Eureka County Economic Development Program P.O. Box 753 Eureka, Nevada 89316 August 2014 TABLE OF CONTENTS PAGE PREPARATION OF THIS CEDS 1 The Planning Team 1 CEDS Committee Resolution 2 Eureka County Commissioners Resolution 3 Relationship to Other Plans 4 THE AREA AND ITS ECONOMY 5 Geographic Features 10 Land Use 10 Vegetation 13 Climate 14 Water Resources 15 Mineral Resources 17 Socioeconomic Characteristics 18 STRENGTHS, WEAKNESSES, OPPORTUNIUTIES AND THREATS 35 ECONOMIC DEVELOMENT GOALS, OBJECTIVES AND TASKS 62 IMPLEMENTATION STRATEGY 71 MEASURING SUCCESS 84 List of Tables Table 1. Eureka County Land Management and Ownership, 2009 11 Table 2. Oil Fields and Production for Eureka County: September – October 2013 13 Table 3. Hydrographic Basin Summaries: Eureka County (Acre Ft.) 15 Table 4. Population Trends: Eureka County with Comparisons to Elko, Lander and White Pine Counties; 2000 – 2030 19 Table 5. Age Distribution for Eureka and Comparisons to Elko, Lander and White Pine Counties; 2013-2030 19 Table 6. Distribution by Sex for Eureka County and Comparisons to Elko, Lander and White Pine Counties1; 2013 – 2030 21 Table 7. Race and Hispanic Origin: Eureka County with Comparisons to Elko, Eureka, Lander and White Pine Counties1; 2013 – 2030 21 Table 8. Employment by Industry for Eureka County with Comparisons to Elko, Lander and White Pine Counties; 2013 22 Table 9. Average Earnings by Industry for Eureka County with Comparisons to Elko, Lander and White Pine Counties; 2013 23 Table 10. Unemployed by Industry for Eureka County with Comparisons to Elko, Lander and White Pine Counties 24 i List of Tables Cont’d.
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												  Mississippian Stratigraphy of the Diamond Peak Area, Eureka County, NevadaMississippian Stratigraphy of the Diamond Peak Area, Eureka County, Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 661 Mississippian Stratigraphy of the Diamond Peak Area, Eureka County, Nevada By DAVID A. BREW With a section on the BIOSTRATIGRAPHY AND AGE OF THE CARBONIFEROUS FORMATIONS By MACKENZIE GORDON, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 661 More than 7,000 feet of Late Mississippian synorogenic detrital clastic and limy sediments of the Chainman and Diamond Peak Formations were deposited in a narrow trough east of the Antler orogenic belt UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 70-608211 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Pare Abstract _________________________________ 1 Stratigraphy Continued Introduction ________________________________ 1 Cretaceous System _____ F9 Acknowledgments ____________________________ 2 Newark Canyon Formation ________ f? Location and geography ______________________ 3 Tertiary System __________ __ F3 Previous work _____________________________ 3 Fanglomerate and megabreccia _ F3 Terminology _______________________________ 3 Igneous rocks _______ JT4 Geologic setting _______________________________ 4 Quaternary deposits ____ F4 Regional stratigraphy _________________________ 4 Alluvium ___________________ _ F4 Regional structure _____________________________
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												  Hydrogeologic Framework and Ground Water in Basin-Fill Deposits of the Diamond Valley Flow System, Central NevadaPrepared in cooperation with Eureka, Lander, and Nye Counties, Nevada and the State of Nevada Department of Conservation and Natural Resources, Division of Water Resources Hydrogeologic Framework and Ground Water in Basin-Fill Deposits of the Diamond Valley Flow System, Central Nevada Scientific Investigations Report 2006-5249 U.S. Department of the Interior U.S. Geological Survey Cover. View looking south from the north end of southern Monitor Valley. Top photo: cover of Rush, F.E. and Everett, D.E., 1964, Ground-water appraisal of Monitor, Antelope, and Kobeh Valleys, Nevada: Nevada Department of Conservation and Natural Resources, Ground-Water Resources - Reconnaissance Report 30. Bottom photo: same view, 2006. Hydrogeologic Framework and Ground Water in Basin- Fill Deposits of the Diamond Valley Flow System, Central Nevada By Mary L. Tumbusch and Russell W. Plume Prepared in cooperation with Eureka, Lander, and Nye Counties, Nevada and the State of Nevada Department of Conservation and Natural Resources, Division of Water Resources Scientific Investigations Report 2006-5249 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Carson City, Nevada: 2006 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS--the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S.