The Nevada Mining Association's White Pine County Wilderness
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Description and Correlation of Geologic Units, Cross
Plate 2 UTAH GEOLOGICAL SURVEY Utah Geological Survey Bulletin 135 a division of Hydrogeologic Studies and Groundwater Monitoring in Snake Valley and Utah Department of Natural Resources Adjacent Hydrographic Areas, West-Central Utah and East-Central Nevada DESCRIPTION OF GEOLOGIC UNITS SOURCES USED FOR MAP COMPILATION UNIT CORRELATION AND UNIT CORRELATION HYDROGEOLOGIC Alluvial deposits – Sand, silt, clay and gravel; variable thickness; Holocene. Qal MDs Lower Mississippian and Upper Devonian sedimentary rocks, undivided – Best, M.G., Toth, M.I., Kowallis, B.J., Willis, J.B., and Best, V.C., 1989, GEOLOGIC UNITS UNITS Shale; consists primarily of the Pilot Shale; thickness about 850 feet in Geologic map of the Northern White Rock Mountains-Hamlin Valley area, Confining Playa deposits – Silt, clay, and evaporites; deposited along the floor of active Utah, 300–400 feet in Nevada. Aquifers Qp Beaver County, Utah, and Lincoln County, Nevada: U.S. Geological Survey Units playa systems; variable thickness; Pleistocene through Holocene. Map I-1881, 1 pl., scale 1:50,000. D Devonian sedimentary rocks, undivided – Limestone, dolomite, shale, and Holocene Qal Qsm Qp Qea Qafy Spring and wetland related deposits – Clay, silt, and sand; variable thickness; sandstone; includes the Guilmette Formation, Simonson and Sevy Fritz, W.H., 1968, Geologic map and sections of the southern Cherry Creek and Qsm Quaternary Holocene. Dolomite, and portions of the Pilot Shale in Utah; thickness about 4400– northern Egan Ranges, White Pine County, Nevada: Nevada Bureau of QTcs 4700 feet in Utah, 2100–4350 feet in Nevada. Mines Map 35, scale 1:62,500. Pleistocene Qls Qlm Qlg Qgt Qafo QTs QTfs Qea Eolian deposits – Sand and silt; deposited along valley floor margins, includes Hintze, L.H., 1963, Geologic map of Utah southwest quarter, Utah Sate Land active and vegetated dunes; variable thickness; Pleistocene through S Silurian sedimentary rocks, undivided – Dolomite; consists primarily of the Board, scale 1:250,000. -
South Steptoe Valley Watershed Restoration Plan Environmental Assessment
U.S. DepartmentoftheInterior Bureau of Land Management South Steptoe Valley Watershed Restoration Plan Environmental Assessment DOI-BLM-NV-L020–2011–0013–EA September 26, 2011 PREPARING OFFICE U.S. Department of the Interior Bureau of Land Management Schell Field Office 702 N. Industrial Way HC33 Box 33500 Ely, NV 89301 (775) 289–1800 South Steptoe Valley Watershed Restoration Plan Environmental Assessment: DOI-BLM- NV-L020–2011–0013–EA September 26, 2011 This page intentionally left blank South Steptoe Valley Watershed iii Restoration Plan Environmental Assessment Table of Contents 1. Introduction ................................................................................................................................ 1 1.1. Identifying Information ..................................................................................................... 1 1.1.1. Title, EA number, and type of project .................................................................... 1 1.1.2. Location of Proposed Action ................................................................................. 1 1.1.3. Name and Location of Preparing Office ................................................................ 1 1.2. Introduction ....................................................................................................................... 1 1.3. Purpose and Need for Action ............................................................................................ 3 1.4. Relationship to Planning .................................................................................................. -
VGP) Version 2/5/2009
Vessel General Permit (VGP) Version 2/5/2009 United States Environmental Protection Agency (EPA) National Pollutant Discharge Elimination System (NPDES) VESSEL GENERAL PERMIT FOR DISCHARGES INCIDENTAL TO THE NORMAL OPERATION OF VESSELS (VGP) AUTHORIZATION TO DISCHARGE UNDER THE NATIONAL POLLUTANT DISCHARGE ELIMINATION SYSTEM In compliance with the provisions of the Clean Water Act (CWA), as amended (33 U.S.C. 1251 et seq.), any owner or operator of a vessel being operated in a capacity as a means of transportation who: • Is eligible for permit coverage under Part 1.2; • If required by Part 1.5.1, submits a complete and accurate Notice of Intent (NOI) is authorized to discharge in accordance with the requirements of this permit. General effluent limits for all eligible vessels are given in Part 2. Further vessel class or type specific requirements are given in Part 5 for select vessels and apply in addition to any general effluent limits in Part 2. Specific requirements that apply in individual States and Indian Country Lands are found in Part 6. Definitions of permit-specific terms used in this permit are provided in Appendix A. This permit becomes effective on December 19, 2008 for all jurisdictions except Alaska and Hawaii. This permit and the authorization to discharge expire at midnight, December 19, 2013 i Vessel General Permit (VGP) Version 2/5/2009 Signed and issued this 18th day of December, 2008 William K. Honker, Acting Director Robert W. Varney, Water Quality Protection Division, EPA Region Regional Administrator, EPA Region 1 6 Signed and issued this 18th day of December, 2008 Signed and issued this 18th day of December, Barbara A. -
The Origin and Evolution of the Southern Snake Range Decollement, East Central Nevada Allen J
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Dayton University of Dayton eCommons Geology Faculty Publications Department of Geology 2-1993 The Origin and Evolution of the Southern Snake Range Decollement, East Central Nevada Allen J. McGrew University of Dayton, [email protected] Follow this and additional works at: https://ecommons.udayton.edu/geo_fac_pub Part of the Geology Commons, Geomorphology Commons, Geophysics and Seismology Commons, Glaciology Commons, Hydrology Commons, Other Environmental Sciences Commons, Paleontology Commons, Sedimentology Commons, Soil Science Commons, Stratigraphy Commons, and the Tectonics and Structure Commons eCommons Citation McGrew, Allen J., "The Origin and Evolution of the Southern Snake Range Decollement, East Central Nevada" (1993). Geology Faculty Publications. 29. https://ecommons.udayton.edu/geo_fac_pub/29 This Article is brought to you for free and open access by the Department of Geology at eCommons. It has been accepted for inclusion in Geology Faculty Publications by an authorized administrator of eCommons. For more information, please contact [email protected], [email protected]. TECTONICS, VOL. 12, NO. 1, PAGES 21-34, FEBRUARY 1993 THE ORIGIN AND EVOLUTION OF INTRODUCTION THE SOUTHERN SNAKE RANGE The origin,kinematic significance and geometrical evolu- DECOLLEMENT, EAST CENTRAL tion of shallowlyinclined normal fault systemsare NEVADA fundamentalissues in extensionaltectonics. Regionally extensivefaults that juxtapose nonmetamorphic sedimentary Allen J. McGrew1 rocksin theirhanging walls againstplastically deformed Departmentof Geology,Stanford University, Stanford, crystallinerocks in their footwallscommand special California attentionbecause they offer rare opportunitiesto characterize kinematiclinkages between contrasting structural levels. Thesefaults, commonly known as detachmentfaults, are the Abstract.Regional and local stratigraphic, metamorphic, subjectsof muchcontroversy. -
CR 21-14 Big Game Quotas for the 2021-2022 Season.Pdf
State of Nevada Department of Wildlife Game Division 6980 Sierra Center Parkway, Ste 120 ● Reno, NV 89511 (775) 688-1500 Fax (775) 688-1987 ____________________________________________________ MEMORANDUM April 20, 2021 To: Nevada Board of Wildlife Commissioners, County Advisory Boards to Manage Wildlife, and Interested Publics From: Mike Scott, Administrator, Game Division Title: Commission Regulation 21-14, 2021 Big Game Quotas for the 2021-2022 Season – For Possible Action Description: The Commission will establish regulations for the numbers of tags to be issued to mule deer, pronghorn antelope, elk, bighorn sheep, and mountain goats for the 2021-22 season Presenter: Wildlife Staff Specialists Cody Schroeder, Cody McKee, and Mike Cox Summary: Generally, the Game Division is recommending lower quotas than in 2020. Nevada is experiencing continued drought conditions which affect big game populations in predominantly negative ways. The Game Division follows the Guidelines for Harvest Management in Nevada to provide the proposed big game tag quotas for each species and Area, Unit, or Unit Group. Game biologists survey big game populations, analyze data, model populations, write status and trend reports for each species and provide quota recommendations for Interested Publics, County Advisory Board members, and Wildlife Commissioners to consider. The recommended quotas are intended to sustain a balance between male-to- female ratios in big game populations while providing recreational opportunity for the hunting public. Employing a team approach in generating quota recommendations, Game Division staff scrutinize survey data, harvest data, population models, and resulting quota recommendations ensuring post-season ratios or other metrics will be met within the harvest guidelines. Should ratios end up above or below the male-to- female ratio objective, adjustments to the quotas are made to address that discrepancy. -
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. Butte Valley fault zone (Class A) No. 1276 Last Review Date: 2000-11-30 citation for this record: Redsteer, M.H., compiler, 2000, Fault number 1276, Butte Valley 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 02:16 PM. Synopsis The Butte Valley fault zone is defined by a series of down-to-the- east scarps and lineaments, southwest of the Cherry Creek Range. Fault movement is described as of possible Holocene age (<10 ka). Reconnaissance photogeologic mapping and limited analysis of range-front morphology are the sources of data. Trench investigations and detailed studies of scarp morphology have not been completed. Name Refers to the southern fault of two defining the Butte Valley fault comments zone of dePolo (1998 #2845). Also mapped by Dohrenwend and others (1992 #2480). It extends about 15 km from Thirtymile Wash on the western side of the Butte Mountains, across Butte Valley to Hunter Point, the southern end of the Cherry Creek Range. Fault ID: Refers to fault number EY8B of dePolo (1998 #2845). County(s) and WHITE PINE COUNTY, NEVADA State(s) Physiographic BASIN AND RANGE province(s) Reliability of Good location Compiled at 1:100,000 scale. -
University of Nevada, Reno Igneous and Hydrothermal Geology of The
University of Nevada, Reno Igneous and Hydrothermal Geology of the Central Cherry Creek Range, White Pine County, Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by David J. Freedman Dr. Michael W. Ressel, Thesis Advisor May, 2018 THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by DAVID JOSEPH FREEDMAN entitled Igneous and Hydrothermal Geology of the Central Cherry Creek Range, White Pine County, Nevada be accepted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Michael W. Ressel, PhD, Advisor John L. Muntean, PhD, Committee Member Douglas P. Boyle, PhD, Graduate School Representative David W. Zeh, PhD, Dean, Graduate School May, 2018 i Abstract The central Cherry Creek Range exposes a nearly intact, 8-km thick crustal section of Precambrian through Eocene rocks in a west-dipping homocline. Similar tilts between Eocene volcanic rocks and underlying Paleozoic carbonates demonstrate that tilting and exhumation largely occurred during post-Eocene extensional faulting, thus allowing for relatively simple paleo-depth determinations of Eocene intrusions and mineral deposits. The study area is cored by the Cherry Creek quartz monzonite pluton (35 km2 exposure; ~132 km2 coincident magnetic anomaly), which was emplaced into Precambrian and Cambrian meta-sedimentary strata between 37.9-36.2 Ma and is exposed along the east side of the range. The pluton and overlying Paleozoic strata are cut by abundant 35.9-35.1 Ma porphyritic silicic dikes. A range of polymetallic mineralization styles are hosted by the intrusive rocks along two deeply-penetrating, high-angle faults and their intersections with favorable Paleozoic units. -
DIVISION C—OTHER PROVISIONS TITLE III—WHITE PINE COUNTY CON- SERVATION, RECREATION, and DE- VELOPMENT Subtitle A—Land Disp
G:\COMP\109\WHITE PINE COUNTY CONSERVATION, RECREATION, A....XML White Pine County Conservation, Recreation, and Development Act of 2006 [Title III of division C of Public Law 109–432] [As Amended Through P.L. 116–9, Enacted March 12, 2019] øCurrency: This publication is a compilation of the text of Public Law 109–432. It was last amended by the public law listed in the As Amended Through note above and below at the bottom of each page of the pdf version and reflects current law through the date of the enactment of the public law listed at https:// www.govinfo.gov/app/collection/comps/¿ øNote: While this publication does not represent an official version of any Federal statute, substantial efforts have been made to ensure the accuracy of its contents. The official version of Federal law is found in the United States Statutes at Large and in the United States Code. The legal effect to be given to the Statutes at Large and the United States Code is established by statute (1 U.S.C. 112, 204).¿ AN ACT To amend the Internal Revenue Code of 1986 to extend expiring provisions, and for other purposes. Be it enacted by the Senate and House of Representatives of the United States of America in Congress assembled, * * * * * * * DIVISION C—OTHER PROVISIONS * * * * * * * TITLE III—WHITE PINE COUNTY CON- SERVATION, RECREATION, AND DE- VELOPMENT SEC. 301. AUTHORIZATION OF APPROPRIATIONS. There are authorized to be appropriated such sums as are nec- essary to carry out this title. SEC. 302. ø16 U.S.C. 1241 note¿ SHORT TITLE This title may be cited as the ‘‘White Pine County Conserva- tion, Recreation, and Development Act of 2006’’. -
"Ground Water in White River Valley, White Pine, Nye, and Lincoln
STATE OF NEVADA OFFICE OF THE STATE ENGINEER WATER RESOURCES BULLETIN No. 8 GROUND WATER IN WHITE RIVER VALLEY, WHITE PINE, NYE, AND LINCOLN COUNTIES, NEVADA By G. B. MAXEY and T. E. EAKIN Prepared in cooperation with the UNITED STATES DEPARTMENT OF THE INTERIOR Geological Survey 1 949 CARSON CITY. NEVADA STATE PRINTING OFFICE JACK MCCARTHY. SUPERINTENDENT 1930 CONTENTS PAGE Foreword ............................................... 5 Abstract ............................................... 7 Introduction .............................................. 9 Location and general features .............................. 12 Drainage ................................................ 14 Climate ................................................ 18 Precipitation ................................................ 18 Temperature ................................................ 19 Vegetation ............................................... 25 Geology and water-bearing characteristics of the rocks . 26 General relations . .............. 26 Older sedimentary and igneous rocks . ............................................. 26 MCCARTHY. SUPERINTENDENT Tertiary and Quaternary alluvial and lacustrine deposits ..... 29 Ground water ................................................ 33 Occurrence ............................................... 33 Springs ............................................... 35 Source and amount of recharge . ............. 40 Movement ............................................... 41 Discharge ............................................... -
The Shrinking Sagebrush Sea
MISSION STATEMENT WildEarth Guardians protects and restores the wildlife, wild places and wild rivers of the American West. Inquiries about this report and WildEarth Guardians' work can be made directly to: Mark Salvo, WildEarth Guardians 503-757-4221, [email protected] Cartography and analyses: Kurt Menke, Bird's Eye View GIS Front cover photo: James Ownby © WildEarth Guardians All rights reserved. No part of this report may be used in any manner whatsoever without written permission from the publisher, WILDEARTH GUARDIANS, except in the case of brief quotations. Inquires should be addressed to: 312 Montezuma Avenue, Santa Fe, NM 87501 The Shrinking Sagebrush Sea Executive Summary In the sagebrush lands of the West… the natural landscape is eloquent of the interplay of forces that have created it. It is spread before us like the pages of an open book in which we can read why the land is what it is and why we should preserve its integrity. But the pages lie unread. Rachel Carson ● Silent Spring (1962) Despite its size, the Sagebrush Sea (scientifically known as “sagebrush steppe”) is one of the most endangered landscapes in North America. The Sagebrush Sea has been reduced in area by as much as 50 percent since European settlement. Livestock grazing, natural gas and oil development, agricultural conversion, roads, fences, powerlines and pipelines, off-road vehicle use, urban sprawl, mining, unnatural fire, and invasive weeds are fragmenting or degrading much of what remains. Greater sage-grouse are a sagebrush obligate species whose range has been significantly reduced with the loss of sagebrush steppe. -
AND SCHELL CREEK DIVISIONS of the James O. Klemmedson
An Inventory of Bristlecone Pine in the Snake, Mount Moriah, Ward Mountain, and Schell Creek Divisions of the Humboldt National Forest Authors Klemmedson, James O.; Beasley, R. Scott Publisher Laboratory of Tree-Ring Research, University of Arizona (Tucson, AZ) Rights Copyright © Arizona Board of Regents. The University of Arizona. Download date 02/10/2021 17:39:02 Link to Item http://hdl.handle.net/10150/302516 Report AN INVENTORY OF BRISTLECONE PINE IN THE SNAKE, MOUNT MORIAH, WARD MOUNTAIN, AND SCHELL CREEK DIVISIONS OF THE HUMBOLDT NATIONAL FOREST Prepared by James O. Klemmedson and R. Scott Beasley* Submitted to REGIONAL FORESTER, U.S. FOREST SERVICE OGDEN, UTAH in accordance with a COOPERATIVE AGREEMENT between the FOREST SERVICE and LABORATORY OF TREE-RING RESEARCH UNIVERSITY OF ARIZONA for A JOINT INVENTORY AND DENDROCHRONOLOGICAL STUDY OF BRISTLECONE PINE * Department of Watershed Management, University of Arizona INTRODUCTION Bristlecone pine, Pinus aristata Engeim., is a species which inhabits high altitudes of the mountainous southwestern United States. It occurs from the Front Range of Colorado through Utah, northern New Mexico and Arizona to the White Mountains of California along the Nevada border in the west. Bristlecone pine commonly occurs in small open groves on arid slopes, but it also grows in association with limber and ponderosa pines, white fir, Douglas - fir, and Engelmann spruce, generally above the 8000 -foot level. This tree has little economic value as a timber species, but does provide a protective and beautifying cover to the landscape. A newly -acquired interst in bristlecone pine stems from the discovery that these trees reach tremendous ages. -
Management Plan for the Great Basin National Heritage Area Approved April 30, 2013
Management Plan for the Great Basin National Heritage Area Approved April 30, 2013 Prepared by the Great Basin Heritage Area Partnership Baker, Nevada i ii Great Basin National Heritage Area Management Plan September 23, 2011 Plans prepared previously by several National Heritage Areas provided inspiration for the framework and format for the Great Basin National Heritage Area Management Plan. National Park Service staff and documents provided guidance. We gratefully acknowledge these contributions. This Management Plan was made possible through funding provided by the National Park Service, the State of Nevada, the State of Utah and the generosity of local citizens. 2011 Great Basin National Heritage Area Disclaimer Restriction of Liability The Great Basin Heritage Area Partnership (GBHAP) and the authors of this document have made every reasonable effort to insur e accuracy and objectivity in preparing this plan. However, based on limitations of time, funding and references available, the parties involved make no claims, promises or guarantees about the absolute accuracy, completeness, or adequacy of the contents of this document and expressly disclaim liability for errors and omissions in the contents of this plan. No warranty of any kind, implied, expressed or statutory, including but not limited to the warranties of non-infringement of third party rights, title, merchantability, fitness for a particular purpose, is given with respect to the contents of this document or its references. Reference in this document to any specific commercial products, processes, or services, or the use of any trade, firm or corporation name is for the inf ormation and convenience of the public, and does not constitute endorsement, recommendation, or favoring by the GBHAP or the authors.