North Schell Restoration Project EA
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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. -
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. -
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’’. -
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. -
High-Elevation Five Needle Pine Cone Collections in California and Nevada
High-elevation white pine cone collections from the Great Basin of Nevada, California, & Utah on National Forest, Bureau of Land Management, National Park, and State lands, 2009 – 2013. Collected 40-50 cones/tree. 2009 (all on NFS land): 3 sites # trees Schell Creek Range, Cave Mtn., NV Pinus longaeva 100 Spring Mtns., Lee Canyon, NV Pinus longaeva 100 White Mtns., Boundary Peak, NV Pinus longaeva 100 2010 (all on NFS land except as noted): 7 sites Carson Range, Mt. Rose, NV Pinus albicaulis 23 Hawkins Peak, CA Pinus albicaulis 26 Luther Creek, CA Pinus lambertiana 15 Monitor Pass, CA Pinus lambertiana 25 Pine Forest Range, NV [BLM] Pinus albicaulis 20 Sweetwater Mtns., NV Pinus albicaulis 20 Wassuk Range, Corey Pk., NV [BLM] Pinus albicaulis 25 2011 (all on NFS land except as noted): 13 sites Fish Creek Range, NV [BLM] Pinus flexilis 25 Fish Creek Range, NV [BLM] Pinus longaeva 25 Grant Range, NV Pinus flexilis 25 Highland Range, NV [BLM] Pinus longaeva 25 Independence Mtns., NV Pinus albicaulis 17 Jarbidge Mtns., NV Pinus albicaulis 25 Pequop Mtns., NV [BLM] Pinus longaeva 25 Ruby Mtns., Lamoille Canyon, NV Pinus albicaulis 25 Ruby Mtns., Lamoille Canyon, NV Pinus flexilis 20 Schell Creek Range, Cave Mtn., NV Pinus flexilis 25 Sweetwater Mtns., NV Pinus flexilis 25 White Pine Range, Mt. Hamilton, NV Pinus flexilis 25 White Pine Range, Mt. Hamilton, NV Pinus longaeva 25 2012 (all on NFS land except as noted): 9 sites Black Mountain, Inyo NF, CA Pinus longaeva 23 Carson Range, LTBMU, NV Pinus albicaulis 25 Egan Range, Toiyabe NF, NV Pinus longaeva 25 Emma Lake, Toiyabe NF, CA Pinus albicaulis 25 Happy Valley, Fishlake NF, UT Pinus longaeva 25 Inyo Mtns., Tamarack Canyon, CA Pinus longaeva 25 Leavitt Lake, Toiyabe NF, CA Pinus albicaulis 25 Mt. -
Monsoon Passage Fact Sheet
Monsoon Passage Fact Sheet Safe haven stepping stones from the Mojave Desert to the Northern Great Basin East Pass a few years after a fire in the Clover Mountains of the southern Great Basin looking down into the Mojave’s Tule Desert © Louis Provencher/TNC Monsoon Passage The connected mountain ranges and wet valley bottoms of this natural highway provide desert tortoises, bighorn sheep, Cooper’s hawk, mule deer and other species escape routes from growing climate impacts, allowing them to find new homes where they can thrive. The region's name comes from being at the western edge of the summer monsoons that provide needed eastern-facing moisture to buffer rising temperatures and a pathway for species moving north. Imagine populations of raptors, small carnivores, small mammals, mule deer, bighorn sheep, passerine birds, insects, and plant species pushed northward or up and around mountains by warming temperatures and changes in precipitation patterns. Non-migratory species flow from the hot Mojave Desert ecoregion to the cooler Columbia Plateau ecoregion passing through the entirety of the Great Basin ecoregion is not easily guaranteed. There are less than five corridors of passably connected mountains ranges and wet valley bottoms that fully allow species movement within a viable thermal environment that may be viewed as steppingstones of safe havens. The Nevada Chapter is proposing one such thermal corridor in eastern Nevada titled Monsoon Passage. The corridor follows the Nevada-Utah border and is mostly in Nevada. For those familiar -
Structural Geology of the Confusion Range, West-Central Utah
Structural Geology of the Confusion Range, West-Central Utah GEOLOGICAL SURVEY PROFESSIONAL PAPER 971 Structural Geology of the Confusion Range, West-Central Utah By Richard K. Hose GEOLOGICAL SURVEY PROFESSIONAL PAPER 971 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1977 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Strrtlory GEOLOGICAL SURVEY V. E. McKelvey, Dirator Library of Congress Cataloging in Publication Data Hose, Richard Kenneth, 1920- Structural geology of the Confusion Range, west-central Utah. (Geological Survey Professional Paper 971) Bibliography: p. 9. Supt. of Docs. no.: I 19.16:971 1. Geology-Utah-Confusion Range. I. Title. II. Series: United States Geological Survey Professional Paper 971. QE170.C59H67 551.8'09792'45 76-608301 For ~ale by the Superintendent of Documents, U.S. Government Printing Office \Vashington, D.C. 20402 Stock Number 024-001-02923-5 CONTENTS Page 1\bstract ------------------------------------------------------------------------------ 1 Introduction -------------------------------------------------------------------------- 1 Structural history ______________________________________________________________________ 1 Late Mesozoic to early Cenozoic orogeny ------------------------------------------------ 3 Structures within the structural trough ------------------------------------------------ 3 Low-angle faults ________________________________________ -------------------------- 3 Evidence for the higher decollement ------------------------------------------------ 4 Evidence -
Spruce Mountain Restoration
B L U.S. Department of the Interior M Bureau of Land Management Spruce Mountain Restoration PREPARING OFFICE U.S. Department of the Interior Bureau of Land Management Wells Field Office 3900 E. Idaho St. Elko, Nevada 89801 United States of America (775) 753–0200 Spruce Mountain Restoration : Environmental Assessment: This page intentionally left blank Spruce Mountain Restoration iii Table of Contents 1. Introduction ................................................................................................................................ 1 1.1. Identifying Information: ................................................................................................... 1 1.1.1. Location of Proposed Action: ................................................................................ 1 1.1.2. Name and Location of Preparing Office: ............................................................... 1 1.2. Purpose and Need for Action: .......................................................................................... 1 2. Proposed Action and Alternatives ............................................................................................ 3 2.1. Alternative A — Proposed Action .................................................................................... 5 2.1.1. Proposed Project Procedures ................................................................................ 14 2.2. Alternative B ................................................................................................................... 20 2.3. Alternative -
Exhibit 3067.Pdf
TABLE OF CONTENTS Page EXECUTIVE SUMMARY CHAPTER 1: Overview Goals, Guidelines 1 Introduction 1 Statement of Purpose Goals and Objectives Institutional Framework 2 Development Process 3 1999 Water Resources Plan 2006 Water Resources Plan Relationship to Other Plans County and Community Plans 4 State Water Plan Other Resource Management Plans, Planning Documents 5 CHAPTER 2: White Pine County Economic Trends, Projections And Water Use 7 Introduction 7 Economic History Historic Water Demand 8 Current Economic Conditions 9 Mining, Industrial Activity Agriculture 10 Tourism, Travel, Retirement and Leisure Employment Patterns Population 11 Current Water Demand and Commitments On-Going Economic Development and Population Growth, 2006-2056 15 Potential Economic Development, 2006-2056 21 Primary Basins 22 Steptoe Valley Spring Valley 24 Snake Valley 25 Butte Valley 25 White River Valley 26 Secondary Basins 26 CHAPTER 3: Water Resources Issues, Goals and Objectives Recommendations, and Policies 29 Issues 29 Physical Environment/Hydrogeological Setting Climate Legal and Regulatory Framework 30 Available Data Planning Context 30 Economic Development Trends, Strategies, White Pine County 31 Factors Outside White Pine County 32 Goals and Objectives 32 Objectives and Strategies Policies 33 Water Quality, Public Health and Safety Conservation and Reuse 35 Drought Conditions 36 Water Supply and Allocation Designated Basins Inter-Basin Transfers Monitoring and Mitigation 37 Administrative Structures 39 Recommendations 41 Evaluation and Implementation