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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. -
Water Resources of Millard County, Utah
WATER RESOURCES OF MILLARD COUNTY, UTAH by Fitzhugh D. Davis Utah Geological Survey, retired OPEN-FILE REPORT 447 May 2005 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES Although this product represents the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, stated or implied, regarding its suitability for a particular use. The Utah Department of Natural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users of this product. This Open-File Report makes information available to the public in a timely manner. It may not conform to policy and editorial standards of the Utah Geological Survey. Thus it may be premature for an individual or group to take action based on its contents. WATER RESOURCES OF MILLARD COUNTY, UTAH by Fitzhugh D. Davis Utah Geological Survey, retired 2005 This open-file release makes information available to the public in a timely manner. It may not conform to policy and editorial standards of the Utah Geological Survey. Thus it may be premature for an individual or group to take action based on its contents. Although this product is the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, expressed or implied, regarding its suitability for a particular use. The Utah Department of Natural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users of this product. -
University of Nevada Reno Determination of Timing Of
University of Nevada Reno J Determination of Timing of Recharge for Geothermal Fluids in The Great Basin Using Environmental Isotopes and Paleoclimate Indicators A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science, in geology by Paul K. Buchanan 1" April, 1990 i MINES LIBRARY Tti GS Li a (ths The thesis of Paul K. Buchanan is approved by University of Nevada Reno April, 1990 11 ACKNOWLEGEMENTS This study was made possible by grant DE-FG07-88ID12784 from the United States Department of Energy, Geothermal Technology Division, administered by the Idaho Operations Office, Idaho Falls, Idaho. Additional financial assistance from the Nevada Section of the Geothermal Resources Council aided in the completion of this thesis. My thanks go to the Nevada geothermal power industry for allowing fluid sampling of deep powerplant production wells. Specifically, Chevron Resources, Oxbow Geothermal, Ormat Energy Systems, Geothermal Food Processors, Tad's Enterprises, Thermochem Inc., Elko Heat Co. and Elko School District are thanked. Thanks also to Dr. Robert Fournier of the United States Geological Survey for providing data on the Coso geothermal system. Michelle Stickles is to be commended for suffering through the proof reading of the initial drafts of this report. Thanks to my advisor, Jim Carr, and my committee members, Mel Hibbard and Gary Haynes, for taking on this project and putting up with my inconsistent scheduling and "last minute" rush. Special thanks to my cohorts at the Division of Earth Sciences and Mackay School of Mines for their cynical attitudes that helped keep it all in perspec- tive, through both the good and the bad times. -
Hydrogeology of Spring, Cave, Dry Lake, and Delamar Valleys Impacts
HYDROGEOLOGY OF SPRING, CAVE, DRY LAKE, AND DELAMAR VALLEYS IMPACTS OF DEVELOPING SOUTHERN NEVADA WATER AUTHORITY’S CLARK, LINCOLN, AND WHITE PINE COUNTIES GROUNDWATER DEVELOPMENT PROJECT Presented to the Office of the Nevada State Engineer on behalf of Protestants White Pine County, Great Basin Water Network, et al. June, 2017 Prepared by: _______________________________________________________________ Thomas Myers, Ph.D. Hydrologic Consultant Reno, NV June 28, 2017 Date Table of Contents Summary ................................................................................................................................................. 1 Introduction ............................................................................................................................................ 3 Method of Analysis .................................................................................................................................. 3 Study Area ........................................................................................................................................... 5 Water Rights Applications and Proposed Pumping Scenarios ............................................................... 8 Conceptual Flow Model ..................................................................................................................... 10 White River Flow System ................................................................................................................... 25 Hydrogeologic Properties of Aquifer Systems -
Water Resources-Reconnaissance
View of Spring Valley looking northwest from the town site of Osceola I I WATER RESOURCES- RECONNAISSANCE SERIES REPORT 33 I WATER RESOURCES APPRAISAL OF SPRING VALLEY, I WHITE PINE AND LINCOLN COUNTIES, NEVADA By I F. EUGENE RUSH Geologist and I S. A. T. KAZMI Geologist I Prepared Cooperatively by the I Geolagicai Survey, U.S. Department of Interior JULY 1965 I I I WATER RESOURCES - RECONNAISSANCE SERIES I Report 33 I I WATER RESOURCES APPRAISAL OF SPRING VALLEY, WHITE PINE AND LINCOLN COUNTIES, NEVADA I By I F. Eugene Rush Geologist I and S. A. T. Kazmi I Geologist I I I I I a I Prepared cooperatively by the Geological Survey, U. Sr Department of the Interior I September, 1965 I I I I CONTENTS Page I Summary 1 Introduction 2 i Purpose and scope of the study 2 , Location and general features 3 Previous work 3 I Climate 4 I Physiography and drainage 6 Numbering system for wells and springs 7 I General hydrogeologic features 7 I Geomorphic features 7 Lithologic and hydrologic features of the rocks 8 I Hydrology 9 I Precipitation 9 Surface water, by Donald O. Moore 12 I General conditions 12 I Estimated average annual runoff 14 Development 17 I Ground water 18 , Occurrence and movement 18 I Recharge 20 Discharge 22 I Evapotranspiration 22 I Springs 22 Subsurface outflow 24 I I",,,,' Contents - Continued I Page Discharge from wells 24 I Water budget 25 I Perennial yield 26 Storage 27 I Chemical quality of the water 27 , Suitability for agricultural use 27 Water quality and its relation to I the ground-water system 28 Development 29 I References cited 34 I List of previously published reports in this series 37 I I I I ,I I I I I I I TABLES Page I Table 1. -
Vol. 85 Thursday, No. 233 December 3, 2020 Pages 77985–78196
Vol. 85 Thursday, No. 233 December 3, 2020 Pages 77985–78196 OFFICE OF THE FEDERAL REGISTER VerDate Sep 11 2014 18:31 Dec 02, 2020 Jkt 253001 PO 00000 Frm 00001 Fmt 4710 Sfmt 4710 E:\FR\FM\03DEWS.LOC 03DEWS khammond on DSKJM1Z7X2PROD with FR-1WS II Federal Register / Vol. 85, No. 233 / Thursday, December 3, 2020 The FEDERAL REGISTER (ISSN 0097–6326) is published daily, SUBSCRIPTIONS AND COPIES Monday through Friday, except official holidays, by the Office PUBLIC of the Federal Register, National Archives and Records Administration, under the Federal Register Act (44 U.S.C. Ch. 15) Subscriptions: and the regulations of the Administrative Committee of the Federal Paper or fiche 202–512–1800 Register (1 CFR Ch. I). The Superintendent of Documents, U.S. Assistance with public subscriptions 202–512–1806 Government Publishing Office, is the exclusive distributor of the official edition. Periodicals postage is paid at Washington, DC. General online information 202–512–1530; 1–888–293–6498 Single copies/back copies: The FEDERAL REGISTER provides a uniform system for making available to the public regulations and legal notices issued by Paper or fiche 202–512–1800 Federal agencies. These include Presidential proclamations and Assistance with public single copies 1–866–512–1800 Executive Orders, Federal agency documents having general (Toll-Free) applicability and legal effect, documents required to be published FEDERAL AGENCIES by act of Congress, and other Federal agency documents of public Subscriptions: interest. Assistance with Federal agency subscriptions: Documents are on file for public inspection in the Office of the Federal Register the day before they are published, unless the Email [email protected] issuing agency requests earlier filing. -
Regional Potentiometric-Surface Map of the Great Basin Carbonate And
U.S. Department of the Interior Scientific Investigations Map 3193 U.S. Geological Survey Sheet 1 of 2 Abstract sites, water levels were measured in several nested wells, including 8 sites where the nested as great. However, water levels in wells throughout Spring and Snake Valleys also appear 114°30' 114°00' 113°30' 113°00' TOOELE COUNTY wells are all in either consolidated rock or basin fill, and 4 sites where the nested wells are to respond to interannual climate variations. 0 0 -15 Water-level measurements from 190 wells were used to develop a potentiometric-surface screened in both basin fill and consolidated rock. Water-level data at nested well sites were USGS site number: 393814113522601 JUAB COUNTY Callao USGS site number: 395355112423601 125 Most water-level records in the study area show no distinct, long-term monotonic trends Deep Creek Fish Springs used to examine vertical differences in hydraulic head. While one location had an upward 5 Well depth: 158 feet 5 Valley -10 Well depth: 90 feet USGS site number: 395331113123901 map of the east-central portion of the regional Great Basin carbonate and alluvial aquifer (rises or declines). However, in the area north of Highway 50 in Snake Valley, water levels Well number: 190 National 130 Well depth: 157 feet Well number: 171 USGS site number: 394133113493901 253 Wildlife Refuge system in and around Snake Valley, eastern Nevada and western Utah. The map area covers vertical gradient of 0.3, vertical hydraulic gradients were generally less than 0.05. These Well number: 188 in five wells (108, 114, 120, 129, and 136) have been declining since about the mid- to late- 10 10 Well depth: Unknown -5 approximately 9,000 square miles in Juab, Millard, and Beaver Counties, Utah, and White small vertical gradients indicate a hydraulic connection between basin fill and consolidated 1980s. -
Effect of Simple Approach on Estimates
2730 N. Deer Run Rd. Carson City, NV 89701 Phone: 775-887-7614 May 19, 2011 MEMORANDUM To: Devin Galloway, Ground-Water Specialist, Western Region, USGS From: Weiquan Dong, Hydrologist, Southern Nevada Water Authority, Ramon C Naranjo, Hydrologist, Nevada WSC, U.S. Geological Survey, and Keith J. Halford, Ground-Water Specialist, Nevada WSC, U.S. Geological Survey Subject: AQUIFER TEST—Analysis of water level fluctuations from pumpage for irrigation during multiple drought years in Snake Valley, HA195, near Needle Point and south of Garrison, Utah Ranges of transmissivity and specific yield of the basin fill and carbonate rock were estimated by analyzing water-level changes in multiple observation wells that were caused by irrigation of 1,800 acres in Snake Valley, HA195, south of Garrison, Utah (Figure 1). Annual effective groundwater withdrawals were estimated between 3,500 and 5,300 acre-feet (ac-ft) during the years 2001–2003. The analysis is referred to as the Needle Point aquifer test because most of the pumpage occurs just west of the carbonate outcrop Needle Point and the observation well that is completed in carbonate rocks is on the northern tip of Needle Point (Figure 1). Hydraulic property estimates from the Needle Point aquifer test will constrain calibration of regional groundwater flow models. Site and Geology The aquifer test occurred near Garrison, UT in Snake Valley where water levels in more than 100 mi² of basin fill and carbonate rock were affected by pumpage for irrigation (Figure 1). The basin fill was pumped largely between 100 and 800 ft below land surface where undifferentiated intervals of silt, sand, and gravel occurred. -
Hydrology of Stock-Water Development on the Public Domain of Western Utah
Hydrology of Stock-Water Development on the Public Domain of Western Utah GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1475-N Prepared as part of the soil and moisture program of the Department of the Interior MAR 12 1963 WRD Hydrology of Stock-Water Development on the Public Domain of Western Utah By CHARLES T. SNYDER HYDROLOGY OF THE PUBLIC DOMAIN GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1475-N Prepared as part of the soil ind moisture program of the Department of the Interior NITED 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 Abstract-. _ _____________________________________________________ 487 Introduction._____________________________________________________ 488 Purpose and scope of the investigation________________________--_ 488 Previous investigations-________________--__-____--____--____-_- 488 Acknowledgments. ____________________________________________ 488 Methods of investigation________:_______________________________ 489 Numbering system___________________________________________ 489 Geography___ ___________________________________________________ 491 Location- _ _ _ _______________________________________________ 491 Climate.._____-_____________-___-___-____-________-__---_ 492 Soils and vegetation_______________________-__________-_____-__ 494 Landf orms __ ________________________________________________ -
Geophysical Unit of Menlo Park, Calif
Prepared in cooperation with the Bureau of Land Management Geophysical Framework Investigations Influencing Ground-water Resources in East-central Nevada and West-central Utah By Janet T. Watt and David A. Ponce With a section on Geologic and Geophysical Basin-by-basin Descriptions By Alan R. Wallace, Janet T. Watt, and David A. Ponce Open-File Report 2007-1163 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, Reston, Virginia 2007 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 Suggested citation: Watt, Janet T., and Ponce, David A., 2007, Geophysical framework investigations influencing ground-water resources in east-central Nevada and west-central Utah, with a section on Geologic and geophysical basin-by-basin descriptions by Wallace, Alan R., Watt, Janet T., and Ponce David A.: U.S. Geological Survey Open-File Report 2007-1163 [http://pubs.usgs.gov/of/2007/1163]. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material -
Digital Representation of 1:1,000,000-Scale Hydrographic Areas of the Great Basin
Digital Representation of 1:1,000,000-scale Hydrographic Areas of the Great Basin Data Series 457 U.S. Department of the Interior U.S. Geological Survey Cover: Map showing 1:1,000,000-scale Great Basin hydrographic area dataset Digital representation of 1:1,000,000-scale Hydrographic Areas of the Great Basin By Susan G. Buto Data Series 457 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia 2009 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 Suggested citation: Buto, S.G., 2009, Digital representation of 1:1,000,000-scale Hydrographic Areas of the Great Basin: U.S. Geological Survey Data Series Report 2009-457, 5 p; Available at http://pubs.usgs.gov/ds/457 Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. iii Contents Abstract ......................................................................................................................................................................... 1 Background ................................................................................................................................................................... 1 Development of the Great Basin Hydrographic Area Digital Dataset ............................................................................. 2 Differences between Nevada and Great Basin Hydrographic Areas............................................................................. -
Great-Basin-Springsnail-Petition.Pdf
BEFORE THE SECRETARY OF THE INTERIOR PETITION TO LIST 42 SPECIES OF GREAT BASIN SPRINGSNAILS FROM NEVADA, UTAH, AND CALIFORNIA AS THREATENED OR ENDANGERED UNDER THE ENDANGERED SPECIES ACT Pyrgulopsis deaconi © Robert Hershler Scanning electron micrograph of shell. Paratype USNM 860676. Scale bar = 1.0 mm. CENTER for BIOLOGICAL DIVERSITY Because life is good. CENTER for BIOLOGICAL DIVERSITY Because life is good. February 17, 2009 Mr. Ken Salazar Department of the Interior 18th and "C" Street, N.W. Washington, D.C. 20240 Dear Mr. Salazar: The Center for Biological Diversity, Tierra Curry, Noah Greenwald, Dr. James Deacon, Don Duff, and The Freshwater Mollusk Conservation Society hereby formally petition the U.S. Fish and Wildlife Service (FWS) to list 42 springsnail species from the Great Basin and Mojave ecosystems in Nevada, Utah, and California as Threatened or Endangered under the Endangered Species Act, and to designate critical habitat for them concurrent with listing. Petitioners file this petition under the Endangered Species Act, 16 U.S.C. sections 1531- 1543 (1982). This petition is filed under 5 U.S.C. section 553(e), and 50 C.F.R. part 424.14 (1990), which grants interested parties the right to petition for issuance of a rule from the Assistant Secretary of the Interior. The petitioners request that Critical Habitat be designated as required by 16 U.S.C. 1533(b)(6)(C) and 50 CFR 424.12, and pursuant to the Administrative Procedures Act (5 U.S.C. 553). Petitioners realize this petition sets in motion a specific process placing definite response requirements on the FWS and very specific time constraints upon those responses.