Hydrogeology of Spring, Cave, Dry Lake, and Delamar Valleys Impacts
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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. -
Appendix L, Bureau of Land Management Worksheets
Palen‐Ford Playa Dunes Description/Location: The proposed Palen‐Ford Playa Dunes NLCS/ ACEC would encompass the entire playa and dune system in the Chuckwalla Valley of eastern Riverside County. The area is bordered on the east by the Palen‐McCoy Wilderness and on the west by Joshua Tree National Park. Included within its boundaries are the existing Desert Lily Preserve ACEC, the Palen Dry Lake ACEC, and the Palen‐Ford Wildlife Habitat Management Area (WHMA). Nationally Significant Values: Ecological Values: The proposed unit would protect one of the major playa/dune systems of the California Desert. The area contains extensive and pristine habitat for the Mojave fringe‐toed lizard, a BLM Sensitive Species and a California State Species of Special Concern. Because the Chuckwalla Valley population occurs at the southern distributional limit for the species, protection of this population is important for the conservation of the species. The proposed unit would protect an entire dune ecosystem for this and other dune‐dwelling species, including essential habitat and ecological processes (i.e., sand source and sand transport systems). The proposed unit would also contribute to the overall linking of five currently isolated Wilderness Areas of northeastern Riverside County (i.e., Palen‐McCoy, Big Maria Mountains, Little Maria Mountains, Riverside Mountains, and Rice Valley) with each other and Joshua Tree National Park, and would protect a large, intact representation of the lower Colorado Desert. Along with the proposed Chuckwalla Chemehuevi Tortoise Linkage NLCS/ ACEC and Upper McCoy NLCS/ ACEC, this unit would provide crucial habitat connectivity for key wildlife species including the federally threatened Agassizi’s desert tortoise and the desert bighorn sheep. -
Arid and Semi-Arid Lakes
WETLAND MANAGEMENT PROFILE ARID AND SEMI-ARID LAKES Arid and semi-arid lakes are key inland This profi le covers the habitat types of ecosystems, forming part of an important wetlands termed arid and semi-arid network of feeding and breeding habitats for fl oodplain lakes, arid and semi-arid non- migratory and non-migratory waterbirds. The fl oodplain lakes, arid and semi-arid lakes support a range of other species, some permanent lakes, and arid and semi-arid of which are specifi cally adapted to survive in saline lakes. variable fresh to saline water regimes and This typology, developed by the Queensland through times when the lakes dry out. Arid Wetlands Program, also forms the basis for a set and semi-arid lakes typically have highly of conceptual models that are linked to variable annual surface water infl ows and vary dynamic wetlands mapping, both of which can in size, depth, salinity and turbidity as they be accessed through the WetlandInfo website cycle through periods of wet and dry. The <www.derm/qld.gov.au/wetlandinfo>. main management issues affecting arid and semi-arid lakes are: water regulation or Description extraction affecting local and/or regional This wetland management profi le focuses on the arid hydrology, grazing pressure from domestic and semi-arid zone lakes found within Queensland’s and feral animals, weeds and tourism impacts. inland-draining catchments in the Channel Country, Desert Uplands, Einasleigh Uplands and Mulga Lands bioregions. There are two broad types of river catchments in Australia: exhoreic, where most rainwater eventually drains to the sea; and endorheic, with internal drainage, where surface run-off never reaches the sea but replenishes inland wetland systems. -
Photograph Taken by David A
Prepared in cooperation with the National Park Service Characterization of Surface-Water Resources in the Great Basin National Park Area and Their Susceptibility to Ground-Water Withdrawals in Adjacent Valleys, White Pine County, Nevada Scientific Investigations Report 2006–5099 U.S. Department of the Interior U.S. Geological Survey Cover: Confluence of Lehman and Baker Creeks, looking west toward Great Basin National Park, White Pine County, Nevada. (Photograph taken by David A. Beck, U.S. Geological Survey, 2003.) Characterization of Surface-Water Resources in the Great Basin National Park Area and Their Susceptibility to Ground-Water Withdrawals in Adjacent Valleys, White Pine County, Nevada By Peggy E. Elliott, David A. Beck, and David E. Prudic Prepared in cooperation with the National Park Service Scientific Investigations Report 2006–5099 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Dirk Kempthorne, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia: 2006 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication 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 materials contained within this report. Suggested citation: Elliott, P.E., Beck, D.A., and Prudic, D.E., 2006, Characterization of surface-water resources in the Great Basin National Park area and their susceptibility to ground-water withdrawals in adjacent valleys, White Pine County, Nevada: U.S. -
Utah Historical Quarterly, Use of the Atomic Bomb
78 102 128 NO. 2 NO. I VOL. 86 VOL. I 148 179 UHQ 75 CONTENTS Departments 78 The Crimson Cowboys: 148 Remembering Topaz and Wendover The Remarkable Odyssey of the 1931 By Christian Heimburger, Jane Beckwith, Claflin-Emerson Expedition Donald K. Tamaki, and Edwin P. Hawkins, Jr. By Jerry D. Spangler and James M. Aton 165 Voices from Drug Court By Randy Williams 102 Small but Significant: The School of Nursing at Provo 77 In This Issue General Hospital, 1904–1924 By Polly Aird 172 Book Reviews & Notices 128 The Mountain Men, the 179 In Memoriam Cartographers, and the Lakes 182 Contributors By Sheri Wysong 183 Utah In Focus Book Reviews 172 Depredation and Deceit: The Making of the Jicarilla and Ute Wars in New Mexico By Gregory F. Michno Reviewed by Jennifer Macias 173 Juan Rivera’s Colorado, 1765: The First Spaniards among the Ute and Paiute Indians on the Trail to Teguayo By Steven G. Baker, Rick Hendricks, and Gail Carroll Sargent Reviewed by Robert McPherson 175 Isabel T. Kelly’s Southern Paiute Ethnographic Field Notes, 1932–1934, Las Vegas NO. 2 NO. Edited by Catherine S. Fowler and Darla Garey-Sage I Reviewed by Heidi Roberts 176 Mountain Meadows Massacre: Collected Legal Papers Edited by Richard E. Turley, Jr., Janiece L. Johnson, VOL. 86 VOL. and LaJean Purcell Carruth I Reviewed by Gene A. Sessions. UHQ Book Notices 177 Cowboying in Canyon Country: 76 The Life and Rhymes of Fin Bayles, Cowboy Poet By Robert S. McPherson and Fin Bayles 178 Dime Novel Mormons Edited by Michael Austin and Ardis E. -
A Great Basin-Wide Dry Episode During the First Half of the Mystery
Quaternary Science Reviews 28 (2009) 2557–2563 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev A Great Basin-wide dry episode during the first half of the Mystery Interval? Wallace S. Broecker a,*, David McGee a, Kenneth D. Adams b, Hai Cheng c, R. Lawrence Edwards c, Charles G. Oviatt d, Jay Quade e a Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, NY 10964-8000, USA b Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512, USA c Department of Geology & Geophysics, University of Minnesota, 310 Pillsbury Drive SE, Minneapolis, MN 55455, USA d Department of Geology, Kansas State University, Thompson Hall, Manhattan, KS 66506, USA e Department of Geosciences, University of Arizona, 1040 E. 4th Street, Tucson, AZ 85721, USA article info abstract Article history: The existence of the Big Dry event from 14.9 to 13.8 14C kyrs in the Lake Estancia New Mexico record Received 25 February 2009 suggests that the deglacial Mystery Interval (14.5–12.4 14C kyrs) has two distinct hydrologic parts in the Received in revised form western USA. During the first, Great Basin Lake Estancia shrank in size and during the second, Great Basin 15 July 2009 Lake Lahontan reached its largest size. It is tempting to postulate that the transition between these two Accepted 16 July 2009 parts of the Mystery Interval were triggered by the IRD event recorded off Portugal at about 13.8 14C kyrs which post dates Heinrich event #1 by about 1.5 kyrs. This twofold division is consistent with the record from Hulu Cave, China, in which the initiation of the weak monsoon event occurs in the middle of the Mystery Interval at 16.1 kyrs (i.e., about 13.8 14C kyrs). -
Ground-Water Resources-Reconnaissance Series Report 20
- STATE OF NEVADA ~~~..._.....,.,.~.:RVA=rl~ AND NA.I...U~ a:~~::~...... _ __,_ Carson City_ GROUND-WATER RESOURCES-RECONNAISSANCE SERIES REPORT 20 GROUND- WATER APPRAISAL OF THE BLACK ROCK DESERT AREA NORTHWESTERN NEVADA By WILLIAM C. SINCLAIR Geologist Price $1.00 PLEASE DO NOT REMO V~ f ROM T. ':'I S OFFICE ;:: '· '. ~- GROUND-WATER RESOURCES--RECONNAISSANCE SERIES .... Report 20 =· ... GROUND-WATER APPRAISAL OF THE BLACK ROCK OESER T AREA NORTHWESTERN NEVADA by William C. Sinclair Geologist ~··· ··. Prepared cooperatively by the Geological SUrvey, U. S. Department of Interior October, 1963 FOREWORD This reconnaissance apprais;;l of the ground~water resources of the Black Rock Desert area in northwestern Nevada is the ZOth in this series of reports. Under this program, which was initiated following legislative action • in 1960, reports on the ground-water resources of some 23 Nevada valleys have been made. The present report, entitled, "Ground-Water Appraisal of the Black Rock Desert Area, Northwe$tern Nevada", was prepared by William C. Sinclair, Geologist, U. s. Geological Survey. The Black Rock Desert area, as defined in this report, differs some~ what from the valleys discussed in previous reports. The area is very large with some 9 tributary basins adjoining the extensive playa of Black Rock Desert. The estimated combined annual recharge of all the tributary basins amounts to nearly 44,000 acre-feet, but recovery of much of this total may be difficult. Water which enters into the ground water under the central playa probably will be of poor quality for irrigation. The development of good produci1>g wells in the old lake sediments underlying the central playa appears doubtful. -
User Notes: Las Cruces, New Mexico, National Wetlands Inventory
USER NOTES : LAS CRUCES, NEW MEXICO, NATIONAL WETLANDS INVENTORY MAP Map Preparation The wetland classifications that appear on the Las Cruces NWI Base Map are in accordance with Cowardin et al .(1977) . The delineations were produced through stereoscope interpretation of 1 :110,000-scale color infrared aerial photographs taken in February, 1971, and 1 :80,000-scale bladk-and-white-aerial photographs taken in March, 1977 . The delineations were enlarged using a zoom transferscope to overlays of 1 :24,000-scale and 1 :62,500-scale . These overlays were then transferred to 1 :100,000-scale to produce the Base Map . Aerial photographs were unavailable for the western portion of the Las Cruces area 1 :62,500-scale map, the western and southern portion of the Afton area 1 :62,500-scale map, and the eastern portions of the White Sands NW, Davies Tank, Newman NW, and Newman SW area 1 :24,000-scale maps . These areas are therefore without wetland designations on the Las Cruces NWI Base Map . Extensive field checks of the delineated wetlands of the Las Cruces NWI Base Map were conducted in June, 1981 to determine the accuracy of the aerial photointerpretation and to provide qualifying descriptions of mapped wetland designations . The user of the map is cautioned that, due to the limitation of mapping primarily through aerial photointerpretation, a small percentage of wetlands may have gone unidentified . Changes in the landscape could have occurred since the time of photography, therefore some discrepancies between the map and current field conditions may exist . Any discrepancies that are encountered in the use of this map should be brought to the attention of Warren Hagenbuck, Regional Wetlands Coordinator, U . -
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. -
Some Desert Watering Places
DEPAETMENT OF THE INTEEIOE UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DiRECTOK WATER-SUPPLY PAPER 224 SOME DESERT WATERING PLACES IN SOUTHEASTEEN CALIFORNIA AND SOUTHWESTERN NEVADA BY WALTER C. MENDENHALL WASHINGTON GOVERNMENT PRINTING OFFICE 1909 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR WATER-SUPPLY PAPEK 224 SOME DESERT WATERING PLACES IN SOUTHEASTEEN CALIFOKNIA AND SOUTHWESTEKN NEVADA BY WALTER C. MENDENHALL WASHINGTON GOVERNMENT PRINTING OFFICE 1909 CONTENTS. Page. Introduction______________________________________ 5 Area considered_________________________________ 5 Mineral resources and industrial developments______________ . 6 Sources of data__________________________________ 7 Physical features__________________________________ 8 General character of the region______________________ 8 Death Valley basin__________________________________ 9 Soda Lake_____________________________________ 30 Salton Sink______________________________________ 10 A great trough_______________________________ 30 Fault lines__________________.____ ______________ 11 Climate______________________. ____ ______________ 11 Water supply_________ _________________________ 13 Origin_________________________________________ 13 Rivers______________________________________ 13 Springs__________________________________________ 15 Finding water_______________________________ 16 Camping places_______________________________ 16 Mountain springs and tanks______________________ 17 Dry lakes____________________________________ -
Comprehensive Conservation Plan, Lake Andes National Wildlife Refuge Complex, South Dakota
Comprehensive Conservation Plan Lake Andes National Wildlife Refuge Complex South Dakota December 2012 Approved by Noreen Walsh, Regional Director Date U.S. Fish and Wildlife Service, Region 6 Lakewood, Colorado Prepared by Lake Andes National Wildlife Refuge Complex 38672 291st Street Lake Andes, South Dakota 57356 605 /487 7603 U.S. Fish and Wildlife Service Region 6, Mountain–Prairie Region Division of Refuge Planning 134 Union Boulevard, Suite 300 Lakewood, Colorado 80228 303 /236 8145 CITATION for this document: U.S. Fish and Wildlife Service. 2012. Comprehensive Conservation Plan, Lake Andes National Wildlife Refuge Complex, South Dakota. Lakewood, CO: U.S. Department of the Interior, U.S. Fish and Wildlife Service. 218 p. Comprehensive Conservation Plan Lake Andes National Wildlife Refuge Complex South Dakota Submitted by Concurred with by Michael J. Bryant Date Bernie Peterson. Date Project Leader Refuge Supervisor, Region 6 Lake Andes National Wildlife Refuge Complex U.S. Fish and Wildlife Service Lake Andes, South Dakota Lakewood, Colorado Matt Hogan Date Assistant Regional Director U.S. Fish and Wildlife Service, Region 6 National Wildlife Refuge System Lakewood, Colorado Contents Summary ....................................................................................................................................... XI Abbreviations .................................................................................................................................. XVII CHAPTER 1–Introduction .....................................................................