A Comprehensive Ecological Land Classification for Utah's West Desert
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Hydrogeologic and Geochemical Characterization of Groundwater Resources in Rush Valley, Tooele County, Utah
Prepared in cooperation with the State of Utah Department of Natural Resources Hydrogeologic and Geochemical Characterization of Groundwater Resources in Rush Valley, Tooele County, Utah Scientific Investigations Report 2011–5068 U.S. Department of the Interior U.S. Geological Survey Cover: Groundwater-supplied stock tank in southwestern Rush Valley, Utah. Hydrogeologic and Geochemical Characterization of Groundwater Resources in Rush Valley, Tooele County, Utah By Philip M. Gardner and Stefan Kirby Prepared in cooperation with the State of Utah Department of Natural Resources Scientific Investigations Report 2011–5068 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2011 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov 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 materials contained within this report. Suggested citation: Gardner, P.M., and Kirby, S.M., 2011, Hydrogeologic and geochemical characterization of groundwater resources in Rush Valley, Tooele County, Utah: U.S. -
Email W/Attached ERM Draft Human Exposure Survey Workplan
Draft Human Exposure Survey Work Plan David Abranovic to: Ken Wangerud 12/21/2012 12:26 PM "[email protected]", Wendy OBrien, Dan Wall, "'Bill Brattin' Cc: ([email protected])", Robert Edgar, "'[email protected]' ([email protected])", "'Scott Everett' ([email protected])", "R. History: This message has been forwarded. Ken Please find attached the Draft Human Exposure Survey Work Plan for your review. I have included both a pdf of the entire document and a word file of the text. Feel free to contact me or Mark Jones at (916) 924-9378 anytime if you have any questions regarding this document. david _____________________________________ David J. Abranovic P.E. Partner ERM West, Inc. 7272 E. Indian School Road, Suite 100 Scottsdale, Arizona 85251 T: 480-998-2401 F: 480-998-2106 M: 602-284-4917 [email protected] www.erm.com One Planet. One Company. ERM. ü Please consider the environment before printing this e-mail CONFIDENTIALITY NOTICE: This electronic mail message and any attachment are confidential and may also contain privileged attorney-client information or work product. The message is intended only for the use of the addressee. If you are not the intended recipient, or the person responsible to deliver it to the intended recipient, you may not use, distribute, or copy this communication. If you have received the message in error, please immediately notify us by reply electronic mail or by telephone, and delete this original message. This message contains information which may be confidential, proprietary, privileged, or otherwise protected by law from disclosure or use by a third party. -
Quaternary Tectonics of Utah with Emphasis on Earthquake-Hazard Characterization
QUATERNARY TECTONICS OF UTAH WITH EMPHASIS ON EARTHQUAKE-HAZARD CHARACTERIZATION by Suzanne Hecker Utah Geologiral Survey BULLETIN 127 1993 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES 0 STATE OF UTAH Michael 0. Leavitt, Governor DEPARTMENT OF NATURAL RESOURCES Ted Stewart, Executive Director UTAH GEOLOGICAL SURVEY M. Lee Allison, Director UGSBoard Member Representing Lynnelle G. Eckels ................................................................................................... Mineral Industry Richard R. Kennedy ................................................................................................. Civil Engineering Jo Brandt .................................................................................................................. Public-at-Large C. Williatn Berge ...................................................................................................... Mineral Industry Russell C. Babcock, Jr.............................................................................................. Mineral Industry Jerry Golden ............................................................................................................. Mineral Industry Milton E. Wadsworth ............................................................................................... Economics-Business/Scientific Scott Hirschi, Director, Division of State Lands and Forestry .................................... Ex officio member UGS Editorial Staff J. Stringfellow ......................................................................................................... -
Flora of the Stansbury Mountains, Utah
Great Basin Naturalist Volume 43 Number 4 Article 11 10-31-1983 Flora of the Stansbury Mountains, Utah Alan C. Taye U.S. Army Intelligence Center and School, Fort Huachuca, Arizona Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Taye, Alan C. (1983) "Flora of the Stansbury Mountains, Utah," Great Basin Naturalist: Vol. 43 : No. 4 , Article 11. Available at: https://scholarsarchive.byu.edu/gbn/vol43/iss4/11 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. FLORA OF THE STANSBURY MOUNTAINS, UTAH Alan C. Taye' Abstract.— The Stansbury Mountains of north central Utah rise over 2000 m above surrounding desert valleys to a maximum elevation of 3362 m on Deseret Peak. Because of the great variety of environmental conditions that can be found in the Stansburys, a wide range of plant species and vegetation types (from shadscale desert to alpine mead- ow) exist there. This paper presents an annotated list of 594 vascular plant species in 315 genera and 78 families. The largest families are Asteraceae (98 species), Poaceae (71), Brassicaceae (33), Fabaceae (27), and Rosaceae (26). Elymiis flcwescens was previously unreported from Utah. Statistical comparison of the Stansbury flora with neighboring mountain floras indicates that the Wasatch Mountains lying 65 km to the east have probably been the primary source area for development of the Stansbury flora. -
Geology of the Southern Stansbury Range Tooele County Utah
~+++++++++++++++++++++++++++++++++++++++++++++++++"~, i UTAH GEOLOGICAL AND MINERALOGICAL SURVEY I AFFILIATED WITH + i+ + * THE COLLEGE OF MINES AND MINERAL INDUSTRIES .:. i UNIVERSITY OF UTAH I f SALT LAKE CITY, UTAH .r. :t.:. .:- i... :i: * GEOLOGY OF THE SOUTHERN :i:.:- i STANSBURY RANGE i + TOOELE COUNTY, UTAH i by .:- .:..: 1 John A. Teichert .:- I.:.. .:. I :i: .: -:. -:. i I+ * *.1- *+ t Bulletin 65 May, 1959 i + PRICE $1.50 i + +-:. ~++++++++++++++++~1-++++++++++++++++++++++++++++++++~ UTAH GEOLOGICAL AND MINERALOGICAL SURVEY The Utah Geological and Mineralogical Survey was authorized by act of the Utah State Legislature in 1931; however, no funds were made available for its establishment until 1941 when the State Government was reorganized and the Utah Geological and Mineralogical Survey was placed within the new State Department of Publicity and Industrial Development where the Survey functioned until July 1, 1949. Effective as of that date, the Survey was trans ferred by law to the College of Mines and Mineral Industries, University of Utah. The Utah Code Annotated 1943, Vol. 2, Title 34, as amended by chapter 46 Laws 0/ Utah 1949, provides that the Utah Geological and Mineralogical Survey "shall have for its objects": 1. "The collection and distribution of reliable information regarding the mineral resources of the State. 2. "The survey of the geological formations of the State with special ref erence to their economic contents, values and uses, such as: the ores of the various metals, coal, oil-shale, hydro-carbons, oil, gas, industrial clays, cement materials. mineral waters and other surface and underground water supplies, mineral fertilizers, asphalt, bitumen, structural materials, road-making ma tE,'rials. -
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. -
Deterministic Earthquake Ground Motions Analysis
A- A-rr"M"17- GEOMATRIX FINAL REPORT DETERMINISTIC EARTHQUAKE GROUND MOTIONS ANALYSIS PRIVATE FUEL STORAGE FACILITY SKULL VALLEY, UTAH Prepared for: Stone & Webster Engineering Corporation CS-028233 J.O. NO. 0599601-005 Prepared by: Geomatrix Consultants, Inc. and William Lettis & Associates, Inc. March 1997 GMX #3801.1 (REV. 9907160167 990709 0) PDR ADOCK 07200022 C PDR Geomatrix Consultants GEOMATRIX SWEC #0599601-005 GMX #3801-1 (REV. 0) DETERMINISTIC EARTHQUAKE GROUND MOTIONS ANALYSIS PRIVATE FUEL STORAGE FACILITY, SKULL VALLEY, UTAH Prepared for: Stone & Webster Engineering Corporation Prepared by: 01, Date: AZý-/d Reviewed by: ¢Date: 3/10/97 Kathryn L. Hanson Approved by: ' Date 3/10/97 Kevin J. Coppersmith QA Category I Geomatrix Consultants, Inc. San Francisco, CA GEOMATRIX TABLE OF CONTENTS PAGE 1.0 INTRODUCTION ........................................................................................................... 1 2.0 SEISMOTECTONIC SETTING ................................................................................. 3 2.1 Seismotectonic Provinces ............................................................................................. 2.2 Tensile Stresses and Active Crustal Extension in the Site Region .......................... 5 3.0 REGIONAL POTENTIAL SEISMOGENIC SOURCES ........................................ 9 3.1 Potential Fault Sources Between 100 and 320 km of the Skull Valley Site ....... 9 3.2 Potential Fault Sources Within 100 km of the Skull Valley Site ......................... 11 3.2.1 Stansbury Fault -
Hydrogeologic and Geochemical Characterization of Groundwater Resources in Pine and Wah Wah Valleys, Iron, Beaver, and Millard Counties, Utah
Hydrogeologic and Geochemical Characterization of Groundwater Resources in Pine and Wah Wah Valleys, Iron, Beaver, and Millard Counties, Utah Prepared by Phillip Gardner, USGS Presented by Thomas Marston, USGS Funding by CICWCD, Bureau of Land Management, Utah Division of Water Rights, USGS Cooperative Water Program Study Objectives • Better understand the groundwater system • Establish baseline hydrologic data - natural variation at selected springs and wells • Evaluate the hydrologic connection between mountain springs & valley aquifers • Use new data to update - conceptual model - groundwater budget via GBCAAS numerical model Approach 1) Monitor spring discharge 2) Well & water level inventory: potentiometric map 3) Update regional groundwater ET estimates: Sevier Lake playa and Tule Valley 4) Geochemistry & environmental tracers - Ages - Flow paths - Sources - Connection between mountain springs and valley aquifers 5) Perform two, multi-well 7-day aquifer tests (1 in each valley) 6) Update GBCAAS numerical model 7) Update groundwater budget estimate Long-term water level trends 566 567 1 568 569 570 662 664 666 2 668 670 4 232 233 3 3 234 235 236 434 1 435 4 2 436 5 437 438 364 365 5 366 367 368 Jan-74 Jan-76 Jan-78 Jan-80 Jan-82 Jan-84 Jan-86 Jan-88 Jan-90 Jan-92 Jan-94 Jan-96 Jan-98 Jan-00 Jan-02 Jan-04 Jan-06 Jan-08 Jan-10 Jan-12 Jan-14 All levels up since 1983 - 1984 Updated water-level data Update based on: • 25 new USGS water levels • 3 reported drillers levels • Utah Alunite water levels • Peak Minerals /CH2MHill levels • Pine -
Potash Brines in the Great Salt Lake Desert, Utah
Please do not destroy or throw away this publication. If you have no further use for it write to the Geological Survey at Washington and ask for a frank to return it DEPARTMENT OF THE INTERIOR Hubert Work, Secretary U. S. GEOLOGICAL SURVEY George Otis Smith, Director Bulletin 795 B BY THOMAS B. NOLAN Contributions to economic geology, 1927, Part I (Pages 25-44) Published June 16,1927 UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON ' 1927 CONTENTS Page Introduction___ 25 Location and settlement _ 26 History of development 26 Acknowledgments- ' _ -^ , 27 Bibliography____ 27 Method of prospecting 28 Geology______ - 29 General features _ 29 Surface features 30 Lake Bonneville beds _ 32 Calcareous clays and sands_____________ ________ 32 Salt___________________________________ 34 Brines __ _ 35 Origin of the brines___ _____ 40 Technical considerations __ _.___ _______________ 43 Summary- _ _ _ _ : ___ 44 ILLUSTEATION Page PLATE 3. Map showing the salinity of the brines underlying the Great Salt Lake Desert, Utah______________________ 40 n POTASH BRINES IN THE GREAT SALT LAKE.DESERT, UTAH By THOMAS B. NOLAN INTRODUCTION During and immediately after the war the brines of-the Salduro Marsh, in the Great Salt Lake Desert, were a source of considerable potash for the domestic supply. Although no p'otash has been pro duced from these brines in the last few years, a continued interest in the area has been shown by a large number of filings, in different parts of the desert, under the potash law of October 2, 1917 (40 Stat. 297), and the regulations issued under that law by the Department of the Interior on March 21, 1918, in Circular 594 (46 L. -
3-5-19 Transcript Bulletin
Looking back at Stansbury, Tooele and Grantsville’s basketball season See B1 TOOELETRANSCRIPT S T C BULLETIN S TUESDAY March 5, 2019 www.TooeleOnline.com Vol. 125 No. 79 $1.00 Boulder kills woman on Stansbury Island hike STEVE HOWE line, with the woman in the STAFF WRITER middle, when she stepped out A 37-year-old woman died of the path and onto a rock, Saturday on Stansbury Island Scharmann said. The rock after a large rock fell on top of began to slide and she tried to her, according to the Tooele jump off it, but the rock landed County Sheriff’s Office. on top of her in the bottom of The Salt Lake area woman, the gully. whose identity has not been Scharmann said the boulder released, was hiking on was about 4 feet by 4 feet by Stansbury Island with her 18 inches and too heavy to husband and a friend Saturday move by hand. He said the trio afternoon, according to Tooele was not on the marked trail County Sheriff’s Lt. Travis from a nearby trailhead and Scharmann. They were walking in SEE BOULDER PAGE A8 ® FRANCIE AUFDEMORTE/TTB PHOTO Tyson Hamilton, the owner of Another Man’s Treasures in Tooele, stands behind the counter of his antique store. Former Tooele New chamber chairman wants cop charged to bring community together with custodial Buy local, tourism, unity, and community spirit top sexual relations Hamilton’s 2019 to-do list STEVE HOWE federal parolee, supervised by TIM GILLIE STAFF WRITER the federal government. EDITOR A Tooele City police officer A Tooele City detective A full-blooded Tooelean, the new has been charged with a felony conducted an investigation, in chairman of the Tooele County Chamber after he allegedly had sexual which he interviewed Dudley of Commerce and Tourism board of relations with a federal parolee and the parolee, the statement directors is fervent about building local during his time as an officer. -
Wilderness Areas on the Uinta-Wasatch-Cache National
Wilderness Areas On The Uinta‐Wasatch‐Cache National Forests “Wilderness is the land that was wild land beyond the frontier...land that shaped the growth of our nation and the character of its people. Wilderness is the land that is rare, wild places where one can retreat from civilization, reconnect with the Earth, and find healing, meaning and significance.” The United States was the first country to define and create designated wilderness areas. In 1964 the Wilderness Act was passed in congress. The Act describes wilderness as the following: "...lands designated for preservation and protection in their natural condition..." Section 2(a) "...an area where the earth and its community of life are untrammeled by man..." Section 2(c) "...an area of undeveloped Federal land retaining its primeval character and influence, without permanent improvement or human habitation..." Section 2(c) "...generally appears to have been affected primarily by the forces of nature, with the imprint of man's work substantially unnoticeable..." Section 2(c) "...has outstanding opportunities for solitude or a primitive and unconfined type of recreation..." Section 2(c) "...shall be devoted to the public purposes of recreation, scenic, scientific, educational, conservation and historic use." Section 4(b) Within the Uinta‐Wasatch‐Cache National Forest there are 9 designated wilderness areas. These areas include: Mount Naomi Wilderness, Wellsville Mountain Wilderness, Mount Olympus Wilderness, Twin Peaks Wilderness, Lone Peak Wilderness, Mount Timpanogos Wilderness, Mount Nebo Wilderness, Deseret Peak Wilderness and the High Uinta Wilderness. Each of these areas offer unique wilderness opportunities and experiences. The Mount Naomi Wilderness was designated in 1984 and includes 44,523 acres. -
Carpenter, R.M., Pandolfi, J.M., P.M. Sheehan. 1986. the Late Ordovian and Silurian of the Eastern Great
MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 69 August 1, 1986 The Late Ordovician and Silurian of the Eastern Great Basin, Part 6: The Upper Ordovician Carbonate Ramp Roger M. Carpenter John M. Pandolfi Peter M. Sheehan MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 69 August 1, 1986 The Late Ordovician and Silurian of the Eastern Great Basin, Part 6: The Upper Ordovician Carbonate Ramp Roger M. Carpenter, Department of Geology, Conoco Inc., 202 Rue Iberville, Lafayette, LA 70508; John M. Pandolfi, Department of Geology, University of California, Davis, California, 95616; Peter M. Sheehan, Department of Geology, Milwaukee Public Museum, 800W. Wells St., Milwaukee, Wisconsin 53233 ISBN 0-89326-122-X © 1986 Milwaukee Public Museum Abstract Two east-west transects examined in western Utah and eastern Nevada preserve Upper Ordovician-Lower Silurian lithofacies along a carbonate ramp transitional between a shelf and basin. Previous investigators have reconstructed this margin as a classic carbonate shelf with an abrupt, linear margin between shelf and slope. However, lithofacies change gradually between shelf and slope and are better explained by a carbonate ramp model. Intertidal and shallow subtidal dolomites are present to the east, with progressively deeper water limestones with increasing fine grained terrigenous content toward the west. Shelf edge reefs or shallow water carbonate margin buildups are absent. Latest Ordovician glacio-eustatic decline in sea level produced a period ofsubaerial exposure in the shallow eastern region. However, deposition continued deeper on the ramp, where shallow-water, cross laminated, massive dolomites were deposited during the glacio-eustatic regression. The carbonate ramp pattern was disrupted in the Middle or early part of the Late Llandovery, when an abrupt margin was established by listric growth faulting.