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A Comprehensive Ecological Land Classification for Utah's West Desert
Western North American Naturalist Volume 65 Number 3 Article 1 7-28-2005 A comprehensive ecological land classification for Utah's West Desert Neil E. West Utah State University Frank L. Dougher Utah State University and Montana State University, Bozeman Gerald S. Manis Utah State University R. Douglas Ramsey Utah State University Follow this and additional works at: https://scholarsarchive.byu.edu/wnan Recommended Citation West, Neil E.; Dougher, Frank L.; Manis, Gerald S.; and Ramsey, R. Douglas (2005) "A comprehensive ecological land classification for Utah's West Desert," Western North American Naturalist: Vol. 65 : No. 3 , Article 1. Available at: https://scholarsarchive.byu.edu/wnan/vol65/iss3/1 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 Western North American Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Western North American Naturalist 65(3), © 2005, pp. 281–309 A COMPREHENSIVE ECOLOGICAL LAND CLASSIFICATION FOR UTAH’S WEST DESERT Neil E. West1, Frank L. Dougher1,2, Gerald S. Manis1,3, and R. Douglas Ramsey1 ABSTRACT.—Land managers and scientists need context in which to interpolate between or extrapolate beyond discrete field points in space and time. Ecological classification of land (ECL) is one way by which these relationships can be made. Until regional issues emerged and calls were made for ecosystem management (EM), each land management institution chose its own ECLs. The need for economic efficiency and the increasing availability of geographic informa- tion systems (GIS) compel the creation of a national ECL so that communication across ownership boundaries can occur. -
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 ......................................................................................................... -
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 -
Juab County Resource Management Plan
Juab County Resource Management Plan: I. Scope and Authority Juab County consists of 2,183,681 acres of land of which the Federal Government controls 1,569,966 acres or 71.90% of the land area. Of the 1,569,966 acres 1,442,917 acres are managed by the Bureau of Land Management, the Forest Service controls 109,917 acres, and the Fish and Wildlife Department controls 17,992 acres. In accordance with law Juab County asserts planning authority over all lands and natural resources within its geographical boundaries including those lands administered by the United States to the maximum extent, provided such plans and policies of Juab County are consistent with federal law. This is so for the following reasons: 1. The United States Constitution at Article I Section 8 Clause 17 grants Congress the power of exclusive legislation only over the District of Columbia and other places purchased by the consent of State Legislatures for the erection of forts, magazines, arsenals, dock-yards, and other needful buildings. The Utah Legislature reinforced this principle at Utah Code 63L-1-201, by ceding jurisdiction to the United States only over those lands used for the purposes spelled out in the U.S. Constitution Article I Section 8 Clause 17. No such lands are located in Juab County. Therefore, there is no constitutional basis for the Federal Government to assert exclusive jurisdiction over any federal land in Juab County. As the Tenth Amendments to the United States Constitution states: “The powers not delegated to the United States by the Constitution, nor prohibited by it to the States, are reserved to the States respectively, or to the people.” 2. -
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. -
Oxidized Zinc Deposits of the United States Part 2
Oxidized Zinc Deposits of the United States Part 2. Utah By ALLEN V. HEYL GEOLOGICAL SURVEY BULLETIN 1135-B A detailed study of the supergene zinc deposits of Utah UNITED 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 Printin~ Office Washin~ton 25, D.C. CONTENTS Page Abstract ____________________ ~------------------------------------- B1 Introduction______________________________________________________ 1 Fieldwork____________________________________________________ 1 Acknowledgments_____________________________________________ 2 Geology__________________________________________________________ 2 Location of the deposits________________________________________ 2 ~ineralogy___________________________________________________ 3 Secondary zinc minerals_ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 4 Smithsonite___ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 4 H emimorphite (calamine) __ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 6 Hydrozincite___ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ 7 Aurichalcite_____ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ 7 VVurtzite_____________________________________________ 8 Other secondary zinc minerals___________________________ 8 Associated minerals__ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ -
Stratigraphy and Microfaunas of the Oquirrh Group in the Southern East ...Tintic Mountains, Utah
Stratigraphy and Microfaunas of the Oquirrh Group in the Southern East ...Tintic Mountains, Utah G E 0 L 0 G I C A L S U R V E Y P R 0 F E S S I 0 N A L P A P E R 1025 Stratigraphy and Microfaunas of the Oquirrh Group in the Southern East rrintic Mountains, Utah By H. T. MORRIS, R. C. DOUGLASS, and R. W. KOPF G E 0 L 0 G I CAL S lJ R V E Y P R 0 FE S S I 0 N A L PAP E R 1025 U N I T E D S T A T E S G 0 V E R N M E N T P R I N T I N G 0 F F I C E , WAS H I N G T 0 N : 1977 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Main en try under title: Morris, Hal Tryon, 1920- Stratigraphy and microfaunas of the Oquirrh Group in the southern East Tintic Mountains, Utah. (Geological Survey Professional Paper 1025) Bibliography: p. 20-22. 1. Geology, Stratigraphic--Pennsylvanian. 2. Geology, Stratigraphic--Permian. 3. Micropaleontology- Utah--Tintic Mountains. 4. Geology--Utah--Tintic Mountains. I. Douglass, Raymond Charles, joint author. II. Kopf, Rudolph William. III. Title. IV. Series: United States. Geological Survey. Professional Paper 1025. QE673.M67 551.7'52 77-10492 For -,ale by the Superintendent of Documents, U.S. GoYernment Printing Office \Vashington, D.C. -
Mesozoic Structure of the Newfoundland Mountains, Utah: Horizontal Shortening and Subsequent Extension in the Hinterland of the Sevier Belt
Mesozoic structure of the Newfoundland Mountains, Utah: Horizontal shortening and subsequent extension in the hinterland of the Sevier belt RICHARD W. ALLMENDINGER | Department of Geological Sciences, Cornell University, Ithaca, New York 14853 TERESA E. JORDAN ABSTRACT ented at a low angle to bedding. Microfabric analysis of recrystallized The Newfoundland Mountains of northwestern Utah preserve an rocks in the contact aureole and unrecrystallized country rocks shows unusually complete record of Mesozoic deformation in the hinterland that most of the intracrystalline strain is pre-latest Jurassic in age and of the Sevier orogenic belt. Structural relations of Paleozoic miogeo- is characterized by layer-parallel shortening. Post-latest Jurassic in- clinal strata with the Newfoundland stock, which has biotite and tracrystalline strain is minor and records shortening originally ori- hornblende K/Ar ages of 153.2 ± 4.6 and 147.7 ± 4.4 m.y., respec- ented nearly vertical. The map geometries, geochronology, and tively, and dated quartz monzonite dikes (with K/Ar biotite ages of microfabric analysis suggest the following structural history (from 150.7 ± 4.5 and 143.7 ± 4.3 m.y. and a muscovite age of 149.1 ± 4.5 oldest to youngest): (1) pre-latest Jurassic regional shortening and m.y.) provide the basis for dating Mesozoic deformation in the range. thrusting and (2) syn- or post-latest Jurassic horizontal extension Geologic mapping at 1:24,000 has identified four geometric classes of during the Mesozoic. In the Cretaceous and early Tertiary, -
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. -
W9200094.Pdf
STATE OF UTAH DEPARTt1EtJT OF tJATURAL RESOURCES Technical Publ ication No. 42 HYDROLOG IC RECOtJNA , SSANCE OF THE tWRTHERN GREAT SALT LAKE DESERT AND SUMMARY HYDROLOGIC RECONNAISSANCE OF NORTHWESTERN UTAH by Jerry C. Stephens, Hydrologist U. S. Geological Survey Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of ~ater Rights 1974 CONTENTS Page Abstract ...........................................•....................... Introduction ••••.•••.••••.••••••••••••••••••••••••••••••••••••••••••••••••• 2 Previous studies and acknowledgments ••••••.•••••••••••••••••••••••••••••••• 3 Hydrologic reconnaissance of the northern Great Salt Lake Desert............................................................ 7 Location and general features •••••••••••.•.••••••••••••••••••.•.•.. 7 Hydrology •••••••••• ................................................ 7 Surface water •• ................................................ 7 Ground water ••••••••••••••••••••••••••••••••••••••••••••••••••• 11 Shallow brine aquifer ••• ................................... 12 Alluvial-fan aquifer ••• .................................... 16 Valley-fill aquifer 20 ot he r aqui fer 5 ••••••••••••••••••••••••••••••••••• 22 Discussion of recharge and discharge estimates ••••••••••••• 23 ~"a te r qua litY••••••• ........................................... 23 Potential for additional water-resources development •• 26 Summary of hydrology of northwestern Utah •••••••••••••••••••••••••••••••••• 26 Surface water .................•..•................................ -
Late Quaternary Environmental Change in the Bonneville Basin, Western USA
Palaeogeography, Palaeoclimatology, Palaeoecology 167 (2001) 243±271 www.elsevier.nl/locate/palaeo Late Quaternary environmental change in the Bonneville basin, western USA D.B. Madsena,*, D. Rhodeb, D.K. Graysonc, J.M. Broughtond, S.D. Livingstonb, J. Hunta, J. Quadee, D.N. Schmitta, M.W. Shaver IIIa aUtah Geological Survey, Salt Lake City, UT 84116, USA bDesert Research Institute, Reno, NV 89512, USA cUniversity of Washington, Seattle, WA 98195, USA dUniversity of Utah, Salt Lake City, UT 84102, USA eUniversity of Arizona, Tucson, AZ 85721, USA Received 9 December 1999; received in revised form 24 July 2000; accepted for publication 7 September 2000 Abstract Excavation and analyses of small animal remains from strati®ed raptor deposits spanning the last 11.5 ka, together with collection and analysis of over 60 dated fossil woodrat midden samples spanning the last 50 ka, provide a detailed record of changing climate in the eastern Great Basin during the late Pleistocene and Holocene. Sagebrush steppe dominated the northern Bonneville basin during the Full Glacial, suggesting that conditions were cold and relatively dry, in contrast to the southern basin, which was also cold but moister. Limber pine woodlands dominated ,13±11.5 ka, indicating increased dryness and summer temperatures ,6±78C cooler than present. This drying trend accelerated after ,11.5 ka causing Lake Bonneville to drop rapidly, eliminating 11 species of ®sh from the lake. From ,11.5±8.2 ka xerophytic sagebrush and shadscale scrub replaced more mesophilic shrubs in a step-wise fashion. A variety of small mammals and plants indicate the early Holocene was ,38C cooler and moister than at present, not warmer as suggested by a number of climatic models.