Ground Water in Juab, Millard, and Iron Counties, Utah

Total Page:16

File Type:pdf, Size:1020Kb

Ground Water in Juab, Millard, and Iron Counties, Utah DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR WATER-SUPPLY PAPER 277 GROUND WATER IN JUAB, MILLARD, AND IRON COUNTIES UTAH BY OSCAR E. MEINZER IN COOPERATION WITH THE STATE OF UTAH CALEB TANNER, STATE ENGINEER WASHINGTON GOVERNMENT PRINTING OFFICE 1911 CONTENTS. Page, Introduction_______________________________________ 9 Location and extent of area__________________________ 9 Purpose of investigation___________________________ 9 Acknowledgments_____________________________________ 10 Physiography______________________________________ 11 Units of discussion_________________________________ 11 Provinces______________________________________ 11 Stream topography_______________________________ 12 Lake topography___________________________________ 12 Wind topography ______________ ________ __ _ _____ 13 Minor basins_____________________________________ 13 Geology __________ ________ _____________ ____ 15 Formations_________________..__________________ 15 Geologic history _______________________________ 1G Rainfall___________________________________________ 18 Geographic distribution ____________________________ 18 Annual variation_________________________ ____ 21 Seasonal variation___________________"____________ 22 Relation to dry farming_____________________ _____ 22 Soil_____________________________________________ 23 Vegetation_______i_________________________________ 24 Streams_______________________________-_-______ 25 Industrial development_________________________________ 26 Occurrence of ground water_____________________ _____ 29 Bedrock_______________________________________ 29 Water in sedimentary rocks________________ _____ 29 Water in igneous rocks__________ _______ ____ 30 Confining function of bedrock_______________ _____ 32 Unconsolidated sediments_____________ _ - _____ 32 Character of sediments________ - ___- 32 Water in stream deposits____ 33 Water in lake deposits_________________ _____ 33 Water in low valleys_____________ _ _ ____ 34 Water on desert flats_____________ ____ 34 Water on alluvial slopes or "bench lauds"____________ 36 Water in high valleys_____ _ 37" Artesian conditions __..____-_ _ - _ 37 Bedrock_______________________________________ 37 Unconsolidated sediments______________ ___ _ ______ 38 Flows in the valleys_____________________________ 38 Flows in the deserts_____ __ __ _____ 40 CONTENTS. Springs____________________________________________ 41 Mountain springs__________________________________ 41 Seepage from unconsolidated sediments__________________ 42 Springs from lava beds______L._________________________________ 43 Hot springs______________________________________ 43 Pool and knoll springs____________:_________________ 44 Quality of ground water________________________________ 45 Substances contained in water and their effects upon its use_____ 45 Water from the mountain areas________________________ 47 Ground water in the valleys__________________________ 47 Ground water in the deserts__________________________ 47 Water from springs________________________________ 48 Irrigation with ground water________________ _________ 49 Developments____________________________________ 49 Prospects_______________________________________ 49 Quantity of water__ ______________________________ 50 Quality of water and soil____________________________ 51 Cost of pumping__________________________________ 51 Value of crops _________________________________ 53 Culinary supplies ___________________________:________ 53 Supplies for dry farms_________________________________ 55 Supplies for the range________________________________ 56 Boiler supplies _____________________________ ;_______ 57 Construction of wells_________________________________ 58 Types of wells in use_______________________________ 58 Drilled wells on alluvial slopes_____________________ 59 " Pit flows" _____________________________________ 59 Irrigation wells ________________________________ 60 The California or "stovepipe" method of well construction_____ 60 Conditions in California_________________________ 60 Description of apparatus and methods_________________ 61 Advantages of California method_____________________ 62 Cost of the wells_______________________________ 63 Watering places on routes of travel______ _ _ 64 Railway stations and their connections___________________ 64 Tintic mining district to Sevier Desert and Joy____________ 05 Oasis to Joy, Fish Springs, and Deep Creek________________ 65 Stage route to Dugway, Fish Springs, and Deep Creek_ __ _ 66 Oasis to Snake Valley__________________- - __ 66 Newhouse to Snake Valley_______________ - ____ 66 Black Rock and Clear Lake to Snake Valley and Ibex_________ 67 Juab Valley,___________________________ 67 Topography and geology______________ 67 Rainfall_______________________________ ____- 68 Streams-_____________________ 69 Springs ______________________________-__ 70 Flowing wells _____________1_________ _ 70 Ground water beneath the bench lands____ 72 Quality of water______._________ ___ 73 Irrigation with ground water______ 74 Culinary supplies _________ 74 CONTENTS. 5 Page. Round, Little, Sage, Dog, and Fernow valleys__________________ 74 Topography ___________________________________ 74 Geology_______________________________________ 75 Rainfall_____________________________________ 75 Water supplies _________________________________ 76 Round Yalley _________________________________ 76 Little Valley__________________________________ 77 Sage Valley __________________________________ 78 Dog and Fernow valleys_______________________ 78 Tintic Valley________________________________________ 78 General features _______________________________ 78 Water resources________________________________ 79 Quality of the water _______________________________ 81 Tintic raining district _____________-I__________________ 81 Geology ______________________________________ 81 Water in limestone and quartzite______________________ 81 Water in igneous rocks and overlying waste-_______________ 82 Springs____________________________________ 82 Wells_________________________________.____ 84 Mines ______________________________________ 85 Domestic and industrial supplies____________________ 85 Pavant Valley ______________________________________ 86 Topography______________________________________ 86 Geology _________________. ________________________ 88 Rainfall _____________________.________________ 88 Streams and mountain springs___________________ 89 - Shallow-water belt ________________________________ 89 Artesian prospects ________________________________ 90 Water beneath the bench lands________________________ 91 Quality of ground water___________________________ 92 Irrigation with ground water________________________ 0.". Culinary supplies ______________________________ 93 Lower Beaver Valley______________________________ 94 Topography and geology________________________ 94 Rainfall_______________________________________ 95 Streams ____________________________________ 95 Springs____________________________________ 95 Black Rock Springs___________________________ 95 Clear Lake Springs ____________________________ 96 Other springs_________________________________ 97 Wells _________________________________________ 97 Wells on the Beaver Bottoms______________________ 97 Goss well____________________________________ 97 Neels well___________________________________ 99 Clear Lake well _______________________________ 100 Swan Lake farm wells__________________ _ ___ 100 Shallow wells in the valley below Black Rock_____________ 101 Old River Bed and Cherry Creek region__________________ 101 General features ________________________-____ 101 Water supplies ______________________________ _ 103 Ground water prospects ___ _________ _ 103 6 . CONTENTS. Page. Drum and Swasey Wash region ___________________________ 104 Wells at Joy_____________________________________ 104 Other water supplies______________________________ 105 Ground-water prospects_____________________________ 106 Sevier Desert______________________________________ 106 Physiography_________________________________.__ 10(5 Rainfall______1________________________________ 10S Ground-water level _______________ _________ ____ 109 Soil___________________________________________ 109 Vegetation_____________________________________ 110 Irrigation _____________________________________ 110 Water-bearing beds________________________________ 111 Wells on the Lynn Bench and Canyon Mountain slope_________ 111 Wells on the low flat______________________________ 112 Artesian conditions ________________________________ 114 Quality of water________________________________ 115 Wah Wah Valley ___________________________________ 117 General features__________________*.____________________ 117 Soil___________________________________________ 118 Rainfall_______________________________________'_ 118 WTater supplies _________________________________ 119 Ground-water prospects ______________________________ 119 Sevier Lake bottoms_________________________________ 119 Fluctuations of the lake level__________________________ 119 Position of the lake________________________________ 120 Quality of the lake water____________________________ 120 Ground-water prospects ____________________________ 121 White Valley_______________________________________ 121 General features___________,____________________ 121 Springs ______________________________________ 122 Ground-water prospects ___________________________ 123 Fish Springs Valley___________________________________
Recommended publications
  • Triangulation in Utah 1871-1934
    UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 913 TRIANGULATION IN UTAH 1871-1934 J. G. STAACK Chief Topographic Engineer UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1940 Tor sale by the Superintendent of Documents, Washington, D. C. Price 20 cents (paper) CONTENTS Page Introduction ______________________________________________________ 1 Scope of report------__-_-_---_----_------------ --__---__ _ 1 Precision __ _ ________________________ _ __________________ _ ___ 1 Instruments used._ _ _ _ _ _ _ _ _ 2 Station marks___- _ _.__ __ __ _ 2 Datum_-_-_-__ __________________________ ______ ______-___.__ 3 Methods of readjustment..._____.-.__..________.___._._...___.__ 4 Form of results__-.________________________ _.___-_____.______ 5 Arrangement__.______________________________ _ ___ _ ________ 6 Descriptions of stations._______________________________________ 6 Azimuths and distances.__ ____-_.._---_--_________ -____ __ __ ^ 7 Maps.__----__-----_-_---__-_--_-___-_-___-__-__-_-_-___.-.__ 7 Personnel_ _ __-----_-_-_---_---------_--__-____-__-_.--_.___ . 7 Projects 9 Uinta Forest Reserve, 1897-98_ 9 Cottonwood and Park City special quadrangles, 1903____ _ 19 Iron Springs special quadrangle, 1905____________________________ 22 Northeastern Utah, 1909.. -_. 26 Eastern Utah, 1910 - . 30 Logan quadrangle, 1913._________-__-__'_--______-___:_____.____ 42 Uintah County, 1913___-__. 48 Eastern Utah, 1914.. ... _ _ .. 55 Northern Utah, 1915 (Hodgeson)_____-___ __-___-_-_-__-_--. _. 58 Northern Utah, 1915 <Urquhart)_.
    [Show full text]
  • North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave
    North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave http://www.desertusa.com/desert.html In most modern classifications, the deserts of the United States and northern Mexico are grouped into four distinct categories. These distinctions are made on the basis of floristic composition and distribution -- the species of plants growing in a particular desert region. Plant communities, in turn, are determined by the geologic history of a region, the soil and mineral conditions, the elevation and the patterns of precipitation. Three of these deserts -- the Chihuahuan, the Sonoran and the Mojave -- are called "hot deserts," because of their high temperatures during the long summer and because the evolutionary affinities of their plant life are largely with the subtropical plant communities to the south. The Great Basin Desert is called a "cold desert" because it is generally cooler and its dominant plant life is not subtropical in origin. Chihuahuan Desert: A small area of southeastern New Mexico and extreme western Texas, extending south into a vast area of Mexico. Great Basin Desert: The northern three-quarters of Nevada, western and southern Utah, to the southern third of Idaho and the southeastern corner of Oregon. According to some, it also includes small portions of western Colorado and southwestern Wyoming. Bordered on the south by the Mojave and Sonoran Deserts. Mojave Desert: A portion of southern Nevada, extreme southwestern Utah and of eastern California, north of the Sonoran Desert. Sonoran Desert: A relatively small region of extreme south-central California and most of the southern half of Arizona, east to almost the New Mexico line.
    [Show full text]
  • Geological Society of America Bulletin
    Downloaded from gsabulletin.gsapubs.org on January 26, 2010 Geological Society of America Bulletin Regional structure and kinematic history of the Sevier fold-and-thrust belt, central Utah Peter G. DeCelles and James C. Coogan Geological Society of America Bulletin 2006;118;841-864 doi: 10.1130/B25759.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. Notes Geological Society of America Downloaded from gsabulletin.gsapubs.org on January 26, 2010 Regional structure and kinematic history of the Sevier fold-and-thrust belt, central Utah Peter G.
    [Show full text]
  • 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.
    [Show full text]
  • Nebo Overthrust, Southern Wasatch Mountains, Utah
    GEOLOGY I YOUNG STUDIES f UNIVERSITY Volume 12 December 1965 r' r' CONTENTS Thrusting in the Southern Wasatch Mountains, Utah ........ Michael J. Brady 3 Nebo Overthrust, Southern Wasatch Mountains, Utah ........ B. Allen Black 55 Paleoecologic implications of Strontium, Calcium, and Magnesium in Jurassic rocks near Thistle, Utah .... Button W. Bordine 91 Paleoecology of the Twin Creek Limestone In the Thistle, Utah area .................................... .... .....Ladell R. Bullock 121 Geolo of the Stockton stock and related intmsives, &1e County, Utah ................................................. John L. Lufkin 149 Stratigraphy and rifera of Ordovician rocks near Columbia Iceads, Jasper National Park, Alberta, Canada .............................................................. .. .... J. Keith Rigby 165 Lower Ordovician conodonts and other microfossils from the Columbia Icefields Section, Alberta, Canada ........................... .. .......... R. L. Ethington and D. L. Clark 185 Publications and maps of the Geology Department ........................... .. ..... 207 Brigham Young University Geology Studies Volume 12 - December 1965 Contents Thrusting in the Southern Wasatch Mountains, Utah ........ Michael J. Brady 3 Nebo Overthrust, Southern Wasatch Mountains, Utah ........ B. Allen Black 55 Paleoecologic irriplications of Strontium, Calcium, and Magnesium in Jurassic rocks near Thistle, Utah .... Burton W. Bordine 91 Paleoecology of the Twin Creek Limestone in the Thistle, Utah area ...................................................
    [Show full text]
  • 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. Scipio Valley faults (Class A) No. 2440 Last Review Date: 2004-07-01 Compiled in cooperation with the Utah Geological Survey citation for this record: Black, B.D., Hylland, M.D., and Hecker, S., compilers, 2004, Fault number 2440, Scipio Valley faults, 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 02:57 PM. Synopsis Late Holocene faults on the western side of Scipio Valley in central Utah. Name Fault ID: Refers to fault number 8-19 of Hecker (1993 #642). comments County(s) and MILLARD COUNTY, UTAH State(s) Physiographic BASIN AND RANGE province(s) Reliability of Good Reliability of Good location Compiled at 1:62,500 scale. Comments: Mapped or discussed by Bjorklund and Robinson (1968 #4546), Bucknam and Anderson (1979 #517), Crone and Harding (1984 #4545), Oviatt (1992 #4544), and Hintze and Davis (2002 #6754, 2003 #6741). Fault traces from 1:100,000- scale mapping of Oviatt (1992 #4544). Geologic setting North- and northeast-trending normal faults along the western side of northern Scipio Valley. Scipio Valley is an elongate graben flanked by horst-block mountain ranges: the Pavant Range and Canyon Mountains on the west and the Valley Mountains on the east.
    [Show full text]
  • 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.
    [Show full text]
  • 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__ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _
    [Show full text]
  • Episodic Dust Events of Utah's Wasatch
    1654 JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY VOLUME 51 Episodic Dust Events of Utah’s Wasatch Front and Adjoining Region W. JAMES STEENBURGH AND JEFFREY D. MASSEY Department of Atmospheric Sciences, University of Utah, Salt Lake City, Utah THOMAS H. PAINTER Jet Propulsion Laboratory, Pasadena, California (Manuscript received 4 January 2012, in final form 4 April 2012) ABSTRACT Episodic dust events cause hazardous air quality along Utah’s Wasatch Front and dust loading of the snowpack in the adjacent Wasatch Mountains. This paper presents a climatology of episodic dust events of the Wasatch Front and adjoining region that is based on surface weather observations from the Salt Lake City International Airport (KSLC), Geostationary Operational Environmental Satellite (GOES) imag- ery, and additional meteorological datasets. Dust events at KSLC—defined as any day [mountain standard time (MST)] with at least one report of a dust storm, blowing dust, and/or dust in suspension with a visi- bility of 10 km or less—average 4.3 per water year (WY: October–September), with considerable in- terannual variability and a general decline in frequency during the 1930–2010 observational record. The distributions of monthly dust-event frequency and total dust flux are bimodal, with primary and secondary maxima in April and September, respectively. Dust reports are most common in the late afternoon and evening. An analysis of the 33 most recent (2001–10 WY) events at KSLC indicates that 11 were associated with airmass convection, 16 were associated with a cold front or baroclinic trough entering Utah from the west or northwest, 4 were associated with a stationaryorslowlymovingfrontorbaroclinictroughwestof Utah, and 2 were associated with other synoptic patterns.
    [Show full text]
  • See for Details and How to Win a Limited Edition Full Curl Rifle
    200 Trophy Permits • $5 per Permit Application FEBRUARY 9–12, 2012 Salt Palace Convention Center Salt Lake City 200 Trophy Permits • $5 per Permit Application J AďLY NOW FOR $5 DRAWINGFEBRUARY FOR 200 BIG GAME 9–12, PERMITS 2012 K SpecialSpecial Salt Palace Convention Center Salt Lake City ThanksThanks J AďLY NOW FOR $5 DRAWING FOR 200 BIG GAME PERMITS K toto ourour TitleTitle 2017 AUCTION SponsorsSponsors 5 CATALOG www.AMMOANDMORESTORE.com THOSE WHO MAKE IT HAPPEN Welcome Sportsmen and Sportswomen! Welcome to the 11th Annual Western Hunting & Conservation Expo. Sportsmen for Fish & Wildlife and the Emmett Burroughs – Mule Deer Foundation Founder Sportsmen for Fish & Wildlife Board of Directors Don Peay – Founder Mule Deer Foundation are excited to bring you this very special hunting and conservation show. Your attendance Mule Deer Foundation Board of Directors Dave Woodhouse – Chairman and purchases help ensure the conservation of our wildlife and wild lands and the future of our hunting and sporting Brian Fienhold – Chairman of the Board Kevin Pritchett – Vice Chairman heritage. Thank you for joining us. Bethany Erb – Vice-Chair of the Board Rusty Aiken Ryan Bronson Brayden Richmond We are proud of how far the Expo has grown the past 11 years and this year promises to be spectacular. Our four- CJ Buck Kurt Wood Aaron Oelger day event features over 375 exhibits offering the finest guides, outfitters, professional hunters, artists, taxidermists, Erik Craythorne Jim Steadman jewelers, furriers and purveyors of fine guns, knives, optics, clothing and sporting equipment for the discerning Bob Jacobs sportsman and sportswoman. Kirstie Pike SFW Mission Fulfillment Board Art Reese Troy Justensen – Mission Fulfillment Board Chairman Daniel Harrison Dave Woodhouse – Vice Chairman/Utah Co.
    [Show full text]
  • Ground Water in Utah's Densely Populated Wasatch Front Area the Challenge and the Choices
    Ground Water in Utah's Densely Populated Wasatch Front Area the Challenge and the Choices United States Geological Survey Water-Supply Paper 2232 Ground Water in Utah's Densely Populated Wasatch Front Area the Challenge and the Choices By DON PRICE U.S. GEOLOGICAL SURVEY WATER-SUPPLY PAPER 2232 UNITED STATES DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1985 For sale by the Branch of Distribution U.S. Geological Survey 604 South Pickett Street Alexandria, VA 22304 Library of Congress Cataloging in Publication Data Price, Don, 1929- Ground water in Utah's densely populated Wasatch Front area. (U.S. Geological Survey water-supply paper ; 2232) viii, 71 p. Bibliography: p. 70-71 Supt. of Docs. No.: I 19.13:2232 1. Water, Underground Utah. 2. Water, Underground Wasatch Range (Utah and Idaho) I. Title. II. Series. GB1025.U8P74 1985 553.7'9'097922 83-600281 PREFACE TIME WAS Time was when just the Red Man roamed this lonely land, Hunted its snowcapped mountains, its sun-baked desert sand; Time was when the White Man entered upon the scene, Tilled the fertile soil, turned the valleys green. Yes, he settled this lonely region, with the precious water he found In the sparkling mountain streams and hidden in the ground; He built his homes and cities; and temples toward the sun; But without the precious water, his work might not be done. .**- ste'iA CONTENTS Page Preface ..................................................... Ill Abstract ................................................... 1 Significance Ground water in perspective ................................ 1 The Wasatch Front area Utah's urban corridor ....................................
    [Show full text]
  • A History of Juab County, Utah Centennial County History Series
    A HISTORY OF fjuab County Pearl D. Wilson with June McNulty and David Hampshire UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF JuaB County Pearl D. Wilson with June McNulty and David Hampshire luab County, one of Utah's earliest created counties, sits along the strategic north-south corridor of the state. Prehistoric and Native American Indian cultures roamed there, as did early Spanish priests and explorers, who left an important record of the area. Trappers and traders wandered the mountains and deserts that create stark contrasts in this geo­ graphically diverse county. Mark Twain, an early traveler through parts of luab, penned interesting insights of the county, which contained portions of the Pony Express and Overland Stage routes. Mormon pioneers arrived to establish farms and ranches. This was followed by the build­ ing of railroads and mineral exploration. Rail traffic for a vast region centered in Nephi, labeled "Little Chicago." To the west, the Tintic Mining District rose as one of Utah's richest gold and silver mining areas, attract­ ing a more ethnically diverse population. From majestic Mount Nebo to streams and lakes and the vast sand dunes of west Juab, the county contains many recreational possibili­ ties. Juab County is rich in history, geogra­ phy, and tradition; this book tells its story. ISBN: 0-913738-20-4 A HISTORY OF Juab County A HISTORY OF ffuaB County Pearl D. Wilson with June McNulty and David Hampshire 1999 Utah State Historical Society Juab County Commission Copyright © 1999 by Juab County Commission
    [Show full text]