Utah History Encyclopedia

Total Page:16

File Type:pdf, Size:1020Kb

Utah History Encyclopedia DEEP CREEK MOUNTAINS Constructing Deep Creek Railroad One of the lesser-known areas of Utah is in the west desert of Tooele and Juab counties near the border between Utah and Nevada. The Deep Creek Mountains form the major geographic feature of the region. The Deep Creek Mountains run in a north-south direction for about thirty miles. They are ruggedly steep and feature huge granite outcroppings, especially at the south end where the mountains reach heights of 12,000 feet in elevation. Ibapah Peak is 12,101 feet and to the immediate north, Haystack Peak rises 12,080 feet above sea level. The Deep Creek Range supplies precious water to the surrounding communities of Callao, Trout Creek and Partoun on the east; Pleasant Valley and Gandy on the south; Gold Hill to the north; and Ibapah (or Deep Creek) to the west. Several crystal clear streams provide perpetual runoff from the high mountain slopes to the valleys below. The vegetation is consistent with desert and mountain ecosystems, depending on elevation and precipitation. One native plant worthy of note is the ancient Bristlecone Pine which is known to be several thousand years old. Wildlife is found in great abundance throughout the area. Rocky Mountain Bighorn sheep and elk have recently been introduced to the Deep Creek Range. Considerable acreage on the mountain range has been designated as wilderness. The area was first inhabited by Goshute Indians. Their descendants continue to live on a reservation immediately to the west of the Deep Creek Range. In 1827 the explorer Jedediah Smith was the first known white man to traverse the region as he searched for a direct route across the Great Basin. Major Howard Egan further explored the area in 1 of 4 the 1850′s, as he assisted George Chorpenning with a U.S. mail contract between Salt Lake and California. By 1858, Chorpenning had built a mail station at Pleasant Valley. The following spring an Indian farm was established by the government at Ibapah. Simultaneously, LDS missionaries were called to colonize and do missionary work among the Indians at Ibapah. Major Egan′s Pony Express station was headquartered at Ibapah in 1860 and another major station was located thirty miles to the east on the other side of the Deep Creeks at Willow Springs (later named Callao). George W. Boyd operated the mail and stage line there and was assisted by Enoch Wallace Tripps and his wife, Julia Boyd Tripp. The Tripps became the first settlers in Callao in 1869. Other early settlers include Kearneys, Bagleys, Timms, Sabeys, and Morehouses. Callao has remained a small farming community, as have Trout Creek, Partoun, and Pleasant Valley. At the time of this writing, no private merchants were in operation, although Callao has had a post office, a school, a hotel, two service stations and a store at one time or another. Partoun has been the site of the West Desert High School in recent years. Several hostile encounters between Indians and whites occurred in the Deep Creek area during the 1860′s as the Indian′s way of life began to be threatened. Indian attacks on Eight Mile and Canyon Stations near Ibapah in 1863 resulted from unprovoked massacres on Indians at Bear River and Skull Valley, Utah. Such Indian attacks were glamorized in media accounts as late as eighty years after. A home station for the Overland Mail and Stage and a telegraph office were established at Deep Creek following the demise of the Pony Express in 1862. The Devine General Store was founded in the 1860′s and has continually operated under different proprietorships to the present. There are two stores, one of which houses a post office in modern Ibapah. The community grew during the 1870′s through the 1890′s as settlers homesteaded sheep and cattle ranches. Some of the early pioneer family names were Worthington, Hudson, Burrington, McCurdy, Bates, Skinner, Goldsmith, Ferguson, Felt, Bonnemort, Weaver, Gash, Snively, Symonds, Lee, and Kelley. After 1880, the Ericksons, Littledikes, Stewarts, Halls, Chastains, Hibbards, Cooks, Mulliners, Sheridans, Parrishs, Georgeattas, and Proberts settled at Ibapah. Other prominent early names after 1910 in Ibapah have been Hicks, West, Christiansen, 2 of 4 and Calloway. Around the turn of the century, as mining districts in the area prospered, Ibapah had up to five saloons functioning and two dances functioning on any given night. Prosperity was further enhanced when the Lincoln Highway was routed through Callao, Gold Hill, and Ibapah from about 1915 to 1927. Sheridan′s hotel, gas, and store, along with Chastain′s post office and store were prominent in that time frame. The Deep Creek valley has had a school at Broadway, Nevada in the 1920′s as well as the Goshute Indian School from about 1915 to 1969, and Ibapah Elementary since 1883, where social functions such as dances, church weddings, and funerals have been held. The Goshute Tribal Council has a community center and the LDS Church built a chapel in 1981. The only large cemeteries in western Tooele County are the community and Goshute cemeteries, both of which are in Deep Creek Valley. Modern conveniences are of recent origin in the Deep Creek country. Electric power was installed in 1972. A paved highway was constructed in 1977 leading from the Ely, Nevada Highway to Ibapah, and private telephones followed in 1986. Gold Hill and Goodwin townsites lie at the northeastern end of the Deep Creek mountains. It has been the scene of several mining booms and busts since the 1870′s, when a lead-silver smelter was built at Clifton mining district near Gold Hill. The first large scale boom occurred in the early 1890′s, when several hundred thousand dollars in gold was shipped out by Colonel James F. Woodman. Up to 1,500 people resided in Gold Hill from 1917 to 1925. The Deep Creek Railroad hauled out hundreds of tons of tungsten during those years. The Gold Hill Standard carried local news and advertisements for such establishments as the Hillcrest Hotel, Goodwin Mercantile, the Gold Hill Pharmacy and pool hall, Bertelson′s grocery & clothing store, the Liberty Garage, the Home Restaurant and Bakery, plus two lumber yards. There was also a post office, a doctor, a dentist, an elementary school, and even a house of ill­ repute. Gold Hill was revived during World War II because the U.S. Government needed arsenic. Almost 100,000 tons of arsenic were mined from 1943 to 1945. Since then, Gold Hill has been a ghost town with only a handful of residents residing there. See: Ronald R. Bateman, Deep Creek Reflections. Salt Lake City: 3 of 4 Publisher′s Press, 1984. Ronald R. Bateman SOURCE... Article is from the Utah History Encyclopedia. Powell, Allan Kent, ed. Salt Lake City, Utah : The University of Utah Press, 1994 USE RESTRICTIONS... The contents of this article may be repurposed for non-commercial, non­ profit, educational use. Distributed by the Utah Education Network eMedia service: http://www.uen.org/emedia Original digital conversion by UCME: Utah Collections Multimedia Encyclopedia project: http://www.uen.org/ucme 4 of 4.
Recommended publications
  • Management Plan for the Great Basin National Heritage Area Approved April 30, 2013
    Management Plan for the Great Basin National Heritage Area Approved April 30, 2013 Prepared by the Great Basin Heritage Area Partnership Baker, Nevada i ii Great Basin National Heritage Area Management Plan September 23, 2011 Plans prepared previously by several National Heritage Areas provided inspiration for the framework and format for the Great Basin National Heritage Area Management Plan. National Park Service staff and documents provided guidance. We gratefully acknowledge these contributions. This Management Plan was made possible through funding provided by the National Park Service, the State of Nevada, the State of Utah and the generosity of local citizens. 2011 Great Basin National Heritage Area Disclaimer Restriction of Liability The Great Basin Heritage Area Partnership (GBHAP) and the authors of this document have made every reasonable effort to insur e accuracy and objectivity in preparing this plan. However, based on limitations of time, funding and references available, the parties involved make no claims, promises or guarantees about the absolute accuracy, completeness, or adequacy of the contents of this document and expressly disclaim liability for errors and omissions in the contents of this plan. No warranty of any kind, implied, expressed or statutory, including but not limited to the warranties of non-infringement of third party rights, title, merchantability, fitness for a particular purpose, is given with respect to the contents of this document or its references. Reference in this document to any specific commercial products, processes, or services, or the use of any trade, firm or corporation name is for the inf ormation and convenience of the public, and does not constitute endorsement, recommendation, or favoring by the GBHAP or the authors.
    [Show full text]
  • Mineral Deposits of the Deep Creek Mountains, Tooele and Juab Counties, Utah
    Mineral Deposits of the Deep Creek Mountains, Tooele and Juab Counties, Utah by K. C. Thomson UTAH GEOLOGICAL AND MINERALOGICAL SURVEY affiliated with THE COLLEGE OF MINES AND MINERAL INDUSTRIES University of Utah, Salt Lake City, Utah BULLETIN 99 PRICE $4.50 JUNE 1973 CONTENTS Page Page Abstract .................................... 1 Alaskite Intrusives ....................... 9 Dike Rocks .............................. 9 Introduction ................................. 3 Porphyry Dikes ......................... 9 Previous Work .............................. 3 Rhyolite Dikes ......................... 9 Physical Geography ........................... 3 Aplite Dikes ........................... 9 Andesite Dikes ......................... 9 Mapping and Analytical Techniques .................. 3 Basalt Dikes ...........................9 Pegmatite Dikes ......................... 9 Location of Mining Areas and Properties .............. 4 Extrusive Rocks ........................... 9 Ignimbrite Sequence ...................... 9 General Geology .............................. .4 Andesite ............................... 9 Stratigraphy . 4 Rhyolite .............................. 9 Precambrian Rocks ........................ .4 Tuff ................................. 9 Trout Creek Sequence ................... .4 Other Extrusive Rocks .................... 9 Johnson Pass Sequence ....................5 Structure ................................. 10 Water Canyon Sequence ................... 5 Southern Qifton Block ..................... 10 Cambrian and Precambrian
    [Show full text]
  • Current Status of Cutthroat Trout Subspecies in the Western Bonneville Basin
    Great Basin Naturalist Volume 38 Number 2 Article 5 6-30-1978 Current status of cutthroat trout subspecies in the western Bonneville Basin Terry J. Hickman Colorado State University, Fort Collins Donald A. Duff U.S. Bureau of Land Management, Salt Lake City, Utah Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Hickman, Terry J. and Duff, Donald A. (1978) "Current status of cutthroat trout subspecies in the western Bonneville Basin," Great Basin Naturalist: Vol. 38 : No. 2 , Article 5. Available at: https://scholarsarchive.byu.edu/gbn/vol38/iss2/5 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]. CURRENT STATUS OF CUTTHROAT TROUT SUBSPECIES IN THE WESTERN BONNEVILLE BASIN Terry J. Hickman' and Donald A. Duff^ Abstract.— Recent discoveries of native cutthroat trout populations in desert mountain ranges on the western fringe of the Bonneville Basin have prompted intensified management efforts by state and federal agencies. Anal- ysis of Snake Valley cutthroat specimens in Trout Creek, Deep Creek Mountain Range, Utah, indicate this is a pure strain of the trout which once inhabited Pleistocene Lake Bonneville and which was thought to be extinct in Utah. The Snake Valley cutthroat is similar to Salmo clarki Utah of the eastern Bonneville Basin; however, electrophoretic and morphomeristic analysis show unique genetic differences brought about by long-term isolation (8,000 years) from the remainder of the Bonneville Basin cutthroat.
    [Show full text]
  • The Birds of the Deep Creek Mountains of Central Western Utah
    UNIVERSITY OF UTAH BIOLOGICAL SERIES Vol. X I January 10, 1955 No. 4 The Birds of The Deep Creek Mountains of Central Western Utah BY WILLIAM H. BEHLE PUBLISHED BY UNIVERSITY OF UTAH SALT LAKE CITY t h e b i r d s o f t h e d e e p c r e e k m o u n t a in s OF CENTRAL WESTERN UTAH BY WILLIAM H. BEHLE In furtherance of a long-time survey of the avifauna of Utah the Deep Creek Mountain region of the central western part of the state was chosen as an area for intensive study. It was expected that gradients would occur in the characters of geographically variable birds between populations from the isolated ranges of the Great Basin and birds from the Wasatch Mountains to the northeast, those mountains that form the abrupt eastern margin of the Great Basin or the high plateaus of central and southern Utah. The Deep Creek region seemed most propitious for collecting a representation of the Great Basin races. While the analysis of the geographical variation was the main objective of the study and large series of the variable birds were desired, in accord with the general practice of making avifaunistic studies of particular regions, samples of other birds were taken when possible, and a study was made of the ecology of the birds of the region. Although the emphasis was on collecting, attention was paid to abundance, behavior, and life history features, as opportunity was afforded. Working out the details of the variation through­ out Utah must await the accumulation of additional material from many other locations, but in the meantime the results of the Deep Creek Mountain survey may well be placed on record to reveal the nature of the avifauna of this portion of Utah.
    [Show full text]
  • University of Nevada, Reno
    University of Nevada, Reno Fine-Grained Volcanic Toolstone Sources and Early Use in the Bonneville Basin of Western Utah and Eastern Nevada A thesis submitted in partial fulfillment of the requirements for the degree of Master of Arts in Anthropology by David Page Dr. Gary Haynes, Thesis Advisor May 2008 © David Page, 2008 All Rights Reserved THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by DAVID J. PAGE Entitled Fine-Grained Volcanic Toolstone Sources and Early Use in the Bonneville Basin of Western Utah and Eastern Nevada be accepted in partial fulfillment of the requirements for the degree of MASTER OF ARTS _____________________________________________________________ Gary Haynes, Ph.D., Advisor _____________________________________________________________ David E. Rhode, Ph.D., Committee Member _____________________________________________________________ Kenneth D. Adams, Ph.D., Graduate School Representative _____________________________________________________________ Marsha H. Read, Ph. D., Associate Dean, Graduate School May, 2008 i Abstract Identifying lithic sources is central to understanding toolstone use by prehistoric hunter-gatherer groups. The distribution of archaeological materials in relation to geologic sources creates a spatial pattern of use that varies through time. These patterns of distribution in conjunction with analysis of technological organization can be used to infer behavior, especially levels of mobility. This thesis presents geochemical data from a wide-scale sourcing
    [Show full text]
  • Goshute Indian Reservations
    Bureau of Indian Affairs Summary for Ely, Duckwater, and Goshute Indian Reservations ELY SHOSHONE INDIAN RESERVATION LOCATION The Ely Shoshone Indian Reservation (Reservation) is located near the town of Ely in White Pine County, in east central Nevada. The Reservation is comprised of three separate parcels covering approximately 111 acres in the Steptoe Valley hydrographic basin (Exhibit 4502). ESTABLISHMENT OF RESERVATION The Ely Reservation was established by an Act of Congress in 1930 (46 Stat. 820) (Exhibit 4503). Subsequent Acts added lands in 1931 (46 Stat. 1122) (Exhibit 4504) and 1977 (91 Stat. 1406) (Exhibit 4505). All of these lands are held in trust by the United States on behalf of the Ely Shoshone Indian Tribe. The Tribe is pursuing additional lands located southwest and southeast of the existing tribal lands. ENVIRONMENT The Reservation is primarily developed as residential, industrial, or commercial areas. If the Tribe succeeds in obtaining additional trust lands, other land uses may be developed. WATER RESOURCES The Reservation receives its municipal and domestic water from the town of Ely. If the Tribe succeeds in obtaining additional trust lands, other land uses may be pursued that require the Tribe to develop their own water resources. Water Rights The Tribe’s water rights have not been adjudicated by an appropriate court. At present, the Tribe has not developed its own water resources on its current land base. If the Tribe obtains additional trust lands, developed water resources and water rights may be needed to develop the lands. 1 DUCKWATER INDIAN RESERVATION LOCATION The Duckwater Indian Reservation (Reservation) is located in Nye County, Nevada in east central Nevada.
    [Show full text]
  • The Goshute Indians of Utah
    The Goshute Indians of Utah Dennis R. Defa The Goshute Indians live in a little known and sparsely populated portion of the state of Utah. There actually are two Goshute reserva­ tions, the largest of which is the Deep Creek Reservation located on the Utah-Nevada border about sixty miles south of Wendover, with a por­ tion of the reservation in each state. The second, and smaller, reservation is located in Skull Valley in Tooele County, about ninety miles west of Salt Lake City. Most people who visit this region of the state view it as a harsh, hard, and unforgiving place and wonder why anyone would choose to live there. However, for the Goshutes this desert region is home and they view it much differently than does the casual visitor. Before white Americans moved into the region, the Goshutes knew the land intimately and took from it all they needed to sustain life. As efficient and effective hunters and gatherers, they understood the fragile nature of the desert and maintained a balance that provided for their needs without destroy­ ing the limited resources of their arid homeland. At the time of their first contacts with whites, the Goshute people lived in the desert regions southwest of the Great Salt Lake. Exact bound­ aries are difficult to determine because of the nature of the land and the proximity of other peoples, but early chroniclers and surveyors provided some written descriptions of the general Goshute homelands. Captain James H. Simpson located the Goshute from the Great Salt Lake to the Un-go-we-ah Range, or Steptoe Mountains, in Nevada.
    [Show full text]
  • Studies of Geology and Hydrology in the Basin Arid Range Province
    Studies of Geology and Hydrology in the Basin arid Range Province, Southwestern United States^ For Isolation of High-Level Radioactive Waste Characterization of the Bbnneville Region, Utah and Kevadt U.S. GEOLOGICAL StJ&VEY Pi*0£ESSIO&AL PAPER 1370-G Prepared in cooperation with the States of Arizona, California, Iti Nevada, Mew Mexico, Texas, and tltah STUDIES OF GEOLOGY AND HYDROLOGY IN THE BASIN AND RANGE PROVINCE, SOUTHWESTERN UNITED STATES, FOR ISOLATION OF HIGH-LEVEL RADIOACTIVE WASTE- CHARACTERIZATION OF THE BONNEVILLE REGION, UTAH AND NEVADA Looking north of Blue Lake Springs at the southwestern margin of the Great Salt Lake Desert, Tooele County, Utah. Springs at and near Blue Lake Springs discharge 23.44 cubic hectometers of water per year. Carbonate rocks of Paleozoic age are exposed immediately to the left of the photograph. Photograph by K.A. Sargent (1984). Studies of Geology and Hydrology in the Basin and Range Province, Southwestern United States, For Isolation of High-Level Radioactive Waste Characterization of the Bonneville Region, Utah and Nevada Edited by M.S. BEDINGER, K.A. SARGENT, and WILLIAM H. LANGER STUDIES OF GEOLOGY AND HYDROLOGY FOR ISOLATION OF HIGH-LEVEL RADIOACTIVE WASTE U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1370-G Prepared in cooperation with the States of Arizona, California, Idaho, Nevada, New Mexico, Texas, and Utah UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1990 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging-in-Publication Data Studies of geology and hydrology in the Basin and Range province, southwestern United States, for isolation of high-level radioactive waste Characterization of the Bonneville region, Utah and Nevada.
    [Show full text]
  • The Resource Management Plan and Record of Decision Rangeland Program Summary
    House Range Resource Area Resource Management Plan And Record of Decision Rangeland Program Summary October 1987 RICHFIELD DISTRICT BUREAU OF LAND MANAGEMENT DEPARTMENT OF THE INTERIOR House Range Resource Area The Resource Management Plan And Record of Decision Rangeland Program Summary October 1987 RICHFIELD DISTRICT BUREAU OF LAND MANAGEMENT DEPARTMENT OF THE INTERIOR Adoption of the House Range Resource Area Resource Management Plan as provided herein is recommended. Date Donald Pendleton Date Area Manager District Manager House Range Resource Area Richfield District Adoption of the House Range Resource Area Resource Management Plan as provided herein is approved. Roland Robison Date Utah State Director READERS GUIDE Chapter 1 briefly describes the resource area, the evolution of the Resource Management Plan (RMP) selected through the planning process, and the alternative plans analyzed in the Draft RMP/Environmental Impact Statement (EIS) for the House Range Resource Area (HRRA), Millard and Juab Counties, Utah. For additional information on the planning process, planning issues, management concerns, and planning criteria, see Chapter 1 of the Draft RMP/EIS, which was published and distributed in March 1986. The RMP in Chapter 2 presents the decisions for future management of public land resources in the HRRA. It is based on Alternative D, The Preferred Alternative. It has been presented in the Draft RMP/EIS and proposed in the Final RMP/EIS. These discussions were expanded to include information required by Federal regulation and Bureau of Land Management (BLM) policy and presented as the proposed RMP in the Final EIS. Resource or program goals and objectives, proposed actions (including need for subsequent detailed site-specific activity plans), support requirements, implementation sequences or priority, and follow up monitoring and evaluation intervals and standards are included in this document.
    [Show full text]
  • STATE of UTAH DEPARTMENT of NATURAL RESOURCES Technical
    STATE OF UTAH DEPARTMENT OF NATURAL RESOURCES Technical Publication No. 24 HYDROLOGIC RECONNAISSANCE OF DEEP CREEK VALLEY, TOOELE AND JUAB COUNTIES, UTAH, AND ELKO AND WHITE PINE COUNTIES, NEVADA by J. W. Hood and K. M. Waddell, Hydrologists U. S. Geological Survey Prepared by the U. S. Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights 1969 CONTENTS Page Abstract 1 Introduction 2 Physiography ...................................... .. 4 Climate 5 Geology 12 Water resources 12 Volume of precipitation 12 Surface water 14 General conditions 14 Available records of flow 16 Runoff 17 Outflow from the valley 18 Ground water 18 Source 18 Estimated average annual recharge 18 Occu rrence and movement 20 Storage 21 Discharge 21 Evapotranspiration 21 Potential evapotranspiration 23 Estimated evapotranspiration 23 Pumpage 24 Outflow of unconsumed spring discharge 25 Ground-water budget 25 Perennial yield 25 Chemical quality of water 26 Mountains 26 Valley 26 Chemical quality of ground water in relation to sources of recharge 26 Domestic supplies 27 Irrigation supplies 28 III CONTENTS--Continued Page Land use and development 28 Past and present development 28 Potential development 30 Proposals for additional studies 30 Selected references 31 Appendix 35 Well- and spring-numbering system 37 Use of metric units 37 Basic data 41 Publications of the Utah Department of Natural Resources, Division of Water Rights 50 ILLUSTRATIONS Page Plate 1. Hydrogeologic maps of the Deep Creek valley drainage basin, Tooele and Juab Counties, Utah, and Elko and White Pine Counties, Nevada In pocket Figure 1. Map showing location of report area in Utah and Nevada and other nearby areas previously studied 3 Figure 2.
    [Show full text]
  • Glaciation in the Great Basin of the Western United States
    Quaternary Science Reviews 20 (2001) 1377}1410 Glaciation in the Great Basin of the Western United States Gerald Osborn *, Ken Bevis Department of Geology and Geophysics, University of Calgary, Calgary, Alberta, T2N 1N4, Canada Department of Natural Sciences, Western Oregon State University, Monmouth, OR 97360, USA Abstract Forty individually named ranges, plateaus, and massifs draining wholly or partly into the Great Basin of the western United States show de"nite evidence of Pleistocene glaciation. The most obvious deposits are a family of moraines designated, among other names, `Tiogaa, `Angel Lakea, and `Pinedalea. Such moraines generally can be traced from range to range away from described type moraines. These deposits have been numerically assigned to Late Wisconsinan glaciation in the Wasatch Range, White Mountains, Boulder Mountain, and Sierra Nevada on the basis of radiocarbon and surface-exposure ages, and have been assigned to Late Wisconsinan time in several other ranges on the basis of relative-age studies. The type Angel Lake moraine, and most other equivalent moraines across the Great Basin, are thick, hummocky, lobate piles of till rather than looping ridges. The thicknesses of the moraines (often 60#m) can be explained by heavy debris loads, and/or glacial advance, retreat, and readvance to the same positions a number of times, which is consistent with recent evidence that multiple Late Wisconsinan advances, possibly related to Heinrich and Dansgaard-Oeschger events, occurred in the Sierra Nevada. Pre-Angel Lake deposits occur in many Great Basin ranges, but it is currently di$cult or perhaps impossible to determine if these deposits are equivalent to each other and what their relationship is to pre-Tioga deposits in the Sierra Nevada.
    [Show full text]
  • A History of Tooele County, Utah Centennial County History Series
    A HISTORY OF Tooele County Compiled by Ouida Blanthorn UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF Tooek County Compiled by Ouida Blanthorn Tooele County is the second-largest county in the state, extending from the ridge line of the Oquirrh Mountains to the state line in the west across a broad portion of northwestern Utah. Human habitation extends back thou­ sands of years to the period of ancient Lake Bonneville. Tooele was one of the first six counties created in Utah and began to be settled as early as 1850 by Mormon pioneers, who made extensive use of the county's rich grazing and timber resources. Tooele County has been known in recent decades for its vast desert expanses, including Bonneville Salt Flats, its mineral resources from both the Great Salt Lake and area moun­ tain ranges, and its uses by the U.S. military for test ranges and various other facilities, including the storage and disposal of chemi­ cal and other weapons. Growth of the county has been rapid in recent years, due in part to its proximity to Salt Lake City, many residents using Tooele County towns as bedroom communities for the Wasatch Front. Controversy currently exists between such residents and those who would expand use of the county for industrial growth and waste disposal, including nuclear- waste repositories. ISBN: 0-913738-44-1 A HISTORY OF Tooele County A HISTORY OF Tooele County Compiled by Ouida Blanthorn 1998 Utah State Historical Society Tooele County Commission Copyright © 1998 by Tooele County Commission All rights reserved ISBN 0-913738-44-1 Library of Congress Catalog Card Number 98-61318 Map by Automated Geographic Reference Center—State of Utah Printed in the United States of America Utah State Historical Society 300 Rio Grande Salt Lake City, Utah 84101-1182 Contents GENERAL INTRODUCTION vii INTRODUCTION ix CHAPTER 1 The Geology and Geography of Tooele County 1 CHAPTER 2 Native Americans in Tooele County 33 CHAPTER 3 Trappers, Surveyors, and Wagon Trains: The Coming of Euro-Americans to Tooele County 45 CHAPTER 4 The Early Settlement of Tooele County ...
    [Show full text]