Methods in Historical Ecology: a Case Study of Tintic Valley, Utah
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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 -
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 -
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 -
Petrogenesis of the Oligocene East Tintic
PETROGENESIS OF THE OLIGOCENE EAST TINTIC VOLCbyANIC FIELD, UTAH Daniel K. Moore1, Jeffrey D. Keith2, Eric H. Christiansen2, Choon-Sik Kim3, David G. Tingey2, Stephen T. Nelson2, and Douglas S. Flamm2 ABSTRACT The early Oligocene East Tintic volcanic field of central Utah, located near the eastern margin of the Basin and Range Province, consists of mafic to silicic volcanic (mostly intermediate-composition lava flows) and shallow intrusive rocks associated with the formation of small, nested calderas. Radiometric ages establish a minimum age for initiation (34.94 ± 0.10 Ma) and cessation (32.70 ± 0.28 Ma) of East Tintic magmatism. The igneous rocks of the field are calc-alkalic, potassic, silica-oversaturated, and met- aluminous, and can be categorized into the following three compositional groups: the shoshonite-trachyte series, the trachyandesite series, and the rhyolite series. Based on composition and phenocryst assemblage, the shoshonite-trachyte series is divided into two groups: a clinopyroxene group and a two-pyroxene group. The rhyolite series consists of three field units: the Packard Quartz Latite, the Fernow Quartz Latite, and the rhyolite of Keystone Springs. The trachyandesite series is by far the most voluminous. This series is also subdivided into a clinopyroxene group and a two-pyroxene group. Temperature and oxygen fugacity estimates indicate that shoshonite-trachyte series magmas were the hottest and least oxidizing and that two-pyroxene trachyandesite series magmas were the coolest and most oxidizing. Clinopyroxene shoshonite-trachyte series magma evolved mainly by fractional crystallization. The high K2O, Rb, and Al2O3/CaO ratios and modest SiO2 enrichment of these rocks appear to result from extensive, high-pressure fractional crystallization of clinopyroxene (without plagioclase). -
Geology of the North Canyon Area, Southern Wasatch Mountains, Utah
NmG UNIVERSITY RESEARCH STUDIES Geology Series Vol. 3 No. 7 July, 1956 GEOLOGY OF THE NORTH CANYON AREA, SOUTHERN WASATCH MOUNTAINS, UTAH by Cleon V. Smith Brigham Young University Departmerit of Geology Pmvo, Utah GEOLOGY OF THE NORTH CANYON AREA, SOUTHERN WASATCH MOUNTAINS, UTAH A thesis submitted to the Faculty of the Department of Geology Br igham Young Univer s ity in partial fulfillment of the requirements for the degree Master of Science by Cleon V. Smith August, 1956 ACKNOWLEDGEMENTS 1' - The writer gratefully acknowledges the assistance of Dr, Harold J. Bissell for help in field work and checking the manuscript, Dr. George H. Hansen for applying ground water information and well logs and Professor Jess R. Bushman for checking the writer's manuscript. The writer is indebted to Dell R. Foutz, for his help in field work and to his brother, Grant B. Smith, for field assistance, The writer expresses sincere appreciation to his wife, Meridee, for her encouragement and cooperation. iii TABLE OF CONTENTS Page ACKNOWLEDGEMENTS . iii LIST OF ILLUSTRATIONS . vi ABSTRACT. .. vii Location and accessibility . 1 Physical features - 1 Field work and laboratory studies . 2 Previous work. 2 GENERAL GEOLOGY Principal features . 3 Sedimentary Rocks . 6 Precambrian System . 6 Big Cottonwood series . 6 Cambrian System. Tintic quartzite . Ophir formation . Teutonic limestone . Dagmar limestone . Herkimer lime stone . Bluebird dolomite . Cole Canyon dolomite . Opex dolomite . Ordovician System 14 Ajax limestone (?) 14 Unconformity at Base of Mississippian . 15 Mississippian System . 15 Gardner dolomite . 15 Pine Canyon limestone . 17 Humbug formatign 19 Quaternary System 19 Landslides . 19 Fans - 19 Alluvium . 21 Igneous Rocks . -
National Register of Historic Places Inventory -- Nomination Form
Form No. 10-300 \Q-'*] UNITED STATES TERIOR NATIONAL PARK SERVICE NATIONAL REGISTER OF HISTORIC PLACES INVENTORY -- NOMINATION FORM SEE INSTRUCTIONS IN HOWTO COMPLETE NATIONAL REGISTER FORMS TYPE ALL ENTRIES -- COMPLETE APPLICABLE SECTIONS NAME HISTORIC RESOURCES OF THE TINTIC MINING DISTRICT (Partial HISTORIC Inventory: Historic and Architectural Properties) AND/OR COMMON LOCATION (A 5 #/ STREET & NUMBER See Item No. 10 —NOT FOR PUBLICATION I CITY. TOWN CONGRESSIONAL DISTRICT * ' __ VICINITY OF STATE CODE /"' GPUNTY CODE i Utah 049 ( <a&v«j w- Utah\Juab 023-049 DCLA SSIFIC ATI ON CATEGORY OWNERSHIP STATUS PRESENT USE —DISTRICT —PUBLIC .^OCCUPIED X-AGRICULTURE —MUSEUM _BUILDING(S) —PRIVATE -XUNOCCUPIED 3LCOMMERCIAL —PARK —STRUCTURE .XBOTH XWORK IN PROGRESS —EDUCATIONAL X_PRIVATE RESIDENCE —SITE PUBLIC ACQUISITION ACCESSIBLE —ENTERTAINMENT —RELIGIOUS —OBJECT _IN PROCESS JCYES: RESTRICTED —GOVERNMENT —SCIENTIFIC X Multiple —BEING CONSIDERED -XYES: UNRESTRICTED ^-INDUSTRIAL —TRANSPORTATION Resource _NO —MILITARY XOTHER: multiple OWNER OF PROPERTY NAME Multiple Ownership STREET & NUMBER CITY, TOWN STATE __ VICINITY OF Utah 0LOCATION OF LEGAL DESCRIPTION COURTHOUSE. REGISTRY OF DEEDs;ETc. juab County Courthouse STREET & NUMBER Main Street CITY. TOWN STATE Nephi Utah O REPRESENTATION IN EXISTING SURVEYS ; TITLE Utah Historic Sites Survey DATE June, 1977 FEDERAL XSTATE COUNTY LOCAL DEPOSITORY FOR SURVEY RECORDS ^3^ state Historical Society CITY, TOWN STATE Salt Lake City Utah CONDITION CHECK ONE CHECK ONE —EXCELLENT —DETERIORATED —UNALTERED ^.ORIGINAL SITE -XGOOD —RUINS ^ALTERED —MOVED DATE_______ _FAIR ^ _UNEXPOSED DESCRIBE THE PRESENT AND ORIGINAL (IF KNOWN) PHYSICAL APPEARANCE The Tintic Mining District, as delineated for this nomination, comprises an area approximately eight miles square and includes the Main and East Tintic areas, since these areas were the most significant and contain all of the historical resources. -
Manual of the Flora of the East Tintic Mountains, Utah
Brigham Young University BYU ScholarsArchive Theses and Dissertations 1975-04-01 Manual of the flora of the east Tintic Mountains, Utah Glen T. Nebeker Brigham Young University - Provo Follow this and additional works at: https://scholarsarchive.byu.edu/etd BYU ScholarsArchive Citation Nebeker, Glen T., "Manual of the flora of the east Tintic Mountains, Utah" (1975). Theses and Dissertations. 8097. https://scholarsarchive.byu.edu/etd/8097 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. MANUALOF THE FLORAOF THE EAST TINTIC MOUNTAINS,UTAH A Thesis Presented to the Department of Botany Brigham Young University In Partial Fulfillment of the Requirements for the Degree Master of Science by Glen T. Nebeker April 1975 TABLEOF CONTENTS Page ACKNOWLEDGEMENTS iii INTRODUCTION. • 1 TAXONOMICTREATMENT 3 Pteridophyta 9 Gymnospermae 9 Dicotyledoneae • 10 Monocotyledoneae 47 SUMMARY 55 BIBLIOGRAPHY. , . 56 i This thesis, by Glen T. Nebeker, is accepted in its present form by the Department of Botany of Brigha Young University as satisfying the thesis requirement for the degree of Master of Science. ii ACKNOWLEDGEMENTS The author wishes to express gratitude to all those who have helped to make this work possible. The author would like to thank Dr. S. L. Welsh of Brigham Young University for his guidance in the selection of the study, counsel and aid in the identification of plant specimens. The author would like to thank Kennecott Copper Corporation, Tintic Division for permission to collect on their property. -
Nature and Origin of the East Traverse Mountains Mega-Landslide, Northern Utah (USA)" (2020)
Brigham Young University BYU ScholarsArchive Theses and Dissertations 2020-12-11 Nature and Origin of the East Traverse Mountains Mega- Landslide, Northern Utah (USA) Rodney Ryan Chadburn Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Physical Sciences and Mathematics Commons BYU ScholarsArchive Citation Chadburn, Rodney Ryan, "Nature and Origin of the East Traverse Mountains Mega-Landslide, Northern Utah (USA)" (2020). Theses and Dissertations. 8771. https://scholarsarchive.byu.edu/etd/8771 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Nature and Origin of the East Traverse Mountains Mega-Landslide, Northern Utah (USA) Rodney Ryan Chadburn A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science Jeffrey D. Keith, Chair Eric H. Christiansen Ron A. Harris Department of Geological Sciences Brigham Young University Copyright © 2020 Rodney Ryan Chadburn All Rights Reserved ABSTRACT Nature and Origin of the East Traverse Mountains Mega-Landslide, Northern Utah (USA) Rodney Ryan Chadburn Department of Geological Sciences, BYU Master of Science The East Traverse Mountains are an E-W trending mountain range dividing Utah and Salt Lake valleys in northern Utah. Geologically perplexing, the nature of the East Traverse Mountains has been under investigation for 140 years. Previously, the mountain range was proposed to be a dismembered but still coherent down-faulted block that experienced 4 km of post-thrusting extension within the Charleston-Nebo thrust sheet. -
Tooele I°X2° Quadrangle, Northwest Utah a CUSMAP Preassessment Study by Holly J
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Tooele I°x2° Quadrangle, Northwest Utah A CUSMAP Preassessment Study by Holly J. Stein1, Viki Bankey1, Charles G. Cunningham2, David R. Zimbelman1, David W. Brickey2* Michael Shubat3, David L. Campbell1, and Mel H. Podwysocki2 Prepared in cooperation with Utah Geological and Mineral Survey Open-File Report 89-0467 1989 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. ^.S. Geological Survey ^Jtah Geological and Mineral Survey Denver, Colorado 606 Black Hawk Way Salt Lake City, UT 84108-1280 2U.S. Geological Survey Reston, Virginia *Now at: EG&G Energy Measurements, Inc. P.O. Box 1912 M.S. H-02 Las Vegas, NV 89125 TABLE OF CONTENTS Page PREFACE.......................................................... 7 SUMMARY.......................................................... 8 INTRODUCTION..................................................... 12 Scientific Gains............................................ 12 Industrial Profits.......................................... 13 Benefits to Other Agencies.................................. 13 GEOLOGY AND THE FORMATION OF MINERAL DEPOSITS.................... 15 The Oquirrh-Uinta Mineral Belt.............................. 15 Rock Types: Age, Structural History, and Relation to Ore Deposits.................................. 18 Precambrian Rocks...................................... 18 Mesozoic Plutons....................................... 22 Eocene and -
Utah's Natural Resources
UTAH’S NATURAL RESOURCES203 8 The state of Utah is endowed with an abundance of natural resources. It contains significant supplies of oil, natural gas, coal, uranium, and oil shale and oil sands; base metals such as copper, beryllium, magnesium and molybdenum; and industrial minerals such as potash, salt, magnesium chloride and gilsonite. Renewable resources in Utah include geothermal, wind and solar energy and timber. As of 2012 proved reserves of oil and natural gas in Utah stood at 613 million barrels of crude oil, 7.8 trillion cubic feet of natural gas, and 268 million barrels of natural gas liquids. As of 2013 there were an estimated 14.9 billion tons of recoverable coal remaining in the state. In addition, Utah hosts an estimated 1.3 trillion barrels of oil contained in the oil shale of the Green River Formation in the Uinta Basin (Johnson et al. 2010). Of this, approximately 77 billion barrels could be considered as a potential economic resource (Vanden Berg 2008). Total energy production in 2013 was valued at $5.2 billion, including almost $3.0 billion from crude oil production, $1.7 billion from natural gas production, and nearly $0.6 billion from coal production. In addition, $423.6 million of natural gas liquids were produced. Nonfuel mineral production was valued at $3.7 billion in 2012, including $2.1 billion from base metal production, $1.2 billion from industrial mineral production, and $0.4 billion from precious metal production. In 2012, copper was the largest contributor to the value of nonfuel minerals in Utah, having an estimated value of $1.4 billion, mostly produced from Rio Tinto’s Bingham Canyon mine. -
Geology of Lake Mountain Utah
~------------------------------------------------------------------------, : UTAH GEOLOGICAL AND MINERALOGICAL SURVEY • • • AFFILIATED WITH ,• : THE COLLEGE OF MINES AND MINERAL INDUSTRIES UNIVERSITY OF UTAH SALT LAKE CITY, UTAH GEOLOGY OF LAKE MOUNTAIN, UTAH BY KENNETH C. BULLOCK Bulletin 41 June, 1951 Price $1.00 ~.--.. -.-------.. --------------------------------------------------------,~ 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 Departement 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 194-3, Vol. 2, Title 34, as amended by chapter 46 Laws of 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 terials, their kind and availability; and the promotion of the marketing of the mineral products of the State. 3. "The investigation of the kind, amount, and availability of the various mineral substances contained in State lands, with a view of the most effective and profitable administration of such lands for the State. -
Preliminary Reuse Investigation Eureka Mills Superfund Site
PRELIMINARY REUSE INVESTIGATION EUREKA MILLS SUPERFUND SITE Prepared by E2 Inc. November 2003 Funded by US EPA Abandoned Mine Lands Team PROJECT SCOPE US EPA’s Abandoned Mine Lands Team (AMLT) is committed to developing creative solutions to the problems posed by the large number of abandoned mine lands across the United States. In September 2003, the AMLT asked the consulting firm E² Inc. to perform a prelimi nary assessment of reuse planning opportunities at the Eureka Mills NPL site in Eureka, Utah. This report summarizes E² Inc.’s preliminary findings, based on the firm’s background research and a site visit on October 14th and 15th, 2003. The City of Eureka faces many of the same challenges encountered by other small, rural mining communities. In addition to the site’s contamination and remediation, the community must deal with a near complete erosion of its economic base. The lack of a primary employer, along with an eroded tax base, creates a serious stress on the local government’s ability to provide basic services, like zoning code enforcement and infrastructure improvements. In addition, the community lacks an array of basic private-sector services (i.e., a grocery store, pharmacy, doctor’s office). While Eureka faces substantial challenges, there are a number of existing local assets that can serve as the basis for revitalizing the economy and preserving the community’s future. Residents in Eureka cherish the high quality of life that they have come to enjoy in the community. This love of community, combined with the area’s natural beauty, nearby recreation opportunities, and the region’s mining heritage, can provide the framework for the restoration of Eureka’s economic vitality.