Mineral Deposits of the Deep Creek Mountains, Tooele and Juab Counties, Utah

Total Page:16

File Type:pdf, Size:1020Kb

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 Rocks ............... 5 Willow Springs Block ...................... 10 Goshute Canyon Formation ................. 5 Spring Creek Block . 11 Lower Cambrian Rocks ...................... 5 Ibapah Stock ............................ 11 Prospect Mountain Quartzite ................ 5 Alteration ................................ 11 Pioche Shale ........................... 5 Silicification .............................. 11 Busby Quartzite ......................... 5 Sericitization .............................. 12 Middle Cambrian Rocks ..................... 6 Si!ication ................................. 12 Abercrombie Formation ................... 6 Young Peak Dolomite ..................... 6 Ore Deposits ................................ 13 Trippe Limestone ........................ 6 General Character and Oassification of Deposits ...... 13 Lamb Dolomite ......................... 6 Pegmatite Dikes . ..... 13 Hicks Formation ........................ 6 Hydrothermal Veins ....................... 13 Upper Cambrian and Lower Ordovician Rocks ...... 6 Hypothermal Veins ..................... 13 Chokecherry Dolomite .................... 6 Mesothermal Veins ...................... 13 Lower Ordovician Rocks ..................... 6 Epithermal Veins ....................... 13 Pogo nip Group ......................... 6 Bedding Replacement Bodies ................... 13 Middle Ordovician Rocks ..................... 7 Contact Metasomatic Deposits ................ 13 Eureka Quartzite . 7 Controls of Mineralization ..................... 13 Upper Ordovician Rocks ..................... 7 Fracture Systems ......................... 14 Fish Haven Dolomite ..................... 7 Stratigraphic Controls ...................... 14 Middle Silurian Rocks ....................... 7 Igneous Relationships ...................... 14 Laketown Dolomite ...................... 7 Extrusive Relationships ..................... 17 Lower Devonian Rocks ...................... 7 Ore Body Zoning ......................... 17 Sevy Dolomite .......................... 7 Alteration of Mineral Deposits .................. 17 Middle Devonian Rocks ...................... 7 Alteration of Pegmatite Dikes ................ 17 Simonson Dolomite ...................... 7 Alteration of Hydrothermal Veins .............. 18 Guilmette Formation ..................... 7 Hypothermal Veins ..................... 18 Upper Mississippian Rocks .................... 7 Mesothermal Veins ...................... 18 Woodman Formation ..................... 7 Epithermal Veins ....................... 18 Ochre Mountain Limestone ................. 7 Alteration of Bedding Replacement Deposits ...... 18 Chainman Shale . 7 Alteration of Contact Metasomatic Deposits ....... 18 Upper Mississippian and Lower Genesis of Original Ore Deposits ................. 18 Pennsylvanian Rocks ..................... 7 Summary, Practical Applications and Manning Canyon Formation ................. 7 Future of the Area ........................ 19 Lower and Middle Pennsylvanian Rocks ........... 7 Ely Formation .......................... 7 Pennsylvanian and Permian Rocks ............... 7 Mines and Prospects ........................... 20 Oquirrh Formation ....................... 7 Sou them Oifton Area . 20 Lower Permian Rocks . 7 Monocco Property ........................ 20 Arcturus Formation ...................... 7 Prospects in Pony Express Canyon ............. 23 Tertiary Rocks ............................ 7 Iron Blowout ......................... 23 Salt Lake Group ........................ 7 Complex Property ...................... 23 Quaternary Sediments ....................... 8 Silver Queen Oaim . 23 Older Alluvium ......................... 8 Overland Canyon Properties .................. 23 Alluvium ............................. 8 Overland and Gold Star Oaims ............. 23 Igneous Rocks .............................. 8 Midland Qaims . 24 Intrusive Rocks ........................... 8 Cyclone and Leap Year Oaims .............. 25 Gold Hill Stock ......................... 8 Laura Claim .......................... 27 Ibapah Stock ........................... 8 Bonanza Group ........................ 27 ii CONTENTS (continued) Page Page Monte del Rey Property .................. 27 15. Geology and workings of the Midnight adit Fortuna Group ........................ 28 on the Midland property in Overland Canyon ...... 25 Proberts Property ....................... 28 16. Geology and workings of the 20Q-foot inclined Midas Property ........................ 28 adit on the Midland property in Overland Canyon ... 25 Utah Oaim ........................... 29 17. Geology and workings of the Cyclone mine Willow Spring Area .......................... 29 in Overland Canyon ........................ 26 Dewey Properties ......................... 29 18. Geology and workings of the Laura adit in North Pass Area .......................... 29 Overland Canyon ......................... 27 Congar Hill Property ....................... 31 19. Geology and workings of the Midas mine in Willow Springs Area . 31 Overland Canyon ......................... 29 Reilly-Goshute Canyons Area ................. 35 20. Geology and workings of the North Pass area ...... 30 Prosperity Property ..................... 3 7 21. Location of claims in the North Pass area ......... 31 Devils Pit-Oro del Rey-Eagles Nest Area ....... 37 22. Geologic map of the Congar Hill area ............ 31 Lower Goshute Canyon Property ............ 38 23. Geologic map and section of the Congar Hill mine ... 32 Silver Queen Property .................... 38 24. Geology and claims in the Willow Springs area, Production ........................... 40 Willow Springs district ...................... 33 Spring Creek Area .......................... 40 25. Geology and workings in plan and section Gold Bond Property ....................... 40 of the Roy mine, Willow Springs area ........... 34 Red Hill Mine ........................... 48 26. Geology and workings of mines in the Trout Creek Properties ..................... 50 Willow Springs area ........................ 36 Apex Property, Mary Oaim and Vicinity ....... 51 27. Diagrammatic geologic section showing Trout Creek Mine and Vicinity ............. 51 stratigraphic relations of mine workings Trout Creek Canyon Prospects .............. 51 in the Reilly-Goshute canyons area ............. 37 Hornet Mine, MacMillan Property and 28. Geology and workings of the Prosperity mine, Eastern Trout Creek Mine ................. 51 Reilly-Goshute canyons area .................. 39 Production ........................... 56 29. Geologic plan and section of the Eagles Nest inclined Singleton Canyon Area ..................... 57 shaft, Reilly-Goshute canyons area .............. 40 Heavenly Hills Prospects .................... 57 30. Geologic map and sample data of the Oro del Rey Water Canyon Mine ....................... 59 mine, Reilly-Goshute canyons area .............. 41 Johnson Canyon Properties .................. 62 31. Plan and section of the Oro del Rey mine, Queen of Sheba and Jumbo Properties .......... 66 Reilly-Goshute canyons area .................. 42 32. West-east geologic sections facing north of the References .................................. 70 Oro del Rey mine vein system ................ 43 33. Geology and workings in plan and section of the Appendix Devils Pit mines, Reilly-Goshute canyons area ...... 44 Logs of holes drilled by Western Beryllium Co. 34. Geology and workings of the Bueno mine, on the Apex Tungsten property ................... 73 Reilly-Goshute canyons area .................. 45 35. Geology and workings in plan and section of the lower Goshute Canyon mines, Reilly-Goshute canyons area ............................ 45 ILLUSTRATIONS 36. Geologic map of the Silver Queen area, Reilly-Goshute canyons area .................. 46 Figure 37. Geologic map of the Gold Bond property I. Index map of the location of the study area ........ 2 in Granite Canyon showing the location of 2. Stratigraphic section in the
Recommended publications
  • Description and Correlation of Geologic Units, Cross
    Plate 2 UTAH GEOLOGICAL SURVEY Utah Geological Survey Bulletin 135 a division of Hydrogeologic Studies and Groundwater Monitoring in Snake Valley and Utah Department of Natural Resources Adjacent Hydrographic Areas, West-Central Utah and East-Central Nevada DESCRIPTION OF GEOLOGIC UNITS SOURCES USED FOR MAP COMPILATION UNIT CORRELATION AND UNIT CORRELATION HYDROGEOLOGIC Alluvial deposits – Sand, silt, clay and gravel; variable thickness; Holocene. Qal MDs Lower Mississippian and Upper Devonian sedimentary rocks, undivided – Best, M.G., Toth, M.I., Kowallis, B.J., Willis, J.B., and Best, V.C., 1989, GEOLOGIC UNITS UNITS Shale; consists primarily of the Pilot Shale; thickness about 850 feet in Geologic map of the Northern White Rock Mountains-Hamlin Valley area, Confining Playa deposits – Silt, clay, and evaporites; deposited along the floor of active Utah, 300–400 feet in Nevada. Aquifers Qp Beaver County, Utah, and Lincoln County, Nevada: U.S. Geological Survey Units playa systems; variable thickness; Pleistocene through Holocene. Map I-1881, 1 pl., scale 1:50,000. D Devonian sedimentary rocks, undivided – Limestone, dolomite, shale, and Holocene Qal Qsm Qp Qea Qafy Spring and wetland related deposits – Clay, silt, and sand; variable thickness; sandstone; includes the Guilmette Formation, Simonson and Sevy Fritz, W.H., 1968, Geologic map and sections of the southern Cherry Creek and Qsm Quaternary Holocene. Dolomite, and portions of the Pilot Shale in Utah; thickness about 4400– northern Egan Ranges, White Pine County, Nevada: Nevada Bureau of QTcs 4700 feet in Utah, 2100–4350 feet in Nevada. Mines Map 35, scale 1:62,500. Pleistocene Qls Qlm Qlg Qgt Qafo QTs QTfs Qea Eolian deposits – Sand and silt; deposited along valley floor margins, includes Hintze, L.H., 1963, Geologic map of Utah southwest quarter, Utah Sate Land active and vegetated dunes; variable thickness; Pleistocene through S Silurian sedimentary rocks, undivided – Dolomite; consists primarily of the Board, scale 1:250,000.
    [Show full text]
  • 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
    [Show full text]
  • 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]
  • STATE of NEVADA Brian Sandoval, Governor
    STATE OF NEVADA Brian Sandoval, Governor DEPARTMENT OF WILDLIFE Tony Wasley, Director GAME DIVISION Brian F. Wakeling, Chief Mike Cox, Big Game Staff Biologist Pat Jackson, Carnivore Staff Biologist Cody McKee, Elk Staff Biologist Cody Schroeder, Mule Deer Staff Biologist Peregrine Wolff, Wildlife Health Specialist Western Region Southern Region Eastern Region Regional Supervisors Mike Scott Steve Kimble Tom Donham Big Game Biologists Chris Hampson Joe Bennett Travis Allen Carl Lackey Pat Cummings Clint Garrett Kyle Neill Cooper Munson Matt Jeffress Ed Partee Kari Huebner Jason Salisbury Jeremy Lutz Kody Menghini Tyler Nall Scott Roberts Cover photo credit: Mike Cox This publication will be made available in an alternative format upon request. Nevada Department of Wildlife receives funding through the Federal Aid in Wildlife Restoration. Federal Laws prohibit discrimination on the basis of race, color, national origin, age, sex, or disability. If you believe you’ve been discriminated against in any NDOW program, activity, or facility, please write to the following: Diversity Program Manager or Director U.S. Fish and Wildlife Service Nevada Department of Wildlife 4401 North Fairfax Drive, Mailstop: 7072-43 6980 Sierra Center Parkway, Suite 120 Arlington, VA 22203 Reno, Nevada 8911-2237 Individuals with hearing impairments may contact the Department via telecommunications device at our Headquarters at 775-688-1500 via a text telephone (TTY) telecommunications device by first calling the State of Nevada Relay Operator at 1-800-326-6868. NEVADA DEPARTMENT OF WILDLIFE 2017-2018 BIG GAME STATUS This program is supported by Federal financial assistance titled “Statewide Game Management” submitted to the U.S.
    [Show full text]
  • Kane County, Utah Resource Management Plan
    Kane County Resource Management Plan Adopted 28 November 2011 KANE COUNTY, UTAH RESOURCE MANAGEMENT PLAN For the Physical Development of the Unincorporated Area Pursuant to Section 17-27-301 of the Utah Code ADOPTED 28 NOVEMBER 2011 Should any part of the Kane County Resource Management Plan be determined invalid, no longer applicable or need modification, those changes shall affect only those parts of the Plan that are deleted, invalidated or modified and shall have no effect on the remainder of the Resource Management Plan. This document was prepared by the Division of Community and Economic Development of the Five County Association of Governments under the guidance and direction of the Kane County Resource Development Committee, Kane County Land Use Authority and the Board of County Commissioners. Funding used to prepare this document came from Kane County contributions, a Regional Planning grant from the Utah Permanent Community Impact Board and a Planning and Technical Assistance Grant from the U.S. Department of Commerce, Economic Development Administration. - 1 - Kane County Resource Management Plan Adopted 28 November 2011 Acknowledgments Every effective planning process includes a multitude of individuals if it is to be successful. This effort is no different. Many individuals have had an impact upon the preparation and adoption of this Plan. However, most important are the residents of Kane County, who have responded to surveys, interviews, and attended public meetings and hearings. All who did so should be commended for their desire to be a participant in determining the future of Kane County. Some specific individuals and groups have had intensive involvement in the Kane County planning process, and are acknowledged below: Kane County Commission Kane County Land Use Authority Doug Heaton, Chairman Shannon McBride, Land Use Administrator Dirk Clayson Tony Chelewski, Chairman Jim Matson Roger Chamberlain Wade Heaton Kane County Staff Robert Houston Verjean Caruso, Co.
    [Show full text]
  • MULE DEER Units 114-115
    Nevada Hunter Information Sheet MULE DEER Units 114-115 LOCATION: Eastern White Pine County – Snake Range. Please see unit descriptions in the Nevada Hunt Book. ELEVATION: From 5,100' in Snake Valley to 12,050' on Mount Moriah. TERRAIN: Gentle to extremely difficult. VEGETATION: Ranges from salt-desert shrub on some valley floors through sage and mixed brush, pinyon/juniper, mountain mahogany and aspen types at mid elevations to aspen/fir/spruce/limber pine/bristlecone pine at higher elevations. Mountainous areas support forest types more than brush, with pinyon and juniper dominating many areas between 6,500’ and 8,000’. Aspen is a minor component in both units. LAND STATUS: The majority of deer habitat is public land administered by either the BLM Ely Field Office or the Ely Ranger District of the Humboldt-Toiyabe National Forest (USFS). Hunting is not permitted on National Park Service lands (Great Basin National Park) located in Unit 115. Note: In 2006, Congress added 11,000 acres to the Mt. Moriah Wilderness in Unit 114 and created a new wilderness area (69,000 acres) on the south end of Unit 115. Vehicles and mechanized equipment, including wheeled game carriers are prohibited in wilderness areas. Contact the Federal Land Management Agency responsible for the area you intend to hunt for more information. Most private land is located on valley bottoms and benches. Private lands do not restrict access to public land. HUNTER ACCESS: Good to fair, based on weather and ground conditions. Access to Unit 114 can be impacted by winter storms. Motorized access is limited by existing roads, terrain and wilderness designations.
    [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]
  • Nevada Forest Insect and Disease Conditions, 2002-2003
    United States Department of Agriculture Forest Service Nevada State and Private Forestry Forest Insect and Disease Forest Health Protection Conditions Report Intermountain Region 2002 - 2003 R4-OFO-TR-04-13 State of Nevada Department of Conservation and Natural Resources Division of Forestry, Western Region Forest Health Specialists Forest Health Protection USDA Forest Service Darren Blackford, Entomologist Ogden Field Office Email: [email protected] Forest Health Protection 4746 S. 1900 E. Elizabeth Hebertson, Pathologist Ogden, UT 84403 Email: [email protected] Phone 801-476-9720 FAX 801-479-1477 John Guyon II, Pathologist Email: [email protected] Steve Munson, Group Leader Email: [email protected] Al Dymerski, Forest Technician Email: [email protected] Brytten Steed, Entomologist Email: [email protected] Valerie DeBlander, Forest Technician Email: [email protected] Division of Forestry State of Nevada State of Nevada Department of Conservation and Department of Conservation and Natural Resources Natural Resources Division of Forestry Division of Forestry Western Region Headquarters 2525 S. Carson Street 885 Eastlake Blvd. Carson City, NV 89701 Carson City, NV 89704 FAX 775-849-2391 Gail Durham, Forest Health Specialist Email:[email protected] John Christopherson, Resource Phone: 775-684-2513 Management Officer Email: [email protected] Rich Harvey, Resource Program Phone: 775-849-2500 ext. 243 Coordinator Email: [email protected] Phone: 775-684-2507 NEVADA FOREST INSECT AND DISEASE CONDITIONS 2002 - 2003 Compiled by: L.Pederson V.Deblander S.Munson L. Hebertson J. Guyon, II K. Matthews P. Mocettini G. Durham T. Johnson D. Halsey A.Dymerski July 2004 Table of Contents Forest Health Conditions Summary................................................................................1 Table 1.
    [Show full text]
  • Methods in Historical Ecology: a Case Study of Tintic Valley, Utah
    This file was created by scanning the printed publication. Errors identified by the software have been corrected; however, some errors may remain. Methods in Historical Ecology: A Case Study of Tintic Valley, Utah Jeffrey A. Creque Neil E. West James P. Dobrowolski Abstract-Through use of repeat photography, archival research, changes in the Tintic landscape over time. The results of and field observation to reconstruct landscape vegetation patterns this study support the view that historical ecological stud­ and changes across a 120 year period in the upper Tintic Valley of ies must employ a range of overlapping methodologies to central Utah, researchers found significant changes in landscape accurately interpret the nature and direction of landscape vegetation pattern over time, including change in pinyon-juniper change. woodland area. Previously reported massive woodland harvest associated with early mining, domestic and agricultural activities Materials and Methods elsewhere in the Intermountain West also took place in Utah. The ----------------- impact on woodland area of the agricultural "bull" fence alone Archival Research was significant. More recent study area woodland expansion also occurred. Because intensive industrial activity associated with This study included an intensive survey of archival mate­ development of the Tintic Mining District occurred prior to the rials for references to Tintic Valley vegetation, records of ore, taking of the study's 1911 photographs, those photos failed to fuelwood and charcoal production, smelting and milling reflect presettlement, or even early settlement, vegetation condi­ activities, and human population in the Valley in the era of tions. Overall, results suggest that historical ecological studies biomass fuels. From this information, estimates of early must employ a range of overlapping methodologies to accurately settlement era (1870-1900) industrial, agricultural, and interpret the nature and direction oflandscape vegetation change.
    [Show full text]
  • Nevada Department of Wildlife Wildlife Heritage Program Project
    Nevada Department of Wildlife Wildlife Heritage Program Project Summaries and State Fiscal Year 2022 Proposals Table of Contents Page Section 1: Summaries of Recently Completed 1-1 and Active Wildlife Heritage Projects Summary Table: Recently Completed and Active 1-2 Wildlife Heritage Projects Project Summaries 1-5 to 1-22 2-1 Section 2: Wildlife Heritage Proposals Submitted for State Fiscal Year 2022 Funding 2-2 Summary Table: Wildlife Heritage Proposals Submitted for FY22 Funding FY22 Proposals (proposal numbers from the 2-5 to 2-193 summary table are found on the upper right corner of each proposal page) Section 1: Summaries of Recently Completed and Active Wildlife Heritage Projects This section provides brief summaries of Wildlife Heritage projects that were recently completed during State Fiscal Year (FY) 2020 and 2021. It also includes brief status reports for projects that were still active as of April 10, 2021. The table on the following pages summarizes key characteristics about each of the projects that are addressed in this section. The financial status of these projects will be updated in early June and in time to be included in the support material for the June Wildlife Heritage Committee Meeting and the Board of Commissioners meeting. 1-1 Recently Completed and Active Wildlife Heritage Projects (active projects and those completed during FY20 and 21; expenditure data is according to DAWN as of April 10, 2021) Heritage Project Heritage Award Dollars Spent as Number Name of Heritage Project Project Manager Amount of April
    [Show full text]
  • 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).
    [Show full text]
  • 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 .
    [Show full text]