Kane County, Utah Resource Management Plan
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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. -
Scoping Report: Grand Staircase-Escalante National
CONTENTS 1 Introduction .............................................................................................................................................. 1 2 Scoping Process ....................................................................................................................................... 3 2.1 Purpose of Scoping ........................................................................................................................... 3 2.2 Scoping Outreach .............................................................................................................................. 3 2.2.1 Publication of the Notice of Intent ....................................................................................... 3 2.2.2 Other Outreach Methods ....................................................................................................... 3 2.3 Opportunities for Public Comment ................................................................................................ 3 2.4 Public Scoping Meetings .................................................................................................................. 4 2.5 Cooperating Agency Involvement ................................................................................................... 4 2.6 National Historic Preservation Act and Tribal Consultation ....................................................... 5 3 Submission Processing and Comment Coding .................................................................................... 5 -
Terrestrial Vertebrate Fauna of the Kaiparowits Basin
Great Basin Naturalist Volume 40 Number 4 Article 2 12-31-1980 Terrestrial vertebrate fauna of the Kaiparowits Basin N. Duane Atwood U.S. Forest Service, Provo, Utah Clyde L. Pritchett Brigham Young University Richard D. Porter U.S. Fish and Wildlife Service, Provo, Utah Benjamin W. Wood Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Atwood, N. Duane; Pritchett, Clyde L.; Porter, Richard D.; and Wood, Benjamin W. (1980) "Terrestrial vertebrate fauna of the Kaiparowits Basin," Great Basin Naturalist: Vol. 40 : No. 4 , Article 2. Available at: https://scholarsarchive.byu.edu/gbn/vol40/iss4/2 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]. TERRESTRIAL VERTEBRATE FAUNA OF THE KAIPAROWITS BASIN N. Diiane Atwood', Clyde L. Pritchctt', Richard D. Porter', and Benjamin W. Wood' .\bstr^ct.- This report inehides data collected during an investigation by Brighani Young University personnel to 1976, as well as a literature from 1971 review. The fauna of the Kaiparowits Basin is represented by 7 species of salamander, toads, mnphihians (1 5 and 1 tree frog), 29 species of reptiles (1 turtle, 16 lizards, and 12 snakes), 183 species of birds (plus 2 hypothetical), and 74 species of mammals. Geographic distribution of the various species within the basin are discussed. Birds are categorized according to their population and seasonal status. -
Bryce Canyon National Park
Lees Ferry, Arizona), White (which surround Utah Zion Canyon), Gray and Pink. Most of the Grand Staircase is now contained within the BLM-managed Grand Staircase - Escalante National Monument. The rocks that give Bryce Canyon its distinctive colors are members of the Claron Formation, a mixed Highlights limestone/sandstone layer, and are also found exposed, with similarly intricate forms, in other nearly locations such as Red Canyon and Cedar Breaks. Erosion: Water is responsible for creating the rock shapes in Bryce Canyon National Park. Rain and melting snow flowing down the Pink Cliffs towards the Paria River form ridges, or fins, which subsequently erode into the spires, pinnacles and other shapes (collectively known as ‘hoodoos’) which are left standing. In time these too erode, and the whole process moves very gradually westwards as more of the cliff is slowly worn away. During the long, cold winters, the cliffs are further weakened by freezing water Bryce Canyon National Park expanding in cracks, resulting in more erosion when the ice Bryce Canyon National Park does not contain one main thaws in spring. canyon, but rather a dozen smaller ravines eroded into the east side of a ridge running approximately north-south at Bryce Canyon Trails: As with most national parks, the best the edge of the Paunsaugunt Plateau in southwest Utah. This way to appreciate Bryce Canyon is to explore away from erosion has resulted in thousands of bizarre and fragile rock the main roads. There are various trails both along the rim formations, large and small, in many subtle shades of pink, and down through the formations, but probably the best white, yellow, orange and red, extending in quite a narrow is the Fairyland Loop Trail, an 8 mile, little-used route which band for over 25 miles along the plateau rim. -
Halls Crossing
National Park Service Glen Canyon National Recreation Area U.S. Department of the Interior Rainbow Bridge National Monument Vol. 10, No. 1, 2014 The official newspaper PHOTO: Bob Moffitt Discover Glen Canyon Welcome! only 13% of Glen Canyon National Recreation overlooks. For spectacular views of the canyon Area. The impounded waters offer unparalleled country, those with 4-wheel drive vehicles Glen Canyon National Recreation Area’s varied water-based recreational opportunities where can visit less accessible areas of the park like expanses of land and water offer more than you can boat, swim, fish, water ski, camp or Alstrom Point or the Burr Trail, which begins you may think. As a unit of the National Park take a boat tour to Rainbow Bridge or Antelope in Glen Canyon and continues into Capitol Reef Service, Glen Canyon preserves and protects Canyon. National Park. over 1.2 million acres for scenic, scientific, and recreational values. Glen Canyon’s vast acreage You may be surprised to know that almost half With such recreational diversity and so many can be divided into three prominent land and of the park is managed as a proposed wilderness places to discover, visitors are often inspired to water areas, each of which offers distinct types area, meaning there is minimal development and return for further exploration. Whether it’s by of experiences for visitors from around the visitors can enjoy a more remote experience. boat, car, or foot, we invite you to experience all globe. that Glen Canyon National Recreation Area has The remainder of the park offers areas that to offer. -
The Lost World of Glen Canyon
- r f 1 / I / I / r llS^ *&v . .".•*' : '•.-• - :•:-.*« •••• '•• i^g. i. A large sandstone arch called Galloway Cave existed on the right bank about 2.25 miles upstream from Glen Canyon Dam. River travelers camped here before the turn of the century and seemed always to build their campfires in the same place, at the downstream corner of the arch. Many also left a record of their presence by uniting their names on the wall with a piece of charcoal. This view shows a Nevills river party preparing for dinner on June 11, 1949. Lake Powell covers this site. Photographs, except Fig. 4, are courtesy of author. The Lost World of Glen Canyon BY P. T. REILLY THOUSANDS OF PEOPLE CRUISE THE SURFACE OF Lake Powell never dream ing of the wonders beneath the waters, features that are not likely to be exposed again in our lifetime, nor in those of our children or grandchildren. In fact, they may never be seen again. This photo graphic collection of landforms will serve as a reminder that our world changes as dramatically in the vertical as it does in the horizontal. Mr. Reilly lives in Sun City, Arizona. Readers may wish to refer to the following: Plan and Profile, Colorado River, Lees Ferry, Arizona, to Mouth of Green River, Utah, Sheet B; Navajo Mountain, Utah- Arizona quadrangle; Lake Canyon, Utah quadrangle; and Mancos Mesa, Utah quadrangle. The Lost World of Glen Canyon 123 Lee's Ferry occupies a unique and important position on the Colorado River because the 1921 measurement by the U.S. -
The Geography of Wildfire
Page 14 ZANE GREY EXPLORER AUGUST 2017 The Geography of Wildfire by Dr. Kevin Blake, Professor Emeritus of Geogrophy Kansas State U niversitY STfrR7- The geography of Wildfire ) 6rytz (1917\ is among the most sig- a, C"n.7on -, N nificant in all of Zane Grey's el Ct ,|r F wrld. western romances. lt weaves t/ l-'lors e _ -o1 I l4\. \' L lAeso together four places that 14,. fK.; por.*lls t) ' 'Pl*tequ) shaped Grey's vision of the West more than any oth- !; P /+) t\ er prior to 1917: Lees Ferry (Grey's fictional name is 1^1 Ko"oL Bostil's Ford), the Grand Canyon, Monument Valley, a ;,t u lo is the I and Wild Horse Mesa. Most importantly, this I menf v 3 €-7* book that launched Monument Valley to worldwide t t{ t:: I fame and thus greatly shaped the image of the Fr rd , ril { American West (Blake, 1995; Harvey, 2OLt). o *T"h;s ;: wh"r. , ln this article, I explain the geography of Wildfire by t 7*e flrc-'| s€'-'s /t ljri\'1 0 9, Aoc,umenf following the chronology of the book from Lees Ferry a-f. in a;tlqli*.;.,;"1- (Y _\i ;* iryated to the Grand Canyon, Monument Valley, and finally \ 2( O, 6Lopr oximale i" .65 mlles +o rlne is a story about a wild rP"wcll I I *si - Wild Horse Mesa. Though this I Piaiedu ? rprileqs*. greatest I horse named Wildfire, and is one of Grey's I I Tui.&1} I oo I a horse stories along with Riders of the Purple Soge 4 J 4. -
Energy and Mineral Resources, Grand Staircase
Circular 93 Utah Geological Survey Illustration Captions View figure: Circular 93 1., 2., 3., 4., 5., 6., 7., 8., 9., 10., 11., 12., 13., 14., 15. A Preliminary Assessment of Energy and Table of Contents 1.Preface Mineral Resources within the Grand 2.Summary 3.Introduction Staircase - Escalante National Monument 4.Geology 5.Kaiparowits Plateau coal Compiled by M. Lee Allison, State Geologist field 6.Oil and Gas Potential Contributors: 7.Tar-sand Resources Robert E. Blackett, Editor 8.Non-fuel Minerals and Thomas C. Chidsey Jr., Oil and Gas Mining David E. Tabet, Coal and Coal-Bed Gas 9.Acknowledgments Robert W. Gloyn, Minerals 10.References Charles E. Bishop, Tar-Sands January 1997 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES CONTENTS PREFACE SUMMARY INTRODUCTION Background Purpose and Scope GEOLOGY Regional Structure Permian through Jurassic Stratigraphy Cretaceous and Tertiary Stratigraphy THE KAIPAROWITS PLATEAU COAL FIELD History of Mining and Exploration Coal Resources Coal Resources on School and Institutional Trust Lands Sulfur Content of Kaiparowits Coal Coal-bed Gas Resources Further Coal Resource Assessments Needed OIL AND GAS POTENTIAL Source Rocks Potential Reservoirs Trapping Mechanisms Exploration and Development Carbon Dioxide Further Oil and Gas Resource Assessments Needed TAR-SAND RESOURCES OF THE CIRCLE CLIFFS AREA NON-FUEL MINERALS AND MINING Manganese Uranium-Vanadium Zirconium-Titanium Gold Copper, Lead and Zinc Industrial and Construction Materials Mining Activity Further Non-Fuel Mineral Resource Assessments Needed ACKNOWLEDGMENTS REFERENCES APPENDIX A: Presidential proclamation APPENDIX B: Summary of the coal resource of Kaiparowits Plateau and its value APPENDIX C: Summary of coal resources on School and Institutional Trust Lands APPENDIX D: Authorized Federal Oil and Gas Leases in the monument ILLUSTRATIONS Figure 1. -
Glen Canyon Unit, CRSP, Arizona and Utah
Contents Glen Canyon Unit ............................................................................................................................2 Project Location...................................................................................................................3 Historic Setting ....................................................................................................................4 Project Authorization .........................................................................................................8 Pre-Construction ................................................................................................................14 Construction.......................................................................................................................21 Project Benefits and Uses of Project Water.......................................................................31 Conclusion .........................................................................................................................36 Notes ..................................................................................................................................39 Bibliography ......................................................................................................................46 Index ..................................................................................................................................52 Glen Canyon Unit The Glen Canyon Unit, located along the Colorado River in north central -
Bryce Canyon National Park From: Utah Place Names
Bryce Canyon National Park from: Utah Place Names BRYCE CANYON NATIONAL PARK (Garfield County) has a north-northeast by south-southwest orientation and runs parallel to the Sevier River, East Fork. The canyon drainage goes into the Paria River. The spectacularly colorful Pink Cliffs, named by Major Powell's survey party at the center of the National Park, are the east escarpment of the Paunsaugunt Plateau. The Pink Cliffs have been sculptured by water, wind, and gravity into pinnacles, columns, cliffs, castles, and shapes of indescribable form and beauty. The park is not a canyon per se, but the edge of a plateau which can be enjoyed from above or from the depths below. The park was established in 1928 by President Hoover. See Bryce Canyon below for name source. BRYCE CANYON (Garfield County) originates in the center of Bryce Canyon National Park and continues east to the Paria River. It was named for Ebenezer Bryce, a pioneer cattleman who homesteaded there in the fall of 1875. Bibliography: Our Pioneer Heritage, 17 vols. Daughters of the Utah Pioneers. (v17). Creer, Leland Hargrave. The Founding of an Empire: The Exploration and Colonization of Utah, 1776 -1856. Salt Lake City: Bookcraft, 1947. Layton, Stanford J. "Fort Rawlins, Utah: A Question of Mission and Means." Utah Historical Quarterly 42 (Winter 1974): 68-83. Utah, A Guide to the State. Work Projects Administration. Comp. by Utah State Institute of Fine Arts, Salt Lake County Commission. New York: Hastings House, 1941. Woodbury, Angus Munn. A History of Southern Utah and Its National Parks. Salt Lake City: State Historical Society, 1950. -
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. -
Geologic Resource Evaluation Report, Bryce Canyon National Park
National Park Service U.S. Department of the Interior Natural Resource Program Center Bryce Canyon National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2005/002 Bryce Canyon National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2005/002 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2005 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly-published newsletters. Views and conclusions in this report are those of the authors and do not necessarily reflect policies of the National Park Service. Mention of trade names or commercial products does not constitute endorsement or recommendation for use by the National Park Service.