Basic Seismological Characterization for Sublette County, Wyoming By
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Page 5 of the 2020 Antelope, Deer and Elk Regulations
WYOMING GAME AND FISH COMMISSION Antelope, 2020 Deer and Elk Hunting Regulations Don't forget your conservation stamp Hunters and anglers must purchase a conservation stamp to hunt and fish in Wyoming. (See page 6) See page 18 for more information. wgfd.wyo.gov Wyoming Hunting Regulations | 1 CONTENTS Access on Lands Enrolled in the Department’s Walk-in Areas Elk or Hunter Management Areas .................................................... 4 Hunt area map ............................................................................. 46 Access Yes Program .......................................................................... 4 Hunting seasons .......................................................................... 47 Age Restrictions ................................................................................. 4 Characteristics ............................................................................. 47 Antelope Special archery seasons.............................................................. 57 Hunt area map ..............................................................................12 Disabled hunter season extension.............................................. 57 Hunting seasons ...........................................................................13 Elk Special Management Permit ................................................. 57 Characteristics ..............................................................................13 Youth elk hunters........................................................................ -
Seismicity, Seismotectonics and Preliminary Earthquake Hazard Analysis of the Teton Region, WY
FINAL TECHNICAL REPORT DEVELOPMENT OF EARTHQUAKE GROUND SHAKING HAZARD MAPS FOR THE YELLOWSTONE- JACKSON HOLE-STAR VALLEY, WYOMING Submitted to the U.S. Geological Survey Under the National Earthquake Hazards Reduction Program Program Element II Evaluate Urban Hazard and Risk USGS Award 05HQGR0026 Prepared by Bonnie Jean Pickering White Department of Geology and Geophysics The University of Utah Salt Lake City, UT 94112 and Robert B. Smith Department of Geology and Geophysics The University of Utah Salt Lake City, UT 94112 Principal Investigator Ivan Wong Seismic Hazards Group URS Corporation 1333 Broadway, Suite 800, Oakland, CA 94612 Phone: (510) 874-3014, Fax: (510) 874-3268 E-mail: [email protected] 26 September 2006 __________________________ This research was supported by the U. S. Geological Survey (USGS), Department of the Interior, under USGS Award Number 05HQGR0026. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied of the U.S. Government. PREFACE The Yellowstone-Jackson Hole-Star Valley corridor is located within the seismically and tectonically active Intermountain Seismic Belt in westernmost Wyoming and eastern Idaho. The corridor has the highest seismic hazard in the Intermountain U.S. based on the U.S. Geological Survey’s National Hazard Maps. The region contains the heavily visited Yellowstone and Teton National Parks and the rapidly growing areas of Jackson Hole and Star Valley. Although there has only been one large earthquake in this region in historical times (1959 moment magnitude [M] 7.5 Hebgen Lake), abundant geologic evidence exists for the past occurrence of surface-faulting earthquakes of M 7 or greater. -
Related Magmatism in the Upper Wind River Basin, Wyoming (USA), GEOSPHERE; V
Research Paper THEMED ISSUE: Cenozoic Tectonics, Magmatism, and Stratigraphy of the Snake River Plain–Yellowstone Region and Adjacent Areas GEOSPHERE The leading wisps of Yellowstone: Post–ca. 5 Ma extension- related magmatism in the upper Wind River Basin, Wyoming (USA), GEOSPHERE; v. 14, no. 1 associated with the Yellowstone hotspot tectonic parabola doi:10.1130/GES01553.1 Matthew E. Brueseke1, Anna C. Downey1, Zachary C. Dodd1, William K. Hart2, Dave C. Adams3, and Jeff A. Benowitz4 12 figures; 2 tables; 1 supplemental file 1Department of Geology, Kansas State University, 108 Thompson Hall, Manhattan, Kansas 66506, USA 2Department of Geology and Environmental Earth Science, Miami University, 118C Shideler Hall, Oxford, Ohio 45056, USA 3Box 155, Teton Village, Wyoming 83025, USA CORRESPONDENCE: brueseke@ ksu .edu 4Geophysical Institute and Geochronology Laboratory, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA CITATION: Brueseke, M.E., Downey, A.C., Dodd, Z.C., Hart, W.K., Adams, D.C., and Benowitz, J.A., 2018, The leading wisps of Yellowstone: Post–ca. 5 Ma ABSTRACT the issue of linking volcanic events to a specific driving mechanism (Fouch, extension-related magmatism in the upper Wind River 2012; Kuehn et al., 2015). Complicating matters, magmatism often continues Basin, Wyoming (USA), associated with the Yellow- The upper Wind River Basin in northwest Wyoming (USA) is located ~80– long after (e.g., millions of years) the upper plate has been translated away stone hotspot tectonic parabola: Geosphere, v. 14, no. 1, p. 74–94, doi:10.1130/GES01553.1. 100 km southeast of the Yellowstone Plateau volcanic field. While the upper from an upwelling plume (Bercovici and Mahoney, 1994; Sleep, 2003; Shervais Wind River Basin is a manifestation of primarily Cretaceous to Eocene Lara- and Hanan, 2008; Jean et al., 2014). -
Systematic Variation of Late Pleistocene Fault Scarp Height in the Teton Range, Wyoming, USA: Variable Fault Slip Rates Or Variable GEOSPHERE; V
Research Paper THEMED ISSUE: Cenozoic Tectonics, Magmatism, and Stratigraphy of the Snake River Plain–Yellowstone Region and Adjacent Areas GEOSPHERE Systematic variation of Late Pleistocene fault scarp height in the Teton Range, Wyoming, USA: Variable fault slip rates or variable GEOSPHERE; v. 13, no. 2 landform ages? doi:10.1130/GES01320.1 Glenn D. Thackray and Amie E. Staley* 8 figures; 1 supplemental file Department of Geosciences, Idaho State University, 921 South 8th Avenue, Pocatello, Idaho 83209, USA CORRESPONDENCE: thacglen@ isu .edu ABSTRACT ously and repeatedly to climate shifts in multiple valleys, they create multi CITATION: Thackray, G.D., and Staley, A.E., 2017, ple isochronous markers for evaluation of spatial and temporal variation of Systematic variation of Late Pleistocene fault scarp height in the Teton Range, Wyoming, USA: Variable Fault scarps of strongly varying height cut glacial and alluvial sequences fault motion (Gillespie and Molnar, 1995; McCalpin, 1996; Howle et al., 2012; fault slip rates or variable landform ages?: Geosphere, mantling the faulted front of the Teton Range (western USA). Scarp heights Thackray et al., 2013). v. 13, no. 2, p. 287–300, doi:10.1130/GES01320.1. vary from 11.2 to 37.6 m and are systematically higher on geomorphically older In some cases, faults of known slip rate can also be used to evaluate ages landforms. Fault scarps cutting a deglacial surface, known from cosmogenic of glacial and alluvial sequences. However, this process is hampered by spatial Received 26 January 2016 Revision received 22 November 2016 radionuclide exposure dating to immediately postdate 14.7 ± 1.1 ka, average and temporal variability of offset along individual faults and fault segments Accepted 13 January 2017 12.0 m in height, and yield an average postglacial offset rate of 0.82 ± 0.13 (e.g., Z. -
Wilderness Study Areas
I ___- .-ll..l .“..l..““l.--..- I. _.^.___” _^.__.._._ - ._____.-.-.. ------ FEDERAL LAND M.ANAGEMENT Status and Uses of Wilderness Study Areas I 150156 RESTRICTED--Not to be released outside the General Accounting Wice unless specifically approved by the Office of Congressional Relations. ssBO4’8 RELEASED ---- ---. - (;Ao/li:( ‘I:I)-!L~-l~~lL - United States General Accounting OfTice GAO Washington, D.C. 20548 Resources, Community, and Economic Development Division B-262989 September 23,1993 The Honorable Bruce F. Vento Chairman, Subcommittee on National Parks, Forests, and Public Lands Committee on Natural Resources House of Representatives Dear Mr. Chairman: Concerned about alleged degradation of areas being considered for possible inclusion in the National Wilderness Preservation System (wilderness study areas), you requested that we provide you with information on the types and effects of activities in these study areas. As agreed with your office, we gathered information on areas managed by two agencies: the Department of the Interior’s Bureau of Land Management (BLN) and the Department of Agriculture’s Forest Service. Specifically, this report provides information on (1) legislative guidance and the agency policies governing wilderness study area management, (2) the various activities and uses occurring in the agencies’ study areas, (3) the ways these activities and uses affect the areas, and (4) agency actions to monitor and restrict these uses and to repair damage resulting from them. Appendixes I and II provide data on the number, acreage, and locations of wilderness study areas managed by BLM and the Forest Service, as well as data on the types of uses occurring in the areas. -
Mineral Resources of the Ferris Mountains Wilderness Study Area, Carbon County, Wyoming
Mineral Resources of the Ferris Mountains Wilderness Study Area, Carbon County, Wyoming &£ %r^ U.S. GEOLOGICAL SURVEY BULLETIN 1757-C .r WYOMING Chapter C Mineral Resources of the Ferris Mountains Wilderness Study Area, Carbon County, Wyoming By MITCHELL W. REYNOLDS U.S. Geological Survey JOHN T. NEUBERT U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1757 MINERAL RESOURCES OF WILDERNESS STUDY AREAS- SOUTHERN WYOMING DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U. S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1988 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Reynolds, Mitchell W. Mineral resources of the Ferris Mountains Wilderness Study Area, Carbon County, Wyoming. (Mineral resources of wilderness study areas southern Wyoming ; ch. C) (U.S. Geological Survey bulletin ; 1757-C) Bibliography: p. Supt. of Docs, no.: I 19.3:1757-C 1. Mines and mineral resources Wyoming Ferris Mountains Wilderness. 2. Ferris Mountains Wilderness (Wyo.) I. Neubert, John T. II. Series. III. Series: U.S. Geological Survey bulletin ; 1757-C. QE75.B9 no. 1757-C 557.3 s [553'.09787'86] 87-600485 [TN24.W8] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine the mineral values, if any, that may be present. Results must be made available to the public and be submitted to the President and the Congress. -
Water Development Office 6920 YELLOWTAIL ROAD TELEPHONE: (307) 777-7626 CHEYENNE, WY 82002 FAX: (307) 777-6819 TECHNICAL MEMORANDUM
THE STATE OF WYOMING Water Development Office 6920 YELLOWTAIL ROAD TELEPHONE: (307) 777-7626 CHEYENNE, WY 82002 FAX: (307) 777-6819 TECHNICAL MEMORANDUM TO: Water Development Commission DATE: December 13, 2013 FROM: Keith E. Clarey, P.G. REFERENCE: Snake/Salt River Basin Plan Update, 2012 SUBJECT: Available Groundwater Determination – Tab XI (2012) Contents 1.0 Introduction .............................................................................................................................. 1 2.0 Hydrogeology .......................................................................................................................... 4 3.0 Groundwater Development .................................................................................................... 15 4.0 Groundwater Quality ............................................................................................................. 21 5.0 Geothermal Resources ........................................................................................................... 22 6.0 Groundwater Availability ...................................................................................................... 22 References ..................................................................................................................................... 23 Appendix A: Figures and Table ....................................................................................................... i 1.0 Introduction This 2013 Technical Memorandum is an update of the September 10, 2003, -
Landsat Evaluation of Trumpeter Swan Historical Nesting Sites In
Eastern Kentucky University Encompass Online Theses and Dissertations Student Scholarship 2014 Landsat Evaluation Of Trumpeter Swan Historical Nesting Sites In Yellowstone National Park Laura Elizabeth Cockrell Eastern Kentucky University, [email protected] Follow this and additional works at: https://encompass.eku.edu/etd Part of the Ecology and Evolutionary Biology Commons, and the Ornithology Commons Recommended Citation Cockrell, Laura Elizabeth, "Landsat Evaluation Of Trumpeter Swan Historical Nesting Sites In Yellowstone National Park" (2014). Online Theses and Dissertations. 222. https://encompass.eku.edu/etd/222 This Open Access Thesis is brought to you for free and open access by the Student Scholarship at Encompass. It has been accepted for inclusion in Online Theses and Dissertations by an authorized administrator of Encompass. For more information, please contact [email protected]. LANDSAT EVALUATION OF TRUMPETER SWAN HISTORICAL NESTING SITES IN YELLOWSTONE NATIONAL PARK By Laura Elizabeth Cockrell Bachelor of Science California State University, Chico Chico, California 2007 Submitted to the Faculty of the Graduate School of Eastern Kentucky University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE May, 2014 Copyright © Laura Elizabeth Cockrell, 2014 All rights reserved ii DEDICATION This thesis is dedicated to my family and friends for their unwavering support during this adventure. iii ACKNOWLEDGMENTS This research was made possible through funding from the Yellowstone Park Foundation and the Society of Wetland Scientists Student Research Grant for support of field work, and by a Graduate Assistantship and Research Assistantship from the Department of Biological Sciences at Eastern Kentucky University. Thank you to Dr. Bob Frederick for his insight and persistence and for providing the GIS lab and to Dr. -
Mineral Occurrence and Development Potential Report Rawlins Resource
CONTENTS 1.0 INTRODUCTION......................................................................................................................1-1 1.1 Purpose of Report ............................................................................................................1-1 1.2 Lands Involved and Record Data ....................................................................................1-2 2.0 DESCRIPTION OF GEOLOGY ...............................................................................................2-1 2.1 Physiography....................................................................................................................2-1 2.2 Stratigraphy ......................................................................................................................2-3 2.2.1 Precambrian Era....................................................................................................2-3 2.2.2 Paleozoic Era ........................................................................................................2-3 2.2.2.1 Cambrian System...................................................................................2-3 2.2.2.2 Ordovician, Silurian, and Devonian Systems ........................................2-5 2.2.2.3 Mississippian System.............................................................................2-5 2.2.2.4 Pennsylvanian System...........................................................................2-5 2.2.2.5 Permian System.....................................................................................2-6 -
Coexisting Discrete Bodies of Rhyolite and Punctuated Volcanism Characterize 1
RESEARCH ARTICLE Coexisting Discrete Bodies of Rhyolite and Punctuated 10.1029/2019GC008321 Volcanism Characterize Yellowstone's Post‐Lava Key Points: • Zircons from Yellowstone's Upper Creek Tuff Caldera Evolution ‐ Basin Member rhyolites yield U Pb Christy B. Till1 , Jorge A. Vazquez2 , Mark E. Stelten2 , Hannah I. Shamloo1 , dates defining crystallization 1,3 populations at ~750–550 and and Jamie S. Shaffer ~350–250 ka 1 2 • Discrete bodies of magma School of Earth and Space Exploration, Arizona State University, Tempe, AZ, USA, U.S. Geological Survey, Menlo Park, characterized the subvolcanic CA, USA, 3Now at Arizona State Geological Sciences, Now at New Mexico State University, Las Cruces, NM, USA system during the Upper Basin Member period and during storage of the Lava Creek Tuff ‐ 206 238 • Abstract Ion microprobe Pb/ U geochronology and trace element geochemistry of the unpolished The geochemical and isotopic ‐ evolution of Yellowstone's rims and sectioned interiors of zircons from Yellowstone caldera's oldest post caldera lavas provide post‐caldera rhyolites suggests a insight into the magmatic system during the prelude and aftermath of the caldera‐forming Lava Creek shift in the magmatic supereruption. The post‐caldera lavas compose the Upper Basin Member of the Plateau Rhyolite and fall assimilation/recharge ratio into two groups based on zircon crystallization age: early lavas with zircon ages between ~750 and 550 ka ‐ Supporting Information: and late lavas with zircon ages between ~350 and 250 ka. Zircons from the early erupted East Biscuit Basin • Supporting Information S1 flow yield U‐Pb dates and trace element compositions, which when considered with the Pb isotopic • Table S1 compositions of their coexisting feldspars and pyroxenes, point to an isotopically distinct parental melt • Table S2 • Table S3 present during crystallization of the Lava Creek magma but untapped by the supereruption. -
Status of Plant Species of Special Concern in US Forest Service
Status of Plant Species of Special Concern In US Forest Service Region 4 In Wyoming Report prepared for the US Forest Service By Walter Fertig Wyoming Natural Diversity Database University of Wyoming PO Box 3381 Laramie, WY 82071 20 January 2000 INTRODUCTION The US Forest Service is directed by the Endangered Species Act (ESA) and internal policy (through the Forest Service Manual) to manage for listed and candidate Threatened and Endangered plant species on lands under its jurisdiction. The Intermountain Region of the Forest Service (USFS Region 4) has developed a Sensitive species policy to address the management needs of rare plants that might qualify for listing under the ESA (Joslin 1994). The objective of this policy is to prevent Forest Service actions from contributing to the further endangerment of Sensitive species and their subsequent listing under the ESA. In addition, the Forest Service is required to manage for other rare species and biological diversity under provisions of the National Forest Management Act. The current Sensitive plant species list for Region 4 (covering Ashley, Bridger-Teton, Caribou, Targhee, and Wasatch-Cache National Forests and Flaming Gorge National Recreation Area in Wyoming) was last revised in 1994 (Joslin 1994). Field studies by botanists with the Forest Service, Rocky Mountain Herbarium, Wyoming Natural Diversity Database (WYNDD), and private consulting firms since 1994 have shown that several currently listed species may no longer warrant Sensitive designation, while some new species should be considered for listing. Region 4 is currently reviewing its Sensitive plant list and criteria for listing. This report has been prepared to provide baseline information on the statewide distribution and abundance of 127 plants listed as “species of special concern” by WYNDD (Table 1) (Fertig and Beauvais 1999). -
Forest Wide Hazardous Tree Removal and Fuels Reduction Project
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