Wyoming Geo-Notes
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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........................................................................ -
Copper King Mine, Silver Crown District, Wyoming (Preliminary Report)
2012 Copper King Mine, Silver Crown District, Wyoming (Preliminary Report) W. Dan Hausel Independent Geologist, Gilbert, Arizona 11/14/2012 COPPER KING MINE, SILVER CROWN DISTRICT W. Dan Hausel, Independent Geologist Gilbert, Arizona Introduction The Silver Crown district (also known as Hecla) lies 20 miles west of Cheyenne and immediately east of Curt Gowdy State Park along the eastern flank of the Laramie Range. The district is visible on Google Earth (search for ‘Hecla, Cheyenne, WY’) and lies within the boundaries of the Laramie 1:100,000 sheet. This area was initially investigated by Klein (1974) as a thesis project, and also by the Wyoming Geological Survey as a potential target for low-grade, large-tonnage, bulk minable gold and copper (Hausel and Jones, 1982). Nearly all mining and exploration activity in the district centered on the Copper King mine and the Hecla ghost-town with its mill constructed to support mining operations in the area (Figure 1). However, the mill was so poorly designed that rejected tailings often assayed higher than the mill concentrates (Figure 2) (Ferguson, 1965). This has been a common problem with many mines in the West – poorly designed mills. For example, four mills constructed nearby in the Colorado-Wyoming State Line district to extract diamonds, rather than copper and gold from 1979 to 1995, also had recovery problems. The last mill built at the Kelsey Lake mine (40o59’38”N; 105o30’05”W) was not only constructed on a portion of the ore body, but also lost many diamonds. After several months of processing, tailings were checked and the first test sample yielded several diamonds including a 6.2 carat stone. -
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. -
OX RANCH Platte County, Wyoming
Specializing in Farm, Ranch, Recreational & Auction Properties Proudly Presents OX RANCH Platte County, Wyoming Located only two hours from the ever-expanding Front Range of Colorado, the OX Ranch is situated in a private yet accessible region of Wyoming that is often overlooked for the quality and quantity of both elk and mule deer. Water, varied terrain providing excellent cover and excess forage make the OX Ranch both a paradise for wildlife, but also a very desirable cattle ranch. LOCATION & ACCESS The OX Ranch is located approximately 35 miles west of Wheatland, Wyoming. Year-round access is provided to the ranch from paved Wyoming Highway 34 and graveled Mule Creek Road. Mule Creek Road traverses through the center of the ranch providing good access to entire ranch. To access the ranch from Wheatland, travel south on I-25 for 5.7 miles; take exit 73 for WY Highway 34, traveling west toward Laramie for 20.6 miles; turn left onto Mule Creek Road, traveling south for 9 miles; turn left into the headquarters. Several towns and cities in proximity to the property include: • Wheatland, Wyoming (population 3,627) 41 miles northeast • Laramie, Wyoming (population 30,816) 58 miles southwest • Torrington, Wyoming (population 6,501) 96 miles northeast • Cheyenne, Wyoming (population 59, 466) 92 miles southeast • Casper, Wyoming (population 59,628) 144 miles north • Scottsbluff, Nebraska (population 15,039) 125 miles east • Fort Collins, Colorado (population 143,986) 122 miles south • Denver, CO Metro Area (population 3,277,309) 186 miles south OX Ranch Page 2 www.ClarkLandBrokers.com SIZE & DESCRIPTION 5,000± deeded acres 3,400± BLM lease acres 640 State of Wyoming lease acres 9,040± TOTAL ACRES The terrain found on the OX Ranch is very diverse and gives the ranch a very large and unique feel. -
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. -
Chapter 3 – Community Profile
Chapter 3: COMMUNITY PROFILE The Physical Environment, Socio-Economics and History of Fremont County Natural and technological hazards impact citizens, property, the environment and the economy of Fremont County. These hazards expose Fremont County residents, businesses and industries to financial and emotional costs. The risk associated with hazards increases as more people move into areas. This creates a need to develop strategies to reduce risk and loss of lives and property. Identifying risks posed by these hazards, and developing strategies to reduce the impact of a hazard event can assist in protecting life and property of citizens and communities. Physical / Environment Geology Much of Fremont County is made up of the 8,500 square mile Wind River Basin. This basin is typical of other large sedimentary and structural basins in the Rocky Mountain West. These basins were formed during the Laramide Orogeny from 135 to 38 million years ago. Broad belts of folded and faulted mountain ranges surround the basin. These ranges include the Wind River Range on the west, the Washakie Range and Owl Creeks and southern Big Horn Mountains on the north, the Casper Arch on the east, and the Granite Mountains on the south. The center of the basin is occupied by relatively un-deformed rocks of more recent age. Formations of every geologic age exist in Fremont County. These create an environment of enormous geologic complexity and diversity. The geology of Fremont County gives us our topography, mineral resources, many natural hazards and contributes enormously to our cultural heritage. Topography Fremont County is characterized by dramatic elevation changes. -
Eocene Green River Formation, Western United States
Synoptic reconstruction of a major ancient lake system: Eocene Green River Formation, western United States M. Elliot Smith* Alan R. Carroll Brad S. Singer Department of Geology and Geophysics, University of Wisconsin, 1215 West Dayton Street, Madison, Wisconsin 53706, USA ABSTRACT Members. Sediment accumulation patterns than being confi ned to a single episode of arid thus refl ect basin-center–focused accumula- climate. Evaporative terminal sinks were Numerous 40Ar/39Ar experiments on sani- tion rates when the basin was underfi lled, initially located in the Greater Green River dine and biotite from 22 ash beds and 3 and supply-limited accumulation when the and Piceance Creek Basins (51.3–48.9 Ma), volcaniclastic sand beds from the Greater basin was balanced fi lled to overfi lled. Sedi- then gradually migrated southward to the Green River, Piceance Creek, and Uinta ment accumulation in the Uinta Basin, at Uinta Basin (47.1–45.2 Ma). This history is Basins of Wyoming, Colorado, and Utah Indian Canyon, Utah, was relatively con- likely related to progressive southward con- constrain ~8 m.y. of the Eocene Epoch. Mul- stant at ~150 mm/k.y. during deposition of struction of the Absaroka Volcanic Prov- tiple analyses were conducted per sample over 5 m.y. of both evaporative and fl uctuat- ince, which constituted a major topographic using laser fusion and incremental heating ing profundal facies, which likely refl ects the and thermal anomaly that contributed to a techniques to differentiate inheritance, 40Ar basin-margin position of the measured sec- regional north to south hydrologic gradient. loss, and 39Ar recoil. -
Oregon Trail Powerpoint Notes
Name: _______________________________________________________ Date: ___________________ Oregon Trail PowerPoint Notes Trails West 1. In 1824, Crow Indians showed a _____________________ the _______________ Pass, which was a trail through the ________________________ that was wide enough for wagons. 2. By the end of the ________________, thousands of people had traveled through the South Pass on a route known as the _____________________________________. The Oregon Trail 3. About how long was the Oregon Trail? ______________________________________________________ ______________________________________________________ 4. The Oregon Trail started in _____________________ and went through the ____________________________________ into present-day _________________________. 5. Describe the trail. ______________________________________________________ ______________________________________________________ The First Travelers 6. Who were two of the first pioneers to travel the Oregon Trail? ______________________________________________________ ______________________________________________________ © Erin Kathryn 2015 7. The Whitmans settled in ________________________ and wanted to teach ___________________________________ about _____________________________. 8. Why was Narcissa Whitman important? ______________________________________________________ ______________________________________________________ 9. ____________________________ helped make maps of the Oregon Trail. 10. Fremont wrote ___________________ describing ____________________________________________________. -
Brooks Lake Lodge And/Or Common Brooks Lake Lodge 2
NPS Form 10-900 (7-81) United States Department of the Interior National Park Service National Register of Historic Places Inventory Nomination Form See instructions in How to Complete National Register Forms Type all entries complete applicable sections_______________ 1. Name historic Brooks Lake Lodge _ _ and/or common Brooks Lake Lodge 2. Location street & number Lower Brooks Lake Shoshone National Forest not for publication city, town Dubois X vicinity of state Wyoming code 056 Fremont code 013 3. Classification Category Ownership Status Present Use district public occupied agriculture museum X building(s) private unoccupied commercial park structure X both X work in progress educational X private residence site Public Acquisition Accessible entertainment religious object _ in process X yes: restricted government scientific X being considered yes: unrestricted industrial transportation no military other: 4. Owner of Property name Kern M. Hoppe (buildings) United States Forest Service (land) street & number 6053 Nicollet Avenue Region 2 (Mountain Region) Box 25127 city, town Minneapolis, 55419__ vicinity of Lakewood state Colorado 80225 5. Location of Legal Description courthouse, registry of deeds, etc. Dubois Ranger District Shoshone National Forest street & number Box 1S6 city, town Duboi state Wyoming 82513 title Wyoming Survey of Historic Sites has this property been determined eligible? yes X no date 1967; revised 1973 federal _X_ state county local depository for survey records Wyoming Recreation Commission 604 East 25th Street city, town Cheyenne state Wyoming 82002 7. Description Condition Check one Check one excellent deteriorated unaltered X original site good ruins X altered moved date N/A JLfalr unexposed Describe the present and original (iff known) physical appearance The Brooks Lake Lodge complex is situated on the western edge of the Shoshone National Forest in northwestern Wyoming, only two miles east of the Continental Divide. -
Fracture Analysis of Circum-Bighorn Basin Anticlines
FRACTURE ANALYSIS OF CIRCUM-BIGHORN BASIN ANTICLINES, WYOMING-MONTANA by Julian Stahl A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Science MONTANA STATE UNIVERSITY Bozeman, Montana November 2015 ©COPYRIGHT by Julian Stahl 2015 All Rights Reserved ii DEDICATION I dedicate this thesis to my brother, Manuel Stahl, who provided me with the inspiration and drive to pursue a degree that I am truly passionate about. iii ACKNOWLEDGEMENTS The research presented in this document would not have been as thought- provoking and thorough without the help of my mentors and peers. My advisor, Dr. David Lageson helped formulate the project idea and was fundamental throughout the course of my study in leading me in the right direction and always being available to answer questions. I would also like to extend my gratitude to my committee members, Dr. Colin Shaw and Dr. Jean Dixon, for providing me with the necessary assistance and expertise. I would also like to thank my fellow geology peers at Montana State University. Without the constant communication and discussions with Mr. Jacob Thacker, Mr. Travis Corthouts and Mrs. Anita Moore-Nall this project would not have come to fruition. I would also like to offer my sincere appreciation to my two field assistants, Mr. Evan Monroe and Miss Amy Yoder, for taking the time out of their lives to help unravel the geology of the Bighorn Basin in the field. I would like to express my gratitude to my entire family, Dr. Johannes Stahl, Ms. Gabriele Stahl and Mr. -
Maps Showing Thermal Maturity of Upper Cretaceous Marine Shales in the Bighorn Basin, Wyoming and Montana
Maps Showing Thermal Maturity of Upper Cretaceous Marine Shales in the Bighorn Basin, Wyoming and Montana Scientific Investigations Map 3285 U.S. Department of the Interior U.S. Geological Survey Cover photograph: Upper part of Cody Shale near Greybull, Wyoming, east flank of the Bighorn Basin. Photograph by R.C. Johnson, 1994. Maps Showing Thermal Maturity of Upper Cretaceous Marine Shales in the Bighorn Basin, Wyoming and Montana By Thomas M. Finn and Mark J. Pawlewicz Scientific Investigations Map 3285 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Finn, T.M., and Pawlewicz, M.J., 2014, Maps showing thermal maturity of Upper Cretaceous marine shales in the Bighorn Basin, Wyoming and Montana: U.S. -
The Washakie Letters of Willie Ottogary
Utah State University DigitalCommons@USU All USU Press Publications USU Press 2000 The Washakie Letters of Willie Ottogary Matthew E. Kreitzer Follow this and additional works at: https://digitalcommons.usu.edu/usupress_pubs Part of the Indigenous Studies Commons Recommended Citation Ottogary, W., & Kreitzer, M. E. (2000). The Washakie letters of Willie Ottogary, northwestern Shoshone journalist and leader, 1906-1929. Logan: Utah State University Press. This Book is brought to you for free and open access by the USU Press at DigitalCommons@USU. It has been accepted for inclusion in All USU Press Publications by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. The Washakie Letters of Willie Ottogary Northwestern Shoshone Journalist and Leader 1906–1929 “William Otagary,” photo by Gill, 1921, National Anthropological Archives, Smithsonian Institution. The Washakie Letters of Willie Ottogary Northwestern Shoshone Journalist and Leader 1906–1929 Edited by Matthew E. Kreitzer Foreword by Barre Toelken Utah State University Press Logan, Utah Copyright © 2000 Utah State University Press All rights reserved Utah State University Press Logan, Utah 84322-7800 Manufactured in the United States of America Printed on acid free paper 0706050403020100 12345678 Ottogary, Willie. The Washakie letters of Willie Ottogary, northwestern Shoshone journalist and leader, 1906–1929 / [compiled by] Matthew E. Kreitzer. p. cm. Includes bibliographical references and index. ISBN 0-87421-401-7 (pbk.) — ISBN 0-87421-402-5 (hardback) 1. Ottogary, Willie—Correspondence. 2. Shoshoni Indians—Utah—Washakie Indian Reservation—Biography. 3. Indian journalists—Utah—Washakie Indian Reservation—Biography. 4. Shoshoni Indians—Utah—Washakie Indian Reservation—Social conditions. 5.