Absaroka Range Beardtongue) Species Conservation Assessment Update
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A Publication of the Wyoming Native Plant Society
Castilleja A Publication of the Wyoming Native Plant Society October 2004, Volume 23, No. 3 www.uwyo.edu/wyndd/wnps/wnps_home.htm In this issue: Relicts and Refugia . 1 Floristic Diversity of Wyoming Counties . 3 Botanical Novitiates Find Botanical Novelty . 4 Critical Habitat for the Colorado Butterfly Plant . 5 Requiem for a Lawnmower – review. 6 Rocky Mountain Natural History – review . .7 Whitebark Pine - excerpt. 8 Cynoglossum boreale – addition to the state flora 9 Raising Livestock and Lowering Carbon Dioxide . 10 Scholarship Announcement . 11 Natives vs. Imposters. 12 Relicts and Refugia By Bonnie Heidel For all of the breath-taking alpine topography of the Medicine Bow Range, some of its heart-thumping botany lies low across rolling expanses. Three years and three stages of peatland research have documented vast Above: Eriophorum gracile (slender cotton-grass) is montane fen systems in the Medicine Bow circumboreal, with outlying distribution in northwestern Range, refugia for eleven rare Wyoming Wyoming, the Medicine Bow Range and South Park in vascular plant species of concern including five Colorado By B. Heidel relict species previously unknown from southern Wyoming. peatlands harbor close to 10% of the rare Peatland rare species are disjunct or Wyoming plant species of concern. peripheral as they are present in Wyoming, Botanists took a plunge into peatlands denizens of high latitudes, not state and with pilot site surveys on the Medicine Bow and regional endemics that are the focus of most the Shoshone national forests to compile a Wyoming Natural Diversity Database botany working list of peatland rare species, flora, and research. However, review of the Wyoming vegetation at a small number of known or plant species of concern list in 2002 compared inferred peatland study sites (Heidel and against regional peatland floras indicated that Laursen 2003 a, b; Mellmann-Brown 2004). -
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). -
2021 Adventure Vacation Guide Cody Yellowstone Adventure Vacation Guide 3
2021 ADVENTURE VACATION GUIDE CODY YELLOWSTONE ADVENTURE VACATION GUIDE 3 WELCOME TO THE GREAT AMERICAN ADVENTURE. The West isn’t just a direction. It’s not just a mark on a map or a point on a compass. The West is our heritage and our soul. It’s our parents and our grandparents. It’s the explorers and trailblazers and outlaws who came before us. And the proud people who were here before them. It’s the adventurous spirit that forged the American character. It’s wide-open spaces that dare us to dream audacious dreams. And grand mountains that make us feel smaller and bigger all at the same time. It’s a thump in your chest the first time you stand face to face with a buffalo. And a swelling of pride that a place like this still exists. It’s everything great about America. And it still flows through our veins. Some people say it’s vanishing. But we say it never will. It will live as long as there are people who still live by its code and safeguard its wonders. It will live as long as there are places like Yellowstone and towns like Cody, Wyoming. Because we are blood brothers, Yellowstone and Cody. One and the same. This is where the Great American Adventure calls home. And if you listen closely, you can hear it calling you. 4 CODYYELLOWSTONE.ORG CODY YELLOWSTONE ADVENTURE VACATION GUIDE 5 William F. “Buffalo Bill” Cody with eight Native American members of the cast of Buffalo Bill’s Wild West Show, HISTORY ca. -
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. -
Dollar Mountain, a Northwestern Wyoming Example
Thesis High Altitude Occupation and Raw Material Procurement: Dollar Mountain, a Northwestern Wyoming Example Submitted by William Thomas Reitze Department of Anthropology In partial fulfillment of the requirements For the Degree Master of Arts Colorado State University Fort Collins, Colorado Fall 2004 Copyright by William Thomas Reitze 2004 All Rights Reserved ii Colorado State University June 8, 2004 WE HERBY RECOMMEND THAT THE THESIS PREPARED UNDER OUR SUPERVISION BY WILLIAM THOMAS REITZE ENTITLED HIGH ALTITUDE OCCUPATION AND RAW MATERIAL PROCURMENT: DOLLAR MOUNTAIN, A NORTHWEST WYOMING EXAMPLE BE ACCEPTED AS FULFILLING IN PART REQUIREMENTS FOR THE DEGREE MASTER OF ARTS. Committee on Graduate Work _________________________________________ Jeffrey Eighmy _________________________________________ Sara Rathburn _________________________________________ Adviser: Lawrence Todd _________________________________________ Departmental Head/Director _________________________________________ iii Abstract of the Thesis High Altitude Occupation and Raw Material Procurement: Dollar Mountain, a Northwestern Wyoming Example Studying past human behavior is best addressed by the study of the remains of human activity through the use of archaeological methods. But the study of these remains of past human behavior must take into account their context, and human behavior must be explained as a landscape based phenomena. This thesis explores the incorporation of geoarchaeological, geomorphological, and archaeological principles into a system of landscape analysis. Through the study of the changing nature of the landscape, a better understanding of human behavioral responses to a dynamic landscape can be gained. The research was conducted as part of the Greybull River Impact Zone Project in the Upper Wood River watershed on the eastern slope of the Absaroka Range of northwestern Wyoming, during the 2003 field season. -
Guide to the Willows of Shoshone National Forest
United States Department of Agriculture Guide to the Willows Forest Service Rocky Mountain Research Station of Shoshone National General Technical Report RMRS-GTR-83 Forest October 2001 Walter Fertig Stuart Markow Natural Resources Conservation Service Cody Conservation District Abstract Fertig, Walter; Markow, Stuart. 2001. Guide to the willows of Shoshone National Forest. Gen. Tech. Rep. RMRS-GTR-83. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 79 p. Correct identification of willow species is an important part of land management. This guide describes the 29 willows that are known to occur on the Shoshone National Forest, Wyoming. Keys to pistillate catkins and leaf morphology are included with illustrations and plant descriptions. Key words: Salix, willows, Shoshone National Forest, identification The Authors Walter Fertig has been Heritage Botanist with the University of Wyoming’s Natural Diversity Database (WYNDD) since 1992. He has conducted rare plant surveys and natural areas inventories throughout Wyoming, with an emphasis on the desert basins of southwest Wyoming and the montane and alpine regions of the Wind River and Absaroka ranges. Fertig is the author of the Wyoming Rare Plant Field Guide, and has written over 100 technical reports on rare plants of the State. Stuart Markow received his Masters Degree in botany from the University of Wyoming in 1993 for his floristic survey of the Targhee National Forest in Idaho and Wyoming. He is currently a Botanical Consultant with a research emphasis on the montane flora of the Greater Yellowstone area and the taxonomy of grasses. Acknowledgments Sincere thanks are extended to Kent Houston and Dave Henry of the Shoshone National Forest for providing Forest Service funding for this project. -
Bighorn Sheep Disease Risk Assessment
Risk Analysis of Disease Transmission between Domestic Sheep and Goats and Rocky Mountain Bighorn Sheep Prepared by: ______________________________ Cory Mlodik, Wildlife Biologist for: Shoshone National Forest Rocky Mountain Region C. Mlodik, Shoshone National Forest April 2012 The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TTY). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, SW., Washington, DC 20250-9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TTY). USDA is an equal opportunity provider and employer. Bighorn Sheep Disease Risk Assessment Contents Background ................................................................................................................................................... 1 Bighorn Sheep Distribution and Abundance......................................................................................... 1 Literature -
The Yellowstone Paleontological Survey
E PALEONT ON O T LO S G W I O C L A L L E National Y Park The Yellowstone Service Department of the Interior Paleontological Survey SURVEY Vincent L. Santucci Yellowstone Center for Resources National Park Service Yellowstone National Park, Wyoming YCR-NR-98-1 1998 How to cite this document: Santucci, V. L. 1998. The Yellowstone Paleontological Survey. Yellowstone Center for Resources, National Park Service, Yellowstone National Park, Wyoming,YCR-NR-98-1. Current address for Vincent L. Santucci is National Park Service, P.O. Box 592, Kemmerer, WY 83101. The Yellowstone Paleontological Survey To Lt. Col. Luke J. Barnett, III “Uncle by blood, brother in spirit!” Vincent L. Santucci Yellowstone Center for Resources National Park Service Yellowstone National Park, Wyoming YCR-NR-98-1 1998 Table of Contents Introduction .................................................................................................... 1 Stratigraphy .................................................................................................... 4 Fossil Chronology........................................................................................... 6 Taxonomy ..................................................................................................... 12 Localities ...................................................................................................... 15 Interpretation ................................................................................................ 19 Paleontological Resource Management....................................................... -
Chapter 3 Description of the Study Area
Chapter 3 Description of the study area Paul Taucher Melissa Thompson Nikolaus Gribb 3-17 The WBRB drainage basin covers approximately 25 percent streams and elevation. Clockwise from the Pryor Mountains in of the state in north-central and northwestern Wyoming, plus Montana, the boundary runs: smaller areas of south-central Montana. Figure 3-1 is an index map of the approximately 678 townships within the WBRB 1. Northward then southeastward along a Pryor mountain in Wyoming (625) and Montana (53). As determined from ridgeline bordering drainage intoWyoming, to the the GIS database developed for this study, the WBRB covers Wyoming/Montana state line; approximately 22,883 square miles (14.65 million acres) 2. Thence eastward along the Wyoming/Montana state line in Wyoming and 894 square miles (0.57 million acres) in and along a divide in the Bighorn Mountains; Montana. The WBRB encompasses federal, state, and privately 3. Thence generally south-southeastward along the arcuate owned land in all or part of eight Wyoming counties: ridge of the Bighorn Mountains to T39N, R87W; 4. Thence generally south-southwestward along a divide on the Casper Arch from T39N, R87W to the northwestern • All of Big Horn, Park, and Hot Springs counties tip of the Rattlesnake Hills, T34N, R89W; • Approximately 95 percent of Washakie County 5. Thence a short distance southeastward along the ridgeline • Approximately 85 percent of Fremont County of the Rattlesnake Hills into T33N, R88W; • Approximately 10 percent of Teton County 6. Thence irregularly west-southwestward along the Beaver • Small, relatively undeveloped parts of northwestern Divide (Beaver Rim) – an irregular drainage divide on Natrona and western Johnson counties the Casper arch north and west of the Granite Mountains – to T30N, R101W, where it meets the Continental Approximately 80 percent of Yellowstone National Park (in Divide; Park and Teton counties) is included in the drainage basin, as is 7. -
6/11/2018 at 6:00 Pm Location: Yellowstone Forever's Gardiner
HIKING NORTHERN YELLOWSTONE'S GEOLOGY #180606 Start: 6/6/2018 at 7:00 p.m. End: 6/11/2018 at 6:00 p.m. Location: Yellowstone Forever’s Gardiner Offices 308 Park Street, Gardiner, MT 59030 Welcome to Yellowstone National Park. If you are a newcomer to the Yellowstone Forever Institute, you will be amazed at what awaits you during each day of exploration. We are glad that you are able to join us in Gardiner, Montana, a wonderful Yellowstone gateway community that many of us at Yellowstone Forever call home. Our goal is to provide you with an enjoyable, high-quality educational experience and a safe and memorable visit to Yellowstone. The following information is provided to help you prepare for your program. Please read it thoroughly and call us at 406.848.2400 or email [email protected] if you have any questions. We recommend all first time visitors seek general park information through the National Park Service at 307.344.2107 or www.nps.gov/yell. Important Information Included in this Document: ● Letter from Your Instructor ● What’s Included ● How to Prepare for this Program ● Suggested Reading ● Yellowstone Forever Park Store Information ● Yellowstone Forever Supporter Information ● Code of Ethics ● Cancellation Policy ● Travel Information ● Supplemental Lodging Information From the Instructor Strap on your pack, lace up your boots, and join a geologist for three full days of hikes to explore the extraordinary geology, diverse ecology, and colorful history and pre-history of Yellowstone’s northern range. Learn why geology was key to Yellowstone becoming the world’s first national park. -
Status of Mineral Resource Information for the Wind River Indian Reservation, Wyoming
STATUS OF MINERAL RESOURCE INFORMATION FOR THE WIND RIVER INDIAN RESERVATION, WYOMING David A. Seeland Earl F. Brauch S. Geological Survey U. S. Bureau of Mines Administrative report BIA-8 1975 CONTENTS SUMMARY AND CONCLUSIONS ................................................. 1 INTRODUCTION ................................................................ 2 ACKNOWLEDGMENTS .......................................................... 2 LAND STATUS ................................................................. 2 GEOLOGY ..................................................................... 2 Setting ................................................................... 2 Rock Units ................................................................ 3 Precambrian ......................................................... 3 Cambrian ........................................................... 4 Flathead Sandstone ............................................. 4 Gros Ventre Formation .......................................... 4 Gallatin Limestone.............................................. 4 Ordovician .......................................................... 4 Bighorn Dolomite .............................................. 4 Devonian ........................................................... 5 Darby Formation ............................................... 5 Mississippian ........................................................ 5 Madison Limestone ............................................. 5 Pennsylvanian ...................................................... -
Climate of Riverton, Wyoming
Climate of Riverton, Wyoming Narrative Summary 1. History Observations taken by dedicated cooperative weather observers in Riverton date back to 1907, even though the National Weather Service (NWS) office on the northwest edge of town did not come into existence until 1995. Until that time, NWS observations were taken in Lander, which date back to the late 19th century. Official NWS observations are now taken by an automated surface observing system (ASOS) at the Riverton Regional Airport. The airport is located on the northwest side of town and sits nearly 600 feet higher than downtown Riverton. However, a cooperative weather observer in Riverton is currently taking daily weather observations to keep the record database intact back to 1907. These records are archived at the National Climatic Data Center (NCDC). Since these cooperative weather observers are volunteers, the record database has some missing data due to observers going on vacation or their unavailability during transition from one observer to another. However, the available data is impressive and was interrogated to create this published climate volume. Cooperative weather observations were used exclusively for this work and all observations were taken in the town of Riverton. 2. Topography Riverton is located in the center of the Wind River Basin at an elevation of 4956 feet msl. The impressive peaks of the Wind River Mountains (elevations over 13,000 feet msl) sit approximately 40 miles southwest of town but the range extends from southwest to west-northwest. The southern extent of the Absaroka Range (elevations over 13,000 feet msl) sits about 75 miles northwest of Riverton with the Owl Creek Mountains (rising above 9,000 feet msl) extending from the Absaroka Range to about 30 miles north of town.