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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). -
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. -
10Macdonald YELL NR Testing UM Final Rpt.Pdf
THE 2010 CLASS III ARCHEOLOGICAL INVESTIGATION FOR SHEEPEATER CLIFF SITE 48YE29, YELLOWSTONE NATIONAL PARK, WYOMING By Matthew Werle Michael Livers, M.A. Prepared For Elaine S. Hale, Archeologist Branch of Environmental Compliance Yellowstone Center for Resources P.O. Box 168 Yellowstone National Park, WY 82190 Submitted by Douglas H. MacDonald, Ph.D., R.P.A. Department of Anthropology University of Montana, Missoula 59812 YELL-2010-SCI-5656 Yellowstone Study No. YELL-05656 December 11, 2011 ABSTRACT The University of Montana archeological team, under the direction of Associate Professor Douglas H. MacDonald, conducted a full inventory of archaeological resources at the Sheepeater Cliff site (48YE29) in 2009- 2010. Yellowstone National Park (YNP) proposes road widening and parking lot additions at the popular visitor attraction. The Sheepeater Cliff site (48YE29) is a prehistoric lithic scatter located near a popular rest stop and parking lot along the Norris to Mammoth Hot Springs Highway, approximately two miles south of Swan Lake Flats, in the northern portion of YNP. The site is three miles southwest of Bunsen Peak, bounded by the Gardner River to the southeast and the columnar basalt cliffs from which it derives its name. The Gardner River meets with Glenn Creek upon exiting the Sheepeater Canyon and then merges with Lava Creek seven miles to the northeast. The river then combines with the Yellowstone just outside of Gardiner, MT. Just upstream of 48YE29 is the nexus of the Gardner River, where Obsidian Creek and Indian Creek unite. 48YE29 was originally recorded by Ann Johnson in 1989. The University of Montana (UM) conducted Class III subsurface testing during the 2009 UM field season as part of a Section 110 inspired proactive management funded by YNP. -
Yellowstone National Park! Renowned Snowcapped Eagle Peak
YELLOWSTONE THE FIRST NATIONAL PARK THE HISTORY BEHIND YELLOWSTONE Long before herds of tourists and automobiles crisscrossed Yellowstone’s rare landscape, the unique features comprising the region lured in the West’s early inhabitants, explorers, pioneers, and entrepreneurs. Their stories helped fashion Yellowstone into what it is today and initiated the birth of America’s National Park System. Native Americans As early as 10,000 years ago, ancient inhabitants dwelled in northwest Wyoming. These small bands of nomadic hunters wandered the country- side, hunting the massive herds of bison and gath- ering seeds and berries. During their seasonal travels, these predecessors of today’s Native American tribes stumbled upon Yellowstone and its abundant wildlife. Archaeologists have discov- ered domestic utensils, stone tools, and arrow- heads indicating that these ancient peoples were the first humans to discover Yellowstone and its many wonders. As the region’s climate warmed and horses Great Fountain Geyser. NPS Photo by William S. Keller were introduced to American Indian tribes in the 1600s, Native American visits to Yellowstone became more frequent. The Absaroka (Crow) and AMERICA’S FIRST NATIONAL PARK range from as low as 5,314 feet near the north Blackfeet tribes settled in the territory surrounding entrance’s sagebrush flats to 11,358 feet at the Yellowstone and occasionally dispatched hunting Welcome to Yellowstone National Park! Renowned snowcapped Eagle Peak. Perhaps most interesting- parties into Yellowstone’s vast terrain. Possessing throughout the world for its natural wonders, ly, the park rests on a magma layer buried just one no horses and maintaining an isolated nature, the inspiring scenery, and mysterious wild nature, to three miles below the surface while the rest of Shoshone-Bannock Indians are the only Native America’s first national park is nothing less than the Earth lies more than six miles above the first American tribe to have inhabited Yellowstone extraordinary. -
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. -
YELLOWSTONE National Park WYOMING - MONTANA- IDAHO
YELLOWSTONE National Park WYOMING - MONTANA- IDAHO UNITED STATES RAILROAD ADMINISTRATION N AT IONAU PARK SERIES Copyright by Hayncs, St. Paul Riverside Geyser—Unlike most Geysers it spouts obliquely instead of vertically. Its arching column of water is thrown into the Fireholc River Page two An Appreciation of Yellowstone National Park By EMERSON HOUGH Author oj "<CTic Mississippi Bubble" "54-40 or Fight" "'Che Way to the West," etc. Written Especially for the United States Railroad Administration FTER every war there comes a day of diligence. Usually war is followed by a rush of soldiers back to the soil. We have 3,000,000 soldiers, a large per cent of whom are seeking farms. This means the early use of every reclaimable acre of American soil. 11 means that the wildernesses of America soon will be no more. Our great National Parks are sections of the old American wilder ness preserved practically unchanged. They are as valuable, acre for acre, as the richest farm lands. They feed the spirit, the soul, the character of America. Who can measure the value, even to-day, of a great national reserve such as the Yellowstone Park? In twenty years it will be beyond all price, for in twenty years we shall have no wild America. The old days are gone forever. Their memories are ours personally. We ought personally to understand, to know, to prize and cherish them. Of all the National Parks Yellowstone is the wildest and most universal in its appeal. There is more to see there—more different sorts of things, more natural wonders, more strange and curious things, more scope, more variety—a longer list of astonishing sights—than any half dozen of the other parks combined could offer. -
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. -
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 ...................................................... -
Yell 264 a Geology Outline of Yellowstone National Park
YELL 264 A GEOLOGY OUTLINE OF YELLOWSTONE NATIONAL PARK Many events have shaped the Yellowstone we see today, and the land is still changing. The following is an outline of some of the significant geological events which have occurred in the area known as Yellowstone National Park. This will help you to understand what forces have shaped the park’s landscape and why there is such an abundance of geothermal activity here. 2.7 BILLION YEARS AGO: The oldest rocks known in Yellowstone were formed. These Precambrian gneisses and schists are exposed in parts of the Gallatin Mountain Range. 570 MILLION YEARS AGO: A 2.1 billion year gap exists between the Precambrian rocks and this time. Probably some uplifting occurred during this period, and a great deal of erosion took place. At this time, the area that is Yellowstone was basically a featureless plain. What rocks are known from this time period may be found on Buffalo Plateau in the north central part of the park. 570 TO 75 MILLION YEARS AGO: For about 500 million years (from Cambrian to the Cretaceous periods), Yellowstone was periodically flooded by shallow seas that covered much of what is the western United States. Many sedimentary rocks found in Yellowstone were formed as deposits in these seas (sandstone, shale, limestone, dolomite, and various “formations” which combine types of rocks). Based on the fossil record, it appears that seas advanced and retreated at least one dozen times in the Yellowstone area. Rocks from this time may be found on Mount Everts, the Gallatin Mountains, and around the Snake River. -
YELLOWSTONE NATIONAL PARK R N C Hard-Sided Camping Units Only C E Perc an Ez Pelic N See Detail Map Above PE L LICAN
Services and Facilities Mammoth Hot Springs Old Faithful Canyon Village West Thumb Fishing Bridge, Lake Village 6239ft 1902m 7365ft 2254m 7734ft 2357m and Grant Village 7733ft 2357m and Bridge Bay 7784ft 2373m 0 0.1 0.5 Km To Gardiner To Madison To Tower-Roosevelt To Lake Village 0 0.5 Km To Canyon Emergencies Check the park news- Mammoth Hot Springs Hotel Grand Geyser Amphitheater For medical or other emer- paper for seasonal dates Fi Duck 0 0.1 Mi 0.5 Post Amphitheater re To Norris 0 0.5 Mi h gencies contact a ranger or of services and facilities. Office o Lake Fishing Bridge le West Thumb Ice Visitor Education call 307-344-7381 or 911. Geyser Amphitheater Hill West Thumb Castle Center Showers-Laundry Ranger station To Geyser Basin Geyser Ri Old Ice Upper Terrace Drive: Park ve Canyon Lodge Medical clinic r Faithful Visitor Headquarters no buses, RVs, or trailers; y Information Station Campground a closed in winter Center To East HISTORIC w Bookstore - Showers Entrance Winter road closures FORT e n Laundry YELLOWSTONE o YELLOWSTONE From early November to Lodging Lake Village Post early May most park roads LOWER Office Lake Lodge UPPER TERRACES Chapel Old Faithful Inn Old Faithful LAKE are closed. The exception Food service TERRACES AREA Geyser Lower Falls is the road in the park AREA Old 308ft Upper Lookout between the North one-way Faithful Falls 94m Fishing Bridge Picnic area To Point Amphitheater North Lodge View Grand Recreational Vehicle Park Entrance and Cooke City. Inspiration hard-sided camping units only Entrance Post Office View Point It is open all year.