Soils of Yellowstone National Park
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The Laccolith-Stock Controversy: New Results from the Southern Henry Mountains, Utah
The laccolith-stock controversy: New results from the southern Henry Mountains, Utah MARIE D. JACKSON* Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland 21218 DAVID D. POLLARD Departments of Applied Earth Sciences and Geology, Stanford University, Stanford, California 94305 ABSTRACT rule out the possibility of a stock at depth. At Mesa, Fig. 1). Gilbert inferred that the central Mount Hillers, paleomagnetic vectors indi- intrusions underlying the large domes are Domes of sedimentary strata at Mount cate that tongue-shaped sills and thin lacco- floored, mushroom-shaped laccoliths (Fig. 3). Holmes, Mount Ellsworth, and Mount Hillers liths overlying the central intrusion were More recently, C. B. Hunt (1953) inferred that in the southern Henry Mountains record suc- emplaced horizontally and were rotated dur- the central intrusions in the Henry Mountains cessive stages in the growth of shallow (3 to 4 ing doming through about 80° of dip. This are cylindrical stocks, surrounded by zones of km deep) magma chambers. Whether the in- sequence of events is not consistent with the shattered host rock. He postulated a process in trusions under these domes are laccoliths or emplacement of a stock and subsequent or which a narrow stock is injected vertically up- stocks has been the subject of controversy. contemporaneous lateral growth of sills and ward and then pushes aside and domes the sed- According to G. K. Gilbert, the central intru- minor laccoliths. Growth in diameter of a imentary strata as it grows in diameter. After the sions are direct analogues of much smaller, stock from about 300 m at Mount Holmes to stock is emplaced, tongue-shaped sills and lacco- floored intrusions, exposed on the flanks of nearly 3 km at Mount Hillers, as Hunt sug- liths are injected radially from the discordant the domes, that grew from sills by lifting and gested, should have been accompanied by sides of the stock (Fig. -
Reconnaissance of the Northwest Rim of the Colorado River Basin
RME -77(Pt. ~ ) / Subject Category :' GEOLOGY 'AND MINERA,LOGY U NI TED STATES ATOMIC ENERGY COMM I SSION RECONN.AISS ...-lliCE OF THE NORTHWEST RIM OF THE COLORADO RIVER BASIN, WAYNE AND GARFIELD COUNTIES, UTAH By Robert C. Ge rhard January 1955 Exploration Division Grand J unct ion Operations Office Grand Junction, Colorado Tech n ic a l In formation Ser v i ce Oak. R i dge Te n nes s ee UNCLASSI FI ED I. REC (o NNA l qSA CE OF THE NORYrI1rJEST Rill OF' THE- COLORA OO RIVER BASIN, .. WAYNE AND GARFIELD COUN TIES, UTAH . .- ABSTRACT About five mont hs ' f:eld work was devoted to examining the Salt Wash and Mossback outcrops i n a 1,0 O-square--mile area along the north-" . west r"JTl of 'thE; Co oraclo River, Wayne and Garfield Counties, Utah.- In the Little Rockies district, oxidized d~posits of vanadium- . _ uranium ore, associated chiefl ; with ca r bonized wood, logs, and plant '. "~. fragments, occur in extremely small lenses in two horizons of the Salt ~~: Wash member of t he Morrison f ormation. Beca use of the small l~ri tic ular : .~. nature of presently known or ebodies, ?hysical ~xploration in t his dist r1c t ~ ~ does not now appear to be econOIll:..ca.J..J.Y f easible. 0 -' • __ - . .. "In the Sout he rn Green River Desert, urap.ium m:i.n era liz~tion a Ssc 'cia ted.} ~ ~'~:' ~ ~' with carbon trash, asphaltite, and copper mi nerals occurs in the lower " -~ .: Mossback channel unit fillino paleochannels cut into the Moenkopi for.mation ~ -:-" .. -
Yellowstone National Park Geologic Resource Evaluation Scoping
Geologic Resource Evaluation Scoping Summary Yellowstone National Park This document summarizes the results of a geologic resource evaluation scoping session that was held at Yellowstone National Park on May 16–17, 2005. The NPS Geologic Resources Division (GRD) organized this scoping session in order to view and discuss the park’s geologic resources, address the status of geologic maps and digitizing, and assess resource management issues and needs. In addition to GRD staff, participants included park staff and cooperators from the U.S. Geological Survey and Colorado State University (table 1). Table 1. Participants of Yellowstone’s GRE Scoping Session Name Affiliation Phone E-Mail Bob Volcanologist, USGS–Menlo Park 650-329-5201 [email protected] Christiansen Geologist/GRE Program GIS Lead, NPS Tim Connors 303-969-2093 [email protected] Geologic Resources Division Data Stewardship Coordinator, Greater Rob Daley 406-994-4124 [email protected] Yellowstone Network Supervisory Geologist, Yellowstone Hank Heasler 307-344-2441 [email protected] National Park Geologist, NPS Geologic Resources Bruce Heise 303-969-2017 [email protected] Division Cheryl Geologist, Yellowstone National Park 307-344-2208 [email protected] Jaworowski Katie Geologist/Senior Research Associate, 970-586-7243 [email protected] KellerLynn Colorado State University Branch Chief, NPS Geologic Resources Carol McCoy 303-969-2096 [email protected] Division Ken Pierce Surficial Geologist, USGS–Bozeman 406-994-5085 [email protected] Supervisory GIS Specialist, Yellowstone Anne Rodman 307-344-7381 [email protected] National Park Shannon GIS Specialist, Yellowstone National Park 307-344-7381 [email protected] Savage Monday, May 16, involved a welcome to Yellowstone National Park and an introduction to the Geologic Resource Evaluation (GRE) Program, including status of reports and digital maps. -
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. -
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. -
Profiles of Colorado Roadless Areas
PROFILES OF COLORADO ROADLESS AREAS Prepared by the USDA Forest Service, Rocky Mountain Region July 23, 2008 INTENTIONALLY LEFT BLANK 2 3 TABLE OF CONTENTS ARAPAHO-ROOSEVELT NATIONAL FOREST ......................................................................................................10 Bard Creek (23,000 acres) .......................................................................................................................................10 Byers Peak (10,200 acres)........................................................................................................................................12 Cache la Poudre Adjacent Area (3,200 acres)..........................................................................................................13 Cherokee Park (7,600 acres) ....................................................................................................................................14 Comanche Peak Adjacent Areas A - H (45,200 acres).............................................................................................15 Copper Mountain (13,500 acres) .............................................................................................................................19 Crosier Mountain (7,200 acres) ...............................................................................................................................20 Gold Run (6,600 acres) ............................................................................................................................................21 -
Yellowstone Wolf Project: Annual Report, 2009
YELLOWSTONE WOLFPROJECT ANNUAL REPORT 2009 Yellowstone Wolf Project Annual Report 2009 Douglas Smith, Daniel Stahler, Erin Albers, Richard McIntyre, Matthew Metz, Kira Cassidy, Joshua Irving, Rebecca Raymond, Hilary Zaranek, Colby Anton, Nate Bowersock National Park Service Yellowstone Center for Resources Yellowstone National Park, Wyoming YCR-2010-06 Suggested citation: Smith, D.W., D.R. Stahler, E. Albers, R. McIntyre, M. Metz, K. Cassidy, J. Irving, R. Raymond, H. Zaranek, C. Anton, N. Bowersock. 2010. Yellowstone Wolf Project: Annual Report, 2009. National Park Ser- vice, Yellowstone Center for Resources, Yellowstone National Park, Wyoming, YCR-2010-06. Wolf logo on cover and title page: Original illustration of wolf pup #47, born to #27, of the Nez Perce pack in 1996, by Melissa Saunders. Treatment and design by Renée Evanoff. All photos not otherwise marked are NPS photos. ii TABLE OF CON T EN T S Background .............................................................iv Wolf –Prey Relationships ......................................11 2009 Summary .........................................................v Composition of Wolf Kills ...................................11 Territory Map ..........................................................vi Winter Studies.....................................................12 The Yellowstone Wolf Population .............................1 Summer Predation ...............................................13 Population and Territory Status .............................1 Population Genetics ............................................14 -
B2158 Pt 08 Text
Previous section Volume contents Processes of Laccolithic Emplacement in the Southern Henry Mountains, Southeastern Utah By Marie Jackson1 CONTENTS References Cited............................................................................................................. 27 FIGURES 1. Simplified geologic map of the south Henry Mountains .......................................... 52 2. Interpretive radially oriented cross sections through Mounts Holmes, Ellsworth, and Hillers ................................................................................................................. 54 3. Zijderveldt plots showing the progressive demagnetization of a diorite porphyry sample from sill A in cross section C–C′.................................................................. 56 4. G.K. Gilbert’s concept of laccoliths in Henry Mountains ........................................ 56 5. Structure contour maps and cross sections of Mounts Holmes, Ellsworth, and Hillers, illustrating C.B. Hunt’s concept of relationships between the stocks and uplifts of the beds ............................................................................................... 57 6. Vertical cross sections showing states in growth of central intrusions and domes in the Henry Mountains ................................................................................. 58 A sequence of sedimentary rocks about 4 km thick was New geologic mapping (Jackson and Pollard, 1988) bent, stretched, and uplifted during the growth of three igne- demonstrates that the sedimentary -
Forest Wide Hazardous Tree Removal and Fuels Reduction Project
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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.