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Geology of the Flathead Formation (Middle Cambrian) on the Perimeter
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects 1978 Geology of the Flathead Formation (Middle Cambrian) on the perimeter of the Bighorn Basin, Beartooth Mountains, and Little Belt Mountains in Wyoming and Montana Joel A. Degenstein University of North Dakota Follow this and additional works at: https://commons.und.edu/theses Part of the Geology Commons Recommended Citation Degenstein, Joel A., "Geology of the Flathead Formation (Middle Cambrian) on the perimeter of the Bighorn Basin, Beartooth Mountains, and Little Belt Mountains in Wyoming and Montana" (1978). Theses and Dissertations. 71. https://commons.und.edu/theses/71 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. GEOLOGY OF THE FLATHEAD FORMATION (MIDDLE CAMBRIAN) ON THE PERIMETER OF THE BIGHORN BASIN, BEARTOOTH MOUNTAINS, AND LITTLE BELT MOUNTAINS IN WYOMING AND MONTANA by Joel A. Degenstein Bachelor of Science in Geology, University of North Dakota, 1976 A Thesis Submitted to the Graduate Faculty of the University of North Dakota in partial fulfillment of the requirements for the degree of Master of Science Grand Forks, North Dakota GEOLCGY LIBl(ARY August lJnivenitJ of Ncrtb Dakoll 1978 / . , '"\'';'.ft. ',I l This Thesis submicted by Joel A, Degenstein in partial fulfill ment of the requirements for the Degree of :·Iast:er of Science from ci:te University of ?forth Dakota is hereby app:.-c,·ed by the Faculty Advisory Col!llllittee under whom the work has been done. -
PARK 0 1 5 Kilometers S Ri South Entrance Road Closed from Early November to Mid-May 0 1 5 Miles G Ra River S Access Sy
To West Thumb North Fa r ll ve YELLOWSTONE NATIONAL PARK 0 1 5 Kilometers s Ri South Entrance Road closed from early November to mid-May 0 1 5 Miles G ra River s access sy ad Grassy Lake L nch Ro a g Ra Reservoir k lag e F - Lake of Flagg Ranch Information Station R n the Woods to o Road not recommended 1 h a Headwaters Lodge & Cabins at Flagg Ranch s d for trailers or RVs. Trailhead A Closed in winter River G r lade C e access re e v k i R SS ERNE CARIBOU-TARGHEE ILD Glade Creek e r W Trailhead k Rive ITH a Falls n 8mi SM S NATIONAL FOREST 13km H Indian Lake IA JOHN D. ROCKEF ELLER, JR. D E D E J To South Bo C Pinyon Peak Ashton one C o reek MEMORIAL PARKWAY u 9705ft lt er Creek Steamboat eek Cr Mountain 7872ft Survey Peak 9277ft 89 C a n erry re B ek o z 191 i 287 r A C o y B o a t il e eek ey r C C r l e w e O Lizard C k r k Creek e e e re k C k e e r m C ri g il ly P z z ri G Jackson Lake North Bitch Overlook Cre ek GRAND BRIDGER-TETON NATIONAL FOREST N O ANY k B C ee EB Cr TETON WILDERNESS W Moose Arizona Island Arizona 16mi Lake k e 26km e r C S ON TETON NY o A u C t TER h OL C im IDAHO r B ilg it P ch Moose Mountain rk Pacic Creek k WYOMING Fo e Pilgrim e C 10054ft Cr re e Mountain t k s 8274ft Ea c Leeks Marina ci a P MOOSE BASIN NATIONAL Park Boundary Ranger Peak 11355ft Colter Bay Village W A k T e E N e TW RF YO r O ALLS CAN C O Colter Bay CE m A ri N g Grand View Visitor Center il L PARK P A Point KE 4 7586ft Talus Lake Cygnet Two Ocean 2 Pond Eagles Rest Peak ay Lake Trailhead B Swan 11258ft er lt Lake o Rolling Thunder -
Grand Teton National Park News Release
National Park Service Grand Teton PO Box 170 U.S. Department of the Interior National Park Moose, Wyoming 83012 FOR IMMEDIATE RELEASE Jackie Skaggs/307.739.3393 January 08, 2010 10-01 Grand Teton National Park News Release Environmental Assessment Available for Public Review on Site Work for Grand Teton National Park Headquarters Rehabilitation Project Grand Teton National Park Superintendent Mary Gibson Scott announced today that the Moose Headquarters Rehabilitation Site Work Environmental Assessment (EA) is now available for public review. This EA will be open to review for 30 days, from January 11 through February 9, 2010. The National Park Service (NPS) proposes to perform site improvements that are designed to enhance visitor services and address employee health and safety deficiencies at Grand Teton National Park’s headquarters area in Moose, Wyoming. The site work would restructure vehicle/pedestrian access points, promote better traffic flow, reduce user-created trails and consolidate pedestrian walkways, and improve way-finding throughout the Moose headquarters complex. The purpose of the proposal is to upgrade and improve conditions in a way that enhances visitors’ experiences while providing a safe, healthy, and functional working/living environment for park employees and their families. The NPS preferred alternative involves the reconfiguration of vehicle and pedestrian traffic within the park administrative area and the Moose river landing access, the removal of several temporary buildings, and restoration work targeted at providing appropriate stormwater management. The proposed improvements are designed to increase visitor and employee safety, refine parking and traffic flow patterns, reduce the built environment, and improve water quality while still preserving the character of the area and protecting natural and cultural resources. -
Denudation History and Internal Structure of the Front Range and Wet Mountains, Colorado, Based on Apatite-Fission-Track Thermoc
NEW MEXICO BUREAU OF GEOLOGY & MINERAL RESOURCES, BULLETIN 160, 2004 41 Denudation history and internal structure of the Front Range and Wet Mountains, Colorado, based on apatitefissiontrack thermochronology 1 2 1Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM 87801Shari A. Kelley and Charles E. Chapin 2New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM 87801 Abstract An apatite fissiontrack (AFT) partial annealing zone (PAZ) that developed during Late Cretaceous time provides a structural datum for addressing questions concerning the timing and magnitude of denudation, as well as the structural style of Laramide deformation, in the Front Range and Wet Mountains of Colorado. AFT cooling ages are also used to estimate the magnitude and sense of dis placement across faults and to differentiate between exhumation and faultgenerated topography. AFT ages at low elevationX along the eastern margin of the southern Front Range between Golden and Colorado Springs are from 100 to 270 Ma, and the mean track lengths are short (10–12.5 µm). Old AFT ages (> 100 Ma) are also found along the western margin of the Front Range along the Elkhorn thrust fault. In contrast AFT ages of 45–75 Ma and relatively long mean track lengths (12.5–14 µm) are common in the interior of the range. The AFT ages generally decrease across northwesttrending faults toward the center of the range. The base of a fossil PAZ, which separates AFT cooling ages of 45– 70 Ma at low elevations from AFT ages > 100 Ma at higher elevations, is exposed on the south side of Pikes Peak, on Mt. -
Ultimate Western Swing Page 2 of 44 Trip Summary
Ultimate Western Swing Page 2 of 44 Trip Summary Day 1 Daily Overview Drive: Los Angeles, CA to Springdale, UT (450 Miles) Welcome to Springdale, Utah Day 2 Daily Overview Welcome to Zion National Park - Zion National Park ACTIVITY: Guided Half-Day Hike of The Narrows - The Narrows, Zion Narrows Tour Note: Confirm late check-out of RV Resort for tomorrow’s excursion (request 1:00 PM check-out time if possible). Day 3 Daily Overview Activity: Sandstone Slot Canyoneering Trip (guided) Drive: Springdale to Bryce Canyon Day 4 Daily Overview Acrivity: Explore Bryce Canyon Day 5 Daily Overview Drive: Bryce to Jackson, WY Welcome to Jackson Hole, Wyoming! - Jackson Hole Day 6 Daily Overview Getting around Jackson Hole and Grand Teton National Park - Jackson Hole Explore Grand Teton National Park - Teton National Forest Page 3 of 44 Day 7 Daily Overview Depart: Jackson to Cody Through Yellowstone (177 Miles) Welcome to Yellowstone National Park! - Yellowstone Park Service Stations, Service Stations Explore the Lewis River Canyon Area - Lewis Falls, Lewis Lake Explore West Thumb, Bridge Bay, Lake Yellowstone, and Hayden Valley Day 8 Daily Overview Welcome to Cody, Wyoming! Activity: Explore Cody Day 9 Daily Overview Drive: Cody to Sage Lodge - Through Cooke City (166 Miles) - Cooke City-Silver Gate, Albright Visitor Center, Sage Lodge Explore Lamar Valley and the Tower-Roosevelt Area. Explore the Mammoth Hot Springs Area. Welcome to Gardiner! - Gardiner Check in at Sage Lodge Day 10 Daily Overview Horseback riding and rafting in Paradise Valley -
Grand Teton National Park Youngest Range in the Rockies
GRAND TETON NATIONAL PARK YOUNGEST RANGE IN THE ROCKIES the town of Moran. Others recognized that dudes winter better than cows and began operating dude ranches. The JY and the Bar BC were established in 1908 and 1912, respectively. By the 1920s, dude ranch- ing made significant contributions to the valley’s economy. At this time some local residents real- ized that scenery and wildlife (especially elk) were valuable resources to be conserved rather than exploited. Evolution of a Dream The birth of present-day Grand Teton National Park involved controversy and a struggle that lasted several decades. Animosity toward expanding governmental control and a perceived loss of individual freedoms fueled anti-park senti- ments in Jackson Hole that nearly derailed estab- lishment of the park. By contrast, Yellowstone National Park benefited from an expedient and near universal agreement for its creation in 1872. The world's first national park took only two years from idea to reality; however Grand Teton National Park evolved through a burdensome process requiring three separate governmental Mt. Moran. National Park Service Photo. acts and a series of compromises: The original Grand Teton National Park, set Towering more than a mile above the valley of dazzled fur traders. Although evidence is incon- aside by an act of Congress in 1929, included Jackson Hole, the Grand Teton rises to 13,770 clusive, John Colter probably explored the area in only the Teton Range and six glacial lakes at the feet. Twelve Teton peaks reach above 12,000 feet 1808. By the 1820s, mountain men followed base of the mountains. -
Yellowstone National Park, Wyoming, Montana and Idaho
From west: Idaho Falls, Ida., via U.S. 20, 191 to Rexburg, Ashton, and West Yellow- stone,110 mi. Fromnorth: Livingston, Mont., The Site Guide via U.S. 89 to Gardiner, $6 mi. More than 500 mi. of roads and numeroustrails provide accessto all cornersof the park in spring, summerand fall. During the winter only the n. and n.e. entrance roads are kept open. Concessionaire-operatedsnowmobile tours YellowstoneNational Park, Wyoming, Montana and Idaho are available to some sectorsof the park, originatingat Mammoth. Location NorthwestWyoming, overlapping into Accommodations Full accommodations are of- Montana on the north and west and Idaho on the west and south. fered from mid-June to Labor Day at all major stationswithin the park. (Limited ac- commodationsare available in early and late Description Essentiallyan elevatedplateau with seasons.)Advance reservationssuggested. an average elevation of about 8,000 ft. Campgroundsare available in and near the Roughlysquare in shape;more than 80% of park. Arrive early during the peak of the the park's 3,471 sq.-mi. area is comprisedof summerseason in order to securea campsite. lodgepolepine forests which occur for the most part at elevationsof 7,000 - 8,000 feet. At higher elevations,in streamvalleys and in glacial kettles on the plateau, Engelmann spruce,subalpine fir and whitebarkpine oc- cur. Timberline in the park is at ap- proximately 10,000 ft. At lower elevations Douglas-firand quaking aspengrow in scat- tered stands.Limber pine and RockyMoun- tain juniper alsooccur in lowerelevations, of- ten along the edgesof sagebrush-grassland communities. Nonforestedterritory in the park is generally comprised of wetland meadows, sagebrush-grassland,subalpine meadows, thermal areas or talus. -
Jackson Lake Lodge Commonly-Asked Wedding Planning Questions
Jackson Lake Lodge Commonly-Asked Wedding Planning Questions Thank you for considering Jackson Lake Lodge for your wedding and reception. We offer the perfect location for your event and will assist you with having a memorable wedding from start to finish. Here are the most frequently asked questions about our property, facilities, and activities. We hope that this will provide you with the information you need to select Jackson Lake Lodge for your special day! What is included in the cost of our reception and dinner? Room rental fees include service staff, tables, chairs, linens, china, flatware and basic setup. The total cost of your wedding reception is based on your menu selections. Events can range from a simple cocktail reception to an elegant served four-course dinner, depending on your taste and budget. What types of event facilities are available for my wedding reception? The Explorers Ballroom This private event room is our premier reception location and can accommodate 50 to 250 guests. The room features elk antler chandeliers, hardwood dance floor and exclusive use of the adjoining Sunset Terrace with unsurpassed Teton Mountain views. The East Mural Room Tucked away in a quiet corner of our fine dining restaurant, The East Mural Room offers semi-private dining with breathtaking views of the Teton mountain range, and can seat up to 100. This space features eight-foot high rosewood and walnut panels with Trapper murals that were commissioned by John D. Rockefeller Jr. and painted by artist Carl Rotors. Please note that some setup and entertainment restrictions apply to this event location. -
Foundation Document Overview Yellowstone National Park Wyoming, Montana, Idaho
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Yellowstone National Park Wyoming, Montana, Idaho Contact Information For more information about the Yellowstone National Park Foundation Document, contact: [email protected] or 307-344-7381 or write to: Superintendent, Yellowstone National Park, PO Box 168, Yellowstone National Park, WY 82190-0168 Park Description Yellowstone became the world’s first national park on March This vast landscape contains the headwaters of several major 1, 1872, set aside in recognition of its unique hydrothermal rivers. The Firehole and Gibbon rivers unite to form the Madison, features and for the benefit and enjoyment of the people. which, along with the Gallatin River, joins the Jefferson to With this landmark decision, the United States Congress create the Missouri River several miles north of the park. The created a path for future parks within this country and Yellowstone River is a major tributary of the Missouri, which around the world; Yellowstone still serves as a global then flows via the Mississippi to the Gulf of Mexico. The Snake resource conservation and tourism model for public land River arises near the park’s south boundary and joins the management. Yellowstone is perhaps most well-known for its Columbia to flow into the Pacific. Yellowstone Lake is the largest hydrothermal features such as the iconic Old Faithful geyser. lake at high altitude in North America and the Lower Yellowstone The park encompasses 2.25 million acres, or 3,472 square Falls is the highest of more than 40 named waterfalls in the park. miles, of a landscape punctuated by steaming pools, bubbling mudpots, spewing geysers, and colorful volcanic soils. -
Grand Teton National Park Wyoming
UNITED STATES DEPARTMENT OF THE INTERIOR RAY LYMAN WILBUR. SECRETARY NATIONAL PARK SERVICE HORACE M.ALBRIGHT. DIRECTOR CIRCULAR OF GENERAL INFORMATION REGARDING GRAND TETON NATIONAL PARK WYOMING © Crandall THE WAY TO ENJOY THE MOUNTAINS THE GRAND TETON IN THE BACKGROUND Season from June 20 to September 19 1931 © Crandill TRIPS BY PACK TRAIN ARE POPULAR IN THE SHADOWS OF THE MIGHTY TETONS © Crandall AN IDEAL CAMP GROUND Mount Moran in the background 'Die Grand Teton National Park is not a part of Yellowstone National Park, and, aside from distant views of the mountains, can not be seen on any Yellowstone tour. It is strongly urged, how ever, that visitors to either park take time to see the other, since they are located so near together. In order to get the " Cathedral " and " Matterhorn " views of the Grand Teton, and to appreciate the grandeur and majestic beauty of the entire Teton Range, it is necessary to spend an extra day in this area. CONTENTS rage General description 1 Geographic features: The Teton Range 2 Origin of Teton Range 2 Jackson Hole 4 A meeting ground for glaciers .. 5 Moraines 6 Outwash plains 6 Lakes 6 Canyons 7 Peaks 7 How to reach the park: By automobile . 7 By railroad 9 Administration 0 Motor camping 11 Wilderness camping • 11 Fishing 11 Wild animals 12 Hunting in the Jackson Hole 13 Ascents of the Grand Teton 13 Rules and regulations 14 Map 18 Literature: Government publications— Distributed free by the National Park Service 13 Sold by Superintendent of Documents 13 Other national parks ' 19 National monuments 19 References 19 Authorized rates for public utilities, season of 1931 23 35459°—31 1 j II CONTENTS MAPS AND ILLUSTRATIONS COVER The way to enjoy the mountains—Grand Teton in background Outside front. -
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. -
Sensitive and Rare Plant Species Inventory in the Salt River and Wyoming Ranges, Bridger-Teton National Forest
Sensitive and Rare Plant Species Inventory in the Salt River and Wyoming Ranges, Bridger-Teton National Forest Prepared for Bridger-Teton National Forest P.O. Box 1888 Jackson, WY 83001 by Bonnie Heidel Wyoming Natural Diversity Database University of Wyoming Dept 3381, 1000 E. University Avenue University of Wyoming Laramie, WY 21 February 2012 Cooperative Agreement No. 07-CS-11040300-019 ABSTRACT Three sensitive and two other Wyoming species of concern were inventoried in the Wyoming and Salt River Ranges at over 20 locations. The results provided a significant set of trend data for Payson’s milkvetch (Astragalus paysonii), expanded the known distribution of Robbin’s milkvetch (Astragalus robbinsii var. minor), and relocated and expanded the local distributions of three calciphilic species at select sites as a springboard for expanded surveys. Results to date are presented with the rest of species’ information for sensitive species program reference. This report is submitted as an interim report representing the format of a final report. Tentative priorities for 2012 work include new Payson’s milkvetch surveys in major recent wildfires, and expanded Rockcress draba (Draba globosa) surveys, both intended to fill key gaps in status information that contribute to maintenance of sensitive plant resources and information on the Forest. ACKNOWLEDGEMENTS All 2011 field surveys of Payson’s milkvetch (Astragalus paysonii) were conducted by Klara Varga. These and the rest of 2011 surveys built on the 2010 work of Hollis Marriott and the earlier work of she and Walter Fertig as lead botanists of Wyoming Natural Diversity Database. This project was initially coordinated by Faith Ryan (Bridger-Teton National Forest), with the current coordination and consultation of Gary Hanvey and Tyler Johnson.