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Bedrock Geology of the Southern Part of Tom Miner Basin Park and Gallatin Counties Montana
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1969 Bedrock geology of the southern part of Tom Miner Basin Park and Gallatin counties Montana Stanley Glenn Todd The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Todd, Stanley Glenn, "Bedrock geology of the southern part of Tom Miner Basin Park and Gallatin counties Montana" (1969). Graduate Student Theses, Dissertations, & Professional Papers. 6080. https://scholarworks.umt.edu/etd/6080 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. ss’i'S ' In presenting this thesis in partial fulfillment of the require^ ments for an advanced degree at Mont.' "a State University, I agree that the Library shall make it freely available for inspection. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by my major professor, or, in his absence, by the Director of Libraries, It is understood that any copying or publica tion of this thesis for financial gain shall not be allowed without mjr written permission. signature Date n ^ . S, ______________ -
COPYRIGHTED MATERIAL COPYRIGHTED I
Avalanche Campground (MT), 66 Big Horn Equestrian Center (WY), Index Avenue of the Sculptures (Billings, 368 MT), 236 Bighorn Mountain Loop (WY), 345 Bighorn Mountains Trail System INDEX A (WY), 368–369 AARP, 421 B Bighorn National Forest (WY), 367 Absaroka-Beartooth Wilderness Backcountry camping, Glacier Big Red (Clearmont, WY), 370 (MT), 225–227 National Park (MT), 68 Big Red Gallery (Clearmont, WY), Academic trips, 44–45 Backcountry permits 370 Accommodations, 413–414 Glacier National Park (MT), Big Salmon Lake (MT), 113 best, 8–10 54–56 Big Sheep Creek Canyon (MT), 160 for families with children, 416 Grand Teton (WY), 325 Big Sky (MT), 8, 215–220 Active vacations, 43–52 Yellowstone National Park Big Sky Brewing Company AdventureBus, 45, 269 (MT—WY), 264 (Missoula, MT), 93 Adventure Sports (WY), 309, 334 Backcountry Reservations, 56 Big Sky Candy (Hamilton, MT), 96 Adventure trips, 45–46 Backcountry skiing, 48 Big Sky Golf Course (MT), 217 AdventureWomen, 201–202 Backroads, 45, 46 Big Sky Resort (MT), 216–217 Aerial Fire Depot and Baggs (WY), 390 Big Sky Waterpark (MT), 131 Smokejumper Center (Missoula, Ballooning, Teton Valley (WY), Big Spring (MT), 188 MT), 86–87 306 Big Spring Creek (MT), 187 Air tours Bannack (MT), 167, 171–172 Big Timber Canyon Trail (MT), 222 Glacier National Park (MT), 59 Bannack Days (MT), 172 Biking and mountain biking, 48 the Tetons (WY), 306 Barry’s Landing (WY), 243 Montana Air travel, 409, 410 Bay Books & Prints (Bigfork, MT), Big Sky, 216 Albright Visitor Center 105 Bozeman, 202 (Yellowstone), 263, 275 -
Boating Regulations
Yellowstone National Park Boating Regulations Motorized Boating Non-Motorized Boating Boating Safety Yellowstone National Park offers a variety of boating experiences. Boating in Yellowstone is a memorable experience and a great way see a different part of the park, but boating in Yellowstone is not without its risks. This brochure has been prepared to Contents assist you in planning ahead and preparing for your boating experience, to help you Boat Registration 1 make your trip as safe as possible and to help you minimize your impact on the & Permit resource so that Yellowstone can be enjoyed by future generations of boaters. Required Equipment 2 Where permitted Motorized boats are allowed only on Lewis Shoshone Lake. Access to other lakes Recommended 4 Lake and Yellowstone Lake. Boat launches requires long portages. are located at Bridge Bay Marina and Grant Equipment Village on Yellowstone Lake and on the Float tubes are considered non-motorized south end of Lewis Lake near the Lewis Lake boats and subject to the same regulations. Prohibitions 6 Campground. Water-skiing, jet skis Additional 7 and related activiti- Canoes, kayaks and other non-motorized Regulations boats are permitted on all park lakes except es are not allowed on any park waters. for Sylvan Lake, Eleanor Lake, Twin Lakes Boating Safety 8 and Beach Springs Lagoon. All park rivers are closed to boating except for Invasive Species 14 the section of the Lewis River between Lewis Lake and Yellowstone Lake 15 Shoshone Lake, where non-motorized boating is Lewis Lake & 19 permitted. The only reasonably accessible Shoshone Lake lakes for canoeing or kayaking are Yellowstone Lake, Lewis Lake and Motorized boat permits and non-motor- Boat Registration ized boat permits (including float tubes) & Permit are availabe in a 7-day denomination or as an annual permit. -
Thesis Winter Ecology of Bighorn Sheep In
THESIS WINTER ECOLOGY OF BIGHORN SHEEP IN YELLOWSTONE NATIONAL PARK Submitted by John L. 01demeyer In partial fulfillment of the requirements for the Degree of Master of Science Colorado State University December 1966 COLORADO STATE m~IVERSI1Y December 1966 WE HEREBY RECOl-lEEND 'lRAT lliE 'IHESIS PREPARED UNDER OUR SUPERVISION BY J onn L. 01demeyer ENTITLED tt'v-linter ecolo&;,( of bighorn sheep in yellowstone National ParkU BE ACCEPTED AS FULFILLING nus PART OF 'mE ~UIIill"LENTS FOR THE DillREE OF EASTER OF SCI~CE. CO:TJli ttee on Graduate Work --- - Examination Satisfacto~ Pennission to publish this thesis or any part of it must be obtained from the Dean of the Graduate School. PJL,ORADO STATE UN !VEKS ITY LI BRARIES i ABSTRACT WIN TER ECOLOOY OF ID:GHORN SHEEP IN YELLOVlS'IDHE NA TI ONAL PARK A bighorn sheep study was conducted on the northern winter range of yellowstone National Park, TNY01~inE from JIDle 1965 to June 1966. The objectives of the study were to census the bighorn population, map the winter bighorn distribution, detennine plant conposition and utilization on irnportant bighorn winter ranees, observe daily feedine habits, and assess the effect of competition on bighorn sheep. ~o hundred twen~ nine bighorn sheep wintered on the northern winter range. These herds were located on Nt. Everts, along the Yellowstone River, on Specimen Ridge, and along Soda Butte Creek. The ewe to ram ratio was 100: 78, the ewe to lamb ra tic waS 100: 47, and the ewe to yearling ratio was 100: 20. Range analysis was done on HacHinn Bench, Specimen Ridge, and Druid Peak. -
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. -
Grant Village Area Map
Yellowstone – Grant Village & West Thumb Area GRANT VILLAGE AREA MAP Page 1 of 18 Yellowstone – Grant Village & West Thumb Area Grant Village to Old Faithful Road Map Page 2 of 18 Yellowstone – Grant Village & West Thumb Area Grant Village to Lake Vicinity Road Map Page 3 of 18 Yellowstone – Grant Village & West Thumb Area Grant Village to the South Entrance Road Map Page 4 of 18 Yellowstone – Grant Village & West Thumb Area Day Hikes Near Grant Village & West Thumb Begin your hike by stopping at a ranger station or visitor center for information. Trail conditions may change suddenly and unexpectedly. Bear activity, rain or snow storms, high water, and fires may temporarily close trails. West Thumb Geyser Basin Trail Stroll through a geyser basin of colorful hot springs and dormant lakeshore geysers situated on the scenic shores of Yellowstone Lake. Trails and boardwalks are handicapped accessible with assistance. Trailhead: West Thumb Geyser Basin, 1/4 mile east of West Thumb Junction Distance: 3/8 mile (1 km) roundtrip Level of Difficulty: Easy; boardwalk trail with slight grade as trail descends to and climbs up from the lake shore Yellowstone Lake Overlook Trail Hike to a high mountain meadow for a commanding view of the West Thumb of Yellowstone Lake and the Absaroka Mountains. Trailhead: Trailhead sign at entrance to West Thumb Geyser Basin parking area Distance: 2 miles (3 km) roundtrip Level of Difficulty: Moderate; mostly level terrain with a moderately strenuous 400-foot elevation gain near the overlook. Shoshone Lake Trail (via DeLacy Creek) Hike along a forest's edge and through open meadows to the shores of Yellowstone's largest backcountry lake. -
COVER Page Data for Quaternary Faults in Western Montana
COVER Page Data for Quaternary faults in western Montana by Kathleen M. Haller, Richard L. Dart, Michael N. Machette, and Michael C. Stickney CONTENTS INTRODUCTION ...................................................................................................................................................... 1 STRATEGY FOR DATA COMPILATION ............................................................................................................ 1 EXPLANATION OF PRIMARY DATA FIELDS................................................................................................... 2 HISTORICAL SEISMICITY.................................................................................................................................... 3 HEBGEN LAKE EARTHQUAKE..................................................................................................................................... 4 SYNOPSIS OF QUATERNARY FAULTING IN WESTERN MONTANA......................................................... 5 LIST OF CONTRIBUTING INDIVIDUALS .......................................................................................................... 7 DEFINITION OF DATABASE TERMS.................................................................................................................. 2 FAULT AND FOLD DATABASE ............................................................................................................................ 5 606, DEADMAN FAULT (CLASS A)............................................................................................................................ -
Geology of Pre-Tertiary Rocks in the Northern Part of Yellowstone National Park, Wyon1ing by EDWARD T
GEOLOGY OF PRE- TERTIARY ROCKS IN THE NORTHERN PART OF YELLOWSTONE NATIONAL PARK, m WYOMING "* ,~ - DivMOri Coforado Distril'l r ih•." n' Geology of Pre-Tertiary Rocks in the Northern Part of Yellowstone National Park, Wyon1ing By EDWARD T. RUPPEL With a section on Tertiary laccoliths, sills, and stocks in and near the Gallatin Range, Yellowstone National Park GEOLOGY OF YELLOWSTONE NATIONAL PARK GEOLOGICAL SURVEY PROFESSIONAL PAPER 729-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 72-600268 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 2401-00242 Yellowstone National Park, the oldest of the areas set aside as part of the national park sys tem, lies amidst the Rocky Mountains in north western Wyoming and adjacent parts of Montana and Idaho. Embracing large, diverse, and complex geologic features, the park is in an area that is critical to the interpretation of many significant regional geologic problems. In order to provide basic data bearing on these problems, the U.S. Geological Survey in 1965 initiated a broad pro gram of comprehensive geologic and geophysical investigations within the park. This program was carried out with the cooperation of the National Park Service, and was also aided by the National Aeronautics and Space Administration, which supported the gathering of geologic information needed in testing and in interpreting results from various remote sensing devices. This professional paper chapter is one of a series of technical geo logic reports resulting from these investigations. -
ACKNOWLEDGMENTS Pat and I Had the Privilege of Working with Many Dedicated and Competent People in the NPS
374 ACKNOWLEDGMENTS Pat and I had the privilege of working with many dedicated and competent people in the NPS. Ranger-Naturalists have carried the heart and soul of the ‘"National Park Idea,” and the “Mystique,” from generation to generation. It was a wonderful experience and privilege to serve with YNP Ranger-Naturalists Bill Baker, Lowell Biddulph, Bill Lewis, Bud Lystrup, George Marler, Ted Parkinson, Wayne Replogle, and Simon Simonian. They helped us understand what it meant to Love Yellowstone. Chet Cantrell, Fred Felsch, and Jim Hughes were dedicated seasonal rangers, and good friends. Rangers Tom Milligan, with wife Sharlene, Nat Lacy, Bert McLaren, and Don Guiton, Secretary Ellen Bratlien, and Park Engineer Tom Hyde and wife Norma, lived in the Mammoth Hot Springs apartment into which we moved in 1957. They all took us under wing and demonstrated the real “family” atmosphere of working for the NPS in those days. When we first arrived in YNP as a permanent Park Ranger, some of the storied permanent rangers were still serving in the Park. They included Chief Ranger Otto Brown; Assistant Chief Rangers Scotty Chapman, Hal Edwards, and Tom Garry; District Rangers Lee Coleman, Les Gunzel, DeLyle Stevens, and Joe Way; Management Assistant Joe Joffe; Assistant Superintendent Warren Hamilton; Chief Naturalist David de Lancey Condon; and Historian Aubrey Haines. It was an honor to serve with these men. Fire Specialist, and later Management Assistant, Dan Nelson and wife Junia consistently befriended us, from Yellowstone to Yosemite to Glacier. Sub-District Rangers Tom Ela, Les Gunzel and Lee Robinson, for whom I worked at Old Faithful, epitomized the best of the NPS; they provided the guidance I needed as a new recruit and were always receptive to input. -
Geology of the Park County
Geology of the Gardiner Area Park County Montana Geology of the Gardiner Area Park County Montana By GEORGE D: FRASER, HENRY A. WALDROP, and HAROLD J. HYDEN GEOLOGICAL SURVEY BULLETIN 1277 General geology near the North Entrance of Yellowstone National Park, with special emphasis on recurrent faulting along the boundary of the Beartooth uplift UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Suoerintendent of Documents, U.S. Government Prlntinll Office WashJ.naton, D.C. 10401 CONTENTS Page Abstract---------------------------------------------------------- 1 Introduction------------------------------------------------------ 3 Location----------------------------------------------------- 3 Fieldwork and acknowledgments _____________ ----------_________ 3 Relation to previous geologic work_______________________________ 5 Regional background and. physiography_----------------- ____ ---~ 6 Precambrian geology_______________________________________________ 7 Metasedimentary rocks_________________________________________ 7 Quartz-biotite schist and quartzite ___________ --------------__ 8 Quartz-amphibole schist and related rocks____________________ 9 Phyllite__________________________________________________ 10 Granite______________________________________________________ 10 Metagabbro__________________________________________________ 11 Structure and geologic history ___________________ ----------______ -
Investigators' Annual Reports Yellowstone
1999 INVESTIGATORS’ ANNUAL REPORTS YELLOWSTONE NATIONAL PARK YELLOWSTONE NATIONAL PARK ABS u89 AR O GE K A im J R RAN on A y Dome Mountain ee n N a C G nk a Y E LATIN OTO Ranch Corwin Springs GAL GALLATIN NATIONAL FOREST Gardiner Hellroaring McLaren Deckard Flats Mountain Mine Site ing Cr. r. Electric Peak Cr. ar Cooke City hC ro alo g ll ff Silver Gate Mammoth u e Slou G H B a rd Ga n Swan Rive er ll tin r Camp a Lake reek Ri Bunsen SHOSHO Roosevelt Buffalo C ve Peak e r Ranch tt lCr. u Tower B sta da ry So C AB Mt. NE NATIO SA ver Holmes Ri R e O Co ton La KA ug Canyon ws m NAL ar ar C Ye l l o R r e Norris Ri A GALLATIN NATIONAL FOREST ek v N e G Madiso r FOREST E Hay er k Vall iv e nR Madison de e er r West iv ey n Gibbo n R C . n Yellowstone Cr Fishing ca t eli er e Creek u P c o ez Per Bridge iv N Tr R Lake ole ireh F Cody To Old Faithful Yellowstone Lake Mt. Doane West AB Shoshone Mt. SA Lake Thumb Stevenson R Grant O K A Lewis k R e Eagle Y A re Lake el Heart lo N C iver Peak l w G e R r Lake st z E e er u o iv hl Mt. n O c e R e B s Sheridan eCreek s R wi iv Bechler u e o r Meadows Le Gr ke na R Thor TARGHEE NATIONAL FOREST S iver ofare Cr. -
Yellowstone Paleontological Survey
Yellowstone Paleontological Survey Introduction Stratigraphy Fossil Chronology Taxonomy Localities Vincent L. Santucci Interpretation Paleontological Resource Management Research Collections and Curation Paleontological Resources Near Yellowstone [email protected] Bibliography Yellowstone Center for Resources Appendix A: Yellowstone Paleontological Survey Proposal National Park Service Yellowstone National Park, Wyoming Appendix B: Yellowstone Paleo-Species List YCR-NR-98-1 1998 Appendix C: RMP Paleontological Project Statements Appendix D: Paleontology Researchers at Yellowstone Appendix E: Fossil Specimens in Park Collections Appendix F: Yellowstone Fossils in Outside Repositories Appendix G: GIS Stratigraphy Maps http://www2.nature.nps.gov/geology/paleontology/surveys/yell_survey/index.htm[5/28/2013 2:13:48 PM] Yellowstone Paleo Survey: Introduction Introduction A survey of Yellowstone's fossil resources was initiated in the same spirit of discovery demonstrated by Captain William Raynolds, Henry Washburn, and Ferdinand Hayden. Rumors of marine reptiles, trilobite mass death assemblages, and even dinosaurs in Yellowstone have lured a team of paleontologists in the same way that the legends of "Colter's Hell" and Jim Bridger's "Tall Tales" have attracted many before. Compared to other natural resources at Yellowstone National Park, fossils have received little attention. Except for the research conducted on the petrified forests, Yellowstone's fossils have remained a relative "paleo-incognita" more than 125 years after the park's establishment. As this survey demonstrates, the lack of paleontological research is not due to a lack of significant fossils. Perhaps historian Aubrey Haines provided the best explanation in his comment, "Past administrations preferred that resources not in the public's eye be left alone" (pers.