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Systematics of Water Temperature and Flow at Tantalus Creek During Calendar Year 2005, Norris Geyser Basin, Yellowstone National Park, Wyoming
Systematics of Water Temperature and Flow at Tantalus Creek During Calendar Year 2005, Norris Geyser Basin, Yellowstone National Park, Wyoming Scientific Investigations Report 2007–5234 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2007 This report and any updates to it are available at: http://pubs.usgs.gov/sir/2007/5234/ For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS — the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Clor, L., Lowenstern, J., Heasler, H, 2007, Systematics of water temperature and flow at Tantalus Creek during calendar year 2005, Norris Geyser Basin, Yellowstone National Park, Wyoming: U.S. Geological Survey Scientific Investigation Report 2007-5234. Cataloging-in-publication data are on file with the Library of Congress (http://www.loc.gov/). Produced in the Western Region, Menlo Park, California Manuscript approved for publication, August 28, 2007 Text edited by James W. Hendley II Layout by David R. Jones FRONT COVER—Tantalus Creek collects nearly all the thermal water discharged at the Norris Geyser Basin, pictured below. -
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. -
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. -
Yellowstone National Park Geology Records Preliminary Inventory Hailey Galper June 2016 Box 1
Yellowstone National Park Geology Records Preliminary Inventory Hailey Galper June 2016 Box 1: John Good. Geology field notes. Photographs, notes, correspondence – Grasshopper Glacier, field notes, photographs, An Interpreter’s Guide to Yellowstone National Park partial draft - Yellowstone, maps and photographs – Sunlight Glacier. Paper records, photographs, maps. 1961-1967 Box 2: Norris Geyser Basin Observation Logs. Paper records – notebooks. 1964-1969 Box 3: Mike Keller. Observation notes and reports, reports on thermal cleaning and possible projects for 2000. Mary Ann Moss. Report on Giant Geyser eruption in November 1996. Tim Thompson. Reports on Ferris Pool and surrounding thermal area. Rocco Paperiello. Observation notes, Giant and Giantess geysers. Records pertaining to Fairyland Basin. Paper records. 1997-2000 Box 4: Geyser observation cards. Arranged alphabetically by geyser name. Handwritten and typed. Paper records. 1935-1937 Box 5: Norris Geyser Basin observation logs. Norris Geyser Basin Museum log books. Paper records – notebooks. 1990-2009 Box 6: Geology reports 2002-2013. **Separation sheet – Geology field reports 2013-2015, Rick Hutchinson notes, 2015. PDF Electronic only. Can be found at: O:/Archives/Digital_Copies/RG1Geo/Geology Reports2013_2015 then by year and title. Paper records and PDF. 2002-2015 Box 7: Mary Ann Moss. Giant Geyser observation records (1989). Norris Geyser Basin thermal feature graphs (2001) and Thermal Reports (1986-1987). George D. Marler. Reports, “Norris Geyser Basin”, “Hot Spring Activity in the Geyser Basins of the Firehole River for the 1960 Season”, “Are Yellowstone Geysers Declining in Activity? (1947)”, presentation notes. Publications. “The Hot Springs of the Yellowstone National Park.” – Carnegie Institution of Washington News Service Bulletin 1936. -
Tower Area Day Hikes Yellowstone National Park
National Park Service U.S. Department of the Interior Tower Area Day Hikes Yellowstone National Park Welcome to the Tower Area The Tower area was a crossroads for Native Americans, trappers, and explorers—and a campsite for presidents. We invite you to spend a few hours hiking in this historic and scenic section of Yellowstone. Always carry rain gear, extra food and water, and other emergency equipment when venturing into the backcountry. Be sure to obtain current trail condition and bear activity information at the Tower Ranger Station or visitor centers. llro He arin eek North g Cr Hiking trail described Ye l Trail not described lo w s Roads to ne Ranger Station R iv Hellroaring e Picnic Area r Garnet Sevice Station Slough Creek To Mammoth Hill Trail Hot Springs k e Lamar Cre Rive ugh r lo S Cautions Petrified Yellowstone Tree River Picnic Area Hydrothermal areas: The thin ground in these areas breaks easily, and often Lost Lake To overlies scalding water. Stay on the trail. Northeast Specimen Entrance All Wildlife: You must stay at least Roosevelt Ridge Trailhead 100 yards (91 m) away from bears and Lodge wolves; and at least 25 yards (23 m) away from all other animals—including birds. Bears: Although your chance of Tower Fall an encounter is low, your safety is not guaranteed. Minimize your risks by making loud noises, To Mount shouting, or singing. Hike in Washburn groups and use caution where & Canyon vision is obstructed. Carry bear spray and know how to use it. Do not hike Fishing: Anglers must have a Yellowstone National Park fishing permit in their pos- after dark. -
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. -
Visiting Lamar Valley & Tower Junction Area of Yellowstone
® Visiting Lamar Valley & Tower Junction Area of Yellowstone Lamar Valley is located in the northeast section of the park, just east of Tower Junction. Home to herds of elk, bison, and several packs of wolves, the Lamar Valley is Yellow - stone's prime location to view wildlife. The best time to see wildlife is in the early morn - ing or late evening. Lamar Valley has the largest concentration of grizzlies in the park, and with a little patience and a lot of luck, you may see one. Be sure to bring along a pair of binoculars or a spotting scope. Lamar Valley is the top destination inside Yel - lowstone Park for viewing wolves. There are also abundant fishing opportunities in the Lamar Valley. Mammoth Springs of Yellowstone Sites of Interest: 1. Tower Falls Overlook At present, there is a partial closure of the Tower Fall trail in effect that unfortunately re - stricts access to the bottom of the waterfall, and will for some time, in the interest of public safety. However, the upper platform at the top of the trail still provides historic views of the falls and remains open to the public. Starting at the parking area for the Tower Fall General Store, this trail leads approximately 100 yards to an overlook of the falls. From there it descends 200 feet (60 m.) via a series of switchbacks to the base of the 132 foot (40m.) fall, where the view is even more dramatic. Trailhead: Starting at the parking area for the Tower Fall General Store Round trip Distance: 1.0 mile (1.6 km.) Level of Difficulty: Somewhat strenuous uphill climb back from the base of the falls 2. -
Yellowstone in the Afterglow: Lessons from the Fires
Yellowstone in the Lessons from the Fires Yellowstone in the Afterglow Lessons from the Fires Yellowstone in the Lessons from the Fires Mary Ann Franke Yellowstone Center for Resources Yellowstone National Park Mammoth Hot Springs, Wyoming 2000 Cover design: Renée Evanoff. Cover photo: Bison on the Cougar Creek Trail, May 1998, by Jeff Henry, Roche Jaune Pictures, Inc., Emigrant, Montana. Other photos: Most of the photos in this book are from the Yellowstone National Park collection and were taken by park staff. Many are the work of Jim Peaco. Other photos taken by park employees include: Ann Deutch (page 56); Roy Renkin (pages 59, 60, and 62); and Eleanor Clark (pages 35 and 39). Photos taken by researchers: John Burger, University of New Hampshire (pages 63 and 86); Diana Tomback, University of Colorado (page 82); this Clark’s nutcracker on Mt. Washburn also appeared on the cover of the Bulletin of the Ecological Society of America, Vol. 80(4); G. Wayne Minshall, Idaho State University (page 88). The wolf photo on page 85 was taken by National Geographic photographer Joel Sartore. The diatom image on page 94 is courtesy of the Automatic Diatom Identification and Classification Project of the Royal Botanic Garden Edin- burgh and the Department of Geography, University of Newcastle. Maps: The maps facing page 1 and on pages 6 and 27 were prepared by Sarah Stevenson with data provided by the Spatial Analysis Center at Yellowstone National Park. Cartoons: (Page 31 top) Copyright 1988, Paul Conrad. Distributed by the Los Angeles Times Syndicate. Reprinted with permission. (Page 31 bottom) Reprinted by permission from National Parks magazine. -
408 1941 Boathouse (Lake)
Index 45th Parallel Pullout 33 Arch Park 29, 270, 326, 331 1926 Boathouse (Lake) 408 Arnica Bypass 1941 Boathouse (Lake) 408 See Natural Bridge Service Rd 1998 Concessions Management Arnica Creek 125, 135, 136, 202 Improvement Act 485 Artemisia Geyser 172, 435, 456 Artemisia Trail 172 A Arthur, Chester A. 401 Artist Paint Pots 209, 215 Abiathar Peak 57 Artist Point 93, 280, 283 Absaroka Mountain Range Ash, Jennie 309, 311, 355 58, 60, 108, 125, 127 Ashton (ID) 300 Administration Building 345 Aspen Dormitory 259, 354 Africa Lake 250 Aspen Turnouts 67 Albright, Horace Asta Spring 174 21, 175, 205, 259 270, 338 Astringent Creek 117 Albright Visitor Center 259, 338, 348 Avalanche Peak Trail 110 Altitude Sickness 7 Avenue A 41 Alum Creek 95, 97, 185 Avenue B American Bison Turnout 98 See Mammoth to Tower Jct American Eden Turnout 63 Avenue C See Officer’s Row Amfac 323, 445 See also Xanterra Avenue of Travel Turnout 204 Amfac Parks and Resorts See Amfac Amphitheater Creek 59 B Amphitheater Springs Thermal Area 238, 239 Bachelor Officer’s Quarters 259 Amphitheater Valley 72, 79 Back Basin 218, 221 Anderson, Ole 309, 311, 364 Bacon Rind Creek 264 Angel Terrace 299 Bacon Rind Creek Trail 264 Antelope Creek 78 Bannock Ford 40, 78 Antelope Creek Picnic Area 78 Bannock Indians 47 Antelope Creek Valley Bannock Indian Trail 39, 45, 47, 48 See Amphitheater Valley 242 Antler Peak 245 Barn’s Hole Road 196, 198, 311 Aphrodite Terrace 299 Baronette Peak 58 Apollinaris Spring 241 Baronette Ski Trail 58 Apollinaris Spring Picnic Area Baronett, John H. -
The Buffalo Chip
The Buffalo Chip Resource Management Newsletter Yellowstone National Park Late summer 2003 What's inside East Fire threatens Fishing Bridge 6 Current BEMO projects 8 Historic sign raises eyebrows 10 UGB update 14 Arch event photos 15 Bear 101's new lite News briefs 20 WHAT'S UP AT NORRIS NOW? by Alice Wondrak Biol By now. many of you probably know that the Back Basin cording to personal observations, this feature has gone from trail at Norris Geyser Basin has been closed to travel due to being a milky, opalescent, quiet pool to a crystal clear pool, concerns for the safety of visitors and employees. Rumors roiling up to three feet in height. Pearl Geyser icccntl ha¥e abounded about this closure; we hope that the follow lowed the same pattern, then became a fumarole. Son vi ing information will clear up some questions that people Green Dragon, formerly a boi i i fumarole, providing researchers with a disturbing look at the astound ing amount of debris that people have thmwninto it over the .last the Facts years. Multiple features in the Back Basin have gone Effective July 23, approximately 5.S00 feel of trail earn; none of their temperatii; ling. prising most of the western portion of Norris's Back Basin On July 22. a new [hernial feature emerged near Son of .1 due to increased ground temperatures Green Dragon, emitting a mudflow that began spattering in the area—temperatures of up to hich is the boil boiling-temperature acidic mud (pH; 11 onto the trail, lead ing point noticeable changes leading up ing interpretive staff to immediately close the trail between to the closure began on July ll, when Echinus Geyser began t Green Dragon and Pearl (icyscr. -
Canyon Junction to Tower Junction Road Improvement YELLOWSTONE National Park ! Wyoming / Montana / Idaho
Environmental Assessment September 2001 Canyon Junction to Tower Junction Road Improvement YELLOWSTONE National Park ! Wyoming / Montana / Idaho i SUMMARY The segment of Grand Loop Road from Canyon Junction to Tower Junction in Yellowstone National Park is in an advanced state of deterioration, primarily due to age. The pavement is rutted from wear and cracking because of poor drainage, poor-quality base material, and increasingly heavy vehicle use. The pavement edge has broken down resulting in an inconsistent 5.8 to 6.7 meters (19 to 22 feet) road width. The road was not designed or constructed to accommodate current traffic volumes, vehicle widths, lengths, and weights. Safety hazards include narrow pavement width, inadequate visibility at pullouts and intersections, steep side slopes, poor road surface, rockfalls, and curve alignments that do not meet modern engineering safety standards. A transportation analysis was completed that concluded that this road segment affords no opportunity for slow vehicles to pull out of the traffic stream to allow other vehicles to see the road ahead and pass. The report further summarized that the narrow width and winding alignment of this road result in poor vehicle operating conditions. These factors, in conjunction with the volume of traffic, result in a "level of service" which reflects very congested traffic flows- with a high probability of long delays to road users. Improvement of the entire Canyon Junction to Tower Junction road segment, 29.3 kilometers (18.4 miles) is proposed. This improvement would take place in two construction phases over a period of four to six years, if funding were available. -
Post-Caldera Volcanism in Yellowstone National Park
POST-CALDERA VOLCANISM IN YELLOWSTONE NATIONAL PARK: PETROGENESIS OF THE INTRACALDERA UPPER BASIN MEMBER OF THE PLATEAU RHYOLITE AND EXTRA-CALDERA MINGLED MAGMA COMPLEXES By CHAD JAMES PRITCHARD A dissertation submitted in partial fulfillment of The requirements for the degree of Doctor of Philosophy WASHINGTON STATE UNIVERSITY School of Earth and Environmental Sciences MAY 2011 ©Copyright by CHAD JAMES PRITCHARD, 2011 All Rights Reserved ©Copyright by CHAD JAMES PRITCHARD, 2011 All Rights Reserved To the Faculty of Washington State University: The members of the Committee appointed to examine the dissertation of CHAD JAMES PRITCHARD find it satisfactory and recommend that it be accepted. Peter B. Larson, Ph.D., Chair Terry L. Spell, Ph.D. John A. Wolff, Ph.D. ii ACKNOWLEDGMENTS I could have only conducted this research with the support and understanding of my wife, Meghan Lunney, of whom I am super-duper grateful. Peter Larson, chair of this committee, was extremely helpful and kind, which is greatly appreciated. I would also like to thank the other members of my committee for their time and energy. World class assistance in the field was given by Allen Anderson, William Starkel, and Kevin Tarbert. Sample analyses were conducted at Washington State University GeoAnalytical Laboratories with appreciated help from Dr. Rick Conrey, Charles Knaack, Dr. Garret Hart, and Dr. Jeffery Vervoort. Sampling permits were issued by Yellowstone National Park, Research Permit Office, with help from Christie L. Hendrix. Acknowledgments specific to each research project are present for Chapters 2 and 3. I would also like to thank the kindly folks and friends in the School of Earth and Environmental Sciences.