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Capitol Reef National Park Geologic Resources Inventory Scoping
Geologic Resources Inventory Workshop Summary Capitol Reef National Park September 27-28, 1999 National Park Service Geologic Resources Division and Natural Resources Information Division Version: Draft of November 5, 1999 EXECUTIVE SUMMARY An inventory workshop was held at Capitol Reef NP on September 27-28, 1999 to view and discuss the park’s geologic resources, to address the status of geologic mapping by both the Utah Geological Survey (UGS) and the United States Geological Survey (USGS) for compiling both paper and digital maps, and to assess resource management issues and needs. Cooperators from the NPS Geologic Resources Division (GRD), Natural Resources Information Division (NRID), Capitol Reef NP, UGS, USGS, and Brigham Young University (BYU) were present for the two-day workshop. (See Appendix A, Capitol Reef NP Geological Resources Inventory Workshop Participants, September 27-28, 1999) Z:\Scoping\scoping_summaries\CARE_scoping_summary_19991105.doc Last printed 11/28/2006 12:16:00 PM Page 1 of 18 Capitol Reef NP GRI Workshop Summary: September 27-28, 1999 (cont'd) Day one involved a field trip throughout the northern extent of Capitol Reef NP co-led by USGS geologists Pete Peterson and George Billingsley. Highlights of the field trip can be found at http://www.nature.nps.gov/grd/geology/gri/ut/care/field_trip_care Day two involved a scoping session to present overviews of the NPS Inventory and Monitoring (I&M) program, the Geologic Resources Division, and the ongoing Geologic Resources Inventory (GRI) for Colorado and Utah. Round table discussions involving geologic issues for Capitol Reef NP included interpretation, soils mapping, paleontologic resources, the UGA Millennium 2000 guidebook featuring the geology of Utah's National and State parks, the status of cooperative geologic mapping efforts, sources of available data, geologic hazards, potential future research topics, and action items generated from this meeting. -
Cathedral Valley Loop @
Cathedral Valley Loop @ www.ontdek-amerika.nl Last Update : Januari 27, 2007 Cathedral Valley Loop INLEIDING Cathedral Valley ligt in het uiterste noorden van Capitol Reef National Park, en is alleen via onverharde wegen bereikbaar. Een van de meest opvallende kenmerken is de aanwezigheid van veel schitterende monolieten, dat zijn apart staande rotsen die hoog boven de omgeving uitsteken. Het woord monoliet is afgeleid van de Griekse woorden ‘monos’ (alleen) en ‘lithos’ (gesteente). Je kan het zeer eenzame gebied – er komen hier maar héél weinig bezoekers – bereiken via de Hartnet Road en de Caineville Wash Road, die samen een 58 mijl lange lus vormen. Via diverse korte zijwegen kan je naar een aantal punten rijden die een panoramisch uitzicht bieden over de weidse omgeving. De route valt deels binnen de parkgrenzen; het deel dat niet tot het park behoort wordt beheerd door het Bureau of Landmanagement. De beste jaargetijden om de Cathedral Valley Loop te rijden zijn de lente en de herfst. Tijdens de winter is de weg vaak te slecht, en tijdens de zomer kan het ondraaglijk heet worden. TOESTAND VAN DE WEG In principe is de weg het hele jaar door open. Vierwielaandrijving is meestal niet nodig, maar een hoge bodemvrijheid (high clearance) is wel absoluut noodzakelijk. Bij goede weersomstandigheden is de weg goed berijdbaar, maar bij slecht weer kan de toestand van de weg drastisch veranderen. Regen en sneeuw kunnen delen van de route onbegaanbaar maken. Informeer daarom altijd vooraf bij het Visitor Center in Capitol Reef National Park naar de conditie van de weg én naar de weersvoorspelling. -
Geology and Stratigraphy Column
Capitol Reef National Park National Park Service U.S. Department of the Interior Geology “Geology knows no such word as forever.” —Wallace Stegner Capitol Reef National Park’s geologic story reveals a nearly complete set of Mesozoic-era sedimentary layers. For 200 million years, rock layers formed at or near sea level. About 75-35 million years ago tectonic forces uplifted them, forming the Waterpocket Fold. Forces of erosion have been sculpting this spectacular landscape ever since. Deposition If you could travel in time and visit Capitol Visiting Capitol Reef 180 million years ago, Reef 245 million years ago, you would not when the Navajo Sandstone was deposited, recognize the landscape. Imagine a coastal you would have been surrounded by a giant park, with beaches and tidal flats; the water sand sea, the largest in Earth’s history. In this moves in and out gently, shaping ripple marks hot, dry climate, wind blew over sand dunes, in the wet sand. This is the environment creating large, sweeping crossbeds now in which the sediments of the Moenkopi preserved in the sandstone of Capitol Dome Formation were deposited. and Fern’s Nipple. Now jump ahead 20 million years, to 225 All the sedimentary rock layers were laid million years ago. The tidal flats are gone and down at or near sea level. Younger layers were the climate supports a tropical jungle, filled deposited on top of older layers. The Moenkopi with swamps, primitive trees, and giant ferns. is the oldest layer visible from the visitor center, The water is stagnant and a humid breeze with the younger Chinle Formation above it. -
2014-2015 Annual Report Director Site Manager Administrative Support Michael T
2014-2015 Annual Report Director Site Manager Administrative Support Michael T. Stevens, Ph.D. Jason Kudulis (July-February) Annette Harrington Associate Professor of Biology Site Manager Custodial & Associate Director Gina Gilson (May-Present) Maintenance Support Keith White Lesa Dean Associate Professor of Assistant Site Manager Developmental Mathematics Darrell Mensel CRFS Staff CRFS Advisory Board Maria Blevins, Ph.D. Travis Lovell Linda Shelton Assistant Professor Assistant Professor of Instructor of of Communication Art & Visual Communication English & Literature Danny Horns, Ph.D. T. Heath Ogden, Ph.D. Paul Weber, Ph.D. Associate Dean, Assistant Professor Assistant Professor of Physics College of Science & Health of Biology Advisory Board Members are Betsy Lindley, Ph.D. Mary Sowder, Ph.D. Utah Valley University (UVU) faculty Associate Professor of Exercise Associate Professor and staff who serve for ~3 years on Science & Outdoor Recreation of Education a rotating schedule. 2 crfs 2014-2015 annual report Four hundred fifty undergraduates visited Capitol Reef Field Station (CRFS) this year in our busiest year ever. To put this number into context, this rate of visitation places us in the top 15% of field stations nationwide.1 The majority of students who visit CRFS are from UVU. Because of our dual mission, UVU is in the uncommon position of having the field station resources of a comprehensive university while serving a high proportion of community-college-going students CRFS who are often underrepresented at field stations.1 Further, CRFS is one of less than ten field stations run by a university Staff and located in a national park. It’s exciting to be part of such a unique, vibrant, and growing enterprise. -
Art of Grand Canyon Lesson Plan
Art of the Grand Canyon Duration 1-3 Days (depending on activities chosen) Location Classroom Key Vocabulary conservation: prevention of excessive or wasteful use of a resource preservation: to protect from harm or destruction wilderness: uncultivated, uninhabited region; wild country icon: person or thing regarded as a representative symbol transcendentalist: one who espoused a philosophical romantic theory that there was an ideal, intuitive reality transcending ordinary life landscape: a picture representing a countryside or land kiva: a chamber built wholly or partially underground, used by Puebloan Indian males for religious rites tourism: the commercial organization and operations of vacations and visits to places of interest environmentalism: preservation of wilderness lands against the encroachment of commercial exploitation reclamation: turning arid land into productive farmland through irrigation Trunk Materials • Kolb Brothers: Grand Canyon Pioneers (KAET Arizona Collection DVD) with viewing guide • 15 Copies of PowerPoint of Grand Canyon Art on CD including the work of Jack Hillers, Thomas Moran, William H. Holmes, the Kolb Brothers, Fred Kabotie, the WPA, the Sierra Club, and Bruce Aiken • Reading/viewing guide (master copy) for each group: The Powell Legacy, The Great Depression, Contemporary Views • Arizona Highways (April 1981) pages 2-5, 28-37, 38-44 • The Majesty of the Grand Canyon: 150 Years in Art (GCA Publication) pages 16-21, 28-29 • The Tertiary History of the Grand Canon District ( Stegner Introduction of 2001 -
USGS General Information Product
Geologic Field Photograph Map of the Grand Canyon Region, 1967–2010 General Information Product 189 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DAVID BERNHARDT, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2019 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Billingsley, G.H., Goodwin, G., Nagorsen, S.E., Erdman, M.E., and Sherba, J.T., 2019, Geologic field photograph map of the Grand Canyon region, 1967–2010: U.S. Geological Survey General Information Product 189, 11 p., https://doi.org/10.3133/gip189. ISSN 2332-354X (online) Cover. Image EF69 of the photograph collection showing the view from the Tonto Trail (foreground) toward Indian Gardens (greenery), Bright Angel Fault, and Bright Angel Trail, which leads up to the south rim at Grand Canyon Village. Fault offset is down to the east (left) about 200 feet at the rim. -
Hawaiian Volcano Observatory, a Post That He Held Until 1984
Evolution of Deformation Studies on Active Hawaiian Volcanoes Scientific Investigations Report 2008–5090 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank Evolution of Deformation Studies on Active Hawaiian Volcanoes By Robert Decker, Arnold Okamura, Asta Miklius, and Michael Poland Scientific Investigations Report 2008–5090 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: 2008 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: Decker, Robert, Okamura, Arnold, Miklius, Asta, and Poland, Michael, 2008, Evolution of defor- mation studies on active Hawaiian volcanoes: U.S. Geological Survey Scientific Investigations Report 2008-5090, 23 p. Cataloging-in-Publication data are on file with the Library of Congress (URL http://www.loc.gov/). Produced in the Western Region, Menlo Park, California Manuscript approved for publication, May 22, 2008 Text edited by Tracey Suzuki Layout and design by Luis Menoyo iii (Photo credit: Dartmouth College Archive) Preface Robert (Bob) Decker was a volcanological pioneer, introducing new technologies for making deformation measurements at active volcanoes and pushing volcanology into new and excit- ing frontiers. -
Crater Lake U.S
National Park National Park Service Crater Lake U.S. Department of the Interior People and Place Crater Lake has long attracted the wonder and admiration of people all over the world. Its depth of 1,932 feet (589 meters) makes it the deepest lake in the United States. The lake was formed after the collapse of an ancient vol cano now called Mount Mazama. This collapse formed a "caldera" which is a Spanish word for "kettle" or "boiler" and is used by geologists to describe a large basin-shaped volcanic depression. This eruption is estimated to have occurred 7,700 years ago. The interaction of people and this place is traceable for at least this many years. European contact is fairly recent, starting in 1853. First Sight In the spring of 1853, eleven miners three members from this party came from Yreka, California stopped in for upon a large body of water sitting in a supplies at Isaac Skeeter's mercantile huge depression. Hillman exclaimed store in Jacksonville, Oregon (approxi that it was the bluest water he had mately 90 miles south of Crater Lake). ever seen. Skeeters suggested the They began bragging that they knew name "Deep Blue Lake." Lack of how to find the legendary "Lost provisions soon drove the miners Cabin" gold mine. Skeeters quickly down the mountains and back to gathered up ten other Oregonians and Jacksonville where they reported the set out, using the information over discovery of the lake. However, heard in his store. The trip was without the prospects of gold and fear financed by John Wesley Hillman, a of the unknown region to the north, 21 year old who had recently returned there was no interest in confirming home from a successful trip to the this discovery. -
The Evolving Landscape of the Columbia River Gorge
The Evolving Landscape of the Columbia River Gorge Jim E. O’Connor Carleton Watkins, photographer, OHS neg., OrHi A reprint from the Oregon Historical Quarterly Special Issue Dissecting the Columbia: Lewis and Clark West of the Divide William L. Lang, guest editor Volume , Number Fall the journal of record for oregon history Jim E. O’Connor The Evolving Landscape of the Columbia River Gorge Lewis and Clark and Cataclysms on the Columbia ravelers retracing lewis and clark’s journey to the Pacific over the past two hundred years have witnessed tre- mendous change to the Columbia River Gorge and its pri- mary feature, the Columbia River. Dams, reservoirs, timber Tharvest, altered fisheries, transportation infrastructure, and growth and shrinkage of communities have transformed the river and valley. This radically different geography of human use and habitation is commonly contrasted with the sometimes romantic view of a prior time provided both by early nineteenth-century chroniclers and present-day critics of the modern condition — an ecotopia of plentiful and perpetual resources sustaining a stable culture from time immemorial. Reality is more com- plicated. Certainly the human-caused changes to the Columbia River and the gorge since Lewis and Clark have been profound; but the geologic his- tory of immense floods, landslides, and volcanic eruptions that occurred before their journey had equally, if not more, acute effects on landscapes and societies of the gorge. In many ways, the Lewis and Clark Expedi- tion can be viewed as a hinge point for the Columbia River, the changes engineered to the river and its valley in the two hundred years since their visit mirrored by tremendous changes geologically engendered in the thousands of years before. -
Mount Mazama and Crater Lake: Growth and Destruction of a Cascade Volcano
U.S. GEOLOGICAL SURVEY and the NATIONAL PARK SERVICE—OURVOLCANIC PUBLIC LANDS Mount Mazama and Crater Lake: Growth and Destruction of a Cascade Volcano or more than 100 years, F scientists have sought to unravel the remarkable story of Crater Lake’s formation. Before Crater Lake came into existence, a cluster of volcanoes dominated the landscape. This cluster, called Mount Mazama (for the Portland, Oregon, climbing club the Mazamas), was destroyed during an enormous explosive eruption 7,700 years ago. So much molten rock was expelled that the summit area collapsed during the eruption to form a large volcanic depression, or caldera. Subsequent smaller eruptions occurred as water began to fill the caldera to eventually form the The cataclysmic eruption deepest lake in the United States. of Mount Mazama 7,700 Decades of detailed scientific years ago began with a towering column of pumice studies of Mount Mazama and and ash, as depicted in this new maps of the floor of Crater painting by Paul Rockwood (image courtesy of Crater Lake reveal stunning details of Lake National Park Museum and Archive Collections). the volcano’s eruptive history and After the collapse of the identify potential hazards from summit of the volcano, the caldera filled with water to future eruptions and earthquakes. form Crater Lake. (Photo by Willie Scott, USGS) formation of Crater Lake and with it the Applegate and Garfield Peaks. During the When Clarence Dutton of the U.S. demise of Mount Mazama. growth of Mount Mazama, glaciers repeatedly Geological Survey (USGS) visited Crater carved out classic U-shaped valleys. -
History of Crater Lake
National Park Service Crater Lake U.S. Department of the Interior Crater Lake National Park History Cleetwood survey expedition, 1886 expedition, survey Cleetwood Crater Lake Has Inspired Crater Lake has long attracted the wonder and admiration of people all over the world. People for Many Its depth of 1,943 feet (592 meters) makes it the deepest lake in the United States, and the Generations seventh deepest in the world. Its fresh water is some of the clearest found anywhere in the world. The interaction of people with this place is traceable at least as far back as the eruption of Mount Mazama. European contact is fairly recent, starting in 1853. Original Visitors A Native American connection with this area has Accounts of the eruption can be found in stories been traced back to before the cataclysmic erup- told by the Klamath Indians, who are the descen- tion of Mount Mazama. Archaeologists have found dants of the Makalak people. The Makalaks lived sandals and other artifacts buried under layers of in an area southeast of the present park. Because ash, dust, and pumice from this eruption approxi- information was passed down orally, there are mately 7,700 years ago. To date, there is little evi- many different versions. The Umpqua people have dence indicating that Mount Mazama was a perma- a similar story, featuring different spirits. The Prehistoric sandals nent home to people. However, it was used as a Makalak legend told in the park film, The Crater found at Fort Rock, Oregon temporary camping site. Lake Story, is as follows: A Legendary Look at The spirit of the mountain was called Chief of the The mighty Skell took pity on the people and stood Formation Below World (Llao). -
Geologic Resource Evaluation Report, Capitol Reef National Park
National Park Service U.S. Department of the Interior Natural Resource Program Center Capitol Reef National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2006/005 Capitol Reef National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2006/005 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2006 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly-published newsletters. Views and conclusions in this report are those of the authors and do not necessarily reflect policies of the National Park Service. Mention of trade names or commercial products does not constitute endorsement or recommendation for use by the National Park Service.