The Hoodoo U.S
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The Hoodoo U.S
National Park Service The Hoodoo U.S. Department of the Interior Bryce Canyon Map & Hiking Guide Fall - Winter - Spring 2010 – 2011 Questions? Bring this newspaper to the Visitor Center! What’s Inside EMERGENCY INFORMATION PAGE 2 Accessibility . 2 Backpacking . 5 Geology . .3 Hiking Map . 5 Information & Services . 2 Natural History Association . 7 Visitor Center Hours Nearby Attractions . 8 Park Map . 4 October 3 – November 6, 2010 Prescribed Fire . 6 8 a.m. – 6 p.m. Ranger Programs . 3 November 7, 2010 – April 2, 2011 Safety . 2 8 a.m. – 4:30 p.m. Trail Guide . 5 Volunteers, Partners & Donors . 7 April 3 - May 7, 2011 Weather . 6 8 a.m. – 6 p.m. Wildlife . 6 Kevin Doxstater Emergencies Call 911 or 435-676-2411 National Park Service Be Safe at U.S. Department of the Interior Bryce Canyon 24–hours a day or contact a Park Ranger Park Headquarters Mailing Address Web How many people die at Bryce? Fortunately, Bryce averages less than 1 435 834-5322 PO Box 640201 Website: www.nps.gov/brca fatality per year. In order of decreasing Fax 435 834-4703 Bryce, Utah 84764-0201 abundance fatalities are caused by: Twitter: brycecanyonNPS •Heart attacks Lost & Found: 435 834-4736 •Falling off cliffs •Lightning Travelers Information Station: Tune radio to 1590 AM for park information •Vehicle accidents Unfortunately, hundreds of serious injuries have also needlessly occurred, Information and Services some out of ignorance, but too many Park Roads Entrance Fees Lodging from ignoring park safety warnings. The main park road is open year-round S Private Vehicle: $25 per vehicle, Bryce Canyon Lodge: Open Top 10 Causes of Bryce Injuries but may be temporarily closed immediately good for 7 days at Bryce Canyon only. -
Geology of the Hoodoo Mountain Area (NTS 104B/14W)
Geology of the Hoodoo Mountain Area (NTS 104B/14W) by M.G. Mihalynuk1, A. Zagorevski2 and F. Cordey3 KEYWORDS: Hoodoo Mountain, Sphaler Creek, Stikine information is included herein; see Mihalynuk et al. assemblage, Stuhini Group, copper porphyry, Galore (2010, 2011a) for additional unit descriptions and Creek, Dirk prospect, Telena prospect, volcanic-hosted previous work. massive sulphide, Rock and Roll, Andrei Icefield, Iskut River LOCATION AND ACCESS INTRODUCTION Hoodoo Mountain area (NTS 104/14W) can be accessed either via the Bronson airstrip to the immediate Hoodoo Mountain area is located between the south, or via the Espaw camp located at kilometre 91 on enormous copper-gold resource defined at Galore Creek the incomplete Galore Creek access road, immediately and the past-producing gold deposits of the Bronson north of the map area. At the time of our field program, Camp. Reserves at Galore Creek in proven and probable both required air transport from Bob Quinn airstrip categories are 528 Mt grading 0.58% Cu, 0.32 g/t Au and located on Highway 37, approximately 400 km by road 6.02 g/t Ag (Gill et al., 2011). In the Bronson Camp, the from both Smithers and Terrace (Figure 1). Bob Quinn Snip mine produced 32 million grams of gold, 12 million airstrip is 60 km from both Bronson airstrip and Espaw grams silver and nearly 250 000 kilograms copper from Camp. about 1.2 million tonnes between 1991 and 1999; Johnny Mountain produced for less than two years with produced, proven, probable and “possible” categories totalling 0.622 Mt at 19.54 g/t Au (MINFILE, 2011). -
S a N R a F a E L S W E
UTAH GEOLOGICAL SURVEY SURVEY NOTES Volume 34, Number 2 June 2002 S AN R AFAEL S WELL TABLE OF CONTENTS Cache Valley Sensitivity and The Vulnerabilty to Pesticides . 1 New Publications . 4 GeoSights: Little Egypt . 5 Director’s Landslide Damaged Six Layton Homes . 6 Perspective Glad You Asked: What are minerals used for? . 8 by Richard G. Allis San Rafael Swell Proposed as New National Monument . 9 Energy News: Growing Importance of Coalbed Gas in Utah . 12 n an eleventh-hour decision as the assumed to be the exact way the Act will actually be administered. A Survey News . 13 Utah legislature ended its session Ithis March, the “Professional Geolo- license will be required for all geologi- cal work relevant to public welfare, or Design by Vicky Clarke gist Licensing Act” was passed, and it has subsequently been signed into law. safeguarding the life, health, property and the environment in Utah. Among Cover: San Rafael Swell, photograph courtesy Utah becomes the 31st state to require of Utah Travel Council. professional geologist licensure, and it several exclusions are subordinates of is the 27th to adopt the National Asso- a licensed professional geologist, indi- State of Utah ciation of State Boards of Geology viduals engaged in teaching or Michael O. Leavitt, Governor (ASBOG) exam as the standard for research in the physical or natural sci- Department of Natural Resources Robert Morgan, Executive Director licensure. The relatively rapid passing ences who are not otherwise engaged UGS Board of the Act is a tribute to the energy, in practicing geology before the public, Robert Robison, Chair enthusiasm and lobbying skills of prac- employees of companies if their work Geoff Bedell Craig Nelson ticing geologists in Utah. -
Mid-Twentieth Century Architecture in Alaska Historic Context (1945-1968)
Mid-Twentieth Century Architecture in Alaska Historic Context (1945-1968) Prepared by Amy Ramirez . Jeanne Lambin . Robert L. Meinhardt . and Casey Woster 2016 The Cultural Resource Programs of the National Park Service have responsibilities that include stewardship of historic buildings, museum collections, archeological sites, cultural landscapes, oral and written histories, and ethnographic resources. The material is based upon work assisted by funding from the National Park Service. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author and do not necessarily reflect the views of the Department of the Interior. Printed 2018 Cover: Atwood Center, Alaska Pacific University, Anchorage, 2017, NPS photograph MID-TWENTIETH CENTURY ARCHITECTURE IN ALASKA HISTORIC CONTEXT (1945 – 1968) Prepared for National Park Service, Alaska Regional Office Prepared by Amy Ramirez, B.A. Jeanne Lambin, M.S. Robert L. Meinhardt, M.A. and Casey Woster, M.A. July 2016 Table of Contents LIST OF ACRONYMS/ABBREVIATIONS ............................................................................................... 5 EXECUTIVE SUMMARY ........................................................................................................................... 8 1.0 PROJECT DESCRIPTION ..................................................................................................................... 9 1.1 Historic Context as a Planning & Evaluation Tool ............................................................................ -
Geographic Names
GEOGRAPHIC NAMES CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES ? REVISED TO JANUARY, 1911 WASHINGTON GOVERNMENT PRINTING OFFICE 1911 PREPARED FOR USE IN THE GOVERNMENT PRINTING OFFICE BY THE UNITED STATES GEOGRAPHIC BOARD WASHINGTON, D. C, JANUARY, 1911 ) CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES. The following list of geographic names includes all decisions on spelling rendered by the United States Geographic Board to and including December 7, 1910. Adopted forms are shown by bold-face type, rejected forms by italic, and revisions of previous decisions by an asterisk (*). Aalplaus ; see Alplaus. Acoma; township, McLeod County, Minn. Abagadasset; point, Kennebec River, Saga- (Not Aconia.) dahoc County, Me. (Not Abagadusset. AQores ; see Azores. Abatan; river, southwest part of Bohol, Acquasco; see Aquaseo. discharging into Maribojoc Bay. (Not Acquia; see Aquia. Abalan nor Abalon.) Acworth; railroad station and town, Cobb Aberjona; river, IVIiddlesex County, Mass. County, Ga. (Not Ackworth.) (Not Abbajona.) Adam; island, Chesapeake Bay, Dorchester Abino; point, in Canada, near east end of County, Md. (Not Adam's nor Adams.) Lake Erie. (Not Abineau nor Albino.) Adams; creek, Chatham County, Ga. (Not Aboite; railroad station, Allen County, Adams's.) Ind. (Not Aboit.) Adams; township. Warren County, Ind. AJjoo-shehr ; see Bushire. (Not J. Q. Adams.) Abookeer; AhouJcir; see Abukir. Adam's Creek; see Cunningham. Ahou Hamad; see Abu Hamed. Adams Fall; ledge in New Haven Harbor, Fall.) Abram ; creek in Grant and Mineral Coun- Conn. (Not Adam's ties, W. Va. (Not Abraham.) Adel; see Somali. Abram; see Shimmo. Adelina; town, Calvert County, Md. (Not Abruad ; see Riad. Adalina.) Absaroka; range of mountains in and near Aderhold; ferry over Chattahoochee River, Yellowstone National Park. -
Geologic Resource Evaluation Report, Bryce Canyon National Park
National Park Service U.S. Department of the Interior Natural Resource Program Center Bryce Canyon National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2005/002 Bryce Canyon National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2005/002 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2005 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. -
Glaciovolcanism at Volcán Sollipulli, Southern Chile: Lithofacies Analysis and Interpretation
Journal of Volcanology and Geothermal Research 303 (2015) 59–78 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Glaciovolcanism at Volcán Sollipulli, southern Chile: Lithofacies analysis and interpretation Stefan M. Lachowycz a,⁎, David M. Pyle a, Jennie S. Gilbert b, Tamsin A. Mather a,KatyMeec, José A. Naranjo d, Laura K. Hobbs b a Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, United Kingdom b Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, United Kingdom c British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 5GG, United Kingdom d Servicio Nacional de Geología y Minería, Avenida Santa María 0104, Santiago, Chile article info abstract Article history: Magma–ice–meltwater interactions produce diverse landforms and lithofacies, reflecting the multitude of factors Received 18 December 2014 that influence glaciovolcanism, including both magmatic (e.g., composition, eruption rate) and glacial (e.g., ice Accepted 20 June 2015 thickness, thermal regime) conditions. This is exemplified by the walls of the partly ice-filled summit caldera Available online 3 July 2015 of Volcán Sollipulli, a stratovolcano in southern Chile, which include lithofacies from eruptions of a wide range of magma compositions beneath or in contact with ice. Here we analyse these lithofacies and hence propose Keywords: new interpretations of the eruptive and glacial history of Sollipulli. The facies include a thick, laterally extensive Volcano–ice interaction fi Glaciovolcanic lithofacies sequence of fragmental glaciovolcanic deposits, comprising massive, ma c lava pillow-bearing hyaloclastite Hyaloclastite overlain by sills and then hyaloclastic debris flow deposits (similar to Dalsheidi-type sequences). -
Explosion Structures in Grande Ronde Basalt of the Columbia Riverbasalt Group, Near Troy, Oregon
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1987 Explosion structures in Grande Ronde basalt of the Columbia Riverbasalt group, near Troy, Oregon Leonard Lee Orzol Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Volcanology Commons Let us know how access to this document benefits ou.y Recommended Citation Orzol, Leonard Lee, "Explosion structures in Grande Ronde basalt of the Columbia Riverbasalt group, near Troy, Oregon" (1987). Dissertations and Theses. Paper 3750. https://doi.org/10.15760/etd.5634 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. AN ABSTRAST OF THE THESIS OF Leonard Lee Orzol for the Master of Science in Geology presented June 12, 1987. Title: Explosion Structures in Grande Ronde Basalt of the Columbia River Basalt Group, near Troy, Oregon. APPROVED BY MEMBERS OF THE THESIS COMMITEE: vin H. Beeson Explosion structures occur in flows of Grande Ronde Basalt in the study area near Troy, Oregon. Data from nineteen stratigraphic sites indicate that the maximum number of flows that contain explosion structures at any one site is six. In the informally named Troy flow, explosion structures are widespread. Each flow that contains explosion structures can be divided into two cooling units. The first cooling units occupy troughs in the pre-eruption topography and are up to 10 meters thick. -
America's Canyonlands
AMERICA’S CANYONLANDS Red rocks sculpted by nature define Bryce Canyon National Park (left) and stunning Antelope Canyon UTAH STORIES BY NEVADA Tauck On-tour Exclusive! Filmed Bryce Canyon National narratives by Ken Burns and Zion National Park Park (8,300 ft.) (4,000 ft.) Dayton Duncan share personal Kanab Lake Powell stories of the dreamers, Page Las Vegas Monument visionaries, idealists and unsung Grand Canyon Valley National Park Glen Canyon heroes whose passions and (7,200 ft.) politics shaped the preservation Oak Creek Canyon of three national parks – Grand Canyon, Bryce Canyon and Zion. Sedona Tauck takes you behind-the-scenes with commentary by the creators of “The National Parks: America’s Best Idea.” Phoenix / Scottsdale Maximum Elevation: 8,300 ft. ARIZONA 1. ARRIVE PHOENIX Tour begins: 5:30 PM, JW Marriott Desert Ridge Resort & Spa. A transfer is included from Phoenix Sky Harbor International Airport to emanate from the town’s natural energy fields or you wish to to the JW Marriott Desert Ridge Resort & Spa. Join us for a experience the scenic beauty of the stunning red-rock landscapes welcome cocktail reception and dinner tonight. Meals D that earned it designation as one of the most beautiful places on Earth, you will soon see why Sedona continues to attract 2. SEDONA / THE GRAND CANYON travelers’ – and movie makers’ – attention. Join us for a guided The vibe in Sedona is inspirational and humbling. Whether you walking tour of this mystical place and enjoy lunch on your own. are seeking the feeling of well-being and balance -
Exploring Earth Science: Mysterious Mounds and Planetary Puzzles 60 Minute Earth Science Lesson Interactive Video Conference Program Teacher’S Guide Grades: 3 - 4
1 Exploring Earth Science: Mysterious Mounds and Planetary Puzzles 60 Minute Earth Science Lesson Interactive Video Conference Program Teacher’s Guide Grades: 3 - 4 Mysterious Mounds and Planetary Puzzles Description Objectives Through processes far too slow for our • Students will be able to able to use feeble human eyes to perceive, the world geological data and observations to has been changing for 4.6 billion years. The distinguish between how different evidence for this is all around us in our landforms originated. rocks, dirt, & soil—if you only know the right • Students will be able to use the concepts clues to look for. Starting with the of erosion, weathering, deposition, and mysterious Serpent Mound in Ohio, and basic plate tectonics to create ending with an extraterrestrial encounter, this program will familiarize your students explanations for how unknown with the ways we understand and recognize landforms originated. various landforms. Ohio’s Learning Standards- Science Grade 3: Earth and Space Science - Earth’s Resources • 3.ESS.1 Earth’s nonliving resources have specific properties Grade 4: Earth and Space Science – Earth’s Surface • 4.ESS.1: Earth’s surface has specific characteristics and landforms that can be identified. • 4.ESS.2: The surface of Earth changes due to weathering • 4.ESS.3: The surface of Earth changes due to erosion and deposition Ohio’s Learning Standards- English Language Arts Grades 3 & 4: Comprehension and Collaboration (SL.3.1, SL.3.2, SL.4.1, SL.4.2) Grades 3 & 4: Presentation of Knowledge and Ideas (SL.3.4, SL.3.6, SL.4.4, SL.4.6) Ohio’s Learning Standards- Mathematics Grade 3: Measurement and Data • 3.MD.5 Recognize area as an attribute of plane figures and understand concepts of area measurement. -
Bryce Canyon National Park History
National Park Service Bryce Canyon U.S. Department of the Interior Bryce Canyon National Park From Curiosity to National Park It is a place that was known to the ancient hunters who wandered this part of North America thousands of years ago. To the Southern Paiute it was known as “Agka-ku-wass-a-wits,” which means red painted faces, and the rock formations were the Legend People, turned to stone by Coyote. For the Mormon Pioneers the canyon they named for Ebenezer Bryce was little more than a curiosity – and a place you wouldn’t want to lose a cow. By the early 20th Century, however, the word began to spread and people today come by the millions to marvel at the wonder and timeless beauty that is Bryce Canyon. Beginnings J.W. Humphrey was transferred to the town over the East Fork of the Sevier River of Panguitch in 1915 as the new Forest and complete a dry weather road to the Supervisor of the Sevier National Forest. plateau’s rim (which ended near the site of At the urging of Forest Service Ranger the present Bryce Canyon Lodge). By late Elias Smith, Humphrey first visited the 1916, two articles were written about the eastern escarpment of the Paunsaugunt canyon, one by Arthur Stevens, a member Plateau and, surprised at the “indescribable of the grazing crew, which was published in beauty” of the canyon, almost immediately a Union Pacific publication, Outdoor Life, began developing plans to publicize what and the other by Humphrey, under the pen he had seen. -
Class Assignment Key Word Search on Weathering I. Physical
ES322 Geomorphology - Class Assignment Key Word Search on Weathering I. Physical Weathering The process in which rocks are eroded and broken down into smaller rocks by natural physical processes such as wind, water, ice, plants, gravity, and climate. The type of a. Exfoliation Rock is buried (ex: Lava chamber or Batholith cools underground) Overtime land above is eroded as tectonic uplift pushes rock up. The rock becomes exposed and flakes off in layers as the overburden of soil and tremendous pressures the rock experienced at the depths in which it formed are lifted. The rock is composed of deep hot lava rocks that are not as stable at the earth's surface and as such are more susceptible to erosion. b. Freeze-Thaw Changing climate throughout the year (ideally that of the 45th parallel) produces conditions whereby rocks freeze and thaw in a relatively wet environment. As rain falls it percolates down through tiny cracks and fractures in the rock and stays there as temperatures drop in the winter and freezes. Due to the density of water compared to ice, the ice expands in volume as it freezes increasing the pressure inside the cracks and expanding them. As this persists the effect is exponential whereby more cracks are formed allowing more water to intrude in and freeze, eventually breaking down the rock. c. Thermal Expansion PV=NRT or the ideal gas law can be used to explain thermal expansion. As the temperature goes up, so must the pressure of the gas on its container or, if the gas is uncontained, higher temperatures result in higher volumes or greater gas diffusion.