Utah's National Parks & Public Lands
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The Effect of the Shrinking Great Salt Lake on Snow Duration in The
University of Utah UNDERGRADUATE RESEARCH JOURNAL Blowing in the wind: The effect of the shrinking Great Salt Lake on snow duration in the Wasatch Mountains. Chase Hodges-Heilmann (Gannet Hallar, Tanner Visnick, Christopher Rapp) Department of Atmospheric Science Introduction Utah has two things that tourists know about, the Great Salt Lake, and the Greatest Snow on Earth. The Great Salt Lake is receding and impacting the seasonal duration of the Greatest Snow on Earth. As the Great Salt Lake shrinks, the more arid surface contributes to more windblown dust. When this dust deposits onto snow, the albedo of the surface is decreased, and thus snow melts quicker. Relevant Literature Health complications, issues with visibility, and climate change are all influenced by windblown dust. Dust from the Great Salt Lake accounts for a total of 7% of all wind-blown dust in the Wasatch mountains (Skiles et al., 2018). Lake Sevier and the Great Salt Lake Desert make up the majority of wind-blown dust on the Wasatch mountains (Hahnenberger and Nicolli, 2012). Although dust from the Great Salt Lake right now isn’t major, the lakebed of the Great Salt Lake is becoming more and more exposed. Since pioneers arrived to Salt Lake City in 1847 the Great Salt Lake has decreased in elevation by 11 feet, which translates to a volume reduction of 48% and exposing nearly half of the lake bed (Wurtsbaugh et al., 2016). A decrease in volume of saline lakes is often attributed to global warming and climate change, but water development and diverting tributaries is also to blame (Wurtsbaugh et al., 2017). -
Monument Valley Meander
RV Traveler's Roadmap to Monument Valley Meander However you experience it, the valley is a wonder to behold, a harsh yet hauntingly beautiful landscape. View it in early morning, when shadows lift from rocky marvels. Admire it in springtime,when tiny pink and blue wildflowers sprinkle the land with jewel-like specks of color. Try to see it through the eyes of the Navajos, who still herd their sheep and weave their rugs here. 1 Highlights & Facts For The Ideal Experience Agathla Peak Trip Length: Roughly 260 miles, plus side trips Best Time To Go: Spring - autumn What To Watch Out For: When on Indian reservations abide by local customs. Ask permission before taking photos, never disturb any of the artifacts. Must See Nearby Attractions: Grand Canyon National Park (near Flagstaff, AZ) Petrified Forest National Park (near Holbrook, AZ) Zion National Park (Springdale, UT) 2 Traveler's Notes Monument Valley Navajo Tribal Park The stretch of Rte. 163 called the Trail of the Ancients in honor of the vanished Anasazis cuts across Monument Valley at the Utah border on its way to the little town of Mexican Hat. Named for a rock formation there that resembles an upside-down sombrero a whimsical footnote to the magnificence of Monument Valley—Mexican Hat is the nearest settlement to Goosenecks State Park, just ahead and to the west via Rtes. 261 and 316. The monuments in the park have descriptive names. They are based on ones imagination. These names were created by the early settlers of Monument Valley. Others names portray a certain meaning to the Navajo people. -
(Asos) Implementation Plan
AUTOMATED SURFACE OBSERVING SYSTEM (ASOS) IMPLEMENTATION PLAN VAISALA CEILOMETER - CL31 November 14, 2008 U.S. Department of Commerce National Oceanic and Atmospheric Administration National Weather Service / Office of Operational Systems/Observing Systems Branch National Weather Service / Office of Science and Technology/Development Branch Table of Contents Section Page Executive Summary............................................................................ iii 1.0 Introduction ............................................................................... 1 1.1 Background.......................................................................... 1 1.2 Purpose................................................................................. 2 1.3 Scope.................................................................................... 2 1.4 Applicable Documents......................................................... 2 1.5 Points of Contact.................................................................. 4 2.0 Pre-Operational Implementation Activities ............................ 6 3.0 Operational Implementation Planning Activities ................... 6 3.1 Planning/Decision Activities ............................................... 7 3.2 Logistic Support Activities .................................................. 11 3.3 Configuration Management (CM) Activities....................... 12 3.4 Operational Support Activities ............................................ 12 4.0 Operational Implementation (OI) Activities ......................... -
Oregon, California, Mormon Pioneer, and Pony Express National Historic Trails Long-Range Interpretive Plan
Harpers Ferry Center National Park Service U.S. Department of the Interior Oregon, California, Mormon Pioneer, and Pony Express National Historic Trails Long-Range Interpretive Plan August 2010 Oregon, California, Mormon Pioneer, and Pony Express National Historic Trails Long-Range Interpretive Plan August 2010 Prepared by: National Trails Intermountain Region & Harpers Ferry Center Interpretive Planning National Park Service U.S. Department of the Interior Photo Credits: National Park Service unless otherwise noted Table of Contents Introduction Planning Background Planning Foundation Vision for the Trails 1 Purpose and Signifi cance of the Trails 1 Trails-Wide Interpretive Themes 6 Trail-Specifi c Sub Themes 8 Interpretive Program Goals 10 Partnership Expectations 11 Recommendations 12 Technical Assistance 13 New Technology 15 Communications and Marketing 15 Topics and Audiences 17 Relationship Building 18 Special Populations 18 Staffi ng Needs 19 Planning Team 19 Appendices 20 Appendix A: Representative Trail-Related Visitor Centers and Interpretive Sites 21 Appendix B: Decade Goals for the National Trails 24 CANADA Rainy Flat ia lumb Pend hea S Co ou Rain ris y Or e d is i ll e ur So uri ead Re Clark ath Fork Fl sso d r Mi Riv lai Washington er . C North Dakota of St Cl ne th air ar Montana o t. Cl k e Nor S Fork wst llo t Yel e h lowstone Y S i mbia nak Colu Minnesota cons e is Portland !( W !( La Grande !( Dallas Oregon Idaho Wisconsi South Dakota Mi ssi Wi ssi lla m ppi ette Wyoming !( Boise Mis s Pocatello ouri Wi sco n si n Casper -
United Airlines Flight 608 Accident Report
.,SA-I 53 File No. 1-0097-47 ) CIVIL AERONAUTICS BOARD I ACCIDENT I W ESTIGATOO I I Adopted: February 2, 1948 . Released: February 3, 19y8 UNITED AIR LlhES, INC., BRYCE CANYON, UTAH, OCTOXR 24, 1947 The Accident - United Air Lines I Flight 608 crashed observed what appeared 'to be white smoke at 1229 MST,2 October 24, 1947, 1 1/2 streaming from the aircraft, followed miles southeast of Bryce Canyon Airport, later by dense black smoke. The first Utah, during an attempted emergency witnesses who observed fire in the bottom landing resulting from a fire in flight. of the aircr8ft at approximately the The aircraft, a Model DC-6, NC 37510, center-section were located approxi- was demolished by impact and fire, and mately 15 miles south of Bryce Canyon. all of the 46 passengers and the crew of Until shortly before the moment of im- 6 were killed. pact,. the aircraft appeared to be under normal control; hawever, no_,witnesses History of the FI ight were located who observed the, crash. Flight 608 departed Los Angeles, Cal- ifornia, at 1023 with its destination I nvest i gat ion Chicago, Illinois, to cruise at 19,000 Immediately after the accident the feet according to visual flight rules. wreckage was protected by Civil Aeronau- Routine position reports were made over tics Administration personnel until a Fontana, Daggett and Silver Lake, Cali- guard was established by the National' fornia; Las Vegas, Nevada; and Sdint Park Service, pending the arrival of George, Utah. During the latter report, Board investigators. During the evening the flight indicated that it estimated of the same day various investigation passing over Bryce Canyon, Utah, at 1222. -
January 2, 2020 Notices to Airmen
U.S. Department of Transportation Federal Aviation Administration NOTICES TO AIRMEN Domestic/International January 2, 2020 Next Issue January 30, 2020 Notices to Airmen included in this publication are NOT given during pilot briefings unless specifically requested by the pilot. An electronic version of this publication is on the internet at http://www.faa.gov/air_traffic/publications/notices Air Traffic Products and Publications Team NOTICES TO AIRMEN - January 2, 2020 Part 2. INTERNATIONAL NOTICES TO AIRMEN Notices to Airmen International GENERAL This part features significant international notices to airmen (NOTAM) information and special notices. The information contained in the International Notices to Airmen section is derived from international notices and other official sources. International notices are of two types: Class One International Notices are those NOTAMs issued via telecommunications. They are made available to the U.S. flying public by the International NOTAM Office (Washington, DC) through the local Flight Service Station (FSS). Class Two International Notices are NOTAMs issued via postal services and are not readily available to the U.S. flying public. The International Notices to Airmen draws from both these sources and also includes information about temporary hazardous conditions which are not otherwise readily available to the flyer. Before any international flight, always update the International Notices to Airmen with a review of Class One International Notices available at your closest FSS. Foreign notices carried in this publication are carried as issued to the maximum extent possible. Most abbreviations used in this publication are listed in ICAO Document DOC 8400. Wherever possible, the source of the information is included at the end of an entry. -
N Red Rock Beauty N Salt Lake City N Outdoor Adventure N Dinosaurs
n Red Rock Beauty n Salt Lake City n Outdoor Adventure n Dinosaurs Plus: Arts, Winter Sports, Golf A SPECIAL SUPPLEMENT TO THE JANUARY 2009 ISSUE OF When you come to Utah, visit TEMPLE SQUARE In the heart of Salt Lake City many venues to choose from... All are Free Brigham Young Historic Park Church Office Building State Street Conference Center Relief Society Building Main Street Lion House and Beehive House North Temple Street Salt Lake Temple Joseph Smith Memorial Building West Temple Street North Visitors' Center Tabernacle South Temple Street South Visitors' Center Museum of Church History and Art Assembly Hall Family History Library Hear the world-famous Mormon See the magnificent spires of the Find your roots in the world’s Tabernacle Choir. Salt Lake Temple. largest collection of genealogical information. Enjoy the imposing 11-foot marble Christus statue at the North Visitors' Center. For information, go to visittemplesquare.com, lds.org/placestovisit, or call 1-800-537-9703 For information about The Church of Jesus Christ of Latter-day Saints, visit mormon.org © 2008 by IRI. 7/08. Printed in the USA. 04089. Illustration of Temple Square by Dilleen Marsh © 1999 IRI. Photo of Mormon Tabernacle Choir © 2001 Busath Photography UTAH Life Elevated Utah. 4 Life Elevated Northern Utah. 8 Salt Lake, Dinosaurland & Everything Inbetween Central Utah . 14 Nordic Traditions & Outdoor Wilderness Southwestern Utah . 16 National Parks, Western History & Rugged Beauty Southeastern Utah . 22 Dinosaurs, Swells & Desert Beauty UTAH – A SPECIAL SUPPLEMENT TO THE JANUARY 2009 ISSUE OF CANADIAN TRAVELLER Published 12 times a year by 88 East Pender Street, Suite 555 Vancouver, BC Canada, V6A 3X3 Contents © 2009 by ACT Communications Inc. -
English Information
National Park Service U.S. Department of the Interior Capitol Reef National Park … the light seems to flow or shine out of the rock rather than to be reflected English from it. – Clarence Dutton, geologist and early explorer of Capitol Reef, 1880s A Wrinkle in the Earth A vibrant palette of color spills across the landscape before bridges, and twisting canyons. Over millions of years geologic forces you. The hues are constantly changing, altered by the play shaped, lifted, and folded the earth, creating this rugged, remote area of light against the towering cliffs, massive domes, arches, known as the Waterpocket Fold. Panorama Point at Sunset Erosion creates waterpockets and potholes that collect The Castle is made of fractured Wingate Sandstone perched upon grey Chinle and red Moenkopi Formations. rainwater and snowmelt, enhancing a rich ecosystem. From the east, the Waterpocket Fold appears as a formidable barrier Capitol Dome reminded early travelers of the US Capitol to travel, much like a barrier reef in an ocean. building and later inspired the name of the park. Creating the Waterpocket Fold Capitol Reef’s defining geologic feature is a wrinkle in Uplift: Between 50 and 70 million years ago, an ancient fault was Earth’s crust, extending nearly 100 miles from Thousand reactivated during a time of tectonic activity, lifting the layers to the Lake Mountain to Lake Powell. It was created over time by west of the fault over 7,000 feet higher than those to the east. Rather three gradual, yet powerful processes—deposition, uplift, than cracking, the rock layers folded over the fault line. -
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. -
Weather and Climate Inventory National Park Service Northern Colorado Plateau Network
National Park Service U.S. Department of the Interior Natural Resource Program Center Fort Collins, Colorado Weather and Climate Inventory National Park Service Northern Colorado Plateau Network Natural Resource Technical Report NPS/NCPN/NRTR—2006/002 ON THE COVER Hickman Bridge—Capitol Reef National Park Photograph copyrighted by Jim Ashby Weather and Climate Inventory National Park Service Northern Colorado Plateau Network Natural Resource Technical Report NPS/NCPN/NRTR—2006/002 WRCC Report 06-03 Christopher A. Davey, Kelly T. Redmond, and David B. Simeral Western Regional Climate Center Desert Research Institute 2215 Raggio Parkway Reno, Nevada 89512-1095 August 2006 U.S. Department of the Interior National Park Service Natural Resource Program Center Fort Collins, Colorado 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 National Park Service 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 designed and published in a professional manner. The Natural Resource Technical Reports series is used to disseminate the peer-reviewed results of scientific studies in the physical, biological, and social sciences for both the advancement of science and the achievement of the National Park Service’s mission. The reports provide contributors with a forum for displaying comprehensive data that are often deleted from journals because of page limitations. Current examples of such reports include the results of research that addresses natural resource management issues; natural resource inventory and monitoring activities; resource assessment reports; scientific literature reviews; and peer reviewed proceedings of technical workshops, conferences, or symposia. -
Jewell Nicoll Geomorph 2011.Pdf
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Geomorphology 129 (2011) 1–13 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Wind regimes and aeolian transport in the Great Basin, U.S.A. Paul W. Jewell a,⁎, Kathleen Nicoll b a Department of Geology and Geophysics, University of Utah, Salt Lake City, UT 84112, United States b Department of Geography, University of Utah, Salt Lake City, UT 84112, United States article info abstract Article history: The modern Great Basin of the interior western United States is characterized by surface winds with Received 23 April 2010 considerable spatial and temporal variabilities. Wind records from the second half of the 20th century for 12 Received in revised form 4 January 2011 Great Basin localities, analyzed with standard aeolian-sediment transport methods developed elsewhere in Accepted 11 January 2011 the world, reflect this complexity. The drift potential (DP) for aeolian deposits is generally moderate (DP 200– Available online 19 January 2011 400) in the western Great Basin and weak (DPb200) in the central Great Basin where winds are predominantly west-southwesterly. -
Creating Memorable Travel Experiences Since 1979 2021
2021 DREAM BOOK LLC CREATING MEMORABLE TRAVEL EXPERIENCES SINCE 1979 One from the Road… When we returned to the road in August, one of our first trips was By the end of the tour, you feel like you just watched Ellen, Dr. Phil across Nevada to pick up the historic (which later and Saturday Night Live. You have truly met the locals once you Lincoln Highway SUCCESS STORIES—A SpECIAl AdvERTISIng SECTIOn became U.S. 50) and make our way back to Sacramento. Small finish walking among the headstones. towns proved to be a good way to gently try and return to traveling. Sure, we would all I didn’t know Wally would even be in town. Last I heard he was prefer not to have to wear a mask and wash buying a camper and heading out to see the world when he retired. our hands every 20 minutes. But if you love For reasons I’m hopeful I’ll hear about some day, he was back in to travel, right now you have to make a few Eureka. compromises. With any luck, those will be short term and we will be able to travel more It’s possible the folks on the trip may have noticed the tear in my eye freely soon. or the crack in my voice when my friend showed up to say hi. Or when he starting telling a couple members of our group about the Our trip went well. We slipped in and out of a cemetery tour and I broke out laughing really loud.