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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). -
June -·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-1- -I -I -I -I
Wasatch Mountain Club JUNE -·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-1- -I -I -I -I I I -·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-· VOLUME 68, NUMBER 6, JUNE 1991 Magdaline Quinlan PROSPECTIVE MEMBER Leslie Mullins INFORMATION Managing Editors IF YOU HA VE MOVED: Please notify the WMC Member COVER LOGO: Knick Knickerbocker ship Director, 888 South 200 East, Suite 111, Salt Lake City, ADVERTISING: Jill Pointer UT 84111, of your new address. ART: Kate Juenger CLASSIFIED ADS: Sue De Vail IF YOU DID NOT RECEIVE YOUR RAMBLER: Con MAILING: Rose Novak, Mark McKenzie, Duke Bush tact the Membership Director to make sure your address is in PRODUCTION: Magdaline Quinlan the Club computer correctly. SKY CALENDAR: Ben Everitt IF YOU WANT TO SUBMIT AN ARTICLE: Articles, preferably typed double spaced, must be received by 6:00 pm THE RAMBLER (USPS 053-410) is published monthly by on the 15th of the month preceding publication. ~fail or de the WASATCH MOUNTAIN CLUB, Inc., 888 South 200 liver to the WMC office or to the Editor. Include your mrne East, Suite 111, Salt Lake City, UT 84111. Telephone: 363- and phone number on all submissions. 7150. Subscription rates of $12.00 per year are paid for by member ship dues only. Second-class Postage paid at Salt IF YOU WANT TO SUBMIT A PHOTO: We wekome Lake City, UT. photos of all kinds: black & white prints, color prints. and slides. Please include captions describing when and whcre POSTMASTER: Send address changes to THE RAM the photo was taken, and the names of the people in it (if you BLER, Membership Director, 888 South 200 East, Suite 111, know). -
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 -
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. -
A History of Beaver County, Utah Centennial County History Series
A HISTORY OF 'Beaver County Martha Sonntag Bradley UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF 'Beaver County Martha Sonntag Bradley The settlement of Beaver County began in February 1856 when fifteen families from Parowan moved by wagon thirty miles north to Beaver Valley. The county was created by the Utah legislature on 31 January 1856, a week before the Parowan group set out to make their new home. However, centuries before, prehistoric peoples lived in the area, obtaining obsidian for arrow and spear points from the Mineral Mountains. Later, the area became home to Paiute Indians. Franciscan Friars Dominguez and Escalante passed through the area in October 1776. The Mormon settlement of Beaver devel oped at the foot of the Tushar Mountains. In 1859 the community of Minersville was es tablished, and residents farmed, raised live stock, and mined the lead deposits there. In the last quarter of the nineteenth century the Mineral Mountains and other locations in the county saw extensive mining develop ment, particularly in the towns of Frisco and Newhouse. Mining activities were given a boost with the completion of the Utah South ern Railroad to Milford in 1880. The birth place of both famous western outlaw Butch Cassidy and inventor of television Philo T. Farnsworth, Beaver County is rich in history, historic buildings, and mineral treasures. ISBN: 0-913738-17-4 A HISTORY OF 'Beaver County A HISTORY OF Beaver County Martha Sonntag Bradley 1999 Utah State Historical Society Beaver County Commission Copyright © 1999 by Beaver County Commission All rights reserved ISBN 0-913738-17-4 Library of Congress Catalog Card Number 98-61325 Map by Automated Geographic Reference Center—State of Utah Printed in the United States of America Utah State Historical Society 300 Rio Grande Salt Lake City, Utah 84101-1182 Contents ACKNOWLEDGMENTS vii GENERAL INTRODUCTION ix CHAPTER 1 Beaver County: The Places That Shape Us . -
Geologic Mapping Marches Forward
I '- TABLE OF CONTENTS Geologic Mapping Marches Forward ...... ... .. ... .. 1 The Director's Malcolm P. Weiss ... .. ... ..... 3 Geologic Mapping in Dixie . .. .. 7 Perspective Teacher's Comer .. .. .. ... 9 Glad You Asked .......... .. .10 bv 1\1. Lee Allison Survey News .. .... .......12 Energy News . .. .. .. .. .... ..14 Preliminary Analysis: Conoco National Monument Well . ...15 There are at most about 35 geologists in Design by Vicky Clarke the national park system and some of those are not doing geology but collect Cover photo: The old Harrisburg town National Park Service Goes Geologic site, with the Pine Valley Mountains in ing entrance fees or the like, or regulat the distance, Washington County, Utah. Recently, while driving back to Salt ing pre-existing mines and oil wells. Photo by Bob Biek. Lake City from Denver, I stopped in at Contrast that with over 900 biologists in Dinosaur National Monument, one of the park system and you can easily see State of Utah the geologic wonders of the region. Be why individual parks focus on plants, Michael 0 . Leavitt, Governor tween the visitor's center and the quar animals, and biodiversity rather than Department of Natural Resources Ted Stewart, Executive Director ry is a spectacular, nearly vertical layer the rocks, fossils, and minerals. of sandstone with prominent ripple UGS Board The Park Service is recognizing this bias Russell C. Babcock, Jr., Chairman marks. Expecting the sign at the base of and two years ago established the Geo Richard R. Kennedy C. William Berge the outcrop to describe this geologic E.H . Deedee O'Brien Jerry Golden logic Resources Division (GRD), based feature, I was surprised to find instead Craig Nelson D. -
Probabilistic Source-To-Sink Analysis of the Provenance of the California Paleoriver: Implications for the Early Eocene Paleog
PROBABILISTIC SOURCE-TO-SINK ANALYSIS OF THE PROVENANCE OF THE CALIFORNIA PALEORIVER: IMPLICATIONS FOR THE EARLY EOCENE PALEOGEOGRAPHY OF WESTERN NORTH AMERICA by Evan Rhys Jones A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology). Golden, Colorado Date __________________________ Signed: _____________________________ Evan Jones Signed: _____________________________ Dr. Piret Plink-Björklund Thesis Advisor Golden, Colorado Date __________________________ Signed: _____________________________ Dr. M. Stephen Enders Interim Department Head Department of Geology and Geological Engineering ii ABSTRACT The Latest Paleocene to Early Eocene Colton and Wasatch Formations exposed in the Roan Cliffs on the southern margin of the Uinta Basin, UT make up a genetically related lobate wedge of dominantly fluvial deposits. Estimates of the size of the river that deposited this wedge of sediment vary by more than an order of magnitude. Some authors suggest the sediments are locally derived from Laramide Uplifts that define the southern margin of the Uinta Basin, the local recycling hypotheses. Other authors suggest the sediments were transported by a river system with headwaters 750 km south of the Uinta Basin, the California paleoriver hypothesis. This study uses source-to-sink analysis to constrain the size of the river system that deposited the Colton-Wasatch Fm. We pay particular attention to the what magnitude and recurrence interval of riverine discharge is preserved in the Colton-Wasatch Fm. stratigraphy, and consider the effects this has on scaling discharge to the paleo-catchment area of the system. We develop new scaling relationships between discharge and catchment area using daily gauging data from 415 rivers worldwide. -
Water Resources of Parowan Valley, Iron County, Utah
Prepared in cooperation with the Utah Department of Natural Resources Water Resources of Parowan Valley, Iron County, Utah Scientific Investigations Report 2017–5033 U.S. Department of the Interior U.S. Geological Survey Cover photograph: Parowan Valley looking east toward the Red Cliffs. Photograph by Tom Marston, U.S. Geological Survey, November 2013. Water Resources of Parowan Valley, Iron County, Utah By Thomas M. Marston Prepared in cooperation with the Utah Department of Natural Resources Scientific Investigations Report 2017–5033 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Acting Director U.S. Geological Survey, Reston, Virginia: 2017 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 http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://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: Marston, T.M., 2017, Water resources of Parowan Valley, Iron County, Utah: U.S. Geological Survey Scientific -
Grand Circle
Salt Lake City Green River - Moab Salt Lake City - Green River 60min (56mile) Grand Junction 180min (183mile) Colorado Crescent Jct. NM Great Basin Green River NP Arches NP Moab - Arches Goblin Valley 10min (5mile) SP Corona Arch Moab Grand Circle Map Capitol Reef - Green River Dead Horse Point 100min (90mile) SP Moab - Grand View Point NP: National Park 80min (45mile) NM: National Monument NHP: National Histrocal Park Bryce Canyon - Capitol Reef Canyonlands SP: State Park Capitol Reef COLORADO 170min (123mile) NP NP Moab - Mesa Verde Monticello Moab - Monument Valley 170min (140mile) NEVADA UTAH 170min (149mile) Bryce Cedar City Canyon NP Natural Bridges Canyon of the Cedar Breaks NM Blanding Ancients NM Mesa Verde - Monument Valley NM Kodacrome Basin SP 200min (150mile) Valley of Hovenweep 40min 70min NM Cortez (24mile) (60mile) Grand Staircase- the Gods 100min Escalante NM Durango Mt. Carmel (92mile) Muley Point Snow Canyon Jct. SP Goosenecks SP Zion NP Kanab Lake Powell Mexican Hat Mesa Verde Rainbow Monument Valley NP Coral Pink Sand Vermillion Page Bridge NM Four Corners Las Vegas - Zion Dunes SP Cliffs NM Navajo Tribal Park Aztec Ruins NM 170min (167mile) Antelope Pipe Spring NM Horseshoe Shiprock Aztec Bend Canyon Mesa Verde - Chinle 200min (166mile) Mt.Carmel Jct. - North Rim Navajo NM 140min (98mile) Kayenta Farmington Monument Valley - Chinle Mesa Verde - Chaco Culture Valley of Fire Page - North Rim Page - Cameron Page - Monument Valley 140min (134mile) 230min (160mile) SP 170min (124mile) 90min (83mile) Grand Canyon- 130min -
Conifers of the San Francisco Mountains, San Rafael Swell, and Roan Plateau Ronald M
Great Basin Naturalist Volume 31 | Number 3 Article 11 9-30-1971 Conifers of the San Francisco Mountains, San Rafael Swell, and Roan Plateau Ronald M. Lanner Utah State University Ronald Warnick Utah State University Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Lanner, Ronald M. and Warnick, Ronald (1971) "Conifers of the San Francisco Mountains, San Rafael Swell, and Roan Plateau," Great Basin Naturalist: Vol. 31 : No. 3 , Article 11. Available at: https://scholarsarchive.byu.edu/gbn/vol31/iss3/11 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. CONIFERS OF THE SAN FRANCISCO MOUNTAINS, SAN RAFAEL SWELL, AND ROAN PLATEAU 1 Ronald M. Lanner2 and Ronald Warnick 2 This is the second in a series of notes on conifer distribution in The Great Basin and adjacent mountain areas. An earlier paper (Lanner, 1971) presented results of field surveys in selected parts of northern Utah. This article will cover three Utah areas further to the south, which represent diverse geological and environmental conditions. The occurrence of previously unrecorded species localities is supported by specimens deposited in the Intermountain Herbarium at Utah State University, Logan, Utah (UTC). San Francisco Mountains The San Francisco Mountains, a typical Great Basin fault-block range, are located in Beaver and Millard counties. The range is ori- ented roughly on a north-south axis and is about 18 miles in length. -
A New Species of Mallophora from the Great Salt Lake Desert (Diptera: Asilidae)
Great Basin Naturalist Volume 18 Number 2 Article 1 11-15-1958 A new species of Mallophora from the Great Salt Lake Desert (Diptera: Asilidae) D. Elmer Johnson University of Utah, Salt Lake City, Utah Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Johnson, D. Elmer (1958) "A new species of Mallophora from the Great Salt Lake Desert (Diptera: Asilidae)," Great Basin Naturalist: Vol. 18 : No. 2 , Article 1. Available at: https://scholarsarchive.byu.edu/gbn/vol18/iss2/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Iinuu. bu::;T. CCU |mar131959 The Great Basin NaturalisL£fl^ Published by the Brigham Young University, Provo, Utah Volume XVIII November 15, 1958 No. 2 A NEW SPECIES OF MALLOPilORA FROM THE (iREAT SALT LAKE DESER 1 (DIPTERA: ASILIDAE)^ D. Elmer Johnson" During the course of an ecological study of the southern exten- tion of the Great Salt Lake Desert of Utah, a number of apparently undescribed species of insects have come to light. One of these, a fly of the family Asilidae. is described below. Mallophora (Mallophorina) pallida, n. sp. Male: Head silvery gray pollinose, somewhat less densly so on the upper front. Pile of lower side of first and all of second antennal segments black, rest of hair of head white. First and third antennal segments black, second segment brown. -
Little Salt Lake (Lake, Iron County) From: Utah Place Names
Little Salt Lake (lake, Iron County) from: Utah Place Names LITTLE SALT LAKE (Iron County) was a seasonal, small, shallow, brackish sink lying north of Parowan* in Parowan Valley. The lake was named in contrast to the larger and better-known Great Salt Lake located near Salt Lake City*. It was also called Parowan Lake. The Piutes called it "Paragoon," which means "vile water." The adjacent town of Paragonah* takes its name from this Indian word. Parowan also evolved from Paragoons, Marsh People, the name of the Piede band living near the water in earlier days. >R9,10W,T33S,SLM; 5,675' (1,730m). Bibliography: Dalton, Luella Adams. History of Iron County Mission. Parowan, UT: n.p., n.d. Layton, Stanford J. "Fort Rawlins, Utah: A Question of Mission and Means." Utah Historical Quarterly 42 (Winter 1974): 68-83. Pratt, Parley P. Autobiography of Parley P. Pratt. Edited by his son, Parley P. Pratt. Salt Lake City: Deseret Book Co., 1970. Reid, Hyrum Lorenzo. Brigham Young's Dixie of the Desert: Exploration and Settlement. Zion National Park, UT: Zion Natural History Association, 1964. EXPLANATION OF SYMBOLS... 1. An asterisk (*) following a place name indicates past or present inhabitation. 2. When a series of letters and numbers are present towards the end of an entry after the ">" symbol, the first group indicates section/township/range as closely as can be pinpointed (i.e., S12,T3S,R4W,SLM, or USM). A section equals approximately one square mile, reflecting U.S. Geological Survey topographic map sections. Because Utah is not completely mapped, some entries are incomplete.