2019 Death Valley Visitor Guide
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June 20, 2017 Movie Year STAR 351 P Acu Lan E, Bish Op a B Erd
Movie Year STAR 351 Pacu Lane, Bishop Aberdeen Aberdeen Restaurant, Olancha Airflite Diner, Alabama Hills Ranch Anchor Alpenhof Lodge, Mammoth Lakes Benton Crossing Big Pine Bishop Bishop Reservation Paiute Buttermilk Country Carson & Colorado Railroad Gordo Cerro Chalk Bluffs Inyo Convict Lake Coso Junction Cottonwood Canyon Lake Crowley Crystal Crag Darwin Deep Springs Big Pine College, Devil's Postpile Diaz Lake, Lone Pine Eastern Sierra Fish Springs High Sierras High Sierra Mountains Highway 136 Keeler Highway 395 & Gill Station Rd Hoppy Cabin Horseshoe Meadows Rd Hot Creek Independence Inyo County Inyo National Forest June Lake June Mountain Keeler Station Keeler Kennedy Meadows Lake Crowley Lake Mary 2012 Gold Rush Expedition Race 2013 DOCUMENTARY 2013 Gold Rush Expedition Race 2014 DOCUMENTARY 2014 Gold Rush Expedition Race 2015 DOCUMENTARY 26 Men: Incident at Yuma 1957 Tristram Coffin x 3 Bad Men 1926 George O'Brien x 3 Godfathers 1948 John Wayne x x 5 Races, 5 Continents (SHORT) 2011 Kilian Jornet Abandoned: California Water Supply 2016 Rick McCrank x x Above Suspicion 1943 Joan Crawford x Across the Plains 1939 Jack Randall x Adventures in Wild California 2000 Susan Campbell x Adventures of Captain Marvel 1941 Tom Tyler x Adventures of Champion, The 1955-1956 Champion (the horse) Adventures of Champion, The: Andrew and the Deadly Double1956 Champion the Horse x Adventures of Champion, The: Crossroad Trail 1955 Champion the Horse x Adventures of Hajji Baba, The 1954 John Derek x Adventures of Marco Polo, The 1938 Gary Cooper x Adventures of Wild Bill Hickok 1951-1958 Guy Madison Affairs with Bears (SHORT) 2002 Steve Searles Air Mail 1932 Pat O'Brien x Alias Smith and Jones 1971-1973 Ben Murphy x Alien Planet (TV Movie) 2005 Wayne D. -
2021 Magazine
July 2021 Welcome to the July 2021 edition of BADWATER® Magazine! We are AdventureCORPS®, producers of ultra-endurance sports events and adventure travel across the globe, and the force behind the BADWATER® brand. This magazine celebrates the entire world-wide Badwater® / AdventureCORPS® series of races, all the Badwater Services, Gear, Drinks, and Clothing, and what we like to call the Badwater Family and the Badwater Way of Life. Adventure is our way of life, so – after the sad and disastrous 2020 when we were not able to host any of our life-changing events – we are pleased to be fully back in action in 2021! Well, make that almost fully: Due to pandemic travel bans still in place, international participation in our USA-based events is not where we want it and that’s really unfortunate. Badwater 135 is the de facto Olympics of Ultrarunning and the 135-Mile World Championship, so we always want as many nationalities represented as possible. (The inside front cover of this magazine celebrates all sixty-one nationalities which have been represented on the Badwater 135 start line over the years.) Our new six-day stage race across Armenia – Artsakh Ultra – will have to wait yet another year to debut in 2022, two years later than planned. But it will be incredible, the ultimate stage race with six days of world-class trail running through several millennia of incredible culture and history, and across the most dramatic and awe-inspiring landscapes. This year, we are super excited to have brought two virtual races to life, first for the 31 days of January, and then for 16 days in April. -
Death Valley National Park
COMPLIMENTARY $3.95 2019/2020 YOUR COMPLETE GUIDE TO THE PARKS DEATH VALLEY NATIONAL PARK ACTIVITIES • SIGHTSEEING • DINING • LODGING TRAILS • HISTORY • MAPS • MORE OFFICIAL PARTNERS T:5.375” S:4.75” PLAN YOUR VISIT WELCOME S:7.375” In T:8.375” 1994, Death Valley National SO TASTY EVERYONE WILL WANT A BITE. Monument was expanded by 1.3 million FUN FACTS acres and redesignated a national park by the California Desert Protection Act. Established: Death Valley became a The largest national park below Alaska, national monument in 1933 and is famed this designation helped focus protection for being the hottest, lowest and driest on one the most iconic landscapes in the location in the country. The parched world. In 2018 nearly 1.7 million people landscape rises into snow-capped mountains and is home to the Timbisha visited the park, a new visitation record. Shoshone people. Death Valley is renowned for its colorful Land Area: The park’s 3.4 million acres and complex geology. Its extremes of stretch across two states, California and elevation support a great diversity of life Nevada. and provide a natural geologic museum. Highest Elevation: The top of This region is the ancestral homeland Telescope Peak is 11,049 feet high. The of the Timbisha Shoshone Tribe. The lowest is -282 feet at Badwater Basin. Timbisha established a life in concert Plants and Animals: Death Valley with nature. is home to 51 mammal species, 307 Ninety-three percent of the park is bird species, 36 reptile species, two designated wilderness, providing unique amphibian species and five fish species. -
Open-File/Color For
Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4). -
Death Valley Springs Geochemical Investigation Yucca Mountain Nuclear Repository, Inyo County Oversight-1998
The HYDRODYNAMICS Group studies in mass and energy transport in the earth Death Valley Springs Geochemical Investigation Yucca Mountain Nuclear Repository, Inyo County Oversight-1998 Submitted to: Inyo County Planning Department: Yucca Mountain Repository Oversight Program March, 1999 Michael J. King, R.G., C.HG. John D. Bredehoeft, Ph.D., NAE The HYDRODYNAMICS Group 16711 76th Avenue West, Edmonds, WA 98026 Phone (425) 787-6728, Fax (425) 742-8493 Page 1 The Hydrodynamics Group DEATH VALLEY SPRINGS GEOCHMICAL INVESTIGATION YUCCA MOUNTAIN NUCLEAR WASTE REPOSITORY, INYO COUNTY OVERSIGHT-1998 EXECUTIVE SUMMARY Yucca Mountain, Nevada is under study as the site of the only proposed high-level nuclear waste repository in the United States. The repository concept uses the philosophy of multiple barriers, both engineered and natural, each of which impedes the movement of radionuclides into the accessible environment. The proposed repository would be in the unsaturated zone in Tertiary tuffaceous rocks. The principal transporting mechanism for radionuclides is moving ground water. Underlying the repository is an extensive Lower Carbonate Aquifer known to be highly permeable. Inyo County, as an affected unit of local government under the Nuclear Waste Policy Act, as amended, is concerned with the connections between the Lower Carbonate Aquifer underlying Yucca Mountain and the carbonate sources of waters in Inyo County, especially the Death Valley region. This report is a summary of the investigations conducted by Inyo County’s consultants, the Hydrodynamics Group, during calendar year 1998. This report presents the results of The Hydrodynamics Group’s 1998 collection of water samples from 23 springs and 2 creeks in Death Valley. -
Distribution of Amargosa River Pupfish (Cyprinodon Nevadensis Amargosae) in Death Valley National Park, CA
California Fish and Game 103(3): 91-95; 2017 Distribution of Amargosa River pupfish (Cyprinodon nevadensis amargosae) in Death Valley National Park, CA KRISTEN G. HUMPHREY, JAMIE B. LEAVITT, WESLEY J. GOLDSMITH, BRIAN R. KESNER, AND PAUL C. MARSH* Native Fish Lab at Marsh & Associates, LLC, 5016 South Ash Avenue, Suite 108, Tempe, AZ 85282, USA (KGH, JBL, WJG, BRK, PCM). *correspondent: [email protected] Key words: Amargosa River pupfish, Death Valley National Park, distribution, endangered species, monitoring, intermittent streams, range ________________________________________________________________________ Amargosa River pupfish (Cyprinodon nevadensis amargosae), is one of six rec- ognized subspecies of Amargosa pupfish (Miller 1948) and survives in waters embedded in a uniquely harsh environment, the arid and hot Mojave Desert (Jaeger 1957). All are endemic to the Amargosa River basin of southern California and Nevada (Moyle 2002). Differing from other spring-dwelling subspecies of Amargosa pupfish (Cyprinodon ne- vadensis), Amargosa River pupfish is riverine and the most widely distributed, the extent of which has been underrepresented prior to this study (Moyle et al. 2015). Originating on Pahute Mesa, Nye County, Nevada, the Amargosa River flows intermittently, often under- ground, south past the towns of Beatty, Shoshone, and Tecopa and through the Amargosa River Canyon before turning north into Death Valley National Park and terminating at Badwater Basin (Figure 1). Amargosa River pupfish is data deficient with a distribution range that is largely unknown. The species has been documented in Tecopa Bore near Tecopa, Inyo County, CA (Naiman 1976) and in the Amargosa River Canyon, Inyo and San Bernardino Counties, CA (Williams-Deacon et al. -
Death Valley Lower Carbonate Aquifer Monitoring Program- Wells Down Gradient of the Proposed Yucca Mountian Nuclear Waste Repository
iU4 MOL.20080509.0010 DEATH VALLEY LOWER CARBONATE AQUIFER MONITORING PROGRAM- WELLS DOWN GRADIENT OF THE PROPOSED YUCCA MOUNTIAN NUCLEAR WASTE REPOSITORY U.S. DEPARTMENT OF ENERGY COOPERATIVE AGREEMENT DE-FC28-06RW12368 YEAR ONE PROJECT REPORT PREPARED BY INYO COUNTY YUCCA MOUNTAIN REPOSITORY ASSESSMENT OFFICE Inyo County completed Year One of U.S. Department of Energy Cooperative Agreement No. DE-FC28-06RW12368. This report presents the results of research conducted within this cooperative agreement in the context of Inyo County's Yucca Mountain oversight program goals and objectives. The Hydrodynamics Group, LLC prepared this report for Inyo County Yucca Mountain repository Assessment Office. The overall goal of Inyo County's Yucca Mountain research program is the evaluation of far-field issues related to potential transport, by ground water, of radionuclide into Inyo County, including Death Valley, and the evaluation of a connection between the Lower Carbonate Aquifer (LCA) and the biosphere. Data collected within the cooperative agreement is included in interpretive illustrations and discussions of the results of our analysis. The central element's of this Cooperative Agreement program was the drilling of exploratory wells, analysis of geochemical data, geophysical surveys, and geological mapping of the Southern Funeral Mountain Range. The culmination of this research was two numerical ground water models of the Southern Funeral Mountain Range and Yucca Mountain region demonstrating the potential of a hydraulic connection between the LCA and the major springs in the Furnace Creek area of Death Valley. 1.0 Introduction The focus of the investigations by the Hydrodynamics Group for Inyo County is to assemble the best possible data on the Paleozoic Carbonate Aquifer, and then to use that data to assess the likelihood of contaminant transport from the planned Yucca Mountain high-level nuclear waste repository to the biosphere in Inyo County. -
NV EAS Plan Attachment 2-Operational Areas
Nevada Emergency Alert System Plan Attachment 2. Nevada EAS Operational Areas ATTACHMENT 2 NEVADA EAS OPERATIONAL AREAS The Nevada EAS Operational Area is divided into three sections. Western Nevada/Eastern California . Southern Nevada/Inyo County, California . Eastern Nevada Jurisdictions within the Nevada EAS Operational Areas Western Nevada/Eastern Eastern Nevada Southern Nevada/Inyo County, California California Carson City Elko County Clark County Churchill County Eureka County Esmeralda County Douglas County Humboldt County Lincoln County Lyon County Lander County Nye County (southern) Mineral County White Pine County Inyo County (CA) Nye County (northern) San Bernardino County (CA) Pershing County Mohave County (AZ) Washoe County Storey County Alpine County (CA)* El Dorado County (CA)* Lassen County (CA) Modoc County (CA)* Mono County (CA) Placer County (CA)* Nevada EAS Operational Areas Plumas County (CA)* . Sierra County (CA)* 2 *Areas east of the Sierra Nevada crest. Italicized text refers to non-Nevada jurisdictions. Southern Inyo County, California covers the area from the village of Independence in the north to the south county line and includes the communities of Shoshone, Death Valley National Park and headquarters, Furnace Creek, Cartagom, Barlett, Stovepipe Wells, Panamint Springs, Keeler, Olancha, Little Lake, Lone Pine, and Lake Owens. The area north of Independence is in Attachment the Western Nevada/Eastern California Operational Area. No broadcast stations in the Northern Inyo County area are able to receive signals from Las Vegas or Reno broadcast stations. Local EAS activations can be made through the use of CAP EAS by originating officials or by going through the California Governor's Office of Emergency Services. -
Ice Rafts Not Sails: Floating the Rocks at Racetrack Playa ͒ Ralph D
Ice rafts not sails: Floating the rocks at Racetrack Playa ͒ Ralph D. Lorenza Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland 20723 ͒ Brian K. Jacksonb NASA Goddard Spaceflight Center, Greenbelt, Maryland 20771 ͒ Jason W. Barnesc Department of Physics, University of Idaho, Moscow, Idaho 83844 ͒ Joe Spitaled Space Science Institute, Boulder, Colorado 80301 ͒ John M. Kellere Department of Physics, California Polytechnic State University, San Luis Obispo, California 93407 ͑Received 15 February 2010; accepted 27 August 2010͒ We suggest that the existence of many of the rock-carved trails at Racetrack Playa in Death Valley National Park is predominantly due to the effect of arbitrarily weak winds on rocks that are floated off the soft bed by small rafts of ice, as also occurs in arctic tidal beaches to form boulder barricades. These ice cakes need not have a particularly large surface area if the ice is adequately thick—the ice cakes allow the rocks to move by buoyantly reducing the reaction and friction forces at the bed, not by increasing the wind drag. The parameter space of ice thickness and extent versus rock size for flotation is calculated and found to be reasonable. We demonstrate the effect with a simple experiment. © 2011 American Association of Physics Teachers. ͓DOI: 10.1119/1.3490645͔ I. INTRODUCTION literature. All the discussions involve a sheet of ice acting as a means of increasing the area on which wind can act ͑for Among the many geological attractions1 in Death Valley example, Ref. 4 refers to ice sheets 20 mϫ20 m and National Park in California is Racetrack Playa. -
Gene Autry Personal Papers and Business Archives T.MSA.28
http://oac.cdlib.org/findaid/ark:/13030/c8zp46v9 No online items Finding Aid to the Gene Autry Personal Papers and Business Archives T.MSA.28 Finding aid prepared by Holly Rose Larson Autry National Center, Autry Library 4700 Western Heritage Way Los Angeles, CA, 90027 (323) 667-2000 ext. 349 [email protected] 2012 January 27 Finding Aid to the Gene Autry T.MSA.28 1 Personal Papers and Business Archives T.MSA.28 Title: Gene Autry Personal Papers and Business Archives Identifier/Call Number: T.MSA.28 Contributing Institution: Autry National Center, Autry Library Language of Material: English Physical Description: 446.0 Linear feet(approximately 300 boxes) Date (inclusive): 1900-2002 Abstract: Orvon Gene Autry (born September 29, 1907 - died October 2, 1998) was a legendary recording and movie star whose career spanned over 60 years in the entertainment industry. Sometimes called “The Singing Cowboy,” Autry was also a broadcast executive for KTLA and owned the Major League baseball team, the Los Angeles Angels, among other business pursuits. Autry also co-founded the Gene Autry Western Heritage Museum, now known as The Autry National Center of the American West, with wife Jackie Autry and Monte and Joanne Hale in 1988. The Gene Autry Personal Papers and Business Archives span from 1900 to 2002 and document Autry’s personal and family life, including wives Ina Mae Spivey and Jackie Ellam; Autry’s military career during World War II; entertainment career; other business holdings; and honors received. Materials include administrative records; advertising material; awards; ephemera; correspondence; photographic material; posters; scrapbooks; and sheet music. -
California State University, Northridge
CALIFORNIA STATE UNIVERSITY, NORTHRIDGE THE CHANGING FACE OF TOURISM IN DEATH VALLEY A thesis submitted in partial fulfillment of the requirements For the degree of Master of Arts in Geography By Tina White December 2013 The thesis of Tina White is approved: ____________________________________ _____________________ Ronald Davidson, Ph.D. Date ____________________________________ _____________________ Edward Jackiewicz, Ph.D. Date ____________________________________ _____________________ Julie E. Laity, Ph.D., Chair Date California State University, Northridge ii ACKNOWLEDGEMENTS I acknowledge, and most heartily thank, the CSUN faculty members who have continuously supported and encouraged me through the (too) many years I have spent working towards this degree. First and foremost, I am grateful for and to my thesis advisor, Professor Julie Laity, who has taught me about physical geography and academic success in the classroom, in the field, and during our talks in her office. And, of course, there is she from whom I have learned so much geomorphology and with whom I have had so much fun in the field: Professor Amalie Orme. To my thesis committee members Ron Davidson and Ed Jackiewicz, thank you so much for your time and assistance; I appreciate your expertise and input. Further, I have been fortunate to have taken classes with and/or had the opportunity to learn informally from the entire CSUN Geography Department faculty teaching from 1997 through the present at one time or another, as well as from some great folks in the CSUN Geology Department. I have learned something from each and every one of you, and will be eternally grateful. I also want to thank multiple employees at Death Valley National Park, in particular Terry Baldino and Alex Cabana and their numerous staff members, who took the time to speak with me about this topic; their input was invaluable and their insights intriguing. -
Trail Formation by Ice-Shoved ``Sailing Stones'' Observed at Racetrack Playa
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Earth Surf. Dynam. Discuss., 2, 1005–1022, 2014 www.earth-surf-dynam-discuss.net/2/1005/2014/ doi:10.5194/esurfd-2-1005-2014 ESURFD © Author(s) 2014. CC Attribution 3.0 License. 2, 1005–1022, 2014 This discussion paper is/has been under review for the journal Earth Surface Dynamics (ESurfD). Trail formation by Please refer to the corresponding final paper in ESurf if available. ice-shoved “sailing stones” observed at Trail formation by ice-shoved “sailing Racetrack Playa stones” observed at Racetrack Playa, R. D. Lorenz et al. Death Valley National Park Title Page 1 2 3 4 5 R. D. Lorenz , J. M. Norris , B. K. Jackson , R. D. Norris , J. W. Chadbourne , Abstract Introduction and J. Ray2 Conclusions References 1 Applied Physics Laboratory, The Johns Hopkins University, Laurel, Maryland, USA Tables Figures 2Interwoof, Santa Barbara, California, USA 3Dept. of Terrestrial Magnetism, Carnegie Institution for Science, Washington, D.C., USA 4Scripps Institution of Oceanography, La Jolla, California, USA J I 5 University of Portland, Oregon, USA J I Received: 17 August 2014 – Accepted: 27 August 2014 – Published: 28 August 2014 Back Close Correspondence to: R. D. Lorenz ([email protected]) Full Screen / Esc Published by Copernicus Publications on behalf of the European Geosciences Union. Printer-friendly Version Interactive Discussion 1005 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract ESURFD Trails in the usually-hard mud of Racetrack Playa in Death Valley National Park attest to the seemingly-improbable movement of massive rocks on an exceptionally flat sur- 2, 1005–1022, 2014 face.