Death Valley FONSI
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Hecastocleideae (Hecastocleidoideae)
Chapter 16 Hecastocleideae (Hecastocleidoideae) Vicki A. Funk and D.J. Nicholas Hind HISTORICAL OVERVIEW AND MORPHOLOGY Carduoideae—'rest of the family' split (see Chapters 12 and 44) and this placement has 100% bootstrap support. Hecastodeis shockleyi A. Gray was described in 1882 and its Its current position is supported by its distinct morphol- unusual morphology and restricted distribution has made ogy and strong support from molecular data. Its near- it sought after for herbarium specimens. This shrub is est downstream neighbor, however, is somewhat tenu- easily identified because of its single flowered heads that ous, because the position of the branch just below it are re-aggregated on a receptacle in groups of one to five (Gochnatieae) has only 65% bootstrap support (Panero heads; each group of heads is subtended by a relatively and Funk 2008) and might collapse into a polytomy large spiny whitish or greenish bract (Fig. 16.1). Gray with Mutisieae s.str. If one does the phylogenetic analysis (1882) commented that is was "a remarkable addition without Hecastodeis, there is no change in the phylogeny to the few known North American Mutisieae, to stand of the family. near Ainsliaea DC. but altogether sui generis and of pecu- liar habit." According to Williams (1977) the generic name Hecastodeis, "... comes from the Greek roots, ekastos TAXONOMY meaning 'each' and kleio meaning 'to shut up'", referring to each flower having its own involucre. The species The genus is monotypic and has always been recognized was named after William H. Shockley one of the first as such since its original description by Gray (1882). -
Mineral Resources and Mineral Resource Potential of the Saline Valley and Lower Saline Wilderness Study Areas Inyo County, California
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Mineral resources and mineral resource potential of the Saline Valley and Lower Saline Wilderness Study Areas Inyo County, California Chester T. Wrucke, Sherman P. Marsh, Gary L. Raines, R. Scott Werschky, Richard J. Blakely, and Donald B. Hoover U.S. Geological Survey and Edward L. McHugh, Clay ton M. Rumsey, Richard S. Gaps, and J. Douglas Causey U.S. Bureau of Mines U.S. Geological Survey Open-File Report 84-560 Prepared by U.S. Geological Survey and U.S. Bureau of Mines for U.S. Bureau of Land Management This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1984 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Mineral resources and mineral resource potential of the Saline Valley and Lower Saline Wilderness Study Areas Inyo County, California by Chester T. Wrucke, Sherman P. Marsh, Gary L. Raines, R. Scott Werschky, Richard J. Blakely, and Donald B. Hoover U.S. Geological Survey and Edward L. McHugh, Clayton M. Rumsey, Richard S. Gaps, and J. Douglas Causey U.S. Bureau of Mines U.S. Geological Survey Open-File Report 84-560 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. 1984 ILLUSTRATIONS Plate 1. Mineral resource potential map of the Saline Valley and Lower Saline Wilderness Study Areas, Inyo County, California................................ In pocket Figure 1. Map showing location of Saline Valley and Lower Saline Wilderness Study Areas, California.............. 39 2. -
Interest and the Panamint Shoshone (E.G., Voegelin 1938; Zigmond 1938; and Kelly 1934)
109 VyI. NOTES ON BOUNDARIES AND CULTURE OF THE PANAMINT SHOSHONE AND OWENS VALLEY PAIUTE * Gordon L. Grosscup Boundary of the Panamint The Panamint Shoshone, also referred to as the Panamint, Koso (Coso) and Shoshone of eastern California, lived in that portion of the Basin and Range Province which extends from the Sierra Nevadas on the west to the Amargosa Desert of eastern Nevada on the east, and from Owens Valley and Fish Lake Valley in the north to an ill- defined boundary in the south shared with Southern Paiute groups. These boundaries will be discussed below. Previous attempts to define the Panamint Shoshone boundary have been made by Kroeber (1925), Steward (1933, 1937, 1938, 1939 and 1941) and Driver (1937). Others, who have worked with some of the groups which border the Panamint Shoshone, have something to say about the common boundary between the group of their special interest and the Panamint Shoshone (e.g., Voegelin 1938; Zigmond 1938; and Kelly 1934). Kroeber (1925: 589-560) wrote: "The territory of the westernmost member of this group [the Shoshone], our Koso, who form as it were the head of a serpent that curves across the map for 1, 500 miles, is one of the largest of any Californian people. It was also perhaps the most thinly populated, and one of the least defined. If there were boundaries, they are not known. To the west the crest of the Sierra has been assumed as the limit of the Koso toward the Tubatulabal. On the north were the eastern Mono of Owens River. -
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. -
Birds of the California Desert
BIRDS OF THE CALIFORNIA DESERT A. Sidney England and William F. Laudenslayer, Jr. i INTRODUCTION i \ 1 The term, "California desert", as used herein, refers to a politically defined region, most of i which is included in the California Desert Conservation Area (CDCA) designated by the Federal Land ; and Management Act of 1976 (FLPMA). Of the 25 million acres in the CDCA, about one-half are i public lands, most of which are managed by the Bureau of Land Management (BLM) according to the "980 P California Desert Conservation Area Plan mandated by FLPMA. The California desert encompasses those portions of the Great Basin Desert (east of the White and lnyo Mountains and A south of the California-Nevada border), the Mojave Desert, and the Colorado Desert which occur " within California; it does not include areas of riparian, aquatic, urban, and agricultural habitats . adjacent to the Colorado River. (Also see chapters on Geology by Norris and Bioclimatology by E3irdsI4 are the most conspicuous vertebrates found in the California deserts. Records exist for at least 425 species (Garrett and Dunn 1981) from 18 orders and 55 families. These counts far exceed those for mammals, reptiles, amphibians and fish, and they are similar to totals for the entire state -- 542 species from 20 orders and 65 families (Laudenslayer and Grenfell 1983). These figures may seem surprisingly similar considering the harsh, arid climates often believed characteristic of I desert environments. However, habiiats found in the California desert range from open water and h marshes at the Salton Sea to pinyon-juniper woodland and limber pinelbristlecone pine forests on a few mountain ranges. -
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. -
Inferences Regarding Aboriginal Hunting Behavior in the Saline Valley, Inyo County, California
Journal of California and Great Basin Anthropology Vol. 2, No. I, pp. 60-79(1980). Inferences Regarding Aboriginal Hunting Behavior in the Saline Valley, Inyo County, California RICHARD A. BROOK HE documented use of stone "hunting a member of the 1861 Boundary Survey Party Tblinds" behind which marksmen hid them reconnoitering the Death Valley region. The selves "ve'/7//-6'o?m-e"i (Baillie-Grohman 1884: chronicler observed: 168) waiting for sheep to be driven along trails, can be found in the writings of a number of . curious structures ... on the tops of early historians (Baillie-Grohman 1884; round bald hills, a short distance to the Spears 1892; Muir 1901; Bailey 1940). Recent northwest of the springs, being low walls of archaeological discoveries of rock features loose stones curved in the shape of a demi lune, about ten feet in length and about believed to be hunting blinds at the Upper three feet high . , . , There were twenty or Warm Springs (Fig. I) in Saline Valley, Inyo thirty of them [Woodward 1961:49], County, California, provide a basis to substan tiate, build upon, and evaluate these observa This paper discusses a series of 60 such piled- tions and the ethnographic descriptions of up boulder features recorded within a I km.^ hunting in the Great Basin (Steward 1933, area at Upper Warm Springs (Fig. 2). 1938, 1941; Driver 1937; Voegelin 1938; The same chronicler offered some tentative Stewart 1941). An examination of these explanations as to their function: features, their location, orientation, and asso ciations in -
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. -
5 Day Itinerary
by a grant from Travel Nevada. Travel from grant a by possible made brochure This JUST 98 MILES NORTH OF LAS VEGAS ON HIGHWAY 95. HIGHWAY ON VEGAS LAS OF NORTH MILES 98 JUST www.beattynevada.org Ph: 1.866.736.3716 Ph: Studio 401 Arts & Salon & Arts 401 Studio Mama’s Sweet Ice Sweet Mama’s Smash Hit Subs Hit Smash VFW Chow VFW Smokin’ J’s BBQ J’s Smokin’ shoot out or two performed by our local cowboys. cowboys. local our by performed two or out shoot Gema’s Café Gema’s historical area you might catch a glimpse of a a of glimpse a catch might you area historical Death Valley Coffee Time Coffee Valley Death of our local eateries. If you are in the downtown downtown the in are you If eateries. local our of Roadhouse 95 Roadhouse After your day trips into the Valley, relax at one one at relax Valley, the into trips day your After Sourdough Saloon & Eatery & Saloon Sourdough lunch at Beatty’s Cottonwood Park. Park. Cottonwood Beatty’s at lunch Hot Stuff Pizza Stuff Hot Store or enjoy walking your dog or having a picnic picnic a having or dog your walking enjoy or Store Mel’s Diner Mel’s Town, the Famous Death Valley Nut and Candy Candy and Nut Valley Death Famous the Town, Happy Burro Chili & Beer & Chili Burro Happy open daily from 10 am to 3 pm, Rhyolite Ghost Ghost Rhyolite pm, 3 to am 10 from daily open The Death Valley Nut & Candy Store Candy & Nut Valley Death The can find in our little town, the Beatty Museum, Museum, Beatty the town, little our in find can LOCAL SHOPS & EATERIES & SHOPS LOCAL Day area, be sure to visit the unique businesses that you you that businesses unique the visit to sure be area, BEATTY Between trips to explore the Death Valley Valley Death the explore to trips Between your plan for each day, and set up a check in time. -
Introduction
1 INTRODUCTION This monograph is an introductory descriptive grammar of Tlimpisa Shoshone, meant to provide both layman and specialist with a basic understanding of how the language works as a linguistic system. In this sense, it is intended to be a "nuts and bolts" grammar with lots of examples illustrating the most important grammatical elements and processes in the language. 1 Tlimpisa Shoshone is a dialect of the language most often called Panamint in the technical literature (e.g., Freeze and Iannucci 1979, Henshaw 1883, Kroeber 1939, Lamb 1958a and 1964, McLaughlin 1987, Miller 1984) . The language is also known as Panamint Shoshone (Fowler and Fowler 1971, Merriam 1904, Miller et al. 1971), Koso (= Coso) or Koso Shoshone (Kroeber 1925, Lamb 1958a), and simply Shoshone (Steward 1938). Panamint and two other closely related languages, Shoshone proper and Comanche, comprise the Central Numic branch of the Numic subfamily of the northern division of the uto-Aztecan family of American Indian languages (see Lamb 1964, Miller 1984, Kaufman and Campbell 1981). Speakers of uto-Aztecan languages occupied more territory in aboriginal America than any other group. More than 30 Uto-Aztecan languages were spoken over a vast area stretching from the Salmon River in central Idaho south through the Great Basin and peripheral areas into the Southwest and through northern and central Mexico. Colonies of Aztecan speakers were also scattered further south into Central America. At the time of 1 UTO-AZTECAN FAMILY Northern Division NUMlC Central Numic -
The California Desert CONSERVATION AREA PLAN 1980 As Amended
the California Desert CONSERVATION AREA PLAN 1980 as amended U.S. DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGEMENT U.S. Department of the Interior Bureau of Land Management Desert District Riverside, California the California Desert CONSERVATION AREA PLAN 1980 as Amended IN REPLY REFER TO United States Department of the Interior BUREAU OF LAND MANAGEMENT STATE OFFICE Federal Office Building 2800 Cottage Way Sacramento, California 95825 Dear Reader: Thank you.You and many other interested citizens like you have made this California Desert Conservation Area Plan. It was conceived of your interests and concerns, born into law through your elected representatives, molded by your direct personal involvement, matured and refined through public conflict, interaction, and compromise, and completed as a result of your review, comment and advice. It is a good plan. You have reason to be proud. Perhaps, as individuals, we may say, “This is not exactly the plan I would like,” but together we can say, “This is a plan we can agree on, it is fair, and it is possible.” This is the most important part of all, because this Plan is only a beginning. A plan is a piece of paper-what counts is what happens on the ground. The California Desert Plan encompasses a tremendous area and many different resources and uses. The decisions in the Plan are major and important, but they are only general guides to site—specific actions. The job ahead of us now involves three tasks: —Site-specific plans, such as grazing allotment management plans or vehicle route designation; —On-the-ground actions, such as granting mineral leases, developing water sources for wildlife, building fences for livestock pastures or for protecting petroglyphs; and —Keeping people informed of and involved in putting the Plan to work on the ground, and in changing the Plan to meet future needs. -
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.