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The Climate of Death Valley, California
THE CLIMATE OF DEATH VALLEY, CALIFORNIA BY STEVEN ROOF AND CHARLIE CALLAGAN The notoriously extreme climate of Death Valley records shows significant variability in the long-term, including a 35% increase in precipitation in the last 40 years. eath Valley National Park, California, is widely known for its extreme hot and Ddry climate. High summer temperatures, low humidity, high evaporation, and low pre- cipitation characterize the valley, of which over 1300 km2 (500 mi2) are below sea level (Fig. 1). The extreme summer climate attracts great interest: July and August visitation in Death Valley National Park has doubled in the last 10 years. From June through August, the average temperature at Furnace Creek, Death Valley [54 m (177 ft) below sea level] is 98°F (37°C).1 Daytime high temperatures typically exceed 90°F (32°C) more than half of the year, and temperatures above 120°F (49°C) occur 1 Weather data are reported here in their original units in to order retain the original level of precision re- corded by the observers. FIG. I. Location map of the Death Valley region. Death Valley National Park is outlined in blue, main roads shown in red, and the portion of the park below sea level is highlighted in white. AFFILIATIONS: ROOF—School of Natural Science, Hampshire E-mail: [email protected] College, Amherst, Massachusetts; CALLAGAN—National Park Service, DOI: 10.1 175/BAMS-84-12-1725 Death Valley National Park, Death Valley, California. In final form 17 January 2003 CORRESPONDING AUTHOR: Dr. Steve Roof, School of Natural © 2003 American Meteorological Society Science, Hampshire College, Amherst, MA 01002 AMERICAN METEOROLOGICAL SOCIETY DECEMBER 2003 BAfft I 1725 Unauthenticated | Downloaded 10/09/21 10:14 PM UTC 5-20 times each year. -
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. -
Hydrologic Basin Death Valley California
Hydrologic Basin Death Valley California GEOLOGICAL SURVEY PROFESSIONAL PAPER 494-B Hydrologic Basin Death Valley California By CHARLES B. HUNT, T. W. ROBINSON, WALTER A. BOWLES, and A. L. WASHBURN GENERAL GEOLOGY OF DEATH VALLEY, CALIFORNIA GEOLOGICAL SURVEY PROFESSIONAL PAPER 494-B A! description of the hydrology, geochemistry, and patternedground of the saltpan UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract BI Hydrology-Continued Hydrology, by Charles B. Hunt and T. W. Robinson_ - 3 Descriptions and discharges of springs and of Introduction- 3 marshes-Continued Fieldwork- 3 Discharge of springs in the Furnace Creek fault Climate- 5 zone B35 Rainfall 5 Evapotranspiration discharge from the valley floor Evaporation 7 above the saltpan 37 Temperature- 8 Divisions of the valley according to sources of Humidity- 10 ground water 37 Wind- 11 Possible sources of water at Cottonball Marsh- 37 Rock types in the Death Valley hydrologic basin --- 11 Possible source of water at springs along Fur- Hard-rock formations 12 nace Creek fault zone 38 Unconsolidated Quaternary deposits 13 Geochemistry of the saltpan by Charles B. Hunt 40 Gravel deposits 13 General features 40 Fine-grained alluvial and playa deposits - 15 Fieldwork and acknowledgments 41 Salt deposits and saliferous playa deposits- 15 Geologic -
Geology of the Panamint Butte Quadrangle, Inyo County, California
Geology of the Panamint Butte Quadrangle, Inyo County, California By WAYNE E; HALL GEOLOGICAL SURVEY BULLETIN 1299 Prepared in cooperation with the California Department of Conservation, Division of Mines and Geology KhCEIVED JUL161971 u.8.1 teuisfiUt, it UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 75-610447 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract_________________________________-_.-______-__--_-_--_--- 1 Introduction. ___________-______--_____--_----.--___--__-__--------- 2 Climate.and vegetation._________.__....__.._____-___________-__ 3 Water supply-________________________________________________ 3 Previous work__________________________.___._____._1________ 4 Acknowledgments- _______________._______..____-__-_---------_- 4 General geology.__________________________-__..____--_----_-_--__-- 5 Precambrian(?) rocks._____________.__________.._----___-___-_-_-__- 7 Paleozoic rocks._____.__.___--________-___-____-_-----_---_--.-.-_- 8 Cambrian System_____________________________________________ 8 Carrara Formation.__________________..-_____--____---__-_- 8 Bonanza King Formation___._.______..__._._.....____.____ 10 Nopah Formation._____...____-_-_.....____________-_-_-__- 11 Ordovician System___________________________________________ 13 Pogonip Group_____-__-______-____-_-..----------_--._-_-_- 13 Eureka Quartzite.______________-_____..___-_-_---_-----_--_ 16 Ely Springs Dolomite__---__-______________________________ 18 Silurian and Devonian Systems___________..__-_-__----_-__-___- 21 Hidden Valley Dolomite......._____________________________ 21 Devonian System_____________________________________________ 22 Lost Burro Formation.....__________________________________ 22 Mississippian System.___._____..____._.._..__.___..._._._..__. -
1995/08/25-Attachment 14 to Reply of the Timbisha Shoshone Yucca
ATTACHMENT 14 RESIDENCE WITHOUT RESERVATION / RESIDENCE WITHOUT RESERVATION: ETHNOGRAPHIC OVERVIEW AND TRADmONAL LAND. USE STUDY, TIMBISHA SHOSHONE, DEATH VALLEY NATIONAL PARK, CALIFORNIA Phase I Catherine S. Fowler, Molly Dufort, Mary Rusco and the Historic Preservation Committee, Timbisha Shoshone Tribe (pauline Esteves, Grace Goad Ed Esteves and Ken Watterson) DRAFT, submitted January IS, 1994 FINAL, submitted August 15, 1995 to the National Park Service Cooperative Agreement CASOOO-92-9003 Cooperative Agreement Order No. CASOll-92-9003 TABLE OF CONTENTS ~ist ()f ~al>s .................................................................................. ~ ..... 1l1 ~ist ()f~i~\lres .......................•..............................................••....•.........." Executive Summuy ............................................................................................................................................................ ix I. IlltrCHillCti()Il .......................................................................................... 1 ll. Environmental, Archaeological, Ethnographic and Historical Overviews ......................................................................................................................................................... 6 Environmental Overview~ ......................................................................... 6 Archaeological Overview ................................................................................................................................. 12 Ethnographic -
Inventory of Amphibians and Reptiles at Death Valley National Park
Inventory of Amphibians and Reptiles at Death Valley National Park Final Report Permit # DEVA-2003-SCI-0010 (amphibians) and DEVA-2002-SCI-0010 (reptiles) Accession # DEVA- 2493 (amphibians) and DEVA-2453 (reptiles) Trevor B. Persons and Erika M. Nowak Common Chuckwalla in Greenwater Canyon, Death Valley National Park (TBP photo). USGS Southwest Biological Science Center Colorado Plateau Research Station Box 5614, Northern Arizona University Flagstaff, Arizona 86011 May 2006 Death Valley Amphibians and Reptiles_____________________________________________________ ABSTRACT As part of the National Park Service Inventory and Monitoring Program in the Mojave Network, we conducted an inventory of amphibians and reptiles at Death Valley National Park in 2002- 2004. Objectives for this inventory were to: 1) Inventory and document the occurrence of reptile and amphibian species occurring at DEVA, primarily within priority sampling areas, with the goal of documenting at least 90% of the species present; 2) document (through collection or museum specimen and literature review) one voucher specimen for each species identified; 3) provide a GIS-referenced list of sensitive species that are federally or state listed, rare, or worthy of special consideration that occur within priority sampling locations; 4) describe park-wide distribution of federally- or state-listed, rare, or special concern species; 5) enter all species data into the National Park Service NPSpecies database; and 6) provide all deliverables as outlined in the Mojave Network Biological Inventory Study Plan. Methods included daytime and nighttime visual encounter surveys, road driving, and pitfall trapping. Survey effort was concentrated in predetermined priority sampling areas, as well as in areas with a high potential for detecting undocumented species. -
The California Deserts: an Ecological Rediscovery
3Pavlik-Ch1 10/9/07 6:43 PM Page 15 Rediscovery Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 16 Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 17 Indians first observed the organisms, processes, and history of California deserts. Over millennia, native people obtained knowledge both practical and esoteric, necessitated by survival in a land of extremes and accumulated by active minds recording how nature worked. Such knowledge became tradition when passed across generations, allowing cul- tural adjustments to the changing environment. The depth and breadth of their under- standing can only be glimpsed or imagined, but should never be minimized. Indians lived within deserts, were born, fed, and raised on them, su¤ered the extremes and uncertainties, and passed into the ancient, stony soils. Theirs was a discovery so intimate and spiritual, so singular, that we can only commemorate it with our own 10,000-year-long rediscov- ery of this place and all of its remarkable inhabitants. Our rediscovery has only begun. Our rediscovery is not based upon living in the deserts, despite a current human pop- ulation of over one million who dwelling east of the Sierra. We do not exist within the ecological context of the land. We are not dependant upon food webs of native plants and [Plate 13] Aha Macav, the Mojave people, depicted in 1853. (H. B. Molhausen) REDISCOVERY • 17 Copyrighted Material 3Pavlik-Ch1 10/9/07 6:43 PM Page 18 Gárces 1776 Kawaiisu Tribal groups Mono Mono Tribe Lake Aviwatha Indian place name Paiute Inyo Owens Valley -
Deserts Province
Province-Specific Conservation Strategies – Deserts 5.6 Deserts Province 5.6.1 Geophysical and Ecological Description of the Province The Deserts Province extends from the California-Mexico border on the south and Colorado River on the southeast north to Topaz Lake on the California-Nevada border (Figure 5.6-1). The province’s western border is formed by the Peninsula Mountain Ranges and Transverse Mountain Range in southern California, and the Sierra Nevada in central California. The province is the extension of desert regions located to the east and south of California in the states of Nevada and Arizona, and in Mexico. The Deserts Province has five different subregions: from north to south these are the Mono subregion, the Southeastern Great Basin, Mojave Desert, Sonoran Desert, and Colorado Desert. Each subregion has unique combinations of climate, topography, ecology, and land-use patterns. The province as a whole is in the rain shadow of mountain ranges that form the western border. The dry landscape created by this barrier is characterized by unique geologic features composed of cliffs, peaks, canyons, dry washes, sand dunes, and large dry lake playas. Elevations are generally low in the southern portion of the province and rise to the north. The elevation in the south (Sonoran and Colorado deserts subregion) is generally below 1,000 feet with the lowest point at 275 feet below sea level in the Salton Trough. The topography of the more northerly portion of the province (Mojave Desert subregion) is characterized by a moderately high plateau: elevations range from 282 feet below sea level in Death Valley to 11,000 feet above sea level in the Panamint Mountains. -
Groundwater Geology and Hydrology of Death Valley National Park
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Groundwater Geology and Hydrology of Death Valley National Park, California and Nevada Natural Resource Technical Report NPS/NRSS/WRD/NRTR—2012/652 ON THE COVER The Amargosa River in the southeast part of Death Valley National Park during a flash flood in February 2005 Photography by: A. Van Luik Groundwater Geology and Hydrology of Death Valley National Park, California and Nevada Natural Resource Technical Report NPS/NRSS/WRD/NRTR—2012/652 M. S. Bedinger Hydrologist U.S. Geological Survey, Retired Carlsborg, WA J. R. Harrill Hydrologist U.S. Geological Survey, Retired Carson City, NV December 2012 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and envi- ronmental constituencies, and the public. The Natural Resource Technical Report Series is used to disseminate 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 mission. The series provides contributors with a forum for displaying comprehensive data that are often deleted from journals because of page limitations. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scien- tifically credible, technically accurate, appropriately written for the intended audience, and designed and pub- lished in a professional manner. -
Death Valley National Monument
DEATH VALLEY NATIONAL MONUMENT CALIFORNIA NEVADA UNITED STATES DEPARTMENT OF THE INTERIOR DEATH VALLEY NATIONAL PARK SERVICE NATIONAL MONUMENT Contents DEATH VALLEY FROM BREAKFAST CANYON Cover Open all year • Regular season, October 15 to May 15 BEFORE WHITE MEN CAME 3 THE HISTORICAL DRAMA 4 cipitation at headquarters during the past TALES WRITTEN IN ROCK AND LANDSCAPE 5 DEATH VALLEY National Monument is distinguished by its desert scenery— 15 years has been 2.03 inches. DESERT WILDLIFE 10 a combination of unusual geology, flora, Summer daytime temperatures in the DESERT PLANTLIFE 11 fauna, and climate. Famed as a scene of valley itself are quite high. The maxi suffering in the gold-rush drama of mum air temperature of 134° F. in the INTERPRETIVE SERVICES 12 1849, Death Valley has long been shade recorded in Death Valley was a WHAT TO SEE AND DO WHILE IN THE MONUMENT 12 known to scientist and layman alike as world record until 1922 when 136.4° F. HOW TO REACH DEATH VALLEY 13 a region rich in scientific and human was reported from El Azizia, Libya. interest. The monument was established Higher locations on the mountains in the MONUMENT SEASON 14 in 1933 and covers almost 3,000 square monument have comfortable daytime WHAT TO WEAR 14 miles. temperatures and cool nights. ACCOMMODATIONS 14 The monument is in the rugged desert From late October until May, the val ADMINISTRATION 15 region east of the Sierra Nevada in east ley climate is usually very pleasant. ern California and southwestern Nevada. Days are often warm and sunny, nights PLEASE HELP PROTECT THIS MONUMENT 15 The valley itself is about 140 miles long, cool and invigorating, with the temper with the forbidding Panamint Range ature seldom below freezing. -
Panamint Range and Valley, Inyo County, California
Geology of the Death Valley Region South Coast Geological Society Guidebook Vol. 16, 1988 I • Historical review of the economic geology of the Panamint Range and Valley, Inyo County, California : . Larry M. Vredenburgh U.S. Bureau of Land Management Bakersfield, California HISTORY OF MINING The first mineral discovery made in the Panamint region is attributed to a member of the ill-fated party of Jayhawkers who crossed Death Valley in the winter of 1849-1850. In one version of the discovery a member of the party picked up a metallic rock and carried it with him to civilization. Sometime later, he took it to a gunsmith to have it fashioned into a gunsite, whereupon the gunsmith di~covered the rock was silver (Chalfant 1936 p. 114-115). Even though the story drifted throughout the state, there was little interest in re discovering the source of silver. Tradition has it that eight years later, in 1858, "Mormons found silver ore in the Panamint Mountains, and produced some bullion from small furnaces at Anvil Springs." (Chalfant 1933 p. 117). One man who has prospected the highest parts of Man ly Peak since 1964 feels he has found the source of the Mormon silver. In May 1860, after the discovery of the Comstock silver mines, a party of men lead by Dr. Darwin French, set out' from Oroville to rediscover the Gunsite lode. They did not find it but they did pave the way for others. On Christmas day of the same year a party led by Dr. S. G. George also looking for the Gunsite lode, discovered antimony at Wildrose Spring, and named their discovery the Christmas Gift mine (Spears 1892 p. -
Two-Stage Formation of Death Valley
Two-stage formation of Death Valley Ian Norton* Jackson School of Geosciences, Institute for Geophysics, University of Texas at Austin, J.J. Pickle Research Campus, Bldg. 196, 10100 Burnet Road (R2200), Austin, Texas 78758-4445, USA ABSTRACT lar to the core complex at Tucki Mountain, (1966), on the basis of the morphology of the at the northern end of the range. The Basin valley and occurrence of strike-slip faults, sug- Extension in Death Valley is usually inter- and Range extensional detachment tracks gested that Death Valley was formed as a strike- preted as a combination of low-angle Basin over the top of the range, with extensional slip pull-apart basin, with the basin forming and Range–style extension and strike slip allochthons perched on the eastern fl anks of between the Northern Death Valley–Furnace associated with the developing Pacifi c-North the range. This modifi ed model for evolution Creek fault to the north and the Southern America plate boundary in western North of Death Valley suggests a strong link between Death Valley fault zone to the south (Fig. 2). America, with these two tectonic regimes timing and style of deformation in the basin This idea has been incorporated into several operating synchronously in Death Valley. with the developing Pacifi c-North America models for the structural evolution of Death Examination of structural, stratigraphic, plate boundary, particularly eastward propa- Valley. Miller and Pavlis (2005) divided these and timing relationships in the region sug- gation of this boundary. models into two categories, depending on how gests that this interpretation needs revision.