Desert Renewable Energy Conservation Plan Land Use Plan
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California Vegetation Map in Support of the DRECP
CALIFORNIA VEGETATION MAP IN SUPPORT OF THE DESERT RENEWABLE ENERGY CONSERVATION PLAN (2014-2016 ADDITIONS) John Menke, Edward Reyes, Anne Hepburn, Deborah Johnson, and Janet Reyes Aerial Information Systems, Inc. Prepared for the California Department of Fish and Wildlife Renewable Energy Program and the California Energy Commission Final Report May 2016 Prepared by: Primary Authors John Menke Edward Reyes Anne Hepburn Deborah Johnson Janet Reyes Report Graphics Ben Johnson Cover Page Photo Credits: Joshua Tree: John Fulton Blue Palo Verde: Ed Reyes Mojave Yucca: John Fulton Kingston Range, Pinyon: Arin Glass Aerial Information Systems, Inc. 112 First Street Redlands, CA 92373 (909) 793-9493 [email protected] in collaboration with California Department of Fish and Wildlife Vegetation Classification and Mapping Program 1807 13th Street, Suite 202 Sacramento, CA 95811 and California Native Plant Society 2707 K Street, Suite 1 Sacramento, CA 95816 i ACKNOWLEDGEMENTS Funding for this project was provided by: California Energy Commission US Bureau of Land Management California Wildlife Conservation Board California Department of Fish and Wildlife Personnel involved in developing the methodology and implementing this project included: Aerial Information Systems: Lisa Cotterman, Mark Fox, John Fulton, Arin Glass, Anne Hepburn, Ben Johnson, Debbie Johnson, John Menke, Lisa Morse, Mike Nelson, Ed Reyes, Janet Reyes, Patrick Yiu California Department of Fish and Wildlife: Diana Hickson, Todd Keeler‐Wolf, Anne Klein, Aicha Ougzin, Rosalie Yacoub California -
People of Snowy Mountain, People of the River: a Multi-Agency Ethnographic Overview and Compendium Relating to Tribes Associated with Clark County, Nevada
Portland State University PDXScholar Anthropology Faculty Publications and Presentations Anthropology 2012 People of Snowy Mountain, People of the River: A Multi-Agency Ethnographic Overview and Compendium Relating to Tribes Associated with Clark County, Nevada Douglas Deur Portland State University, [email protected] Deborah Confer University of Washington Follow this and additional works at: https://pdxscholar.library.pdx.edu/anth_fac Part of the Social and Cultural Anthropology Commons, and the Sustainability Commons Let us know how access to this document benefits ou.y Citation Details Deur, Douglas and Confer, Deborah, "People of Snowy Mountain, People of the River: A Multi-Agency Ethnographic Overview and Compendium Relating to Tribes Associated with Clark County, Nevada" (2012). Anthropology Faculty Publications and Presentations. 98. https://pdxscholar.library.pdx.edu/anth_fac/98 This Report is brought to you for free and open access. It has been accepted for inclusion in Anthropology Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Pacific West Region: Social Science Series National Park Service Publication Number 2012-01 U.S. Department of the Interior PEOPLE OF SNOWY MOUNTAIN, PEOPLE OF THE RIVER: A MULTI-AGENCY ETHNOGRAPHIC OVERVIEW AND COMPENDIUM RELATING TO TRIBES ASSOCIATED WITH CLARK COUNTY, NEVADA 2012 Douglas Deur, Ph.D. and Deborah Confer LAKE MEAD AND BLACK CANYON Doc Searls Photo, Courtesy Wikimedia Commons -
Ecoregions of Nevada Ecoregion 5 Is a Mountainous, Deeply Dissected, and Westerly Tilting Fault Block
5 . S i e r r a N e v a d a Ecoregions of Nevada Ecoregion 5 is a mountainous, deeply dissected, and westerly tilting fault block. It is largely composed of granitic rocks that are lithologically distinct from the sedimentary rocks of the Klamath Mountains (78) and the volcanic rocks of the Cascades (4). A Ecoregions denote areas of general similarity in ecosystems and in the type, quality, Vegas, Reno, and Carson City areas. Most of the state is internally drained and lies Literature Cited: high fault scarp divides the Sierra Nevada (5) from the Northern Basin and Range (80) and Central Basin and Range (13) to the 2 2 . A r i z o n a / N e w M e x i c o P l a t e a u east. Near this eastern fault scarp, the Sierra Nevada (5) reaches its highest elevations. Here, moraines, cirques, and small lakes and quantity of environmental resources. They are designed to serve as a spatial within the Great Basin; rivers in the southeast are part of the Colorado River system Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the Ecoregion 22 is a high dissected plateau underlain by horizontal beds of limestone, sandstone, and shale, cut by canyons, and United States (map): Washington, D.C., USFS, scale 1:7,500,000. are especially common and are products of Pleistocene alpine glaciation. Large areas are above timberline, including Mt. Whitney framework for the research, assessment, management, and monitoring of ecosystems and those in the northeast drain to the Snake River. -
Ground-Magnetic Studies of the Amargosa Desert Region, California and Nevada
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY GROUND-MAGNETIC STUDIES OF THE AMARGOSA DESERT REGION, CALIFORNIA AND NEVADA Richard J. Blakely, John W. Hillhouse, and Robert L. Morin U.S. Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025 Open-File Report 2005-1132 2005 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. GROUND-MAGNETIC STUDIES OF THE AMARGOSA DESERT REGION, CALIFORNIA AND NEVADA Richard J. Blakely, John W. Hillhouse, and Robert L. Morin ABSTRACT High-resolution aeromagnetic surveys of the Amargosa Desert region, California and Nevada, exhibit a diverse array of magnetic anomalies reflecting a wide range of mid- and upper-crustal lithologies. In most cases, these anomalies can be interpreted in terms of exposed rocks and sedimentary deposits. More difficult to explain are linear magnetic anomalies situated over lithologies that typically have very low magnetizations. Aeromagnetic anomalies are observed, for example, over thick sections of Quaternary alluvial deposits and spring deposits associated with past or modern ground-water discharge in Ash Meadows, Pahrump Valley, and Furnace Creek Wash. Such deposits are typically considered nonmagnetic. To help determine the source of these aeromagnetic anomalies, we conducted ground-magnetic studies at five areas: near Death Valley Junction, at Point of Rocks Spring, at Devils Hole, at Fairbanks Spring, and near Travertine Springs. Depth-to-source calculations show that the sources of these anomalies lie within the Tertiary and Quaternary sedimentary section. -
NUREG-1710 Vol 1 History of Water
NUREG-1710 Vol. 1 History of Water Development in the Amargosa Desert Area: A Literature Review i I I I I I I I U.S. Nuclear Regulatory Commission Advisory Committee on Nuclear Waste Washington, DC 20555-0001 AVAILABILITY OF REFERENCE MATERIALS IN NRC PUBLICATIONS 7 NRC Reference Material Non-NRC Reference Material As of November 1999, you may electronically access Documents available from public and special technical NUREG-series publications and other NRC records at libraries include all open literature items, such as NRC's Public Electronic Reading Room at books, journal articles, and transactions, Federal http://www.nrc.pov/reading-rm.html. Register notices, Federal and State legislation, and Publicly released records include, to name a few, congressional reports. Such documents as theses, NUREG-series publications; Federal Register notices; dissertations, foreign reports and translations, and applicant, licensee, and vendor documents and non-NRC conference proceedings may be purchased correspondence; NRC correspondence and internal from their sponsoring organization. memoranda; bulletins and information notices; inspection and investigative reports; licensee event reports; and Commission papers and their attachments. Copies of industry codes and standards used in a substantive manner in the NRC regulatory process are NRC publications in the NUREG series, NRC maintained at- regulations, and Title 10, Energy, in the Code of The NRC Technical Library Federal Regulations may also be purchased from one Two White Flint North of these two sources. 11545 Rockville Pike 1. The Superintendent of Documents Rockville, MD 20852-2738 U.S. Government Printing Office Mail Stop SSOP Washington, DC 20402-0001 These standards are available in the library for Intemet: bookstore.gpo.gov reference use by the public. -
Cyprinodon Nevadensis Mionectes Ash Meadows Amargosa Pupfish
Ash Meadows Amargosa pupfsh Cyprinodon nevadensis mionectes WAP 2012 species due to impacts from introduced detrimental aquatc species, habitat degradaton, and federal endangered status. Agency Status NV Natural Heritage G2T2S2 USFWS LE BLM-NV Sensitve State Prot Threatened Fish NAC 503.065.3 CCVI Presumed Stable TREND: Trend is stable to increasing with contnued on-going restoraton actvites. DISTRIBUTION: Springs and associated springbrooks, outlow stream systems and terminal marshes within Ash Meadows Natonal Wildlife Refuge, Nye Co., NV. GENERAL HABITAT AND LIFE HISTORY: This species is isolated to warm springs and outlows in Ash Meadows NWR including Point of Rocks, Crystal Springs, and the Carson Slough drainage. Pupfshes feed generally on substrate; feeding territories are ofen defended by pupfshes. Diet consists of mainly algae and detritus however, aquatc insects, crustaceans, snails and eggs are also consumed. Spawning actvity is typically from February to September and in some cases year round. Males defend territories vigorously during breeding season (Soltz and Naiman 1978). In warm springs, fsh may reach sexual maturity in 4-6 weeks. Reproducton variable: in springs, pupfsh breed throughout the year, may have 8-10 generatons/year; in streams, breeds in spring and summer, 2-3 generatons/year (Moyle 1976). In springs, males establish territories over sites suitable for ovipositon. Short generaton tme allows small populatons to be viable. Young adults typically comprise most of the biomass of a populaton. Compared to other C. nevadensis subspecies, this pupfsh has a short deep body and long head with typically low fn ray and scale counts (Soltz and Naiman 1978). CONSERVATION CHALLENGES: Being previously threatened by agricultural use of the area (loss and degradaton of habitat resultng from water diversion and pumping) and by impending residental development, the TNC purchased property, which later became the Ash Meadows NWR. -
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. -
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 -
A Transect Across the Death Valley Extended Terrane, California Michael S
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. B1, 2010, 10.1029/2001JB000239, 2002 Assessing vertical axis rotations in large-magnitude extensional settings: A transect across the Death Valley extended terrane, California Michael S. Petronis and John W. Geissman Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico, USA Daniel K. Holm Department of Geology, Kent State University, Kent, Ohio, USA Brian Wernicke and Edwin Schauble Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA Received 11 September 2000; revised 7 May 2001; accepted 14 July 2001; published 18 January 2002. [1] Models for Neogene crustal deformation in the central Death Valley extended terrane, southeastern California, differ markedly in their estimates of upper crustal extension versus shear translations. Documentation of vertical axis rotations of range-scale crustal blocks (or parts thereof) is critical when attempting to reconstruct this highly extended region. To better define the magnitude, aerial extent, and timing of vertical axis rotation that could mark shear translation of the crust in this area, paleomagnetic data were obtained from Tertiary igneous and remagnetized Paleozoic carbonate rocks along a roughly east-west traverse parallel to about 36°N latitude. Sites were established in 7 to 5 Ma volcanic sequences (Greenwater Canyon and Brown’s Peak) and the 10 Ma Chocolate Sundae Mountain granite in the Greenwater Range, 8.5 to 7.5 Ma and 5 to 4 Ma basalts on the east flank of the Black Mountains, the 10.6 Ma Little Chief stock and upper Miocene(?) basalts in the eastern Panamint Mountains, and Paleozoic Pogonip Group carbonate strata in the north central Panamint Mountains. -
Proceedings of the Desert Fishes Council 2003
Proceedings of the Desert Fishes Council VOLUME XXXV 2003 ANNUAL SYMPOSIUM 16 - 19 November Death Valley California, U.S.A. Edited by Dean A. Hendrickson Texas Natural History Collection University of Texas at Austin 10100 Burnet Road, PRC 176 / R4000 Austin, Texas 78758-4445, U.S.A. and Lloyd T. Findley Centro de Investigación en Alimentación y Desarrollo, A.C.-Unidad Guaymas Carretera al Varadero Nacional Km. 6.6, “Las Playitas” Apartado Postal 284, Guaymas, Sonora 85400, MÉXICO published: online December 1, 2004; in print January 15, 2005 - ISSN 1068-0381 P.O. Box 337 Bishop, California 93515-0337 760-872-8751 Voice & Fax e-mail: [email protected] PROCEEDINGS OF THE DESERT FISHES COUNCIL – VOL.XXXV (2003 SYMPOSIUM) MISSION / MISIÓN The mission of the Desert Fishes Council is to preserve the biological integrity of desert aquatic ecosystems and their associated life forms, to hold symposia to report related research and management endeavors, and to effect rapid dissemination of information concerning activities of the Council and its members . OFFICERS / OFICIALES President: Paul C. Marsh, Arizona State University, School of Life Sciences, P.O Box 874501, Tempe, AZ 85287-4501 Immediate Past President: David Propst, Conservation Services División, New Mexico Department of Game and Fish, Santa Fe, NM 87504 Executive Secretary: E. Phil Pister, P.O. Box 337, Bishop, California 93515-0337 COMMITTEES / COMITÉS Executive Committee: Michael E. Douglas, Anthony A. Echelle (Member-at-Large), Dean A. Hendrickson, Nadine Kanim, Paul C. Marsh, E. Phil Pister, David L. Propst, Jerome Stefferud Areas Coordinator: Nadine Kanim Awards: Astrid Kodric Brown Membership: Jerome Stefferud Proceedings Co-Editors: Lloyd T. -
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. -
Late Quaternary Stratigraphy and Luminescence Geochronology of the Northeastern Mojave Desert
ARTICLE IN PRESS Quaternary International 166 (2007) 61–78 Late Quaternary stratigraphy and luminescence geochronology of the northeastern Mojave Desert Shannon A. Mahana,Ã, David M. Millerb, Christopher M. Mengesc, James C. Younta aUnited States Geological Survey, Box 25046 MS 974, Denver, CO 80225, USA bUnited States Geological Survey, 345 Middlefield Road, MS 973, Menlo Park, CA 94025, USA cUnited States Geological Survey, 520 N. Park Ave., Tucson, AZ 85719-5035, USA Available online 8 January 2007 Abstract The chronology of the Holocene and late Pleistocene deposits of the northeastern Mojave Desert have been largely obtained using radiocarbon ages. Our study refines and extends this framework using optically stimulated luminescence (OSL) to date deposits from Valjean Valley, Silurian Lake Playa, Red Pass, and California Valley. Of particular interest are eolian fine silts incorporated in ground- water discharge (GWD) deposits bracketed at 185–140 and 20–50 ka. Alluvial fan deposits proved amenable for OSL by dating both eolian sand lenses and reworked eolian sand in a matrix of gravel that occurs within the fan stratigraphy. Lacustrine sand in spits and bars also yielded acceptable OSL ages. These OSL ages fill gaps in the geochronology of desert deposits, which can provide data relevant to understanding the responses of several depositional systems to regional changes in climate. This study identifies the most promising deposits for future luminescence dating and suggests that for several regions of the Mojave Desert, sediments from previously undated landforms can be more accurately placed within correct geologic map units. Published by Elsevier Ltd. 1. Introduction Previous chronologic studies in the northeastern Mojave Desert area include magneto-stratigraphic studies and Extracting paleoclimatic and paleoenvironmental infor- tephrochronology of the upper Pliocene to middle Quatern- mation from terrestrial deposits is an important area of ary Tecopa beds (Hillhouse, 1987; Sarna-Wojcicki et al., Quaternary geologic research.