NUREG-1710 Vol 1 History of Water
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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. -
Big Springs Ethnographic Assessment
Pah ¡chi (From Big Spring Running Down) ig Springs Ethnographic Assessment US -J5 Corridor Study OURCE GROUP REPORT NO. 34 Prepared by: Nevada ` Department of Transportation Division of Environmental Services and Federal Highway Administration Environmental Consultants: Louis Berger & Associates, Inc. Las Vegas, Nevada September 1998 THE UNIVERSITY OF ARIZONA Pah hu wichi(From Big Spring Running Down): Big Spring Ethnographic Assessment US 95 Corridor Study September 1998 BUREAU OF APPLIED RESEARCH IN ANTHROPOLOGY TABLE OF CONTENTS List of Tables v List of Figures vii Acknowledgments vii Foreword x Chapter One Study Overview 1 Brief Description of the Project 1 Cultural Affiliation and Involved American Indian Tribes 2 The Bureau of Applied Research in Anthropology 3 Native American Cultural Resource Revitalization 3 University of Arizona Study Team 4 Selection of Interview Sites 5 Interview Forms and Analysis 10 Data Analysis 10 Chronology of Work 13 Daily Schedule 13 Chapter Two Contextualizing Indian Opinions 15 Paiute Views of Their Culture 15 Creation Stories 18 Traditional Southern Paiute Political Units 20 The High Chiefs 20 Chiefs of Alliance 21 Disease and Sociopolitical Disruption 22 1840 - 1875 Depopulation 24 1875 -1900 Depopulation 24 Twentieth Century High Chiefs 26 Chief Tecopa 26 Continuities in Southern Paiute Political Leadership 26 Chief Penance 26 Chief Skinner 27 Technical Terms 28 Technical Term #1: Cultural Affiliation 28 Traditional Period 28 Aboriginal Period 29 Historic Period 29 Ownership of Land 30 Response -
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. -
Elko County Nevada Water Resource Management Plan 2017
Elko County Nevada Water Resource Management Plan 2017 Echo Lake - Ruby Mountains Elko County Board of Commissioners Elko County Natural Resource Management Advisory Commission December 6, 2017 Executive Summary The Elko County Water Resource Management Plan has been prepared to guide the development, management and use of water resources in conjunction with land use management over the next twenty-five (25) years. Use by decision makers of information contained within this plan will help to ensure that the environment of the County is sustained while at the same time enabling the expansion and diversification of the local economy. Implementation of the Elko County Water Resource Management Plan will assist in maintaining the quality of life enjoyed by residents and visitors of Elko County now and in the future. Achievement of goals outlined in the plan will result in water resources found within Elko County being utilized in a manner beneficial to the residents of Elko County and the State of Nevada. The State of Nevada Water Plan represents that Elko County will endure a loss of population and agricultural lands over the next twenty-five years. Land use and development patterns prepared by Elko County do not agree with this estimated substantial loss of population and agricultural lands. The trends show that agricultural uses in Elko County are stable with minimal notable losses each year. Development patterns represent that private lands that are not currently utilized for agricultural are being developed in cooperation and conjunction with agricultural uses. In 2007, Elko County was the largest water user in the State of Nevada. -
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 -
Spatially-Explicit Modeling of Modern and Pleistocene Runoff and Lake Extent in the Great Basin Region, Western United States
Spatially-explicit modeling of modern and Pleistocene runoff and lake extent in the Great Basin region, western United States Yo Matsubara1 Alan D. Howard1 1Department of Environmental Sciences University of Virginia P.O. Box 400123 Charlottesville, VA 22904-4123 Abstract A spatially-explicit hydrological model balancing yearly precipitation and evaporation is applied to the Great Basin Region of the southwestern United States to predict runoff magnitude and lake distribution during present and Pleistocene climatic conditions. The model iteratively routes runoff through, and evaporation from, depressions to find a steady state solution. The model is calibrated with spatially-explicit annual precipitation estimates and compiled data on pan evaporation, mean annual temperature, and total yearly runoff from stations. The predicted lake distribution provides a close match to present-day lakes. For the last glacial maximum the sizes of lakes Bonneville and Lahontan were well predicted by linear combinations of decrease in mean annual temperature from 0 to 6 °C and increases in precipitation from 0.8 to 1.9 times modern values. Estimated runoff depths were about 1.2 to 4.0 times the present values and yearly evaporation about 0.3 to 1 times modern values. 2 1. Introduction The Great Basin of the southwestern United States in the Basin and Range physiographic province contains enclosed basins featuring perennial and ephemeral lakes, playas and salt pans (Fig. 1). The Great Basin consists of the entire state of Nevada, western Utah, and portions of California, Idaho, Oregon, and Wyoming. At present it supports an extremely dry, desert environment; however, about 40 lakes (some reaching the size of present day Great Lakes) episodically occupied the Great Basin, most recently during the last glacial maximum (LGM) [Snyder and Langbein, 1962; Hostetler et al., 1994; Madsen et al., 2001]. -
Global Patterns and Environmental Controls of Perchlorate and Nitrate Co-Occurrence in Arid and Semi-Arid Environments W
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by UNL | Libraries University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln NASA Publications National Aeronautics and Space Administration 2015 Global patterns and environmental controls of perchlorate and nitrate co-occurrence in arid and semi-arid environments W. Andrew Jackson Texas Tech University, [email protected] J. K. Böhlke U.S. Geological Survey, 431 National Center, Reston, VA Brian J. Andraski U.S. Geological Survey, 2730 N. Deer Run Rd, Carson City, NV Lynne Fahlquist U.S. Geological Survey, 1505 Ferguson Ln, Austin, TX Laura Bexfield U.S. Geological Survey, 5338 Montgomery Blvd. NE, Suite 400, Albuquerque, NM See next page for additional authors Follow this and additional works at: http://digitalcommons.unl.edu/nasapub Jackson, W. Andrew; Böhlke, J. K.; Andraski, Brian J.; Fahlquist, Lynne; Bexfield, Laura; Eckardt, Frank D.; Gates, John B.; Davila, Alfonso F.; McKay, Christopher P.; Rao, Balaji; Sevanthi, Ritesh; Rajagopalan, Srinath; Estrada, Nubia; Sturchio, Neil; Hatzinger, Paul B.; Anderson, Todd A.; Orris, Greta; Betancourt, Julio; Stonestrom, David; Latorre, Claudio; Li, Yanhe; and Harvey, Gregory J., "Global patterns and environmental controls of perchlorate and nitrate co-occurrence in arid and semi-arid environments" (2015). NASA Publications. 210. http://digitalcommons.unl.edu/nasapub/210 This Article is brought to you for free and open access by the National Aeronautics and Space Administration at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in NASA Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors W. Andrew Jackson, J. -
The Letters of Helen J. Stewart
The Letters of Helen J. Stewart Nevada State Museum, Las Vegas 2009 Made possible by a 2008 grant from the Nevada Museums Association Copyright © 2009 by Nevada State Museum, Las Vegas Nevada Department of Cultural Affairs Jim Gibbons, Governor Mike Fischer, Director of Department of Cultural Affairs Peter Barton, Interim Director of Division of Museums & History [Previous page: Helen Jane Wiser Stewart, 1870s. Nevada State Museum, Las Vegas. Stewart Collection] Table of Contents Introduction…………………………………………………………………………….ii Acknowledgements …………………………………………………………………..iii Editor’s Note on the Text …………………………………………………………….iv Letters 1882 – 1899……………………………………………………………………………….1 1900 – 1905………………………………………………………………………………29 1906 – 1910………………………………………………………………………………52 1911 – 1915………………………………………………………………………………77 1916 – 1920………………………………………………………………………………95 1921 – 1926 and 1938………………………………………………………………….139 Name Glossary………………………………………………………………………..180 i Introduction Helen Jane Wiser Stewart (1854 – 1926) was a woman of indomitable spirit. Although born in Springfield, Illinois and raised in Galt, California, Helen J. Stewart became “Las Vegas’ best known and best beloved pioneer woman.” 1 Helen J. Stewart came to southern Nevada in 1882 where her husband, Archibald, had taken over the former Gass Ranch. Renamed the Stewart Ranch-- also known as the Las Vegas Ranch—Helen and Archie managed a productive farm and offered their tree-shaded springs as an oasis for travelers, miners, cattlemen, and others passing through the valley. After her husband died in 1884, Helen continued running the ranch until 1902 when she sold it to the San Pedro, Los Angeles, and Salt Lake Railroad. The city of Las Vegas was founded on this land in 1905. Her role in the town’s future is only one of the reasons Stewart is lovingly called the First Lady of Las Vegas.2 Helen J. -
Early Pliocene (Pre–Ice Age) El Niño–Like Global Climate: Which El Niño?
Early Pliocene (pre–Ice Age) El Niño–like global climate: Which El Niño? Peter Molnar* Department of Geological Sciences and Cooperative Institute for Research in Environmental Science (CIRES), University of Colo- rado, Boulder, Colorado 80309-0399, USA Mark A. Cane Lamont-Doherty Earth Observatory, Columbia University, 61 Route 9W, Palisades, New York 10964-8000, USA ABSTRACT warmest region extending into the eastern- in part from theoretical predictions for how the most Pacifi c Ocean, not near the dateline as structure of the upper ocean and its circulation Paleoceanographic data from sites near occurs in most El Niño events. This inference have changed over late Cenozoic time (e.g., the equator in the eastern and western Pacifi c is consistent with equatorial Pacifi c proxy Cane and Molnar, 2001; Philander and Fedorov, Ocean show that sea-surface temperatures, data indicating that at most a small east-west 2003). Not surprisingly, controversies continue and apparently also the depth and tempera- gradient in sea-surface temperature seems to to surround hypothesized stimuli for switches ture distribution in the thermocline, have have existed along the equator in late Mio- both from permanent El Niño to the present-day changed markedly over the past ~4 m.y., from cene to early Pliocene time. Accordingly, such ENSO state and from ice-free Laurentide and those resembling an El Niño state before ice a difference in sea-surface temperatures may Fenno-Scandinavian regions to the alternation sheets formed in the Northern Hemisphere account for the large global differences in cli- between glacial and interglacial periods that has to the present-day marked contrast between mate that characterized the earth before ice occurred since ca. -
Ethnographic Study: (1) Indian Springs and (2) the Rock Shelter
Nevada Test and Training Range, Nellis Air Force Base Legislative Environmental Impact Statement Native American Ethnographic Studies Study Area for Alternative 3B May 15 – 17, 2018 Contract Number: W912G-14-D-0014 Task Order/Deliverable: DS01 (P010176981) Far Western Job Number: 2007 FRS Account Number: 4021230 Prepared By: University of Arizona CGTO Writers Committee Dr. Richard Stoffle Richard Arnold [email protected] Office: (520) 621-2462 Kenny Anderson Cell: (520) 907-2330 Charlie Bulletts Christopher Sittler Maurice Churchill Christopher “Mintie” Johnson Barbara Durham Cameron Kays Ronald Escobar Grace Penry Danelle Gutierrez Mailing: University of Arizona Linda Otero P.O. Box 210030 Tucson, AZ 85721-0030 Sean Scruggs August 15, 2018 ACKNOWLEDGEMENTS This report is the outcome of the efforts of many individuals. These research findings represent the integrated efforts of Nellis Air Force Base (Nellis AFB), the Native American Interaction Program, and the 17 Native American tribes listed below. Additionally, the authors would like to express their sincere appreciation to Far Western and Leidos for their continued support throughout this project. This project was made possible by the efforts of Joanna Roberson, Principal Investigator and Desert Branch Manager at Far Western Anthropological Research Group, Inc., Daron Duke, Principal and Branch Director at Far Western Anthropological Research Group, Inc., Kevin Akstulewicz, Senior Principal Environmental Scientist at Leidos, Inc., and Kish LaPierre, Cultural Resource Manager at Nellis AFB. This report was prepared at the Bureau of Applied Research in Anthropology (BARA), School of Anthropology, University of Arizona. We offer sincere thanks to the School of Anthropology Professor and Director Diane Austin for her guidance throughout the project. -
The Nevada Mineral Industry 1999
Nevada Bureau of Mines and Geology Special Publication MI-1999 Metals Industrial Minerals The Nevada Oil and Gas Mineral Industry Geothermal 1999 Exploration Development Mining Processing This report, twenty-first of an annual series, describes 1999 mineral, oil and gas, and geothermal activities and accomplishments in Nevada: production statistics, exploration and development including drilling for petroleum and geothermal resources, discoveries of orebodies, new mines opened, and expansion and other activities of existing mines. Statistics of known gold and silver deposits, and directories of mines and mills are included. Mackay School of Mines UNIVERSITY OF NEVADA RENO University and Community College System of Nevada 2000 Board of Regents Thalia Dondero, Chair Mark Alden David L. Phillips Jill Derby Howard Rosenberg Dorothy Gallagher Douglas Seastrand Douglas R. Hill Steve Sisolak Thomas E. Kirkpatrick Tom Weisner Jane Nichols, Interim Chancellor University of Nevada, Reno Joseph N. Crowley, President Mackay School of Mines Jane C.S. Long, Dean Nevada Bureau of Mines and Geology Jonathan G. Price, Director/State Geologist Scientific Research Staff Research and Administrative Support Staff Economic Geology Administration and Publication Sales Stephen B. Castor, Research Geologist Terri M. Garside, Executive Secretary John W. Erwin, Geophysicist (Emeritus) Cheryl Steed, Management Assistant Liang-Chi Hsu, Research Mineralogist (Emeritus) Charlotte Stock, Sales Manager Daphne D. LaPointe, Research Geologist Analytical Laboratory, Sample Curation, and Keith Papke, Industrial Minerals Geologist (Emeritus) Geologic Information Joseph V. Tingley, Research Geologist David Davis, Geologic Information Specialist Engineering Geology Paul J. Lechler, Chief Chemist/Geochemist John W. Bell, Research Engineering Geologist Mario Desilets, Chemist/Quality Assurance Officer Geoffrey Blewitt, Research Professor Bret Pecoraro, Laboratory Assistant Craig M.