Nevada Hydrographic Areas and Sub-Areas/Listed Alphabetically by Area Name Basin Area Area Area Num
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Index of Surface-Water Records to September 30, 1970 Part 1 0.-The Great Basin
Index of Surface-Water Records to September 30, 1970 Part 1 0.-The Great Basin Index of Surface-Water Records to September 30, 1970 Part 1 0.-The Great Basin GEOLOGICAL SURVEY CIRCULAR 660 Wa1hington J9 77 United States Department of the Interior ROGERS C. B. MORTON, Secretary Geological Survey W. A. Radlinski, Acting Director Free on application to the U.S. Geological Survey, Washington, D.C. 20242 Index of Surface-Water Records to September 30, 1970 Part 10.-The Great Basin INTRODUCTION This report lists the streamflow and reservoir stations in The Great Basin for which records have been or arn to be published in reports of the Geological Survey for periods through September 30, 1970. It supersedes Geologf.cal Survey Circular 580, It was updated by personnel of the Data Reports Unit, Water Resources Division, Geologf.cal Survey. Basic data on surface-water supply have been published in an annual series of water-supply papers consisting of several volumes, including one each for the States of Alaska and Hawaii. The area of the other 48 States is divided into 14 parts whose boundaries coincide with certain natural drainage lines. Prior to 1951, the records for the 48 Stnes were published inl4volumes,oneforeachof the parts. From 1951 to 1960, the records for the 48 States were publis"ed annually in 18 volumes, there being 2 volumes each for Parts 1, 2, 3, and 6. Beginning in 1961, theannualseriesofwater-supplypapers on surface-water supply was changed to a 5-year sel'1'es, and records for the period 1961-65 were published in 37 volumes, there being 2 or more volumes for each of 11 prrts and one each for parts 10, 13, 14, 15 (Alaska) and 16 (Hawaii and other Pacific areas). -
Conservation Genetics of a Desert Fish Species: the Lahontan Tui Chub
Conserv Genet (2015) 16:743–758 DOI 10.1007/s10592-015-0697-1 RESEARCH ARTICLE Conservation genetics of a desert fish species: the Lahontan tui chub (Siphateles bicolor ssp.) Amanda J. Finger • Bernie May Received: 7 August 2014 / Accepted: 20 January 2015 / Published online: 1 February 2015 Ó Springer Science+Business Media Dordrecht 2015 Abstract Analysis of the genetic diversity and structure continuing to maximize habitat size and quality to preserve of declining populations is critical as species and popula- overall genetic diversity, evolutionary potential, and eco- tions are increasingly fragmented globally. In the Great logical processes. Basin Desert in particular, climate change, habitat alter- ation, and fragmentation threaten aquatic habitats and their Keywords Microsatellite Á Desert fishes Á Tui chub Á endemic species. Tui chubs, including the Lahontan tui Great Basin Á Walker Lake Á Dixie Valley chub and Dixie Valley tui chub, (Siphateles bicolor ssp.) are native to the Walker, Carson, Truckee and Humboldt River drainages in the Great Basin Desert. Two popula- Introduction tions, Walker Lake and Dixie Valley, are under threat from habitat alteration, increased salinity, small population The field of conservation genetics operates on the premise sizes, and nonnative species. We used nine microsatellite that the genetic diversity of a population has consequences markers to investigate the population genetic structure and for its health and viability (Frankham 2002). Small popu- diversity of these and nine other tui chub populations to lations in particular are at greater risk of extinction due to provide information to managers for the conservation of demographic (e.g. stochastic or catastrophic events Lande both Walker Lake and Dixie Valley tui chubs. -
Nevada and Utah Springsnail Species Descriptions Introduction……………………………………………………………………………………………………………………………………………….………………..2 1] Amnicola Limosa
Appendix A: Nevada and Utah Springsnail Species Descriptions Introduction……………………………………………………………………………………………………………………………………………….………………..2 1] Amnicola limosa ...................................................... Mud Amnicola ............................................................................... 4 2] Assiminea infima ..................................................... Badwater Snail .............................................................................. 6 3] Colligyrus greggi ..................................................... Rocky Mountain Duskysnail ........................................................... 8 4] Eremopyrgus eganensis........................................... Steptoe Hydrobe ......................................................................... 10 5] Fluminicola coloradoensis ....................................... Green River Pebblesnail ............................................................... 12 6] Fluminicola dalli ...................................................... Pyramid Lake Pebblesnail ............................................................ 14 7] Fluminicola turbiniformis ........................................ Turban Pebblesnail ...................................................................... 16 8] Fluminicola virginius ............................................... Virginia Mountains Pebblesnail .................................................... 18 9] Juga acutifilosa ....................................................... Topaz Juga ................................................................................. -
BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 42, Part I, 1997
BRIGHAM YOUNG UNIVERSITY GEOLOGICAL SOCIETY OF AMERICA FIELD TRIP GUIDE BOOK 1997 ANNUAL MEETING SALT LAKE CITY, UTAH PAR' EDITED BY PAUL KARL LINK AND BART J. KOWALLIS VOIUME 42 I997 PROTEROZOIC TO RECENT STRATIGRAPHY, TECTONICS, AND VOLCANOLOGY, UTAH, NEVADA, SOUTHERN IDAHO AND CENTRAL MEXICO Edited by Paul Karl Link and Bart J. Kowallis BRIGHAM YOUNG UNIVERSITY GEOLOGY STUDIES Volume 42, Part I, 1997 CONTENTS Neoproterozoic Sedimentation and Tectonics in West-Central Utah ..................Nicholas Christie-Blick 1 Proterozoic Tidal, Glacial, and Fluvial Sedimentation in Big Cottonwood Canyon, Utah ........Todd A. Ehlers, Marjorie A. Chan, and Paul Karl Link 31 Sequence Stratigraphy and Paleoecology of the Middle Cambrian Spence Shale in Northern Utah and Southern Idaho ............... W. David Liddell, Scott H. Wright, and Carlton E. Brett 59 Late Ordovician Mass Extinction: Sedimentologic, Cyclostratigraphic, and Biostratigraphic Records from Platform and Basin Successions, Central Nevada ............Stan C. Finney, John D. Cooper, and William B. N. Beny 79 Carbonate Sequences and Fossil Communities from the Upper Ordovician-Lower Silurian of the Eastern Great Basin .............................. Mark T. Harris and Peter M. Sheehan 105 Late Devonian Alamo Impact Event, Global Kellwasser Events, and Major Eustatic Events, Eastern Great Basin, Nevada and Utah .......................... Charles A. Sandberg, Jared R. Morrow and John E. Warme 129 Overview of Mississippian Depositional and Paleotectonic History of the Antler Foreland, Eastern Nevada and Western Utah ......................................... N. J. Silberling, K. M. Nichols, J. H. Trexler, Jr., E W. Jewel1 and R. A. Crosbie 161 Triassic-Jurassic Tectonism and Magmatism in the Mesozoic Continental Arc of Nevada: Classic Relations and New Developments ..........................S. J. -
Great Basin Restoration Initiative Area: Geographic Area Determination Methodology
Great Basin Restoration Initiative Area: Geographic Area Determination Methodology Mike “Sherm” Karl Rangeland Management Specialist Rangeland, Soil, Water & Air Group Washington, DC Bruce M. Durtsche Wildlife Biologist National Science and Technology Center Denver, CO Karen Morgan GIS Specialist Orkand Corporation National Science and Technology Center Denver, CO June 21, 2001 INTRODUCTION The Great Basin Restoration Initiative (GBRI) originated in the wake of the disastrous fire season of 1999, in which 1.7 million acres of public land burned, mostly in Nevada. Today, more than 25 million acres of the Great Basin are dominated by exotic annual grasses and noxious weeds, with additional acres dominated by pinyon pine/juniper. The health of these lands is in jeopardy, attributable to (1) exotic annual grasses such as cheatgrass, which are flammable and have increased the incidence and spread of wildland fires, resulting in even more loss of native vegetation and habitat, and further increases of cheatgrass as time goes by, and (2) woodlands dominated by pinyon pine and/or juniper species, which have invaded what once was sagebrush- steppe and sagebrush, attributable to fire suppression, excessive livestock grazing pressure, and climate change, individually or in combination. A restoration effort, on a large geographic scale, needs to be undertaken to stop the downward ecological trends in the Great Basin. The restoration effort needs to be focused on the geographic area where Great Basin vegetation is present and where fuel loads of the native plant communities has been altered by cheatgrass, other flammable annual plants, and woody vegetation such as pinyon pine and juniper species. -
Nevada Springs Conservation Plan Acknowledgements
Nevada SpriNgS Conservation Plan ackNowledgemeNtS We would like to thank the Nevada Division of State Lands Conservation and Resource Protection Grant Program, known as ‘Question 1 Program’ and the U.S. Environmental Protection Agency for funding the development of this Springs Conservation Plan. Without the support of Nevada voters who passed Question 1 in 2002 to ‘protect, preserve, and obtain the benefits of the property and natural resources of this state’, this effort to support conservation of Nevada’s aquatic biodiversity would not have been possible. The Springs Conservation Plan working group dedicated time and travel to multiple workshops to ensure the content of this plan represented a multi-agency effort. Special thanks to Don Sada, Jennifer Newmark, Victor Cobos, and Bob Conrad for their extra time and commitment that facilitated the integration of the data collection and planning components of this project. Finally, we would like to acknowledge the individuals who reviewed this Plan and provided valuable comments. Recommended Citation: Abele, S.L. (ed.) 2011. Nevada Springs Conservation Plan. Springs Conservation Plan Working Group. The Nature Conservancy, Reno, NV. Cover photo: Charnock Ranch, Nevada. © Janel Johnson about this rePort introduction ................................3 How do we determine if a Spring is Healthy? ..................9 what are the concerns for the Future? ......................... 15 taking action to conserve Nevada’s Springs ................... 23 Significant Spring landscapes ..............................27 Next Steps for Springs conservation in Nevada.........36 references ............................... 39 appendix 1 ............................... 41 Ash Springs, Pahranagat Valley, NV. © Christiana Manville appendix 2 ................................47 he purpose of this Plan is to summarize the current condition, identify future threats, and highlight necessary actions to con- serve some of nevada’s most significant aquatic environments. -
University of Nevada, Reno Reconciling Western Toad
University of Nevada, Reno Reconciling Western toad phylogeography with Great Basin prehistory A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geography by Pete M. Noles Dr. Jill S. Heaton/Thesis Advisor December, 2010 THE GRADUATE SCHOOL We recommend that the thesis prepared under our supervision by PETE M. NOLES entitled Reconciling Western toad phylogeography with Great Basin prehistory be accepted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Jill S. Heaton, Ph.D., Advisor Scott A. Mensing, Ph.D., Committee Member Kenneth E. Nussear, Ph.D., Committee Member C. Richard Tracy, Ph.D., Graduate School Representative Marsha H. Read, Ph. D., Associate Dean, Graduate School December, 2010 i ABSTRACT This study marks the first attempt to study historical processes that may be responsible for the contemporary geographic distribution and phylogeny of Great Basin Western toads (Anaxyrus boreas spp.). The dynamic aquatic history of the Great Basin was evaluated as a potential model for early toad dispersal into regions which would later become arid and isolated, affecting gene flow and eventually promoting allopatric speciation. This research was accomplished by exploring the spatial and historical relationships among Western toad clades and Great Basin drainages. Toad clades that are distributed over large areas, and are composed of many populations, tend to fall within the confines of regional, riverine drainages. Smaller, more genetically distant clades are generally harbored in small, riverless drainage basins. Dates of estimated evolutionary divergence among Western toad clades varied considerably using rates of molecular substitution that are reasonable for this organism. -
Dixie Meadows Geothermal Exploration Project
Stillwater Field Office, Nevada FINAL ENVIRONMENTAL ASSESSMENT Ormat Technologies, Inc. Dixie Meadows Geothermal Exploration Project DOI-BLM-NV-C010-2011-0516-EA U.S. Department of the Interior Bureau of Land Management Carson City District Stillwater Field Office 5665 Morgan Mill Road Carson City, NV 89701 775-885-6000 December 2011 It is the mission of the Bureau of Land Management to sustain the health, diversity, and productivity of the public lands for the use and enjoyment of present and future generations. DOI-BLM-NV-C010-2011-0516-EA DIXIE MEADOWS GEOTHERMAL EXPLORATION PROJECT – ORMAT TECHNOLOGIES, INC. DECEMBER 2011 ENVIRONMENTAL ASSESSMENT i TABLE OF CONTENTS 1.0 INTRODUCTION/PURPOSE AND NEED ....................................................................1 1.1 PURPOSE AND NEED ..................................................................................................3 1.2 LAND USE PLAN CONFORMANCE STATEMENT ..........................................................4 1.3 PLANS, STATUTES, AND OTHER REGULATIONS .........................................................4 2.0 PROPOSED ACTION AND ALTERNATIVES.............................................................5 2.1 PROPOSED ACTION ...................................................................................................5 2.1.1 Project Access ..............................................................................................6 2.1.2 Operations Plan ............................................................................................8 2.1.2.1 -
Pluvial Lakes and Estimated Pluvial Climates of Nevada
NEVADA BUREAU OF MINES AND GEOLOGY BULLETIN 94 PLUVIAL LAKES AND ESTIMATED PLUVIAL CLIMATES OF NEVADA M. D. MIFFLIN AND M. M. WHEAT (Prepared in cooperation with Water Resources Center, Desert Research Institute, University of Nevada System) MACKAY SCHOOL OF MINES UNIVERSITY OF NEVADA • RENO 1979 UNIVERSITY OF NEVADA SYSTEM Board of Regents Robert Cashell, Chairman James L. Buchanan, II Louis E. Lombardi, M.D. Lilly Fong Brenda D. Mason Chris Karamanos John McBride Molly Knudtsen John Tom Ross Donald H. Baepler, Chancellor UNIVERSITY OF NEVADA • RENO Joseph N. Crowley, President MACKAY SCHOOL OF MINES Arthur Baker III, Dean First edition, first printing, 1979: 1500 copies Composed in IBM Press Roman type at the Nevada Bureau of Mines and Geology Printed by Messenger Graphics, Phoenix, Arizona Composition: Janet Amesbury For sale by Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada, 89557. Price $4.00 CONTENTS FOREWORD 5 ACKNOWLEDGEMENTS 5 ABSTRACT 5 INTRODUCTION 6 Previous Investigations 6 The Quantitative Problem 8 The Quantitative Approach 8 Pluvial Lake Mapping 10 Mapping Procedure 10 Age Relationships 11 Lake Distributions 15 Basin Overflow in Lahontan Time 27 Basin Overflow in Pre-Lahontan Time 30 Modern Climate and Estimation of Pluvial Climate 37 Precipitation and Temperature 37 Runoff 39 Evaporation 40 Comparison of Climates 40 Estimated Full Pluvial Climate 43 Evaluation of Lake Lahontan 43 Modern Hydrologic Indices 44 Other Estimates of Pluvial Climates 47 CONCLUSIONS 49 REFERENCES 50 APPENDIX 53 PLATE 1—LATE QUATERNARY PLUVIAL LAKES IN NEVADA in pocket 3 FOREWORD ble aid in the statistical analyses included in this report. -
Why Is Nevada Hot Stuff
WHY IS NEVADA IN HOT WATER? STRUCTURAL CONTROLS AND TECTONIC MODEL OF GEOTHERMAL SYSTEMS IN THE NORTHWESTERN GREAT BASIN James E. Faulds1, Mark Coolbaugh2, Geoffrey Blewitt1, and Christopher D. Henry1 1Nevada Bureau of Mines and Geology and 2Great Basin Center for Geothermal Energy, University of Nevada, Reno, NV 89557 Keywords: Walker Lane, Great Basin, tectonics, structural controls, geothermal systems, Nevada, strike-slip faults, normal faults, strain transfer ABSTRACT In the western Great Basin, the Walker Lane is a system of right-lateral strike-slip faults accommodating ~15-25% of relative motion between the Pacific and North American plates. Relatively high rates of recent (<10 Ma) west-northwest extension absorb northwestward declining dextral motion in the Walker Lane, diffusing that motion into the Basin-Range. Abundant geothermal fields cluster in several northeast-trending belts in the northern Great Basin (e.g. Humboldt structural zone and Black Rock Desert region) and collectively define a broad, northeast-trending zone of high heat flow. Individual fields are largely controlled by north-northeast-striking normal faults. The Walker Lane begins losing displacement to the northwest in west-central Nevada near the southeast margin of the high heat-flow region. The abundant geothermal fields may therefore result from a transfer of northwest-trending dextral shear in the Walker Lane to west-northwest extension in the northern Great Basin. Enhanced extension favors dilation and deep circulation of aqueous solutions along north-northeast-striking faults. The individual belts of geothermal fields probably reflect loci of strain transfer. INTRODUCTION Within the Great Basin of the western US, geothermal fields are in greatest abundance in northern Nevada and neighboring parts of northeast California and southernmost Oregon (Fig.