Biota of Lake Mead: Annotated Checklist and Bibliography
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Tectonic Influences on the Spatial and Temporal Evolution of the Walker Lane: an Incipient Transform Fault Along the Evolving Pacific – North American Plate Boundary
Arizona Geological Society Digest 22 2008 Tectonic influences on the spatial and temporal evolution of the Walker Lane: An incipient transform fault along the evolving Pacific – North American plate boundary James E. Faulds and Christopher D. Henry Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada, 89557, USA ABSTRACT Since ~30 Ma, western North America has been evolving from an Andean type mar- gin to a dextral transform boundary. Transform growth has been marked by retreat of magmatic arcs, gravitational collapse of orogenic highlands, and periodic inland steps of the San Andreas fault system. In the western Great Basin, a system of dextral faults, known as the Walker Lane (WL) in the north and eastern California shear zone (ECSZ) in the south, currently accommodates ~20% of the Pacific – North America dextral motion. In contrast to the continuous 1100-km-long San Andreas system, discontinuous dextral faults with relatively short lengths (<10-250 km) characterize the WL-ECSZ. Cumulative dextral displacement across the WL-ECSZ generally decreases northward from ≥60 km in southern and east-central California, to ~25 km in northwest Nevada, to negligible in northeast California. GPS geodetic strain rates average ~10 mm/yr across the WL-ECSZ in the western Great Basin but are much less in the eastern WL near Las Vegas (<2 mm/ yr) and along the northwest terminus in northeast California (~2.5 mm/yr). The spatial and temporal evolution of the WL-ECSZ is closely linked to major plate boundary events along the San Andreas fault system. For example, the early Miocene elimination of microplates along the southern California coast, southward steps in the Rivera triple junction at 19-16 Ma and 13 Ma, and an increase in relative plate motions ~12 Ma collectively induced the first major episode of deformation in the WL-ECSZ, which began ~13 Ma along the N60°W-trending Las Vegas Valley shear zone. -
Lake Mead National Recreation Area Lake Meadsummer 2013 National Recreation Area
National Park Service Park Newspaper U.S. Department of the Interior Lake Mead National Recreation Area Lake MeadSummer 2013 National Recreation Area Borrow a Lifejacket insure the proper size. The loaner lifejackets including education, warnings and citations. The point of the rule isn't to ticket boaters, but to Drowning is the number one cause of fatalities at must be returned before dusk to allow ensure that the most polluting engines are kept Lake Mead National Recreation Area. This loss rangers to inspect and properly store them. off the lake. As time passes, the number of non- of life can be prevented by wearing a lifejacket. Please remember to never leave children compliant PWCs will decline through attrition. unattended. Drowning is preventable if you put on a lifejacket. Wear One for Life! PWCs that meet the standards through the use of direct-injection two-stroke or New Personal Watercraft four-stroke engines are not subject to this prohibition and are still allowed on the lakes. Regulation in Effect Engines that meet the regulations should have an In an effort to safeguard the waters within Lake emission control information label that clearly Mead National Recreation Area, personal water- states that they conform to clean emissions stan- craft (PWC) must now meet 2006 Environmental dards. Boats are not impacted by this regulation. Protection Agency emission standards in order to operate within the park. This includes the waters of A list of frequently asked questions and PWC Lake Mead, Lake Mohave and the Colorado River. models that meet the emissions standards can be This year there are new Lifejacket Loaner found online at: Stations at Boulder Beach and Cottonwood “Lake Mead supplies drinking water for millions www.nps.gov/lake/parkmgmt/twostroke.htm. -
Chapter One – Existing Conditions
Laughlin Land Use Plan Adopted - July 2017 ACKNOWLEDGEMENTS Clark County Board of Commissioners: Laughlin Town Advisory Board: Steve Sisolak, Chair James Maniaci, Chair Susan Brager, Vice-Chair Kathy Ochs, Vice-Chair Larry Brown Stephanie Bethards Chris Giunchigliani Bruce Henry Marilyn Kirkpatrick Gina Mackey Mary Beth Scow Tammy Harris, Secretary Lawrence Weekly Brian Paulson, County Liaison Office of County Manager: Planning Commission: Yolanda King, Manager Dan Shaw, Chair Randy Tarr, Assistant Manager J. Dapper, Vice-Chair Jeff Wells, Assistant Manager Edward Frasier III Kevin Schiller, Assistant Manager Vivian Kilarski Tom Morley Department of Comprehensive Planning: Nelson Stone Nancy Amundsen, Director Donna Tagliaferrri Community Planning Team: Mario Bermudez, Planning Manager Shane Ammerman, Assistant Planning Manager Kevin Smedley, Principal Planner & Project Lead Paul Doerr, Senior Planner Chris LaMay, GIS Analyst Garrett TerBerg, Principal Planner Michael Popp, Sr. Management Analyst Justin Williams, Parks Planner Ron Gregory, Trails Assistant Planning Manager Scott Hagen, Senior Planner Laughlin Land Use Plan 2017 i ii Laughlin Land Use Plan TABLE OF CONTENTS Introduction ............................................................................................................. 1 State Law ............................................................................................................ 1 Background ......................................................................................................... 1 Purpose -
Las Vegas Wash and Lake Mead
Publications (WR) Water Resources 1996 Synthetic organic compounds: Las Vegas Wash and Lake Mead National Water Quality Assessment Program (NAWQA): Nevada Basin and Range Follow this and additional works at: https://digitalscholarship.unlv.edu/water_pubs Part of the Biogeochemistry Commons, Desert Ecology Commons, Environmental Indicators and Impact Assessment Commons, Environmental Monitoring Commons, Fresh Water Studies Commons, Natural Resource Economics Commons, Natural Resources and Conservation Commons, Natural Resources Management and Policy Commons, Sustainability Commons, and the Water Resource Management Commons Repository Citation National Water Quality Assessment Program (NAWQA): Nevada Basin and Range (1996). Synthetic organic compounds: Las Vegas Wash and Lake Mead. Available at: https://digitalscholarship.unlv.edu/water_pubs/79 This Technical Report is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Technical Report in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/or on the work itself. This Technical Report has been accepted for inclusion in Publications (WR) by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. INTRODUCTION and industrial compounds), polycyclic aromatic hydrocarbons (PAH's), phthalales, and phenols were detected at one or both The Nevada Basin and Range (NVBR) study unit of the of these sites. Many of these compounds are persistent in the U.S. -
Reptile and Amphibian List RUSS 2009 UPDATE
National CHistoricalhaco Culture Park National ParkNational Service Historical Park Chaco Culture U.S. DepartmentNational of Park the Interior Service U.S. Department of the Interior Reptiles and Amphibians MEXICAN SPADEFOOT TOAD (SPEA MULTIPLICATA) Best seen on summer nights after rains, the Mexican spadefoot toad is one of two spadefoot toads located in the canyon. Look for rock art in the park representing this amphibian. EASTERN COLLARED LIZARD (CROTAPHYTUS COLLARIS) These brightly colored (turquoise, yellow, and black) lizards are a favorite of many park visitors. Highly visible and very common in the park, watch for these creatures near Pueblo Alto and nearly all of the sites. EASTERN FENCE OR SAGEBRUSH LIZARD (SCELOPORUS GRACIOSUS) Found in all of the habitats in Chaco, the fence lizard is the most abundant lizard in the canyon. You can see them climbing on rocks, at the Chacoan buildings and around the Visitor Center. TIGER SALAMANDER (ABYSTOMA TIGRINUM) The tiger salamander occurs throughout the park environs, but is not commonly seen. Their larvae have been seen in pools of water in the Chaco Wash. WESTERN RATTLESNAKE (CROTALUS VIRIDIS) Chaco does host a population of rattlesnakes! PLATEAU STRIPED WHIPTAIL (CNEMIDOPHORUS VALOR) Don’t be too alarmed, the snakes tend to be rather Also very visible in the park, the whiptail can be shy. Watch for them in the summer months par- seen on many trails in the frontcountry and ticularly along trails and sunning themselves on backcountry. paved roads. Avoid hitting them! EXPERIENCE YOUR AMERICA Amphibian and Reptile List Chaco Culture National Historical Park is home to a wide variety of amphibians and reptiles. -
Petition to List the Relict Leopard Frog (Rana Onca) As an Endangered Species Under the Endangered Species Act
BEFORE THE SECRETARY OF INTERIOR PETITION TO LIST THE RELICT LEOPARD FROG (RANA ONCA) AS AN ENDANGERED SPECIES UNDER THE ENDANGERED SPECIES ACT CENTER FOR BIOLOGICAL DIVERSITY SOUTHERN UTAH WILDERNESS ALLIANCE PETITIONERS May 8, 2002 EXECUTIVE SUMMARY The relict leopard frog (Rana onca) has the dubious distinction of being one of the first North American amphibians thought to have become extinct. Although known to have inhabited at least 64 separate locations, the last historical collections of the species were in the 1950s and this frog was only recently rediscovered at 8 (of the original 64) locations in the early 1990s. This extremely endangered amphibian is now restricted to only 6 localities (a 91% reduction from the original 64 locations) in two disjunct areas within the Lake Mead National Recreation Area in Nevada. The relict leopard frog historically occurred in springs, seeps, and wetlands within the Virgin, Muddy, and Colorado River drainages, in Utah, Nevada, and Arizona. The Vegas Valley leopard frog, which once inhabited springs in the Las Vegas, Nevada area (and is probably now extinct), may eventually prove to be synonymous with R. onca. Relict leopard frogs were recently discovered in eight springs in the early 1990s near Lake Mead and along the Virgin River. The species has subsequently disappeared from two of these localities. Only about 500 to 1,000 adult frogs remain in the population and none of the extant locations are secure from anthropomorphic events, thus putting the species at an almost guaranteed risk of extinction. The relict leopard frog has likely been extirpated from Utah, Arizona, and from the Muddy River drainage in Nevada, and persists in only 9% of its known historical range. -
HUNTER INFORMATION SHEET DESERT BIGHORN Unit 266
HUNTER INFORMATION SHEET DESERT BIGHORN Unit 266 LOCATION: Unit 266 is situated in southern Clark County and comprises the northern portion of the Eldorado Mountains. ELEVATION: Elevations range from 656' at lake level (Lake Mohave) to 3,773' above Oak Creek Canyon. TERRAIN: Topographic features vary from rolling hills on the western margin of bighorn sheep habitat to the sheer, vertical cliffs characteristic of Black Canyon. VEGETATION: Vegetation is typical of the Mojave Desert=s creosote bush scrub community. Prominent vegetative types within this community include creosote and white bursage. LAND STATUS: The majority of the area that offers opportunities to hunt bighorn sheep lies within the Lake Mead National Recreation Area, and is administered by the National Park Service. A minor portion of bighorn sheep habitat is within the jurisdiction of the Bureau of Land Management, Las Vegas District. HUNTER ACCESS: Hunter access is considered good given the network of National Park Service approved roads. Some hunters opt to use boats to learn their area, and to access points which would otherwise be more difficult to reach on foot. Note: Please be aware that sections of this unit are in a wilderness area. Motorized equipment, mechanized transport, including wheeled game carriers and chainsaws, are prohibited in wilderness areas. Contact the Federal Management Agency responsible for this area for more information. MAP REFERENCE: Maps are available for purchase from BLM, or through private vendors such as Mercury Blueprint & Supply Co. (Las Vegas), Desert Outfitters (Las Vegas) or Oakman=s (Reno). At a minimum, hunters should possess the United States Geologic Survey, Boulder City 1:100,000-scale topographic map (30 x 60 minute quadrangle). -
Yanawant: Paiute Places and Landscapes in the Arizona Strip
Yanawant Paiute Places and Landscapes in the Arizona Strip Volume Two OfOfOf The Arizona Strip Landscapes and Place Name Study Prepared by Diane Austin Erin Dean Justin Gaines December 12, 2005 Yanawant Paiute Places and Landscapes in the Arizona Strip Volume Two Of The Arizona Strip Landscapes and Place Name Study Prepared for Bureau of Land Management, Arizona Strip Field Office St. George, Utah Prepared by: Diane Austin Erin Dean Justin Gaines Report of work carried out under contract number #AAA000011TOAAF030023 2 Table of Contents Preface……………………………………………………………………………………………ii i Chapter One: Southern Paiute History on the Arizona Strip………………………………...1 Introduction.............................................................................................................................. 1 1.1 Early Southern Paiute Contact with Europeans and Euroamericans ........................... 5 1.2 Southern Paiutes and Mormons ........................................................................................ 8 1.3 The Second Powell Expedition......................................................................................... 13 1.4 An Onslaught of Cattle and Further Mormon Expansion............................................ 16 1.5 Interactions in the First Half of the 20 th Century ......................................................... 26 Chapter Two: Southern Paiute Place Names On and Near the Arizona Strip 37 Introduction ........................................................................................................................... -
The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology
EXHIBIT 89 The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology Dr. Saxon E. Sharpe, Dr. Mary E. Cablk, and Dr. James M. Thomas Desert Research Institute May 2007 Revision 01 May 2008 Publication No. 41231 DESERT RESEARCH INSTITUTE DOCUMENT CHANGE NOTICE DRI Publication Number: 41231 Initial Issue Date: May 2007 Document Title: The Walker Basin, Nevada and California: Physical Environment, Hydrology, and Biology Author(s): Dr. Saxon E. Sharpe, Dr. Mary E. Cablk, and Dr. James M. Thomas Revision History Revision # Date Page, Paragraph Description of Revision 0 5/2007 N/A Initial Issue 1.1 5/2008 Title page Added revision number 1.2 “ ii Inserted Document Change Notice 1.3 “ iv Added date to cover photo caption 1.4 “ vi Clarified listed species definition 1.5 “ viii Clarified mg/L definition and added WRPT acronym Updated lake and TDS levels to Dec. 12, 2007 values here 1.6 “ 1 and throughout text 1.7 “ 1, P4 Clarified/corrected tui chub statement; references added 1.8 “ 2, P2 Edited for clarification 1.9 “ 4, P2 Updated paragraph 1.10 “ 8, Figure 2 Updated Fig. 2007; corrected tui chub spawning statement 1.11 “ 10, P3 & P6 Edited for clarification 1.12 “ 11, P1 Added Yardas (2007) reference 1.13 “ 14, P2 Updated paragraph 1.14 “ 15, Figure 3 & P3 Updated Fig. to 2007; edited for clarification 1.15 “ 19, P5 Edited for clarification 1.16 “ 21, P 1 Updated paragraph 1.17 “ 22, P 2 Deleted comma 1.18 “ 26, P1 Edited for clarification 1.19 “ 31-32 Clarified/corrected/rearranged/updated Walker Lake section 1.20 -
Fish and Wildlife
Appendix B Upper Middle Mainstem Columbia River Subbasin Fish and Wildlife Table 2 Wildlife species occurrence by focal habitat type in the UMM Subbasin, WA. -
4 References
4 References Agricultural Extension Office. 2000. Sedges. Available at: http://aquaplant.tamu.edu/Emergent%20Plants/Sedges/Sedges.htm Accessed April 2004 Allen, D.B., B.J. Flatter, J. Nelson and C. Medrow. 1998. Redband Trout Oncorhynchus mykiss gairdneri Population and Stream Habitat Surveys in Northern Owyhee County and the Owyhee River and Its Tributaries. 1997. Idaho BLM Technical Bulletin No. 98-14. American Fisheries Society, Idaho Chapter (AFS). 2000. Fishes of Idaho. Available at < http://www.fisheries.org/idaho/fishes_of_idaho.htm>. Accessed November 2003. American Ornithologists’ Union (AOU). 1957. Check-list of North American Birds. 5th edition. American Ornithological Union, Washington, DC. Anderson, A. E., and O. C. Wallmo. 1984. Odocoileus hemionus. Mammalian Species 219:1– 9. Anderson, J. L., K. Bacon, and K. Denny. 2002. Salmon River Habitat Enhancement. Annual Report 2001. Shoshone-Bannock Tribes, Fort Hall, ID. 14 pp. Anderson, M., P. Bourgeron, M. T. Bryer, R. Crawford, L. Engelking, D. Faber-Langendoen, M. Gallyoun, K. Goodin, D. H. Grossman, S. Landaal, K. Metzler, K. D. Patterson, M. Pyne, M. Reid, L. Sneddon, and A. S. Weakley. 1998. International Classification of Ecological Communities: Terrestrial Vegetation of the United States. Volume II. The National Vegetation Classification System: List of Types. The Nature Conservancy, Arlington, VA. Arno, S. F. 1979. Forest Regions of Montana. Research Paper INT-218. U.S. Department of Agriculture, U.S. Forest Service, Intermountain Forest and Range Experiment Station. Arno, S.F. 1980. Forest Fire History in the Northern Rockies. Journal of Forestry 78:460–464. Aubry, K. B., Koehler, G. M., and J. R. Squires. -
Utah Geological Association Publication 30.Pub
Utah Geological Association Publication 30 - Pacific Section American Association of Petroleum Geologists Publication GB78 239 CENOZOIC EVOLUTION OF THE NORTHERN COLORADO RIVER EXTEN- SIONAL CORRIDOR, SOUTHERN NEVADA AND NORTHWEST ARIZONA JAMES E. FAULDS1, DANIEL L. FEUERBACH2*, CALVIN F. MILLER3, 4 AND EUGENE I. SMITH 1Nevada Bureau of Mines and Geology, University of Nevada, Mail Stop 178, Reno, NV 89557 2Department of Geology, University of Iowa, Iowa City, IA 52242 *Now at Exxon Mobil Development Company, 16825 Northchase Drive, Houston, TX 77060 3Department of Geology, Vanderbilt University, Nashville, TN 37235 4Department of Geoscience, University of Nevada, Las Vegas, NV 89154 ABSTRACT The northern Colorado River extensional corridor is a 70- to 100-km-wide region of moderately to highly extended crust along the eastern margin of the Basin and Range province in southern Nevada and northwestern Arizona. It has occupied a criti- cal structural position in the western Cordillera since Mesozoic time. In the Cretaceous through early Tertiary, it stood just east and north of major fold and thrust belts and also marked the northern end of a broad, gently (~15o) north-plunging uplift (Kingman arch) that extended southeastward through much of central Arizona. Mesozoic and Paleozoic strata were stripped from the arch by northeast-flowing streams. Peraluminous 65 to 73 Ma granites were emplaced at depths of at least 10 km and exposed in the core of the arch by earliest Miocene time. Calc-alkaline magmatism swept northward through the northern Colorado River extensional corridor during early to middle Miocene time, beginning at ~22 Ma in the south and ~12 Ma in the north.