Siota of Lake Mead Lake Lake Mead Report Series NEVADA - ARIZONA UNITED STATES DEPARTMENT of the INTERIOR - NATIONAL PARK SERVICE 92085355 9 2 0 8 5 3 5 5 \

Total Page:16

File Type:pdf, Size:1020Kb

Siota of Lake Mead Lake Lake Mead Report Series NEVADA - ARIZONA UNITED STATES DEPARTMENT of the INTERIOR - NATIONAL PARK SERVICE 92085355 9 2 0 8 5 3 5 5 \ 92085355 9 2 0 8 5 3 5 5 Siota of Lake Mead lational Recreation Area NEVADA - ARIZONA BIRDS OF THE LAKE MEAD NATIONAL RECREATION AREA LAME Technical Report No. 1 November 1978 Lake Mead Report Series UNITED STATES DEPARTMENT OF THE INTERIOR - NATIONAL PARK SERVICE \ BIOTA OF THE LAKE MEAD NATIONAL RECREATION AREA Nevada/ Arizona The first major survey of the biological resources of the Lake Mead National Recreation Area was initiated in 1974 as a joint endeavor between the National Park Service and the University of Nevada/Las Vegas under the auspices of the Cooperative National Park Resources Studies Unit, University of Nevada/Las Vegas. This research program consists of a series of interdisciplinary investiga­ tions that deal with the plants and animal life of the Lake Mead National Recreation Area and closely adjoining lands. Final reports that result from these studies will be reproduced in a LAKE MEAD PROJECT TECHNICAL REPORT SERIES that will be supplemented by technical papers published as Project Contributions in scientific journals. Cover Drawing by Pat Hansen COOPERATIVE NATIONAL PARK RESOURCES STUDIES UNIT UNIVERSITY OF NEVADA, LAS VEGAS Department of Biological Sciences Las Vegas, Nevada 89154 BIRDS OF THE LAKE MEAD NATIONAL RECREATION AREA LAME Technical Report No. 1 November 1978 by John G. Blake Charles L. Douglas, Unit Leader Senior Research Scientist no-I nv* QH-3C5.1.KI4- NATIONAL PARK SERVICE/UNIVERSITY OF NEVADA, LAS VEGAS Contract Nos. CX 8000-4-0031/CX 8000-6-0034 Contribution Number CPSJ/UNLV 008/09 ï z o t s & r Bateau of ßedamatioa Denver, CO BIRDS OF THE LAKE MEAD NATIONAL RECREATION AREA NEVADA/ARIZONA b y 1 John G. Blake LAME Technical Report No. 1 November 1978 o Wesley E. Niles „ Charles L. Douglas'* 3 Project Directors ■*Dept. of Ecology, Ethology and Evolution, University of Illinois, Champaign ^Dept. of Biological Sciences, University of Nevada, Las Vegas 3 Cooperative National Park Resources Studies Unit/University of Nevada, Las Vegas % fountains OVERTOM- [ ’S i**'lO'" Billy Cool* P . o k # bitter r id g e Bottlfni Mete »> MUD HILLS -I # ! NEVADA i? CLARK Z COUNTY :’n— - o. NEVADA CLARK ( "\) J I Cothtdrol l y r> CA I \ t»“ 0 Ç-. Í * T-/1 ARIZONA ---------- -------------(--------V Cold V p*okok ^ *> 1: l-r- But* ÖSunnto r. Bowl Of MOHAVE \COUNTY i Min J\ f ir * ^URTAInK j^ , _ r ^ < C o tilo Homblln j " * Pooh N) Min. I ' “ -C\londtng J Whilraoro Bonolil® Point ■ • Poek !___4L. ___la.ôViï'ïï.J LAKE * MEAD a m i <1 I_ _ _!xj Oollonbough‘ “ K> LAKE MEAD.> M r CotJ »*b \ ,,ÌW” \ a Crs» V A t Pomi .-V 1 0 r L ^ / Canyon Point i r j i » \y ) \ ^ ( i _________ I 3 6 ° O O1 r - f / ’ y ¡ O “ 0“"* I Wilton ¿ o ™ . \ . J ^ •-J is ] • f M J •— H - --------- ~ ^^Young Tgÿ'Poml1L Amei f\ J Co Ido n _ . _ i Ruto Pooh \ .X 11 J? ARIZONA \ / : MOHAVE \ COUNTY ./Thumb 'V /"t—. / V- C . < L ____P - ‘ EXPLANATION Lake Mead National Recreation Area Boundary a . Corral ¡ACoppor * Mtn Landing Strip I 4 c^N» Springs ! Block ! O^t^-SSi- Primary Roads ----------j-------------- Boundary of Grand Canyon Nationol Park I J {^Fourth (Park wos expanded in 1975 to incorporate Of July 0 WI Cottonwood "] » Coyt V o li oy j BuU area north of Colorado River that formerly wos in the LMNRA) y LOWER COLORADO REGION LAKE MEAD NATIONAL RECREATION AREA K A R IZ O N A -N EVADA #< \ -------- ! r i-- . Doylt OomJj \ i 1 0 1 2 3 4 8 6 v / te a l* of m iitt "io o ■|f> JUNE 1975 " í / * to __________________________________________________\L______________________________________________ TABLE OF CONTENTS Map of the Lake Mead National Recreation Area......................... i Introduction .......................................................... 1 Previous Work.......................................................... 1 Species Composition................................. '. .............. 2 Desert scrub...................................................... 3 R i p a r i a n .......................................................... 4 W o o d l a n d .................................................... 4 Aquatic............................................ 5 Distribution of families........................................ 5 D i s c u s s i o n ............................................. 6 Nonpasserines vs. passerines. ............................ 6 Terrestrial habitats............................................ 7 S|pecies Accounts ................................... • ............... 8 Residential status .................... 8 Abundance classification........................................ 8 Distribution records............................................ 9 Acknowledgements .....'............................................ 10 Table 1. Seasonal distribution, by habitat, of birds found within the Lake Mead National Recreation Area ............... 11 Table 2. Seasonal distribution of avifauna by habitat .............. 31 Table 3. Distribution of non-passerine families occurring on the Lake Mead National Recreation Area ................... 32 Table 4. Distribution of passerine families occurring on the Lake Mead National Recreation Area, according to seasonal status and habitat..................................34 Table 5. Distribution of families by habitat ......................... 35 • Table 6. Seasonal distribution of permanent, sunnier, permanent and sunnier combined, and winter residents of terrestrial habitats within the Lake Mead National Recreation Area . 35 Families Gaviidae. : .................................................... 36 Podicipedidae .................................................... 37 Hydrobat idae ...................................................... 40 Pelecanidae................................................’. 40 Sulidae.................................................... .. 42 ii Families (continued) Phalacrocoracidae 42 Fregatidae . 43 Ardeidae . 44 Ciconiidae . 49 Threskiornithidae 49 An at id ae . 50 Cathartidae. 65 Accipitridae . 66 Pandionidae. 72 Falconidae . 73 Phasianidae. 75 Meleagrididae. .. 77 Gruidae. 77 Rallidae . 78 Charadriidae . 79 Scolopacidae . 82 Recurvirostridae .91 Phalaropodidae . 93 Stercorariidae . 94 Laridae. .... 94 A l c i d a e ........ 101 Coluiribidae . 102 Cuculidae. 104 Tytonidae. 105 Strigidae. 106 Caprimulgidae. 109 Ap od id ae . 111 Trochilidae. 112 Alcedinidae. 114 P i c i d a e ........ 115 Tyrannidae . 119 Alaudidae. 127 Hirundinidae . 128 Corvidae .... 131 iii Families (continued) Paridae........................................................... 135 Sittidae.........................................................137 C e r t h i i d a e ................ 138 Cinclidae.........................................................138 Troglodytidae.....................................................139 Mimidae...........................................................143 Turdidae.........................................................147 Sylviidae.........................................................150 Motacillidae .................................................. 153 Bombycillidae........................................... 153 Ptilogonoatidae.................................................. 154 Laniidae.........................................................155 Sturnidae.........................................................157 Vireonidae.......................................................157 Parulidae.........................................................160 Ploceidae.........................................................172 Icteridae.........................................................173 Thraupidae.......................................................179 Fringillidae .................................................. 180 Literature Cited.......................................................200 Index................................................................. 208 i u n m j c r i o N The Lake Mead National Recreation Area (LMNRA) contains within its boundaries a wide range of habitats, including: lake and riverine areas, marshes, riparian zones, desert scrub and woodland. Such a diversity of habitats, spread over 2500 square miles, supports a large and diverse assemblage of bird species. The number and taxonomic type of birds present varies considerably both between habitats and between seasons. The recreation area provides suitable year-round conditions for some species, while others utilize the area only during the summer or winter. A large number of species and individuals are present on the LMNRA during the spring and/or fall migrations; particularly influential in this respect are the expanded riparian and aquatic areas that resulted from development of the area for production of hydroelectric power and for recreation. Continued visitor use, combined with additional development, may be expected to further influence the bird fauna. Although much of the LMNRA is fairly well known biologically, there still remain areas that are not well studied. In order to document the occurrence and distribution of the flora and fauna of the LMNRA, the U.S. National Park Service, in cooperation with the University of Nevada, Las Vegas, instituted a Resources Basic Inventory. The present report is part of that larger study and includes information on the bird fauna of the recreation area. For each species known to occur, or known to have occurred sometime in the past, on the LMNRA, all known reports (eg. specimens, literature citations, observations) are included, together with the localities in which the bird was reported. Additionally, there is a
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • Lake Mead National Recreation Area Cycle 5 Report
    5RDG,QYHQWRU\DQG&RQGLWLRQ$VVHVVPHQW Lake Mead National Recreation Area LAKE Cycle 5 Report Prepared By: Federal Highway Administration Road Inventory Program (RIP) Data Collected: 05/2012 Report Date: 01/2013 Lake Mead National Recreation Area in Nevada and Arizona ^_ ^_ Salt Lake City ^_ Carson City Cheyenne Denver^_ ! Colorado Springs Las Vegas ! !Long Beach ! ! Anaheim ! Lake MeadAlbuquerque^_ Santa Ana National Recreation! Area !San Diego Phoenix ^_! Mesa Tucson ! El Paso ! DCV = Data Collection Vehicle TABLE OF CONTENTS SECTION PAGE 1. INTRODUCTION 1 - 1 2. PARK ROUTE INVENTORY 5RXWH,'V6XEFRPSRQHQWV &KDQJHV5HSRUW $V$SSOLFDEOH 2 – 1 3. PARK SUMMARY INFORMATION 3DYHG5RXWH0LOHVDQG3HUFHQWDJHVE\)XQFWLRQDO&ODVVDQG3&5 3 – 1 '&95RDG&RQGLWLRQ6XPPDU\ 3 – 3 4. PARK ROUTE LOCATION MAPS 5RXWH/RFDWLRQ.H\0DS 4 – 1 5RXWH/RFDWLRQ$UHD0DS 4 – 2 5RXWH&RQGLWLRQ.H\0DS±3&50LOHE\0LOH 4 – 12 5RXWH&RQGLWLRQ$UHD0DS±3&50LOHE\0LOH 4 – 13 5. PAVED ROUTE CONDITION RATING SHEETS &563DJHV 5 – 1 6. MANUALLY RATED PAVED ROUTE CONDITION RATING SHEETS 0553DJHV 6 – 1 7. PARKING AREA CONDITION RATING SHEETS 3DYHG3DUNLQJ$UHD3DJHV 7 – 1 8. ROUTE MAINTENANCE FEATURES SUMMARIES '&95RXWH0DLQWHQDQFH)HDWXUHV6XPPDU\ 8 – 1 6WUXFWXUH/LVW 8 – 3 9. ROUTE MAINTENANCE FEATURES ROAD LOGS 5RXWH0DLQWHQDQFH)HDWXUHV5RDG/RJV 9 – 1 10. APPENDIX ([SODQDWLRQRI&KDQJHVWRWKH5,3,QGH[(TXDWLRQVDQG'HWHUPLQDWLRQRI3&5 10 – 1 ([SODQDWLRQRIWKH([FHOOHQW*RRG)DLUDQG3RRU&RQGLWLRQ'HVFULSWLRQV 10 – 2 'HVFULSWLRQRI5DWLQJ6\VWHP 10 – 3 6XUIDFH'LVWUHVVHV 10 – 5 ,QGH[)RUPXODV 10 – 12 'DWD&ROOHFWLRQ9HKLFOH6XEV\VWHPV 10 – 16 *HRGDWDEDVH±%DFNJURXQGDQG0HWDGDWD 10 – 19 *ORVVDU\RI7HUPVDQG$EEUHYLDWLRQV 10 – 20 Section 1 Introduction Lake Mead National Recreation Area INTRODUCTION The Federal Highway Administration, (FHWA), in the mid 1970s, was charged with the task of identifying surface condition deficiencies and corrective priorities on National Park Service (NPS) roads and parkways.
    [Show full text]
  • 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.
    [Show full text]
  • What a Gully
    ~~GOLLY9 WHAT A GULLY / History does not record the words spoken by Don Garcia Lopez de Cardenas, proud captain of Castile, that memorable day in 1540 when he and his companions looked into the Grand Canyon, the first Europeans to do so. In all probability those words were strong, soldierly expletives, although a footsore scribe, of a poetical bent, recorded for posterity and prying eyes in Spain that the buttes and towers of the Canyon which "appeared from above to be the height of a man were higher than the tower of the Cathedral of Seville." An apt description, my capitan! The gentle Father Garces came along in 1776 and was quite .impressed by the canyon, giving it the name of "Puerto de Bucareli" in honor of a great Viceroy of Spain. James 0. Pattie, trapper and mountain man, arrived at the canyon in 1826, the first American tourist to visit there. Unfortunately there were no comfortable Fred Harvey accommoda­ tions awaiting him and he was pretty disgusted .with the whole thing . "Horrid mountains ," he wrote . Lt . Joseph Ives , an explorer, came to the "Big Canyon" in 1857 and "paused in wondering delight" but found the region "altogether valueless. Ours has been the first and will doubtless be the last party of whites to visit this profitless locality ," was his studied opinion. But the lieutenant's feet probably were hurting him and he should be forgiven his hasty words . John Wesley Powell, twelve years later, arrived at the canyon the exc1tmg way - by boat down the Colorado. To him it was the "Grand" Canyon and so to all the world it has been ever since.
    [Show full text]
  • Comprehensive Survey of Sedimentation in Lake Mead, 1948-49
    Comprehensive Survey of Sedimentation in Lake Mead, 1948-49 GEOLOGICAL SURVEY PROFESSIONAL PAPER 295 Prepared in collaboration with the U.S. Depart­ ment of the Interior, Bureau of Reclamation; U.S. Department of the Navy, Chief of Naval Opera­ tions', Bureau of Ships, Bureau of Ordnance, Bureau of Naval Personnel, Hydrographic Ojfice, and Navy Electronics Laboratory; U.S. Department ofCommerce, Coast and Geodetic Survey; University of California, Scripps Institution of Oceanography Comprehensive Survey of Sedimentation in Lake Mead, 1948-49 By W. O. SMITH, C. P. VETTER, G. B. CUMMINGS, and others GEOLOGICAL SURVEY PROFESSIONAL PAPER 295 Prepared in collaboration with the U.S. Depart­ ment of the Interior, Bureau of Reclamation; U.S. Department of the Navy, Chief of Naval Opera- tions, Bureau of Ships, Bureau of Ordnance, Bureau of Naval Personnel, Hydrographic Office, and Navy Electronics Laboratory; U.S. Department ofCommerce,Coast andGeodetic Survey; University of California, Scripps Institution of Oceanography UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1960 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. FOREWORD Reservoirs are becoming an increasingly prominent separate inquiry. The importance of evaporation al­ feature of the American landscape. Built for flood ready has led to a separate report on the heat budget. mitigation and to change a fluctuating river into a de­ These problems relate to all reservoirs; but, because pendable source of water for irrigation, power, and of the great size of Lake Mead, the importance and other purposes, they are predestined, like natural lakes, complexity of the problems there reach major propor­ to be destroyed sometime following their creation.
    [Show full text]
  • Comprehensive Survey of Sedimentation in Lake Mead, 1948-49
    Comprehensive Survey of Sedimentation in Lake Mead, 1948-49 GEOLOGICAL SURVEY PROFESSIONAL PAPER 295 Prepared in collaboration with the U.S. Depart- ment of the Interior, Bureau of Reclamation; U.S. Department of the Navy, Chief of Naval Opera- tions', Bureau of Ships, Bureau of Ordnance, Bureau of Naval Personnel, Hydrographic Ojfice, and Navy Electronics Laboratory; U.S. Department ofCommerce, Coast and Geodetic Survey; University of California, Scripps Institution of Oceanography F. INTERPRETATION OF THE LEVELING DATA By C. R. LONGWELL, Yale University Leveling data from the Hoover Dam net are pre- viated basins are shown in plate 4. Alluvium extends sented graphically in two ways. First, the net is di- to considerable depth in the interior parts of nearly all vided into 19 segments, and along each segment the data wide intermont basins; and in some basins that are on altitudes are represented in profile in plate 4. For bounded by large faults, the thick alluvial cover reaches the entire net, differences in level are available covering to the borders of adjacent ranges. On the other hand, the interval 1935 to 1940-41. These differences, along in some wide areas the alluvium above bedrock is thin each segment of the net, are shown by the relation of a or of only moderate thickness. Thus some but not all dotted line to a straight line marked 0. Similarly, the of the highland boundaries shown in plate 4 mark im- total differences for the interval 1935 to 1949-50 are portant changes in subsurface conditions. shown by the relation of a dashed line to the straight The eastern lines of the level net are near the major zero line, in all segments of the net for which these dif- Grand Wash fault zone, which separates the Basin ferences are available.
    [Show full text]
  • 3. Affected Environment
    3. Affected Environment 3.1 Introduction This chapter provides a description of the existing social, economic, and environmental settings for the area affected by the three build alternatives and the No Build Alternative. The affected environment is described for each resource of concern in the Boulder City/ U.S. 93 Corridor Study project area. The discussion contains study methodologies, background information, descriptive data, issues, and values that have a bearing on possible impacts and mitigation measures (described in detail in Chapter 4) and on the selection of the preferred alternative. This EIS was prepared consistent with National Environmental Policy Act of 1969 (NEPA) Council on Environmental Quality (CEQ) regulations (40 CFR 1500. et seq) and the FHWA Guidance for Preparing and Processing Environmental and Section 4(f) Documents (FHWA Technical Advisory T 6640.8A, October 30, 1987). This guidance lists potentially adverse impacts most commonly encountered by highway projects and directs that these factors should be discussed for each reasonable alternative where a potential for impact exists. Environmental and socioeconomic factors potentially impacted by the proposed project are analyzed in detail in this chapter. Factors that were found to have no potential for project-related impacts and are not discussed in this chapter are as follows: x Joint Development x Farmland x Wild and Scenic Rivers x Coastal Barriers x Coastal Zone Impacts The following additional technical studies were prepared for the Boulder City/U.S. 93 Corridor Study DEIS, and they are available through NDOT (contact Daryl James at 775/888-7013 for additional information): x Air Quality x Noise x Biological Resources x Water Quality x Wetlands x Floodplains x Archaeological Resources x Historic Resources x Land Use x Visual Resources x Economics x Social Impacts x Hazardous Waste T012004001SCO/ DRD1333.DOC/ 050740004 3-1 3.
    [Show full text]
  • Ca-Lower-Colorado-River-Valley-Pkwy
    I • I I I ) I I A REPORT TO THE CONGRESS OF THE UNITED STATES ---1 I 'I I I I THE LOWER I COLORADO I RIVER I VALLEY • PARKWAY I I D- '°'le> F; 1-e. ·• NFS- ' f\CAc:.+... \ V"C. , ~ P,of>oseol I ~~~~=-'~c f~l~~c~~w I THE LOWER COLORADO I filVERVALLEYPARKWAY I I I A proposal for a National Parkway and Scenic Recreation Road System along the Lower Colorado River Valley in 'I California, Arizona, and Nevada. I NATIONAL PARK .i DENVER SEfiViC I ·-.-:. a.t ..1flkllb""ll.--';,.i. n II"~ r.· " •· \..' ;: · I ;:~::::.;.;:;.:J I I I U.S. DEPARTMENT OF THE INTERIOR National Park Service I in cooperation with Lower Colorado River Office Bureau of Land Management • PLE~\SE RtTUR?j TO: I February 1969 I , lJnited States Department of the Interior OFFICE OF THE SECRETARY I WASHINGTON, D.C. 20240 I I Dear Mr. President: We are pleased to transmit herewith. a report on the feasibility anc;l desirability of developing a nation~l p;;i.rkwa,y and sc;enic recreation I road system within. the Lower C9l9rado River· Vaiiey in Arizona, Califo~nia, and Nevada, from the Lake Mead National Recreation I Area and Davis Dam on the north to the International Boup.d:;i.ry ~ith Mexico on the south in: the vicinity of San Luis, Arizqna arid Mexic.o.· . ·. ' .. ·.' . ·. I This :i;eport is based on ci. study 11,'lade by the Lower Col<;>rado River Office ap.d the NatiQnal :Par~ Service pf this Depa.rtmep.t with engineerin.g assistance by the Buqlau of Public Roads of the Departmep.t of .
    [Show full text]