Appendix L, Bureau of Land Management Worksheets
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California Vegetation Map in Support of the DRECP
CALIFORNIA VEGETATION MAP IN SUPPORT OF THE DESERT RENEWABLE ENERGY CONSERVATION PLAN (2014-2016 ADDITIONS) John Menke, Edward Reyes, Anne Hepburn, Deborah Johnson, and Janet Reyes Aerial Information Systems, Inc. Prepared for the California Department of Fish and Wildlife Renewable Energy Program and the California Energy Commission Final Report May 2016 Prepared by: Primary Authors John Menke Edward Reyes Anne Hepburn Deborah Johnson Janet Reyes Report Graphics Ben Johnson Cover Page Photo Credits: Joshua Tree: John Fulton Blue Palo Verde: Ed Reyes Mojave Yucca: John Fulton Kingston Range, Pinyon: Arin Glass Aerial Information Systems, Inc. 112 First Street Redlands, CA 92373 (909) 793-9493 [email protected] in collaboration with California Department of Fish and Wildlife Vegetation Classification and Mapping Program 1807 13th Street, Suite 202 Sacramento, CA 95811 and California Native Plant Society 2707 K Street, Suite 1 Sacramento, CA 95816 i ACKNOWLEDGEMENTS Funding for this project was provided by: California Energy Commission US Bureau of Land Management California Wildlife Conservation Board California Department of Fish and Wildlife Personnel involved in developing the methodology and implementing this project included: Aerial Information Systems: Lisa Cotterman, Mark Fox, John Fulton, Arin Glass, Anne Hepburn, Ben Johnson, Debbie Johnson, John Menke, Lisa Morse, Mike Nelson, Ed Reyes, Janet Reyes, Patrick Yiu California Department of Fish and Wildlife: Diana Hickson, Todd Keeler‐Wolf, Anne Klein, Aicha Ougzin, Rosalie Yacoub California -
Arid and Semi-Arid Lakes
WETLAND MANAGEMENT PROFILE ARID AND SEMI-ARID LAKES Arid and semi-arid lakes are key inland This profi le covers the habitat types of ecosystems, forming part of an important wetlands termed arid and semi-arid network of feeding and breeding habitats for fl oodplain lakes, arid and semi-arid non- migratory and non-migratory waterbirds. The fl oodplain lakes, arid and semi-arid lakes support a range of other species, some permanent lakes, and arid and semi-arid of which are specifi cally adapted to survive in saline lakes. variable fresh to saline water regimes and This typology, developed by the Queensland through times when the lakes dry out. Arid Wetlands Program, also forms the basis for a set and semi-arid lakes typically have highly of conceptual models that are linked to variable annual surface water infl ows and vary dynamic wetlands mapping, both of which can in size, depth, salinity and turbidity as they be accessed through the WetlandInfo website cycle through periods of wet and dry. The <www.derm/qld.gov.au/wetlandinfo>. main management issues affecting arid and semi-arid lakes are: water regulation or Description extraction affecting local and/or regional This wetland management profi le focuses on the arid hydrology, grazing pressure from domestic and semi-arid zone lakes found within Queensland’s and feral animals, weeds and tourism impacts. inland-draining catchments in the Channel Country, Desert Uplands, Einasleigh Uplands and Mulga Lands bioregions. There are two broad types of river catchments in Australia: exhoreic, where most rainwater eventually drains to the sea; and endorheic, with internal drainage, where surface run-off never reaches the sea but replenishes inland wetland systems. -
A Great Basin-Wide Dry Episode During the First Half of the Mystery
Quaternary Science Reviews 28 (2009) 2557–2563 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev A Great Basin-wide dry episode during the first half of the Mystery Interval? Wallace S. Broecker a,*, David McGee a, Kenneth D. Adams b, Hai Cheng c, R. Lawrence Edwards c, Charles G. Oviatt d, Jay Quade e a Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, NY 10964-8000, USA b Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512, USA c Department of Geology & Geophysics, University of Minnesota, 310 Pillsbury Drive SE, Minneapolis, MN 55455, USA d Department of Geology, Kansas State University, Thompson Hall, Manhattan, KS 66506, USA e Department of Geosciences, University of Arizona, 1040 E. 4th Street, Tucson, AZ 85721, USA article info abstract Article history: The existence of the Big Dry event from 14.9 to 13.8 14C kyrs in the Lake Estancia New Mexico record Received 25 February 2009 suggests that the deglacial Mystery Interval (14.5–12.4 14C kyrs) has two distinct hydrologic parts in the Received in revised form western USA. During the first, Great Basin Lake Estancia shrank in size and during the second, Great Basin 15 July 2009 Lake Lahontan reached its largest size. It is tempting to postulate that the transition between these two Accepted 16 July 2009 parts of the Mystery Interval were triggered by the IRD event recorded off Portugal at about 13.8 14C kyrs which post dates Heinrich event #1 by about 1.5 kyrs. This twofold division is consistent with the record from Hulu Cave, China, in which the initiation of the weak monsoon event occurs in the middle of the Mystery Interval at 16.1 kyrs (i.e., about 13.8 14C kyrs). -
Ground-Water Resources-Reconnaissance Series Report 20
- STATE OF NEVADA ~~~..._.....,.,.~.:RVA=rl~ AND NA.I...U~ a:~~::~...... _ __,_ Carson City_ GROUND-WATER RESOURCES-RECONNAISSANCE SERIES REPORT 20 GROUND- WATER APPRAISAL OF THE BLACK ROCK DESERT AREA NORTHWESTERN NEVADA By WILLIAM C. SINCLAIR Geologist Price $1.00 PLEASE DO NOT REMO V~ f ROM T. ':'I S OFFICE ;:: '· '. ~- GROUND-WATER RESOURCES--RECONNAISSANCE SERIES .... Report 20 =· ... GROUND-WATER APPRAISAL OF THE BLACK ROCK OESER T AREA NORTHWESTERN NEVADA by William C. Sinclair Geologist ~··· ··. Prepared cooperatively by the Geological SUrvey, U. S. Department of Interior October, 1963 FOREWORD This reconnaissance apprais;;l of the ground~water resources of the Black Rock Desert area in northwestern Nevada is the ZOth in this series of reports. Under this program, which was initiated following legislative action • in 1960, reports on the ground-water resources of some 23 Nevada valleys have been made. The present report, entitled, "Ground-Water Appraisal of the Black Rock Desert Area, Northwe$tern Nevada", was prepared by William C. Sinclair, Geologist, U. s. Geological Survey. The Black Rock Desert area, as defined in this report, differs some~ what from the valleys discussed in previous reports. The area is very large with some 9 tributary basins adjoining the extensive playa of Black Rock Desert. The estimated combined annual recharge of all the tributary basins amounts to nearly 44,000 acre-feet, but recovery of much of this total may be difficult. Water which enters into the ground water under the central playa probably will be of poor quality for irrigation. The development of good produci1>g wells in the old lake sediments underlying the central playa appears doubtful. -
Rice Valley Groundwater Basin Bulletin 118
Colorado River Hydrologic Region California’s Groundwater Rice Valley Groundwater Basin Bulletin 118 Rice Valley Groundwater Basin • Groundwater Basin Number: 7-4 • County: Riverside, San Bernardino • Surface Area: 189,000 acres (295 square miles) Basin Boundaries and Hydrology This groundwater basin underlies Rice Valley in northeast Riverside and southeast San Bernardino Counties. Elevation of the valley floor ranges from about 675 feet above sea level near the center of the valley to about 1,000 feet along the outer margins. The basin is bounded by nonwater- bearing rocks of the Turtle Mountains on the north, the Little Maria and Big Maria Mountains on the south, the Arica Mountains on the west, and by the West Riverside and Riverside Mountains on the east. Low-lying alluvial drainage divides form a portion of the basin boundaries on the northwest and northeast, and the Colorado River bounds a portion of the basin on the east. Maximum elevations of the surrounding mountains range to about 2,000 feet in the Arica Mountains, about 3,000 feet in the Big Maria Mountains, and 5,866 feet at Horn Peak in the Turtle Mountains (Bishop 1963; Jennings 1967; USGS 1971a, 1971b, 1983a, 1983b, 1983c). Annual average precipitation ranges from about 3 to 5 inches. Surface runoff from the mountains drains towards the center of the valley, except in the eastern part of the valley, where Big Wash drains to the Colorado River (USGS 1971a, 1971b, 1983a, 1983b, 1983c). Hydrogeologic Information Water Bearing Formations Alluvium is the water-bearing material that forms the basin and includes unconsolidated Holocene age deposits and underlying unconsolidated to semi-consolidated Pleistocene deposits (DWR 1954, 1963). -
User Notes: Las Cruces, New Mexico, National Wetlands Inventory
USER NOTES : LAS CRUCES, NEW MEXICO, NATIONAL WETLANDS INVENTORY MAP Map Preparation The wetland classifications that appear on the Las Cruces NWI Base Map are in accordance with Cowardin et al .(1977) . The delineations were produced through stereoscope interpretation of 1 :110,000-scale color infrared aerial photographs taken in February, 1971, and 1 :80,000-scale bladk-and-white-aerial photographs taken in March, 1977 . The delineations were enlarged using a zoom transferscope to overlays of 1 :24,000-scale and 1 :62,500-scale . These overlays were then transferred to 1 :100,000-scale to produce the Base Map . Aerial photographs were unavailable for the western portion of the Las Cruces area 1 :62,500-scale map, the western and southern portion of the Afton area 1 :62,500-scale map, and the eastern portions of the White Sands NW, Davies Tank, Newman NW, and Newman SW area 1 :24,000-scale maps . These areas are therefore without wetland designations on the Las Cruces NWI Base Map . Extensive field checks of the delineated wetlands of the Las Cruces NWI Base Map were conducted in June, 1981 to determine the accuracy of the aerial photointerpretation and to provide qualifying descriptions of mapped wetland designations . The user of the map is cautioned that, due to the limitation of mapping primarily through aerial photointerpretation, a small percentage of wetlands may have gone unidentified . Changes in the landscape could have occurred since the time of photography, therefore some discrepancies between the map and current field conditions may exist . Any discrepancies that are encountered in the use of this map should be brought to the attention of Warren Hagenbuck, Regional Wetlands Coordinator, U . -
Some Desert Watering Places
DEPAETMENT OF THE INTEEIOE UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DiRECTOK WATER-SUPPLY PAPER 224 SOME DESERT WATERING PLACES IN SOUTHEASTEEN CALIFORNIA AND SOUTHWESTERN NEVADA BY WALTER C. MENDENHALL WASHINGTON GOVERNMENT PRINTING OFFICE 1909 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR WATER-SUPPLY PAPEK 224 SOME DESERT WATERING PLACES IN SOUTHEASTEEN CALIFOKNIA AND SOUTHWESTEKN NEVADA BY WALTER C. MENDENHALL WASHINGTON GOVERNMENT PRINTING OFFICE 1909 CONTENTS. Page. Introduction______________________________________ 5 Area considered_________________________________ 5 Mineral resources and industrial developments______________ . 6 Sources of data__________________________________ 7 Physical features__________________________________ 8 General character of the region______________________ 8 Death Valley basin__________________________________ 9 Soda Lake_____________________________________ 30 Salton Sink______________________________________ 10 A great trough_______________________________ 30 Fault lines__________________.____ ______________ 11 Climate______________________. ____ ______________ 11 Water supply_________ _________________________ 13 Origin_________________________________________ 13 Rivers______________________________________ 13 Springs__________________________________________ 15 Finding water_______________________________ 16 Camping places_______________________________ 16 Mountain springs and tanks______________________ 17 Dry lakes____________________________________ -
Comprehensive Conservation Plan, Lake Andes National Wildlife Refuge Complex, South Dakota
Comprehensive Conservation Plan Lake Andes National Wildlife Refuge Complex South Dakota December 2012 Approved by Noreen Walsh, Regional Director Date U.S. Fish and Wildlife Service, Region 6 Lakewood, Colorado Prepared by Lake Andes National Wildlife Refuge Complex 38672 291st Street Lake Andes, South Dakota 57356 605 /487 7603 U.S. Fish and Wildlife Service Region 6, Mountain–Prairie Region Division of Refuge Planning 134 Union Boulevard, Suite 300 Lakewood, Colorado 80228 303 /236 8145 CITATION for this document: U.S. Fish and Wildlife Service. 2012. Comprehensive Conservation Plan, Lake Andes National Wildlife Refuge Complex, South Dakota. Lakewood, CO: U.S. Department of the Interior, U.S. Fish and Wildlife Service. 218 p. Comprehensive Conservation Plan Lake Andes National Wildlife Refuge Complex South Dakota Submitted by Concurred with by Michael J. Bryant Date Bernie Peterson. Date Project Leader Refuge Supervisor, Region 6 Lake Andes National Wildlife Refuge Complex U.S. Fish and Wildlife Service Lake Andes, South Dakota Lakewood, Colorado Matt Hogan Date Assistant Regional Director U.S. Fish and Wildlife Service, Region 6 National Wildlife Refuge System Lakewood, Colorado Contents Summary ....................................................................................................................................... XI Abbreviations .................................................................................................................................. XVII CHAPTER 1–Introduction ..................................................................... -
CALIFORNIA BIGHORN SHEEP Unit 034
Nevada Hunter Information Sheet CALIFORNIA BIGHORN SHEEP Unit 034 LOCATION: This unit is located northwest of the town of Winnemucca. The unit is bounded on the north by the Leonard Creek - Knotted Creek - Summit Lake -Idaho Canyon Road, is bounded on the east by Units 031 and 035, the south by Unit 041, and on the west by Unit 012. ELEVATION: Elevations range from 8,600' at the top of the Black Rock Range to 3,848' at the lowest portion of the Black Rock Desert. TERRAIN: The Black Rock Range is the main mountain range in the unit and runs in a north/south direction. The side canyons are steep, rugged and drain into the valley floor or basins surrounding the mountain. The majority of the basin is comprised of the Black Rock Desert. VEGETATION: The desert floor has no vegetation or is sparsely vegetated with salt shrubs. The foothill country to the 6,500-foot elevation is dominated by sagebrush. Above 6,500', sites typically have aspen in the drainages, islands of mahogany, and shrubs and grasses. LAND STATUS: Approximately 85% of the unit is public lands. The balance is private lands associated with agriculture or mining. The Summit Lake Indian reservation is located in the northwest portion of the unit and is closed to hunting and fishing. HUNTER ACCESS: Within the Black Rock Desert-High Rock Canyon Emigrant Trails National Conservation Area (NCA) signed into law 12/21/2000, there are a number of newly created Wilderness Areas. No motorized or mechanical vehicles or equipment are allowed inside these areas. -
Palen Solar Project Water Supply Assessment
Palen Solar Project Water Supply Assessment Prepared by Philip Lowe, P.E. February 2018 Palen Solar Project APPENDIX G. WATER SUPPLY ASSESSMENT Contents 1. Introduction ......................................................................................................................... 1 2. Project Location and Description ...................................................................................... 1 3. SB 610 Overview and Applicability .................................................................................... 3 4. Chuckwalla Valley Groundwater Basin .............................................................................. 4 4.1 Basin Overview and Storage ......................................................................................................... 4 Groundwater Management ............................................................................................................ 5 4.2 Climate .......................................................................................................................................... 5 4.3 Groundwater Trends ...................................................................................................................... 5 4.4 Groundwater Recharge .................................................................................................................. 7 Subsurface Inflow ......................................................................................................................... 7 Recharge from Precipitation ......................................................................................................... -
California Desert Protection Act of 1993 CIS-NO
93 CIS S 31137 TITLE: California Desert Protection Act of 1993 CIS-NO: 93-S311-37 SOURCE: Committee on Energy and Natural Resources. Senate DOC-TYPE: Hearing DOC-NO: S. Hrg. 103-186 DATE: Apr. 27, 28, 1993 LENGTH: iii+266 p. CONG-SESS: 103-1 ITEM-NO: 1040-A; 1040-B SUDOC: Y4.EN2:S.HRG.103-186 MC-ENTRY-NO: 94-3600 INCLUDED IN LEGISLATIVE HISTORY OF: P.L. 103-433 SUMMARY: Hearings before the Subcom on Public Lands, National Parks, and Forests to consider S. 21 (text, p. 4-92), the California Desert Protection Act of 1993, to: a. Expand or designate 79 wilderness areas, one wilderness study area in the California Desert Conservation Area, and one natural reserve. b. Expand and redesignate the Death Valley National Monument as the Death Valley National Park and the Joshua Tree National Monument as the Joshua Tree National Park. c. Establish the Mojave National Park and the Desert Lily Sanctuary. d. Direct the Department of Interior to enter into negotiations with the Catellus Development Corp., a publicly owned real estate development corporation, for an agreement or agreements to exchange public lands or interests for Catellus lands or interests which are located within the boundaries of designated wilderness areas or park units. e. Withdraw from application of public land laws and reserve for Department of Navy use certain Federal lands in the California desert. f. Permit military aircraft training and testing overflights of the wilderness areas and national parks established in the legislation. Title VIII is cited as the California Military Lands Withdrawal and Overflights Act of 1991. -
Hydrogeology of Spring, Cave, Dry Lake, and Delamar Valleys Impacts
HYDROGEOLOGY OF SPRING, CAVE, DRY LAKE, AND DELAMAR VALLEYS IMPACTS OF DEVELOPING SOUTHERN NEVADA WATER AUTHORITY’S CLARK, LINCOLN, AND WHITE PINE COUNTIES GROUNDWATER DEVELOPMENT PROJECT Presented to the Office of the Nevada State Engineer on behalf of Protestants White Pine County, Great Basin Water Network, et al. June, 2017 Prepared by: _______________________________________________________________ Thomas Myers, Ph.D. Hydrologic Consultant Reno, NV June 28, 2017 Date Table of Contents Summary ................................................................................................................................................. 1 Introduction ............................................................................................................................................ 3 Method of Analysis .................................................................................................................................. 3 Study Area ........................................................................................................................................... 5 Water Rights Applications and Proposed Pumping Scenarios ............................................................... 8 Conceptual Flow Model ..................................................................................................................... 10 White River Flow System ................................................................................................................... 25 Hydrogeologic Properties of Aquifer Systems