Chapter G. Mineral Resource Potential of the Virgin River Area Of

Total Page:16

File Type:pdf, Size:1020Kb

Chapter G. Mineral Resource Potential of the Virgin River Area Of Mineral Resource Assessment of Selected Areas in Clark and Nye Counties, Nevada, Edited by Steve Ludington U.S. Geological Survey Scientific Investigations Report 2006-5197 Prepared in cooperation with the Nevada Bureau of Mines and Geology and the University of Nevada, Las Vegas Chapter I. Mineral Resource Potential of the Rainbow Gardens Area of Critical Environmental Concern, Clark County, Nevada By Stephen B. Castor, Steve Ludington, Brett T. McLaurin, and Kathryn S. Flynn Summary and Conclusions and representatives of companies with mining operations in and near the areas were contacted. The Rainbow Gardens Area of Critical Environmen- Definitions of mineral resource potential and certainty tal Concern (ACEC) contains known deposits of gypsum, levels are given in appendix 1, and are similar to those out- as well as prospects for limestone, silica, lithium, copper, lined by Goudarzi (1984). uranium, and sand and gravel aggregate. Only gypsum has been mined in significant quantities, and the PABCO (Apex) gypsum mine, immediately adjacent to the ACEC, is a major Lands Involved gypsum source, producing more than 1,000,000 short tons of gypsum annually. The Rainbow Gardens ACEC is east of Las Vegas and The ACEC contains areas of high mineral resource southeast of Interstate 15 (fig. 1). The ACEC is bounded on potential for gypsum deposits in the Tertiary Muddy Creek the southeast and east by the Lake Mead National Recreation Formation and areas of moderate mineral resource potential Area and on the north by Nellis Air Force Base. It is accessed for gypsum in the Mesozoic Moenkopi Formation. Areas with most easily from Nevada State Highway 143 (Lake Mead high potential for limestone deposits are found in the northern Boulevard) and by several secondary and primitive roads part of the ACEC. There is an area with moderate potential for that branch off of this highway. It may also be accessed from lithium (hectorite clay) deposits. The potential for undiscov- Hollywood Boulevard in southeast Las Vegas and by primi- ered deposits of silica, uranium, and metals is low. tive roads in that area. A legal description of these lands is The ACEC has areas with high, moderate, and low included in appendix 2. potential for crushed-stone aggregate deposits. Unconsolidated material in the ACEC has high potential for sand and gravel aggregate deposits. Physiographic Description The Rainbow Gardens ACEC is named for an area of colorful rock strata near its southeastern boundary. Near its Introduction western boundary, it includes Frenchman Mountain, a rug- ged ridge that forms the eastern backdrop for Las Vegas and This report was prepared for the U.S. Bureau of Land reaches elevations of more than 1,200 m. The northwest part Management (BLM) to provide information for land plan- of the ACEC includes Sunrise Mountain, which is more than ning and management, and, specifically, to determine min- 1,000 m in height. The lowest part of the ACEC is at an eleva- eral resource potential in accordance with regulations at 43 tion of about 440 m along its southern boundary in Las Vegas CFR 2310, which governs the withdrawal of public lands. Wash, which drains into Lake Mead to the east. Streams and The Clark County Conservation of Public Land and Natu- washes in the Rainbow Gardens ACEC drain westward into ral Resources Act of 2002 temporarily withdraws the lands Las Vegas basin and eastward into Lake Mead. described herein from mineral entry, pending final approval of an application for permanent withdrawal by the BLM. This report provides information about mineral resource potential of these lands. Geologic Setting The Rainbow Gardens ACEC was studied in the field to confirm descriptions of the geology that were gleaned from The Rainbow Gardens ACEC is in the Basin and Range the scientific literature. Samples were collected and analyzed, Physiographic Province, which is characterized by north- I2 Mineral Resource AssessmentofSelectedAreasinClarkandNyeCounties,Nevada 115°0'0"W 114°52'30"W 36°15'0"N Ths Gypsum prospects uPzc uPzc lPzc Exploratory uPzs oil well Ths uPzc Sandia Rock sand and gravel Ths uPzc lPzc pit uPzc uPzs AP-248 Abandoned lt Ths u uPzc uPzs Ths a uPzc sand and gravel F JTRs uPzs uPzs uPzc Ths pits n uPzc uPzc uPzc a uPzc m JTRs Pabco (Apex) uPzc h uPzc uPzs uPzc Scale 1:24,000 c gypsum mine n e uPzc Boulevard Fa ult Tsy r uPzc and mill F Tvy Tvy AP-247 Qu uPzs JTRs uPzc Pioneer Xm Qu Copper prospect JTRs gypsum mine lPzc uPzc Ths Uranium prospect RAINBOW GARDENS Ths Ths lPzs ACEC Tvy JTRs Ths Tvy Qu uPzc North Rainbow Gardens Tvy Qu Ths gypsum mines AP-129 uPzc Exploratory oil well Tvy AP-125 JTRs AP-126 Frenchman Ti Abandoned AP-127 Mill Site sand and gravel JTRs Tvy pits GoldButteACEC AP-131 East Rainbow Gardens White Eagle AP-130 gypsum mines gypsum mines 36°7'30"N AP-128 Fren Exploratory chman Fault Tsy oil well Tsy Qu Tvy Ths Tvy Tsy Tvy Ths Kilometers 024681 Xm Figure 1. Generalized geology of the Rainbow Gardens Area of Critical Environmental Concern, showing mines, prospects, and locations of analyzed samples. Geology modified from Stewart and Carlson (1978). Rainbow Gardens ACEC I3 EXPLANATION trending mountain ranges and intervening valleys. However, the ACEC lies near the border of this province with the Colo- Qu Undivided surficial deposits (Pleistocene and rado Plateaus Province and exposes Paleozoic and Mesozoic Holocene)—Alluvial, colluvial, lake, playa, landslide, strata that are similar to those of the Colorado Plateaus. The terrace, and eolian sand deposits geology of the region is characterized by rocks ranging in age QTs Sedimentary rocks (Pliocene and Pleistocene)—Mostly from Proterozoic through Miocene that are cut by a complex lake and alluvial deposits of late Cenozoic extensional faults. Important regional struc- Tsy Young sedimentary rocks (middle Miocene to Pliocene)—Alluvial, lacustrine, and fluvial deposits. tural features include the Lake Mead Fault system, the Las Locally includes minor amounts of tuff. Includes Muddy Vegas Valley shear zone, and steep to moderately dipping nor- Creek Formation mal faults. The Las Vegas Valley shear zone is a major west- Ths Horse Spring Formation (upper Oligocene and northwest-striking right-lateral fault zone that extends across Miocene)—Clastic and tuffaceous sedimentary rocks; much of southern Nevada. It has accommodated as much as includes some volcanic rocks, limestone, and gypsum 65 km of dextral displacement to the northwest of the ACEC Tvy Young volcanic rocks (middle and upper Miocene)- (Longwell, 1974; Wernicke and others, 1988; Deubendorfer Rhyolite, andesite, and basalt lava flows, tuff, and and Black, 1992) and is associated with large-magnitude tuffaceous sediments clockwise rotation of adjacent rocks. The Lake Mead Fault Ti Intrusive rocks (Oligocene and Miocene)—Aphanitic, porphyritic, and coarsely crystalline rocks ranging in system is a major east-northeast-striking left-lateral fault zone composition from gabbro to granite (Anderson, 1973) that appears to merge with the right-lateral JTRs Sedimentary rocks (Triassic and Jurassic)—Shale, Las Vegas Valley shear zone. mudstone, siltstone, sandstone, and carbonate rock; some sparse volcanic rock. Includes Lower Jurassic Glen Canyon Group (Kayenta and Moenave Formations, Aztec Sandstone) and Chinle and Moenkopi Formations Geology uPzc Carbonate rocks (Mississippian to Permian)— The Rainbow Gardens ACEC has been completely Limestone, dolomite, and some shale. May include Kaibab, Callville, Monte Cristo, and Redwall mapped geologically at 1:24,000 scale (Bingler, 1977; Bell Limestones, Toroweap Formation, and Bird Spring and Smith, 1980; Matti and others, 1993; Castor and others, Formation 2000; Deubendorfer, 2003). Rock units range in age from uPzs Sedimentary rocks (uppermost Devonian to Permian) — Proterozoic through late Miocene. Proterozoic schist and Siltstone, sandstone, shale, and conglomerate; some gneiss, exposed along the western base of Frenchman Moun- limestone, dolomite, chert, and gypsum. May include Queantoweap Sandstone, Hermit Formation, Coconino tain (Matti and others, 1993), is overlain by relatively thin Sandstone, Supai Group, and Pakoon Formation lower Cambrian sandstone and shale units and then by a thick lPzc Dolomite and Limestone (Cambrian to Devonian) — sequence of carbonate-dominated Cambrian, Devonian, and Dolomite, limestone, and minor amounts of Mississippian to Permian rocks. Mesozoic rocks, mainly com- sandstone,shale, and siltstone. May include Muav posed of shallow marine to nonmarine Triassic and Jurassic Limestone, Frenchman Mountain Dolomite, and redbeds, with some carbonate and gypsum beds, are capped Bonanza King ? and Nopah and Sultan Formations by eolian sandstone. Rocks of the uppermost Oligocene to lPzs Sedimentary rock (Cambrian)—Sandstone, shale, and middle Miocene Horse Spring Formation and a red sandstone limestone. May include Pioche Shale, Lyndon Limestone, and Chisholm Shale unit described by Bohannon (1984) are mainly composed of Xm Metamorphic rocks (Paleoproterozoic)—Undivided nonmarine red sandstone, with some carbonate rocks and tuff. metasedimentary, metavolcanic, and gneissic rocks, The Muddy Creek Formation, which is mostly composed of including locally abundant amphibolite and pegmatite. poorly indurated sandstone and siltstone with local gypsum, May also include Paleoproterozoic granitoid rocks limestone, and conglomerate units, filled late Miocene basins. contact, certain The Paleozoic and Mesozoic strata are conformable, but the break between the youngest Mesozoic unit (Jurassic Aztec fault, certain Sandstone) and the oldest Tertiary unit (basal part of the Horse fault, approximate Spring Formation) is marked by a low-angle unconformity. The Rainbow Gardens ACEC contains six major struc- fault, concealed tural elements: the Frenchman Mountain block, Sunrise thrust fault Mountain block, Boulder Basin, Nellis Basin, Gale Hills block, and Las Vegas Valley. The Frenchman Mountain block mine or prospect is bounded by the Frenchman Fault and Las Vegas Valley on AP-001 sample site, with sample nmber the west, the Sunrise Mountain block on the north, and the Boulder Basin on the east.
Recommended publications
  • State Route 160 (Blue Diamond Road) Corridor Study
    State Route 160 (Blue Diamond Road) Corridor Study Final Report August 31, 2006 Booz Allen Hamilton with Civilwise Inc. Table of Contents RTC SR-160 Corridor Study TABLE OF CONTENTS 1.0 EXECUTIVE SUMMARY ............................................................................... 1-1 2.0 CURRENT CONDITIONS OF STUDY AREA ................................................... 2-1 2.1 Description of SR-160....................................................................................2-1 2.2 Geographic Boundaries ..................................................................................2-1 2.3 Communities Served......................................................................................2-1 2.4 Current Zoning and Community Plans ..............................................................2-3 2.4.1 Clark County ......................................................................................2-3 2.4.2 2004 Land Use Plan for Enterprise.........................................................2-3 2.5 Current Land Use ..........................................................................................2-4 2.5.1 Public Facilities Needs Assessment ........................................................2-5 2.6 Future Growth ..............................................................................................2-6 2.6.1 Transit-Supportive Land-Use Actions .....................................................2-7 2.6.2 Recent Growth Management Activities .................................................2-13 2.6.3
    [Show full text]
  • Assembly Committee on Government Affairs-April 4
    MINUTES OF THE MEETING OF THE ASSEMBLY COMMITTEE ON GOVERNMENT AFFAIRS Seventy-Ninth Session April 4, 2017 The Committee on Government Affairs was called to order by Chairman Edgar Flores at 8:13 a.m. on Tuesday, April 4, 2017, in Room 3143 of the Legislative Building, 401 South Carson Street, Carson City, Nevada. The meeting was videoconferenced to Room 4404B of the Grant Sawyer State Office Building, 555 East Washington Avenue, Las Vegas, Nevada. Copies of the minutes, including the Agenda (Exhibit A), the Attendance Roster (Exhibit B), and other substantive exhibits, are available and on file in the Research Library of the Legislative Counsel Bureau and on the Nevada Legislature's website at www.leg.state.nv.us/App/NELIS/REL/79th2017. COMMITTEE MEMBERS PRESENT: Assemblyman Edgar Flores, Chairman Assemblywoman Dina Neal, Vice Chairwoman Assemblywoman Shannon Bilbray-Axelrod Assemblyman Chris Brooks Assemblyman Richard Carrillo Assemblyman Skip Daly Assemblyman John Ellison Assemblywoman Amber Joiner Assemblyman Al Kramer Assemblyman Jim Marchant Assemblyman Richard McArthur Assemblyman William McCurdy II Assemblywoman Daniele Monroe-Moreno Assemblywoman Melissa Woodbury COMMITTEE MEMBERS ABSENT: None GUEST LEGISLATORS PRESENT: Assemblywoman Lesley E. Cohen, Assembly District No. 29 Assemblyman Elliot T. Anderson, Assembly District No. 15 Assemblyman James Ohrenschall, Assembly District No. 12 Minutes ID: 655 *CM655* Assembly Committee on Government Affairs April 4, 2017 Page 2 STAFF MEMBERS PRESENT: Jered McDonald, Committee Policy
    [Show full text]
  • Sunrise Mountain Landfill 1999 Administrative Record
    SFUND RECORDS CTR 2095573 - FINAL - REGULATORY COMPLIANCE AUDIT REPORT Sunrise Mountain Landfill Las Vegas, Nevada ASI Project Manager C_)JamesD. ShsMer 002541 PREFACE Regulatory Compliance Audits A regulatory compliance audit of a solid waste landfill consists of an examination based on the requirements of Federal regulations 40 CFR Parts 241 and 257, proposed Federal regulations 40 CFR Part 258. and existing State regulations. Conduct of a regulatory compliance audit includes a review of landfill case file records, supporting documents, and landfill operating practices; interviews with individuals familiar with the operation of the landfill; identification of site conditions; a visual inspection of the facility; and a determination of whether or not hazardous wastes have been or are being disposed of in excess of amounts normally found in household wastes. 0025*2 TABLE OF CONTENTS Section Page PREFACE II TABLE OF CONTENTS Ill LIST OF TABLES v LIST OF FIGURES v EXECUTIVE SUMMARY vl 1.0 INTRODUCTION 1 1.1 Program Purpose, Scope, and Objectives 1 1.2 Pre-lnspection Activities 3 1.3 On-Site Audit Activities 4 1.4 Post-Inspection Activities 5 2.0 FACILITY ENVIRONMENTAL PROFILE 6 2.1 Facility Description 6 2.1.1 Facility Location 6 2.1.2 Environmental Information 7 2.1.2.1 Topography 7 2.1.2.2 Land Use 7 2.1.2.3 Climate 9 2.1.2.4 Biological Features 9 2.1.2.5 Surface Water 10 2.1.2.6 Geology 10 2.2 Facility History 16 2.2.1 History of Owners, Lessees, and Operators 16 2.2.2 History of Site Operations 17 2.2.3 Regulatory History 19 in 002543
    [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]
  • Mineral Resources of the La Madre Mountains Wilderness Study Area, Clark County, Nevada
    Mineral Resources of the La Madre Mountains Wilderness Study Area, Clark County, Nevada U.S. GEOLOGICAL SURVEY BULLETIN 1730-A Chapter A Mineral Resources of the La Madre Mountains Wilderness Study Area, Clark County, Nevada By JAMES E. CONRAD and HARLAN N. BARTON U.S. Geological Survey DAVID A. LIPTON U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1730-A MINERAL RESOURCES OF WILDERNESS STUDY AREAS: SOUTHERN NEVADA DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1986 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center, Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Conrad, James E. Mineral resources of the La Madre Mountains Wilderness Study Area, Clark County, Nevada. U.S. Geological Survey Bulletin 1730-A Bibliography: p. 9 Supt. of Docs. No.: I 19.3:1730-A 1. Mines and mineral resources Nevada La Madre Mountains Wilderness. 2. Geology Nevada La Madre Mountains Wilderness. 3. La Madre Mountains Wilderness (Nev.) I. Barton, Harlan N. II. Lipton, David A. (David Abraham), 1954- . III. Title. IV. Series. QE75.B9 No. 1730-A 557.3 s 86-600162 [TN424.N3] [553'.0979'13] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Area The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine the mineral values, if any, that may be present.
    [Show full text]
  • Rocks at the GBSSRL Reception Counter
    Rocks at the Reception Counter of the Great Basin Science Sample and Records Library All the rocks in the wooden core boxes on the front of the reception counter are from Nevada. They include some geologically and historically significant rocks: the Nevada State Rock (sandstone), one of the oldest rocks in Nevada (2.5-billion-year-old gneiss from Angel Lake), rocks from the “Great Unconformity” separating Precambrian gneiss and Cambrian sandstone (from Frenchman Mountain, where rocks like those at the base of the Grand Canyon are exposed), ore from the Comstock Lode at Virginia City (important in statehood, our nickname, the Silver State, and the motto “Battle Born”), rock from the top of Slide Mountain (which, as measured by high-precision global positioning system instruments, moved up and to the northeast in 2003 in response to probable magma injection at the north end of Lake Tahoe), and some of the youngest rocks in Nevada (caliche from Las Vegas Valley and ferricrete from Geiger Grade). These rocks have been cut to simulate diamond drill core. The Great Basin Science Sample and Records Library houses many boxes of core and cuttings from various mineral, oil, geothermal, and water exploration holes drilled in the State. Slabs of a few different background rocks provide contrast with the Nevada- shaped pieces. The countertop itself is polished Juparana Columbo "granite," which is actually, by geological definitions, a gneiss; it comes from India and looks somewhat like 1.7-billion-year-old gneiss from southern Nevada. Except where noted, the samples were collected by Jon Price, State Geologist and Director of the Nevada Bureau of Mines and Geology.
    [Show full text]
  • Environmental Assessment: Red Rock Hazardous Fuels Reduction Project
    B L M U.S. Department of the Interior Bureau of Land Management Environmental Assessment Red Rock Hazardous Fuels Reduction Project January 25, 2012 DRAFT PREPARING OFFICE U.S. Department of the Interior Bureau of Land Management Southern Nevada District Office 4701 North Torrey Pines Dr. Las Vegas, Nevada 89130 USA (702)515–5000 Environmental Assessment: Red Rock Hazardous Fuels Reduction Project January 25, 2012 Environmental Assessment ii Table of Contents 1. Introduction ................................................................................................................................ 1 1.1. Background ....................................................................................................................... 1 1.2. Brome ................................................................................................................................ 3 1.3. Identifying Information: ................................................................................................... 3 1.3.1. Title, EA number, and type of project: .................................................................. 3 1.3.2. Location of Proposed Action: ................................................................................ 4 1.3.3. Name and Location of Preparing Office: ............................................................... 4 1.3.4. Identify the subject function code, lease, serial, or case file number: ................... 5 1.3.5. Applicant Name: ...................................................................................................
    [Show full text]
  • Current Knowledge and Conservation of Cylindropuntia Multigeniculata (Cactaceae), the Blue Diamond Cholla
    Current Knowledge and Conservation of Cylindropuntia multigeniculata (Cactaceae), the Blue Diamond cholla Marc A. Baker Southwest Botanical Research 1217 Granite Lane Chino Valley, AZ 86323 (928) 636-0252 15 June 2005 Status report prepared for U. S. Fish and Wildlife Service, Nevada State Office 1340 Financial Boulevard, suite 234, Reno NV 89502. (775) 861 6300 with funds provided through Project Agreement in cooperation with Prescott College, Prescott, Arizona SUMMARY : The typical form of the Blue Diamond cholla, Cylindropuntia multigeniculata , is now known to occur from north of Las Vegas, near Gass Peak, in the Las Vegas Range, southwest into the La Madre Mountain area, south to Blue Diamond, and then southeast into the McCullough Range. The knowledge of new localities is largely owing to efforts of Gina Glenne of the U.S. Fish & Wildlife Service, and Pat Putnam and Jed Botsford of the Bureau of Land Management. Prior to these discoveries, the Blue Diamond cholla was known to occur only at its type locality in the Blue Diamond Hills, just west of Las Vegas. Current surveys indicate that populations of C. multigeniculata conservatively occupy at least 25km² with densities averaging 23 individuals per hectare, thus the conservative estimate of number of individuals is 56,500. This estimate does not include at least one population in the Sheep Range that appear to be comprised of individuals morphologically intermediate between C. multigeniculata and C. whipplei var. whipplei . Populations of C. multigeniculata with consistently spiny fruits occur from Bonelli Peak, Gold Butte area of eastern Clark County, Nevada, south into the White Hills and Black Mountains of Mojave County, Arizona.
    [Show full text]
  • An Interview With
    An Interview with Win BrownOral History produced by Robert D. McCracken Nye County Town History Project Nye County, Nevada Tonopah 2009 COPYRIGHT 2009 Nye County Town History Project Nye County Commissioners Tonopah, Nevada 89049 DeAnna Brown and her husband Darryll Brown 2007 Gwendolyn and Leon Hughes, 1945. From left: Georgie Ann Bell and unidentified woman picking cotton. Pahrump Ranch, Pahrump, Nevada, 1937. Red Schoolhouse, Pahrump, Nevada. From left: Norma Steve, Ben Spencer (his mother was Pahrump's postmistress), Don Ward, Marie Hughes (DeAnna's aunt), DeAnna Hughes (fifth grade), Okemah Spencer (Ben Spencer's sister), 1952. From left: Leon Hughes, DeAnna Hughes, Larry Hughes, Gwendolyn Hughes, 1945. Cabin at Lost Lobo Mine, west side of Charleston Mountains above Pahrump Valley, Nevada, 1990. Portal of Lost Lobo Mine, west side of Charleston Mountains, Nevada, 1990. Children of Gwendolyn and Leon Hughes, 1954. Back row, from left: Leonard, Pam, Oneta, Michael. Front row, from left: Sharon, DeAnna (holding Raymond), and Larry. Children of John and Beryl Hughes, 1942. Standing, from left: Maxine Hughes, Betty Hughes, Byron Hughes, Bea Hughes, Leon Hughes and wife Gwendolyn. Sitting, from left: Baby DeAnna Hughes, John Hughes (DeAnna's grandfather), Kenneth Hughes, Beryl Hughes (DeAnna's grandmother), and Marie Hughes. CONTENTS Preface xi Acknowledgments xiii Introduction xv CHAPTER ONE 1 DeAnna's parents and their life in California; her grandfather John's ranch in Pahrump in the 1930s; DeAnna's childhood, traveling between Pahrump and California; her father, Leon's, attempt to grow cotton in Pahrump early on; John Hughes's mine; living at the Blue Diamond Mine and commuting to high school in Las Vegas; schooling in California and in Pahrump; life in Pahrump before a good road connected it to other communities; working in the cotton fields as a youngster; Leon's farming at the north end of the Pahrump Valley.
    [Show full text]
  • 185 IBLA 375 Decided June 10, 2015
    GYPSUM RESOURCES, LLC 185 IBLA 375 Decided June 10, 2015 United States Department of the Interior Office of Hearings and Appeals Interior Board of Land Appeals 801 N. Quincy St., Suite 300 Arlington, VA 22203 GYPSUM RESOURCES, LLC IBLA 2012-113 Decided June 10, 2015 Appeal from a decision of the Field Manager, Red Rock/Sloan (Nevada) Field Office, Bureau of Land Management, accepting a relinquishment of an access road right-of-way, and closing the right-of-way file. NVN-065968. Affirmed. 1. Federal Land Policy and Management Act of 1976: Rights-of-Way–Rights-of-Way: Act of January 21, 1895– Rights-of-Way: Cancellation--Rights-of-Way: Federal Land Policy and Management Act of 1976 BLM properly accepts a relinquishment of a right-of-way, originally issued pursuant to section 1 of the Act of January 21, 1895, 43 U.S.C. § 956 (1970) (later conformed to a right-of-way under Title V of the Federal Land Policy and Management Act of 1976, 43 U.S.C. §§ 1761-1771 (2006)), and closes the right-of-way file, when the current holder of the right-of-way relinquishes its rights in the right-of-way. BLM properly deems the current holder to be the party presently holding the right-of-way, as a matter of record with BLM, not the current owner of title to private lands accessed by the right-of-way, which, unbeknownst to BLM, had passed by a series of deeds that transferred the lands, together with all “appurtenances.” APPEARANCES: James H. Walton, Esq., and James A.
    [Show full text]
  • Chapter 3 Affected Environment
    Las Vegas Disposal Boundary Chapter 3 Chapter 3 Affected Environment Final EIS December 2004 Las Vegas Disposal Boundary Chapter 3 THIS PAGE INTENTIONALLY LEFT BLANK Final EIS December 2004 Las Vegas Disposal Boundary Chapter 3 CHAPTER 3 AFFECTED ENVIRONMENT The affected environment is the baseline from BLM lands within the disposal boundary area. which to identify and evaluate environmental The purpose of the surveys was to identify the changes resulting from the proposed action and presence of sensitive environmental resources and alternatives. This chapter focuses on the human to locate potential hazardous materials sites. Bio- environment that has the potential to be affected logical field surveys covered the desert tortoise by implementing the land sale and land use ac- and sensitive plant species including the Las Ve- tions. The human environment potentially af- gas bearpoppy, Las Vegas buckwheat, and pen- fected is interpreted comprehensively to include stemon. Surveys were also completed to locate the natural and physical resources and the rela- historic sites, archaeological sites, and paleon- tionship of people with those resources [40 Code tological resources, and to identify lands with po- of Federal Regulations (CFR) §1508.14]. The tential hazardous materials present. affected environment discussed in this chapter includes air quality, earth resources, water re- 3.1 AIR QUALITY sources, biological resources, cultural and histori- cal resources, Native American concerns, visual Air resources are characterized by the existing resources, land use, recreation and wilderness re- concentrations of various pollutants and the cli- sources, range resources, hazardous materials, matic and meteorological conditions that influ- social and economic conditions, and environ- ence the quality of the air.
    [Show full text]
  • Chapter 4 Affected Environment and Impacts of MSHCP and Alternatives
    Clark County MSHCP/EIS 4. Affected Environment/Impacts of MSHCP & Alternatives Chapter 4 Affected Environment and Impacts of MSHCP and Alternatives 4.1 Setting Clark County is located in the southernmost tip of Nevada, as shown in Figure 4-1. It is bordered on the north by Lincoln County, Nevada; on the east by Mojave County, Arizona; on the southwest by San Bernardino and Inyo Counties, California; and on the west by Nye County, Nevada. It covers approximately 7,880 square miles, or about 7 percent of the state’s total area. It is Nevada’s most populated county, with an estimated 1997 population of 1,170,113, or about 67 percent of the state total (Clark County Department of Comprehensive Planning 1997). Elevations within Clark County range from 450 feet above mean sea level along the Colorado River to 11,918 feet at Charleston Peak (see Figure 4-1). Much of the county has features that are characteristic of the Great Basin, such as mountain ranges that extend in a north-south direction and erode laterally to long, narrow desert valleys. The mountain ranges are generally steep and composed primarily of bedrock. Wide alluvial fans or aprons extend from the base of the mountains and level out to basin lowlands. The basin lowlands have been continually filling since the mountains were originally formed and have a surface generally composed of fine sand, silt, and clay. The Las Vegas Valley extends in a northwest-southeast direction with the Spring Mountains to the west; the Pintwater, Desert, Sheep, and Las Vegas Mountains to the north; Frenchman Mountain to the east; and the Bird Spring and McCullough mountain ranges to the south.
    [Show full text]