Mineral Resources of the Nopah Range Wilderness Study Area, Inyo County, California

Total Page:16

File Type:pdf, Size:1020Kb

Mineral Resources of the Nopah Range Wilderness Study Area, Inyo County, California Mineral Resources of the Nopah Range Wilderness Study Area, Inyo County, California U.S. GEOLOGICAL SURVEY BULLETIN 1709-C Chapter C Mineral Resources of the Nopah Range Wilderness Study Area, Inyo County, California By AUGUSTUS K. ARMSTRONG, COLE L. SMITH, and GEORGE L. KENNEDY U.S. Geological Survey CHARLES SABINE and RONALD T. MAYERLE U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1709 MINERAL RESOURCES OF WILDERNESS STUDY AREAS: NORTHEASTERN CALIFORNIA DESERT CONSERVATION AREA, CALIFORNIA DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1987 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 Mineral resources of the Nopah Range Wilderness Study Area, Inyo County, California. (U.S. Geological Survey Bulletin 1709-C) Bibliography Supt. of Docs. No.: I 19.3:1709-C 1. Mines and mineral resources California Nopah Range Wilderness. 2. Geology California Nopah Range Wilderness. 3. Nopah Range Wilderness (Calif.) I. Armstrong, Augustus K. II. Series. QE75.B9 No. 1709-C 557.3 s 86-600386 [TN24.C2] |553'.09794'87] 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. Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a mineral survey of the Nopah Range Wilderness Study Area (CDCA-150), California Desert Conservation Area, Inyo County, California. CONTENTS Summary Cl Abstract 1 Character and setting 1 Identified resources 3 Mineral resource potential 3 Introduction 3 Area description 3 Previous and present studies 3 Acknowledgments 5 Appraisal of identified resources 5 Mining and mineral exploration history 5 Mines and prospects 5 Nancy Ann mine 5 Barnett prospect 6 Black Raven prospect 6 Golden Eagle prospect 6 Zeolite minerals 6 Borate minerals 7 Assessment of mineral resource potential 7 Geology 7 Geochemistry 8 Analytical methods 8 Results of survey 8 Mineral and energy resource potential 8 Silver, lead, and zinc 9 Gold, molybdenum, and lead 9 Copper 9 Limestone, quartzite, and sand and gravel 9 Zeolites and borates 9 Oil and gas 10 Geothermal energy 10 Recommendations for further study 10 References cited 10 Appendixes Definition of levels of mineral resource potential and certainty of assessment 15 Resource/reserve classification 16 Geologic time chart 17 PLATE [ In pocket] 1. Mineral resource potential map of the Nopah Range Wilderness Study Area, Inyo County, California FIGURES 1. Index map showing location of the Nopah Range Wilderness Study Area, Inyo County, California C2 2. Map showing mineral resource potential of the Nopah Range Wilderness Study Area, Inyo County, California 4 TABLE 1. Mines, prospects, and mineral workings in and adjacent to the Nopah Range Wilderness Study Area CIS MINERAL RESOURCES OF WILDERNESS STUDY AREAS: NORTHEASTERN CALIFORNIA DESERT CONSERVATION AREA, CALIFORNIA Mineral Resources of the Nopah Range Wilderness Study Area, Inyo County, California #y Augustus K. Armstrong, Cole L. Smith and George L. Kennedy U.S. Geological Survey Charles Sabine and Ronald T. Mayerle U.S. Bureau of Mines SUMMARY area. However, the resource potential of these Abstract commodities is low. The mineral resource potential for oil and gas and geothermal energy is low in the At the request of the Bureau of Land study area. Management, 109,061 acres of the Nopah Range Wilderness Study Area (CDCA-150) were originally Character and Setting designated for study by the U.S. Geological Survey and the U.S. Bureau of Mines. Subsequently, in 1983, the The Nopah Range Wilderness Study Area is study area was decreased to the current 97,151 acres. located in southeastern Inyo County, California, This report presents the results of a mineral survey of approximately 15 mi east of the south end of Death part of the Nopah Wilderness Study Area. In this Valley National Monument and 2 mi southwest of the report, the area studied is referred to as "the California-Nevada border (fig. 1). The study area lies wilderness study area," or simply "the study area." within the Basin and Range geomorphic province and There has been little mining activity in the encompasses most of the Nopah Range, the region. Workings within and near the wilderness study southernmost part of the Resting Spring Range, and area consist of one mine, three prospects, and one the intervening part of Chicago Valley. The Nopah zeolite occurrence, none of which has identified Range, underlain predominantly by carbonate rocks of resources. Four localities within the revised study Cambrian through Pennsylvanian (see geologic time area have mineral resource potential: (1) a 3-mi-long chart in appendix) age, 570 to 290 million years before area on the northwest side of the Nopah Range with the present (Ma), is characterized by deep canyons, moderate resource potential for undiscovered silver, ridges, and rugged topography; precipices of 1,000 ft lead, and zinc resources; (2 and 3) two areas on the or more are common. By contrast, the southern part southeastern side of the study area have low resource of the Resting Spring Range, which is underlain potential for undiscovered silver and lead resources, predominantly by Late Proterozoic fine-grained and (4) an area on the east-central side of the range terrigenous sedimentary rocks, is more subdued has low resource potential for gold, molybdenum, and topographically. Minor amounts of volcanic rocks are lead resources. In the southern part of the Resting present in both ranges. The flanks of the ranges are Spring Range west of the study area, one area has low marked by coalescing alluvial fans that merge with potential for copper and 2 areas have low potential for lacustrine deposits in the surrounding valleys. zeolite (clinoptilolite). The resource potential for Elevations in the area range from 1,800 ft at the south copper is unknown within the study area. The resource end of Chicago Valley to 6,394 ft on Nopah Peak. potential for borates and (or) zeolites in the Chicago Mining activity in the study area has been very Valley is unknown. There are numerous limestone, limited, and only the Nancy Ann mine (fig. 2) has a quartzite, and sand and gravel deposits in the study history of production. C1 115M5' 36°30 DEATH VALLEY NATIONAL MONUMENT Death Valley Junction APPROXIMATE BOUNDARY OF NOPAH RANGE WILDERNESS STUDY AREA(CDCA-150) DEATH VALLEY NATIONAL MONUMENT 35°30' Figure 1. Index map showing location of the Nopah Range Wilderness Study Area, Inyo County, California. C2 Identified Resources INTRODUCTION None of the mines or prospects in the study area have identified mineral resources. At the Nancy Ann Area Description mine (fig. 2), approximately 490 tons of mineralized rock are left in the old workings and an additional 290 At the request of the Bureau of Land tons are still on the dump. This material contains an Management, 109,061 acres of the Nopah Range estimated 650 oz of silver, 20,000 Ib of lead, and Wilderness Study Area (CDCA-150) in the southeast 63,000 Ib of zinc; at current (1986) market values, this corner of Inyo County, California (fig. 1) were is insufficient to warrant mining and does not originally designated for study. Subsequently, in 1983, constitute an economic resource. the study area was decreased to the current 97,151 Miocene tuff in the Resting Spring Range acres. The areas excluded were the north tip of the contains less than 100,000 tons of zeolitized material Nopah Range, the southern part of the Resting Spring that averages 63 percent (±20 percent) zeolite Range, and the adjacent part of Chicago Valley. This clinoptilolite (fig. 2). The deposit is currently too report covers the original area established in 1980. small to be an economic resource. The Nopah Range is rugged and cut by deep Carbonate rocks underlie most of the Nopah canyons; sharp ridges and precipices of more than Range; a major deposit (greater than 20 million tons) 1,000 ft are common. The topography of the Resting of limestone on the northwest side of the Nopah Range Spring Range is more subdued. Elevations in the area was identified by Bowen (1973, pi. 1). This deposit is range from about 1,800 ft in Chicago Valley to 6,394 ft far from large markets and is not likely to be on Nopah Peak. The climate is arid and vegetation is developed in the foreseeable future. Existing quarries sparse. in the Spring Mountains, east of the study area, will Primary access to the study area is provided by most likely continue to meet limestone requirements California State Highway 178 to the north and west for local markets. and by a paved county road that leads eastward from Sand and gravel are plentiful in the study area, Tecopa along the south margin of the study area. Jeep but alternate sources are readily available closer to trails in Chicago Valley and along the east margin of local markets. the study area from California Valley northward along Pahrump Valley to Highway 178 provide secondary access. Mineral Resource Potential Mineral resource potential in the study area was evaluated on the basis of investigations conducted by the U.S. Geological Survey from 1981 to 1983 and by Previous and Present Studies the U.S. Bureau of Mines in 1983. Mineral resource potential was determined for lead, silver, copper, zinc, A detailed stratigraphy of the Nopah and Resting gold, molybdenum, and the zeolite clinoptilolite (fig.
Recommended publications
  • 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
    [Show full text]
  • Birds of the California Desert
    BIRDS OF THE CALIFORNIA DESERT A. Sidney England and William F. Laudenslayer, Jr. i INTRODUCTION i \ 1 The term, "California desert", as used herein, refers to a politically defined region, most of i which is included in the California Desert Conservation Area (CDCA) designated by the Federal Land ; and Management Act of 1976 (FLPMA). Of the 25 million acres in the CDCA, about one-half are i public lands, most of which are managed by the Bureau of Land Management (BLM) according to the "980 P California Desert Conservation Area Plan mandated by FLPMA. The California desert encompasses those portions of the Great Basin Desert (east of the White and lnyo Mountains and A south of the California-Nevada border), the Mojave Desert, and the Colorado Desert which occur " within California; it does not include areas of riparian, aquatic, urban, and agricultural habitats . adjacent to the Colorado River. (Also see chapters on Geology by Norris and Bioclimatology by E3irdsI4 are the most conspicuous vertebrates found in the California deserts. Records exist for at least 425 species (Garrett and Dunn 1981) from 18 orders and 55 families. These counts far exceed those for mammals, reptiles, amphibians and fish, and they are similar to totals for the entire state -- 542 species from 20 orders and 65 families (Laudenslayer and Grenfell 1983). These figures may seem surprisingly similar considering the harsh, arid climates often believed characteristic of I desert environments. However, habiiats found in the California desert range from open water and h marshes at the Salton Sea to pinyon-juniper woodland and limber pinelbristlecone pine forests on a few mountain ranges.
    [Show full text]
  • Pahrump-Tecopa.Pdf
    Old Spanish National Historic Trail Pahrump, Nevada and Tecopa, California Public Scoping Meetings April 5-6, 2006 Amargosa Valley Desert National Wildlife Refuge 9 2 Y W Nellis Air Force Base H E T A Indian Springs T S U Moapa River Indian Reservation S HW Y 95 Nellis Air Force Base Desert National Wildlife Refuge 3 7 3 Y 56 Dry Lake STA Death Valley W TE 1 HWY H Y 16 W 9 S E T H A T TE T A A E T S ST H S T U W A S Y T H 4 Ash Meadows National Wildlife Refuge E W 0 Y H 9 W 3 Y 1 6 Funeral Mountains Wilderness STATE HWY 190 157 WY E H TAT STATE HWY 190 S 6 1 Argus Range Wilderness Y 04 W 6 Toiyabe National Forest Y H HW E E T AT A ST T U S S H W Y 9 5 Pahrump B 72 U N. Las Vegas 3 S 167 Y 1 STATE HWY 147 STATE HWY HW 0 E 6 T Y TA S W Surprise Canyon Wilderness H E Las Vegas Resting Spring Range Wilderness T STATE HWY 159 A T Death Valley National Park S S Winchester T A T S E TA T H E W H STATE HWY 593 W 3 Paradise Y E. Las Vegas S 5 Y T 1 1 1 5 A 9 4 7 T Y 6 E Y W 8 H HW 4 S W Y 0 STATE HWY 152 U 6 H 1 8 60 N Y 7 E 1 T W e A Y H T v Blue Diamond W S Argus Range Wilderness C E H T a A Henderson E 46 a d T HWY 1 T TE S STA A l a U T i f S US HWY 93 S Nopah Range Wilderness o H Y 466 W US HW r Arden Y n I 515 93 ia Shoshone Boulder City Mount Wilson Wilderness Sloan Manly Peak Wilderness Ibex Wilderness South Nopah Range Wilderness Pahrump Valley Wilderness I 15 Tecopa 5 9 S T Y AT E Goodsprings W S U L H T I A S N TE E S HW H R U Y W a D 165 a Y ST 9 AT 3 n E H d WY 16 a 1 Jean o z v Trona i e r N North Mesquite Mountains Wilderness A
    [Show full text]
  • A Transect Across the Death Valley Extended Terrane, California Michael S
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. B1, 2010, 10.1029/2001JB000239, 2002 Assessing vertical axis rotations in large-magnitude extensional settings: A transect across the Death Valley extended terrane, California Michael S. Petronis and John W. Geissman Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico, USA Daniel K. Holm Department of Geology, Kent State University, Kent, Ohio, USA Brian Wernicke and Edwin Schauble Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA Received 11 September 2000; revised 7 May 2001; accepted 14 July 2001; published 18 January 2002. [1] Models for Neogene crustal deformation in the central Death Valley extended terrane, southeastern California, differ markedly in their estimates of upper crustal extension versus shear translations. Documentation of vertical axis rotations of range-scale crustal blocks (or parts thereof) is critical when attempting to reconstruct this highly extended region. To better define the magnitude, aerial extent, and timing of vertical axis rotation that could mark shear translation of the crust in this area, paleomagnetic data were obtained from Tertiary igneous and remagnetized Paleozoic carbonate rocks along a roughly east-west traverse parallel to about 36°N latitude. Sites were established in 7 to 5 Ma volcanic sequences (Greenwater Canyon and Brown’s Peak) and the 10 Ma Chocolate Sundae Mountain granite in the Greenwater Range, 8.5 to 7.5 Ma and 5 to 4 Ma basalts on the east flank of the Black Mountains, the 10.6 Ma Little Chief stock and upper Miocene(?) basalts in the eastern Panamint Mountains, and Paleozoic Pogonip Group carbonate strata in the north central Panamint Mountains.
    [Show full text]
  • The California Desert CONSERVATION AREA PLAN 1980 As Amended
    the California Desert CONSERVATION AREA PLAN 1980 as amended U.S. DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGEMENT U.S. Department of the Interior Bureau of Land Management Desert District Riverside, California the California Desert CONSERVATION AREA PLAN 1980 as Amended IN REPLY REFER TO United States Department of the Interior BUREAU OF LAND MANAGEMENT STATE OFFICE Federal Office Building 2800 Cottage Way Sacramento, California 95825 Dear Reader: Thank you.You and many other interested citizens like you have made this California Desert Conservation Area Plan. It was conceived of your interests and concerns, born into law through your elected representatives, molded by your direct personal involvement, matured and refined through public conflict, interaction, and compromise, and completed as a result of your review, comment and advice. It is a good plan. You have reason to be proud. Perhaps, as individuals, we may say, “This is not exactly the plan I would like,” but together we can say, “This is a plan we can agree on, it is fair, and it is possible.” This is the most important part of all, because this Plan is only a beginning. A plan is a piece of paper-what counts is what happens on the ground. The California Desert Plan encompasses a tremendous area and many different resources and uses. The decisions in the Plan are major and important, but they are only general guides to site—specific actions. The job ahead of us now involves three tasks: —Site-specific plans, such as grazing allotment management plans or vehicle route designation; —On-the-ground actions, such as granting mineral leases, developing water sources for wildlife, building fences for livestock pastures or for protecting petroglyphs; and —Keeping people informed of and involved in putting the Plan to work on the ground, and in changing the Plan to meet future needs.
    [Show full text]
  • Late Quaternary Stratigraphy and Luminescence Geochronology of the Northeastern Mojave Desert
    ARTICLE IN PRESS Quaternary International 166 (2007) 61–78 Late Quaternary stratigraphy and luminescence geochronology of the northeastern Mojave Desert Shannon A. Mahana,Ã, David M. Millerb, Christopher M. Mengesc, James C. Younta aUnited States Geological Survey, Box 25046 MS 974, Denver, CO 80225, USA bUnited States Geological Survey, 345 Middlefield Road, MS 973, Menlo Park, CA 94025, USA cUnited States Geological Survey, 520 N. Park Ave., Tucson, AZ 85719-5035, USA Available online 8 January 2007 Abstract The chronology of the Holocene and late Pleistocene deposits of the northeastern Mojave Desert have been largely obtained using radiocarbon ages. Our study refines and extends this framework using optically stimulated luminescence (OSL) to date deposits from Valjean Valley, Silurian Lake Playa, Red Pass, and California Valley. Of particular interest are eolian fine silts incorporated in ground- water discharge (GWD) deposits bracketed at 185–140 and 20–50 ka. Alluvial fan deposits proved amenable for OSL by dating both eolian sand lenses and reworked eolian sand in a matrix of gravel that occurs within the fan stratigraphy. Lacustrine sand in spits and bars also yielded acceptable OSL ages. These OSL ages fill gaps in the geochronology of desert deposits, which can provide data relevant to understanding the responses of several depositional systems to regional changes in climate. This study identifies the most promising deposits for future luminescence dating and suggests that for several regions of the Mojave Desert, sediments from previously undated landforms can be more accurately placed within correct geologic map units. Published by Elsevier Ltd. 1. Introduction Previous chronologic studies in the northeastern Mojave Desert area include magneto-stratigraphic studies and Extracting paleoclimatic and paleoenvironmental infor- tephrochronology of the upper Pliocene to middle Quatern- mation from terrestrial deposits is an important area of ary Tecopa beds (Hillhouse, 1987; Sarna-Wojcicki et al., Quaternary geologic research.
    [Show full text]
  • An Inventory of Trilobites from National Park Service Areas
    Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 179 AN INVENTORY OF TRILOBITES FROM NATIONAL PARK SERVICE AREAS MEGAN R. NORR¹, VINCENT L. SANTUCCI1 and JUSTIN S. TWEET2 1National Park Service. 1201 Eye Street NW, Washington, D.C. 20005; -email: [email protected]; 2Tweet Paleo-Consulting. 9149 79th St. S. Cottage Grove. MN 55016; Abstract—Trilobites represent an extinct group of Paleozoic marine invertebrate fossils that have great scientific interest and public appeal. Trilobites exhibit wide taxonomic diversity and are contained within nine orders of the Class Trilobita. A wealth of scientific literature exists regarding trilobites, their morphology, biostratigraphy, indicators of paleoenvironments, behavior, and other research themes. An inventory of National Park Service areas reveals that fossilized remains of trilobites are documented from within at least 33 NPS units, including Death Valley National Park, Grand Canyon National Park, Yellowstone National Park, and Yukon-Charley Rivers National Preserve. More than 120 trilobite hototype specimens are known from National Park Service areas. INTRODUCTION Of the 262 National Park Service areas identified with paleontological resources, 33 of those units have documented trilobite fossils (Fig. 1). More than 120 holotype specimens of trilobites have been found within National Park Service (NPS) units. Once thriving during the Paleozoic Era (between ~520 and 250 million years ago) and becoming extinct at the end of the Permian Period, trilobites were prone to fossilization due to their hard exoskeletons and the sedimentary marine environments they inhabited. While parks such as Death Valley National Park and Yukon-Charley Rivers National Preserve have reported a great abundance of fossilized trilobites, many other national parks also contain a diverse trilobite fauna.
    [Show full text]
  • Regional Stratigraphy of Oligocene and Lower Miocene Strata in the Yucca Mountain Region
    * *0Ad REGIONAL STRATIGRAPHY OF OLIGOCENE AND LOWER MIOCENE STRATA IN THE YUCCA MOUNTAIN REGION Prepared for U.S. Nuclear Regulatory Commission Contract NRC-02-97-009 Prepared by Danielle A. Murray John A. Stamatakos Kenneth D. Ridgway Center for Nuclear Waste Regulatory Analyses San Antonio, Texas July 2002 CONTENTS Section Page FIGURES ............... ................ TABLES ................ ................ .vii ACKNOWLEDGMENTS .... ................ ..... ix EXECUTIVE SUMMARY .... ................ ..... xi 1 INTRODUCTION ...... ................ .... 1-1 1.1 Purpose........ ................ .... 1-1 1.2 Scope ......... ................ .... 1-2 2 GEOLOGIC SETTING .. 2-1 OLIGOCENE AND LOWER MIOCENE STRATIGRAPHY ..... 3-1 ...... 3 . 3.1 Outcrop Stratigraphy ............................ 3-1 ...... 3.1.1 Funeral Mountains ....................... ...... 3.1.2 Nevada Test Site ........................ 3-7 ...... 3.1.3 Oligocene and Lower Miocene Lithostratigraphy . ..... 3.2 Subsurface Stratigraphy ......................... 3-12 ..... 3.2.1 Nye County Well NC-EWDP-1 DX ........... 3-13 ..... 3.2.2 Nye County Well NC-EWDP-2DB ........... 3-15 ..... 3.2.3 Nye County Well NC-EWDP-3D ............ ..... 3.3 Correlation of Well Stratigraphy to Outcrop Exposures . ..... 3.3.1 Nye County Well NC-EWDP-2DB ........... ..... 3.3.2 Nye County Well NC-EWDP-1 DX ........... ..... 3.3.3 Nye County Well NC-EWDP-3D ............ ..... 4 CROSS SECTIONS ......................................... ........... 4.1 Regional Cross Section ................................
    [Show full text]
  • Biological Goals and Objectives
    Appendix C Biological Goals and Objectives Draft DRECP and EIR/EIS APPENDIX C. BIOLOGICAL GOALS AND OBJECTIVES C BIOLOGICAL GOALS AND OBJECTIVES C.1 Process for Developing the Biological Goals and Objectives This section outlines the process for drafting the Biological Goals and Objectives (BGOs) and describes how they inform the conservation strategy for the Desert Renewable Energy Conservation Plan (DRECP or Plan). The conceptual model shown in Exhibit C-1 illustrates the structure of the BGOs used during the planning process. This conceptual model articulates how Plan-wide BGOs and other information (e.g., stressors) contribute to the development of Conservation and Management Actions (CMAs) associated with Covered Activities, which are monitored for effectiveness and adapted as necessary to meet the DRECP Step-Down Biological Objectives. Terms used in Exhibit C-1 are defined in Section C.1.1. Exhibit C-1 Conceptual Model for BGOs Development Appendix C C-1 August 2014 Draft DRECP and EIR/EIS APPENDIX C. BIOLOGICAL GOALS AND OBJECTIVES The BGOs follow the three-tiered approach based on the concepts of scale: landscape, natural community, and species. The following broad biological goals established in the DRECP Planning Agreement guided the development of the BGOs: Provide for the long-term conservation and management of Covered Species within the Plan Area. Preserve, restore, and enhance natural communities and ecosystems that support Covered Species within the Plan Area. The following provides the approach to developing the BGOs. Section C.2 provides the landscape, natural community, and Covered Species BGOs. Specific mapping information used to develop the BGOs is provided in Section C.3.
    [Show full text]
  • Structural Geology of the Montgomery Mountains and the Northern Half of the Nopah and Resting Spring Ranges, Nevada and California
    Structural geology of the Montgomery Mountains and the northern half of the Nopah and Resting Spring Ranges, Nevada and California B. C. BURCHFIEL Department of Earth and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139 G. S. HAMILL IV Research and Development Company, Box 36506, Houston, Texas 77036 D. E. WILHELMS U.S. Geological Survey. 345 Middlefield Road. Menlo Park. California 94025 ABSTRACT Ranges, for the most part in California. The area lies between the Amargosa and Pahrump Valleys and southwest of the Spring More than 7,500 m of upper Precambrian and Paleozoic sedi- Mountains (Fig. 1). The generalized geologic map of the area mentary rocks in the area of the Montgomery Mountains and the (Fig. 2) is produced from a more detailed map published in the northern half of the Nopah and Resting Spring Ranges represent a Geological Society of America Map and Chart Series (Burchfiel typical Cordilleran miogeosynclinal sequence. During Mesozoic and others, 1982). The detailed map adjoins the western edge of a time, after a period of earlier Mesozoic folding and high-angle map of the Spring Mountains (at the same scale) by Burchfiel and faulting, these rocks were cut by thrust faults that divided the rock others (1974). sequence into four structural units in the Resting Spring Range and R. B. Rowe was the first geologist to make observations in the the Montgomery Mountains. From the top down, the units are: map area, and his rather limited study is reported in the regional (1) the Montgomery thrust plate, (2) the Baxter thrust plate, (3) the compilation of Spurr (1903).
    [Show full text]
  • Pahrump Valley Winery 9
    PAHRUMP VALLEY WINERY/NEVADA WINE CELLARS REVISED VERSION (4) 9 – 1- 16 COVER Pahrump Valley Winery Offering Award-winning winery business an hour from Las Vegas! COVER PAGE If you’re surprised to learn: that just 50 minutes from Las Vegas is a winery with more than 430 national awards; that there is an opportunity to open a “tasting room” location on or near the famed Las Vegas Strip, and that you have potential access to more than 43 million new customers - hold onto your corkscrews, this offer will have you singing Viva Las Vegas! Gladstein Group (logo) For more information or to schedule a showing contact: Sam Gladstein: 702-992-7657; [email protected] Price available on request. EXECUTIVE SUMMARY Located a 50-minute scenic drive from the famed Las Vegas Strip in Pahrump, Nevada, the Pahrump Valley Winery is owned and operated, since 2003, by Bill and Gretchen Loken. The owners have invested more than $1.7 million on renovation, expansion and fixed assets since 2005. Pahrump Valley Winery generates the vast majority of its revenue through the sale of bottled wine directly to consumers via its tasting room, and through food and beverage sales via its Symphony’s Restaurant. The Pahrump Valley Winery wine portfolio includes three brands produced from grapes grown on-property along with grapes purchased from Nevada and California growers. The wines have received more than 430 national awards. Pahrump Valley Winery and its Symphony’s Restaurant have a loyal following among Las Vegas and Southern Nevada residents in addition to national and international visitors who frequent the Las Vegas Strip.
    [Show full text]
  • Inventory of Amphibians and Reptiles at Death Valley National Park
    Inventory of Amphibians and Reptiles at Death Valley National Park Final Report Permit # DEVA-2003-SCI-0010 (amphibians) and DEVA-2002-SCI-0010 (reptiles) Accession # DEVA- 2493 (amphibians) and DEVA-2453 (reptiles) Trevor B. Persons and Erika M. Nowak Common Chuckwalla in Greenwater Canyon, Death Valley National Park (TBP photo). USGS Southwest Biological Science Center Colorado Plateau Research Station Box 5614, Northern Arizona University Flagstaff, Arizona 86011 May 2006 Death Valley Amphibians and Reptiles_____________________________________________________ ABSTRACT As part of the National Park Service Inventory and Monitoring Program in the Mojave Network, we conducted an inventory of amphibians and reptiles at Death Valley National Park in 2002- 2004. Objectives for this inventory were to: 1) Inventory and document the occurrence of reptile and amphibian species occurring at DEVA, primarily within priority sampling areas, with the goal of documenting at least 90% of the species present; 2) document (through collection or museum specimen and literature review) one voucher specimen for each species identified; 3) provide a GIS-referenced list of sensitive species that are federally or state listed, rare, or worthy of special consideration that occur within priority sampling locations; 4) describe park-wide distribution of federally- or state-listed, rare, or special concern species; 5) enter all species data into the National Park Service NPSpecies database; and 6) provide all deliverables as outlined in the Mojave Network Biological Inventory Study Plan. Methods included daytime and nighttime visual encounter surveys, road driving, and pitfall trapping. Survey effort was concentrated in predetermined priority sampling areas, as well as in areas with a high potential for detecting undocumented species.
    [Show full text]