Mineral Resources of the Providence Mountains Wilderness Study Area, San Bernardino County, California

Total Page:16

File Type:pdf, Size:1020Kb

Mineral Resources of the Providence Mountains Wilderness Study Area, San Bernardino County, California Mineral Resources of the Providence Mountains Wilderness Study Area, San Bernardino County, California U.S. GEOLOGICAL SURVEY BULLETIN 1712-D Chapter D Mineral Resources of the Providence Mountains Wilderness Study Area, San Bernardino County, California By RICHARD J. GOLDFARB, DAVID M. MILLER, ROBERT W. SIMPSON, and DONALD B. HOOVER U.S. Geological Survey PHILLIP R. MOYLE, JERRY E. OLSON, and RICHARD S. GAPS U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1712 MINERAL RESOURCES OF WILDERNESS STUDY AREAS: CENTRAL CALIFORNIA DESERT CONSERVATION AREA DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1988 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 Providence Mountains Wilderness Study Area, San Bernardino County, California. U.S. Geological Survey Bulletin 1712-D Bibliography Supt. of Docs. No.: I 19.3:1712-D 1. Mines and mineral resources California Providence Mountains Wilderness. 2. Providence Mountains wilderness (Calif.) I. Goldfarb, R.J. II. Series. QE75.B9 No. 1712-D 557.3s 87-600296 [553'.09794'95] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas 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 part of the Providence Mountains Wilderness Study Area (CDCA-263), California Desert Conservation Area, San Bernardino County, California. CONTENTS Summary Dl Abstract 1 Character and setting 2 Identified resources 3 Mineral resource potential 3 Introduction 3 Acknowledgments 5 Appraisal of identified resources 5 Mining and exploration history 5 Mines, prospects, claims, and mineralized outcrops 8 Gold, silver, copper, lead, and zinc 8 Placer gold 10 Iron 10 Molybdenum 10 Industrial minerals 12 Recreational minerals 12 Appraisal of resources 12 Assessment of mineral resource potential 14 Geology 14 Geologic setting 14 Description of rock units 14 Structure 15 Alteration 16 Geochemistry 16 Methods 16 Interpretation of geochemical data 17 Geophysics 20 Aeromagnetic data 20 Gravity data 21 Electrical geophysical data 21 Mineral and energy resources 22 Silver, gold, copper, lead, zinc, and tungsten 22 Iron 23 Nonmetallic resources 24 Recommendations for further work 25 References cited 25 Appendixes Definition of levels of mineral resource potential and certainty of assessment 31 Resource/reserve classification 32 Geologic time chart 33 PLATE [in pocket] 1. Mineral resource potential and geologic map of the Providence Mountains Wilderness Study Area FIGURES 1. Index map showing location of the Providence Mountains Wilderness Study Area, San Bernardino County, California D2 2. Map showing generalized mineral resource potential for the Providence Mountains Wilderness Study Area, San Bernardino County, California 4 3. Map showing location of mines, prospects, mineralized outcrops, and land status in the Providence Mountains Wilderness Study Area, San Bernardino County, California 7 TABLES 1. Recorded production from nonferrous metallic lode deposits within and adjacent to the Providence Mountains Wilderness Study Area D6 2. Identified mineral resources and occurrences in the Providence Mountains Wilderness Study Area 11 3. Anomalous concentrations of selected elements in nonmagnetic heavy-mineral- concentrate samples as determined by semiquantitative emission spectrometry 17 4. Maximum reported concentrations for mineralized vein samples or replacement bodies 18 5. Summary description of mines, prospects, and mineralized outcrops in and adjacent to the Providence Mountains Wilderness Study Area, San Bernardino County, California 34 VI MINERAL RESOURCES OF WILDERNESS STUDY AREAS: CENTRAL CALIFORNIA DESERT CONSERVATION AREA Mineral Resources of the Providence Mountains Wilderness Study Area, San Bernardino County, California By Richard J. Goldfarb, David M. Miller, Robert W. Simpson, and Donald B. Hoover U.S. Geological Survey Phillip R. Moyle, Jerry E. Olson, and Richard S. Gaps U.S. Bureau of Mines SUMMARY long tons of indicated or inferred subeconomic iron resources ranging from 50 to 60 percent iron, and the Abstract Vulcan mine-Burro prospect contains a subeconomic iron resource of about 3 million long tons. The study area also contains large deposits of subeconomic The Providence Mountains Wilderness Study Area limestone, dolomite, quartzite, sand and gravel, and (CDCA-263) lies within the eastern Mojave Desert stone resources. about 35 mi southeast of Baker, Calif., and the part on Much of the central part and the southeast which mineral surveys were requested encompasses corner of the study area have high or moderate about 63,300 acres in the northern Providence mineral resource potential for gold, silver, copper, Mountains and the Colton Hills and is contiguous with lead, zinc, and tungsten in quartz vein and carbonate- the Providence Mountains State Recreation Area. replacement deposits. Smaller regions in the south- Geological, geochemical; geophysical, and mineral central and southeastern parts of the study area show surveys of the study area were conducted by the U.S. high or moderate potential for iron resources Geological Survey and U.S. Bureau of Mines between associated with skarn deposits. An unknown potential 1982 and 1985 to appraise the identified mineral is present in the north-central part of the study area resources (known) and to assess the mineral resource for molybdenum resources and for gold and silver potential (undiscovered) of the area. resources in low-grade bulk-tonnage deposits. An The study area includes parts of the Trojan unknown potential for oil and gas resources occurs mining district. More than 700 workings and along the western edge of the study area. The entire mineralized outcrops were examined during this study, study area has a low potential for undiscovered including 467 workings within the study area; in this resources of gold in alluvium, uranium, geothermal report they are grouped into 162 properties. Twelve energy, limestone, dolomite, and quartzite for mines in and near the study area produced at least industrial use and voluminous deposits of sand, gravel, 6,425 tons of ore containing about 300 oz of gold, and dimension stone. Much of the rock underlying the 92,000 oz of silver, 25,000 Ib of copper, 72,000 Ib of rugged terrain adjoining the Providence Mountains lead, and 2,300 Ib of zinc. The Vulcan mine-Burro State Recreation Area on the west has no or low prospect on the south boundary of the study area potential for mineral resources, as does the mesa area produced 2.6 million long tons of iron. Eight in the northern Colton Hills. In this report, any properties within and on the boundary of the study reference to the Providence Mountains Wilderness area contain a total of about 310,000 tons of indicated Study Area refers only to that part of the and (or) inferred subeconomic gold and (or) silver wilderness study area for which mineral surveys were resources. Two properties contain a total of 340,000 requested. D1 Character and Setting Providence Mountains State Recreation Area. The study area includes rugged, sparsely forested The Providence Mountains Wilderness Study Area mountains exceeding 7,000 ft in elevation, 500- to comprises most of the Providence Mountains north of 1,000-ft-high mesas north of the Colton Hills, and Foshay Pass, east of Kelso and the Union Pacific lowland hills and plains at about 3,400 ft elevation in Railroad, and south of roads traversing Macedonia and the Colton Hills and at 2,200 ft elevation near Kelso. Wild Horse Canyons, and includes much of the Colton The study area is underlain by diverse rock types Hills west of Black Canyon Road <fig. 1). Bordering that represent a long and complex geologic history. the southeastern part of the study area is the Outcrops of Proterozoic (see geologic time chart in Kelso Mountains Tough Nut 'pring 35°00r Cornfield Spring IL (Blair Ranch Providence S APPROXIMATE BOUNDARY Devils Playground PROVIDENCE MOUNTAINS C o 11 o iT WILDERNESS STUDY AREA Hills (CDCA-263) Clipper Valley Granite Mountains Figure 1. Location of the Providence Mountains Wilderness Study Area, San Bernardino County, California. D2 appendix for explanation of rock ages) gneiss and system is associated with felsic intrusions, breccia, granite are widespread in the northern part of the and intense quartz-sericite alteration in upper Globe study area. A thick sequence of Paleozoic sandstone, Wash. Intensely altered and silicified rocks along the limestone, and dolomite is found at the higher ridge northeast of Summit Spring delineates a tract elevations in the Providence Mountains. Jurassic and having unknown potential for low-grade bulk-tonnage Cretaceous granitoid rocks of varying composition are gold and silver. The entire study area has a low widespread in the Colton Hills, in the northern and resource potential for gold in placer deposits, uranium, western parts of the study area, and in the Foshay Pass and geothermal energy, and unknown potential for oil area. Tertiary volcanic rocks underlie prominent
Recommended publications
  • Providence Mountains State Recreation Area 38200 Essex Road Or P.O
    Our Mission Providence The mission of California State Parks is to provide for the health, inspiration and In the middle of the education of the people of California by helping Mountains to preserve the state’s extraordinary biological Mojave Desert, Jack and diversity, protecting its most valued natural and State Recreation Area cultural resources, and creating opportunities Ida Mitchell shared with for high-quality outdoor recreation. thousands of fortunate visitors the cool beauty of the caverns’ magnificent “draperies” and “coral California State Parks supports equal access. pipes” formations. Prior to arrival, visitors with disabilities who need assistance should contact the park at (760) 928-2586. If you need this publication in an alternate format, contact [email protected]. CALIFORNIA STATE PARKS P.O. Box 942896 Sacramento, CA 94296-0001 For information call: (800) 777-0369 (916) 653-6995, outside the U.S. 711, TTY relay service www.parks.ca.gov Providence Mountains State Recreation Area 38200 Essex Road or P.O. Box 1 Essex, CA 92332 • (760) 928-2586 © 2010 California State Parks (Rev. 2017) V isitors to Providence Mountains State that left abundant shell-covered organisms Recreation Area are greeted by the sight on the sea floor. of jagged slopes of gray limestone, topped The shells and plant materials that settled by volcanic peaks of red rhyolite. Located on the sea bottom eventually became on the eastern slope of the Providence limestone. As the restless land heaved Mountains Range, the park lies within the upward, these formations were pushed boundaries of the 1.6-million acre Mojave above the level of the former ocean bed.
    [Show full text]
  • Understanding the Source of Water for Selected Springs Within Mojave Trails National Monument, California
    ENVIRONMENTAL FORENSICS, 2018 VOL. 19, NO. 2, 99–111 https://doi.org/10.1080/15275922.2018.1448909 Understanding the source of water for selected springs within Mojave Trails National Monument, California Andy Zdon, PG, CHg, CEGa, M. Lee Davisson, PGb and Adam H. Love, Ph.D.c aTechnical Director – Water Resources, PARTNER ENGINEERING AND SCIENCE, INC., Santa Ana, CA, Sacramento, CA; bML Davisson & Associates, Inc., Livermore, CA; cVice President/Principal Scientist, Roux Associates, Inc., Oakland, CA ABSTRACT KEYWORDS While water sources that sustain many of the springs in the Mojave Desert have been poorly Water resources; clipper understood, the desert ecosystem can be highly dependent on such resources. This evaluation mountains; bonanza spring; updates the water resource forensics of Bonanza Spring, the largest spring in the southeastern groundwater; forensics; Mojave Desert. The source of spring flow at Bonanza Spring was evaluated through an integration isotopes of published geologic maps, measured groundwater levels, water quality chemistry, and isotope data compiled from both published sources and new samples collected for water chemistry and isotopic composition. The results indicate that Bonanza Spring has a regional water source, in hydraulic communication with basin fill aquifer systems. Neighboring Lower Bonanza Spring appears to primarily be a downstream manifestation of surfacing water originally discharged from the Bonanza Spring source. Whereas other springs in the area, Hummingbird, Chuckwalla, and Teresa Springs, each appear to be locally sourced as “perched” springs. These conclusions have important implications for managing activities that have the potential to impact the desert ecosystem. Introduction above Bonanza Spring. Identification of future impacts General information and data regarding springs in the from water resource utilization becomes problematic if Mojave Desert are sparse, and many of these springs are initial baseline conditions are unknown or poorly under- not well understood.
    [Show full text]
  • Breeding Avifaunas of the New York Mountains and Kingston Range: Islands of Conifers in the Mojave Desert of California
    BREEDING AVIFAUNAS OF THE NEW YORK MOUNTAINS AND KINGSTON RANGE: ISLANDS OF CONIFERS IN THE MOJAVE DESERT OF CALIFORNIA STEVEN W. CARDIFF and J.V. REMSEN, Jr., Museum of Zoologyand Depart- ment of Zoology,Louisiana State University,Baton Rouge, Louisiana70893-3216 Quantificationof speciesturnover rates on islandsin the context of the equilibriumtheory of island biogeography(MacArthur and Wilson 1967) dependson accurateinventories of the biotataken at appropriateintervals in time. Inaccuratehistorical data concerningspecies composition is a sourceof error that must be avoided when calculatingturnover rates (Lynch and Johnson1974). Johnson's(1974) analysisof historicalchanges in species compositionand abundanceexemplifies the importanceof sound avifaunal inventoriesfor later comparison. In this paper, we present data to provide future researchers with a baseline from which to calculate turnover rates for the breeding avifaunas of two conifer "islands" in the Mojave Desert in California. Islandbiogeography of isolatedmountain ranges forming conifer "islands" in the Great Basin has been studiedby Brown (1971, 1978) for mammals and Johnson(1975) for birds.An analysisof breedingbird turnoverrates for a coniferisland in the Mojave Desert(Clark Mountain, California)is in prog- ress (N.K. Johnson pers. comm.). Detailed and accurate surveysof the breedingavifaunas of the Sheep and Springranges of southwesternNevada (Johnson 1965) and the Providence Mountains, San Bernardino Co., California (Johnson et al. 1948) provide data from other Mojave Desert rangesfor comparisonwith data we presentbelow. STUDY AREAS New York Mountains. The New York Mountains extend from about 14 km west of Cima east to the Nevada border in extreme eastern San Bernardino Co., California. The highestpoint, New York Peak (7532 ft--2296 m), is 39.5 km southeastof Clark Mountain (7929 ft = 2417 m) and 118 km south of CharlestonPeak (11,919 ft=3633 m) in the Spring Mountainsof Nevada.
    [Show full text]
  • Mojave National Preserve Management Plan for Developed
    Mojave National Preserve—Management Plan for Developed Water Resources CHAPTER 3: AFFECTED ENVIRONMENT Introduction This chapter describes the unique factors that influence water resource management in the Preserve and the resources that could be affected by the implementation of any of the alternatives described in Chapter 2: Alternatives. The resource descriptions provided in this chapter serve as a baseline to compare the potential effects of the management actions proposed in the alternatives. The following resource topics are described in this chapter: • Environmental Setting • Cultural Resources • Water Resources • Wilderness Character • Wildlife Environmental setting and water resources are important for context and are foundational for water resource management, but are not resources that are analyzed for effects. Resource issues that were considered and dismissed from further analysis are listed in Chapter 1: Purpose of and Need for Action and are not discussed further in this EA. A description of the effects of the proposed alternatives on wildlife, cultural resources, and wilderness character is presented in Chapter 4: Environmental Consequences. Environmental Setting The Preserve includes an ecologically diverse yet fragile desert ecosystem consisting of vegetative attributes that are unique to the Mojave Desert, as well as components of the Great Basin and Sonoran Deserts. Topography The topography of the Preserve is characteristic of the mountain and basin physiographic pattern, with tall mountain ranges separated by corresponding valleys filled with alluvial sediments. Primary mountain ranges in the Preserve, from west to east, include the Granite, Kelso, Providence, Clark, New York, and Piute Mountains. Major alluvial valleys include Soda Lake (dry lake bed), Shadow Valley, Ivanpah Valley, Lanfair Valley, and Fenner Valley.
    [Show full text]
  • Mojave National Preserve U.S
    National Park Service Mojave National Preserve U.S. Department of the Interior Science Newsletter Sweeney Granite Mountains Desert Research Center: an Interview with Director Dr. Jim André James M. André1 and Debra L. Hughson2 A significant factor in the amount of high quality research conducted in Mojave National Preserve is the Sweeney Granite Mountains Desert Research Center, part of the University of California Natural Reserve System. In this issue we interview its Director, Dr. Jim André. Dr. André is a research botanist who completed the Preserve’s Vascular Plant Inventory for the National Park Service Inventory and Monitoring Program. The Sweeney Granite Mountains Desert Research Center (GMDRC) is one of 37 protected research sites operated by the University of California Natural Reserve System (UC NRS). This system of outdoor classrooms and laboratories The Sweeney Granite Mountains Desert Research Center is located in Granite Cove at the base of the Granite Mountains. makes relatively undisturbed examples of the state’s diverse ecosystems available with support facilities for long-term Debra – Some of the people who were to researchers, teachers, and students research projects and multi-week field instrumental in the formation of the UC In this Issue: courses. Established in 1978, the Natural Reserve System, such as Ken Sweeney Granite Mountains Desert Norris and Wilbur Mayhew, were very • Page 1. Sweeney Granite Mountains active in this area of the Mojave Desert. Desert Research Center: an Interview with Research Center encompasses 3,496 Director Dr. Jim André hectares (8,639 acres) of the pristine and In fact one of the student camps is called rugged Granite Mountains in the East Norris Camp.
    [Show full text]
  • UC Berkeley Paleobios
    UC Berkeley PaleoBios Title Bonnima sp. (Trilobita; Corynexochida) from the Chambless Limestone (Lower Cambrian) of the Marble Mountains, California: First Dorypygidae in a cratonic region of the southern Cordillera Permalink https://escholarship.org/uc/item/8fq03184 Journal PaleoBios, 30(2) ISSN 0031-0298 Author Foster, John R. Publication Date 2011-10-19 DOI 10.5070/P9302021790 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PaleoBios 30(2):45–49, October 19, 2011 © 2011 University of California Museum of Paleontology Bonnima sp. (Trilobita; Corynexochida) from the Chambless Limestone (Lower Cambrian) of the Marble Mountains, California: First Dorypygidae in a cratonic region of the southern Cordillera JOHN R. FOSTER Museum of Western Colorado, P.O. Box 20,000, Grand Junction, CO 81502; [email protected] A trilobite pygidium, likely referable to the genus Bonnima, is the first evidence of a member of the Corynexochida reported from the Lower Cambrian (Dyeran Stage) Chambless Limestone of the southern Marble Mountains in the Mojave Desert of California. This specimen represents the first occurrence of the family Dorypygidae in the cratonic facies of the Lower Cambrian in the California-western Nevada region, as all of the few previous reports of the family (mostly Bonnia) have been from much thicker, more distal open-shelf deposits far to the northwest in the White- Inyo—Esmeralda County region of California and Nevada. Although still relatively rare, the occurrence of Dorypygidae across a range of environments biofacies realms in this area is typical of their distribution in other regions. INTRODUCTION from 5 cm to 1 m thick, and these beds generally decrease in The Chambless Limestone is a Lower Cambrian unit ex- thickness upward in the formation.
    [Show full text]
  • Granite Mountains Resource Survey
    GRANITE MOUNTAINS RESOURCE SURVEY Natural and Cultural Values of the Granite Mountains, Eastern Mojave Desert, California Edited by Bruce A. Stein and Sheridan F. Warrick Publication no. 1 Environmental Field Program University of California, Santa Cruz 1979 This material is based upon work supported by the National Science Founda­ tion under student Originated Studies Grant No. SPI 78-03739. Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the authors and do n0t necessarily reflect the views of the National Science Foundation. ~ Copyright 1979 by the Environmental Field Program, University of California, Santa Cruz. ii Left to right, standing:*Bruce Bannerman, Bruce Stein, Shoo Shoo Salasky, Larry Minden, Ken Hart, Lorie Cahn, Ann Harvey, Dan Warrick. Left to right, seated: Joanne Kerbavaz, Kent Johnson, Helen Gibbons. AUTHORS AND TASKS Lorie Cahn .. Geology Helen Gibbons Geology Ken Hart. Vegetation and Flora Ann Harvey. Cultural Resources and Land Use Kent Johnson. Birds Joanne Kerbavaz Cultural Resources and Land Use Larry Minden .. Reptiles and Amphibians Sheryl Salasky. Mammals Bruce Stein Project Director, Vegetation and Flora Dan Warrick Project Coordinator, Vegetation and Flora *Bruce Bannerman conducted a concurrent photographic project on the aesthetic resources of the Granite Mountains. There are men charged with the duty of examining the construction of the plants, animals, and soils which are the instruments of the great orchestra. These men are called professors. Each selects one instrument and spends his life taking it apart and describing its strings and sound- ing boards . A professor may pluck the strings of his own instrument, but never that of another, and if he listens for music he must never admit it to his fellows or to his students.
    [Show full text]
  • Birds of Eagle Mountain, Joshua Tree National Monument, California
    BIRDS OF EAGLE MOUNTAIN, JOSHUA TREE NATIONAL MONUMENT, CALIFORNIA A. TOWNSEND PETERSON, Committeeon EvolutionaryBiology, The Universityof Chicago, Chicago, Illinois60637 The Little San Bernardino Mountains of Riverside and San Bernardino Countiesin southernCalifornia support a peninsulaof oak-pine woodland runningsoutheast from the higherSan BernardinoMountains (Figure 1). In spiteof the continuityof the woodland connectingthe two ranges,the birds of the Little San BernardinoMountains are remarkablydifferentiated from populationsto the west. Three subspeciesrequiring woodland are endemic to the range: a Mountain Quail, Oreortyxpictus russel!i, a Plain Titmouse, Parus inornatusmohavensis, and a Bushtit,Psaltriparus minimus sociabilis (Miller 1946), and another, a ScrubJay, Aphelocomacoerulescens cana, is endemic to the nearby Eagle Mountains (Miller 1946, Pitelka 1951). Miller (1946), Pitelka (1951), and Miller and Stebbins (1964) discussed three alternativehypotheses for the originof thesedifferentiated populations. (1) The peninsularestricts gene flow from populationsto the west. (2) The differentiatedpopulations represent intergrades or hybridsbetween popula- tions in the San Bernardino Mountains to the west and the Providence Mountainsto the northeast.(3) A thirdhypothesis is one of faunalrelaxation. Becauseas recently as 8000 years ago the Mojave Desert contained pin- yon-juniper woodland (Wells and Berger 1967, Van Devender 1977), dif- ferentiatedpopulations in the Little San Bernardino Mountains and other mountainranges farther east may representremnants of what was once a continuous distribution (Grinnell and Swarth 1913, Miller and Stebbins 1964). Hence, they may showtraits that are eitherancestral or intermediate owing to historicalgenetic interchange. Information on populationsof these speciesin the bits of woodland be- tween the Little San Bernardino Mountains and the Providence Mountains is criticalto assessingthe latter two hypotheses.The Eagle Mountains,the BullionMountains, the Old Woman Mountains,and othersprovide elevated landscapes(Figure 1).
    [Show full text]
  • Things to Do Within 100 Miles of Barstow Secured in Writing from the Author
    Permission to re-print must be Things To Do Within 100 Miles of Barstow secured in writing from the author. Courtesy of Route 66 Mother Road Museum, Barstow CA Approx. Distance from Websites & Additional Info Name Description Mother Websites may not be updated regularly. Call ahead for current Road information. Museum Afton Canyon Natural The Mojave River flows above ground in the Afton Check with the Bureau of Land Management office in 1 Area Canyon area. Sometimes called the “Grand Canyon of Barstow for up-to-date info. the Mojave,” it is considered a good spot for bird and http://www.blm.gov/ca/index.html wildlife viewing. Kit Carson, Jedediah Smith, & John Bureau of Land Charles Fremont are some of the early western Road conditions can change from deep sand in explorers who passed through the area. The historic summer to mud and washed-out sections after rain. Management Mojave Road is nearby. 35 miles Avoid canyons during thunderstorms due to possible 2601 Barstow Road violent flash floods. Plan accordingly, as no food, Barstow, CA 92311 The Route 66 Mother Road Museum in Barstow has water or gasoline may be available for miles. Always (760) -252-6000 numerous books for sale on areas to explore, such as notify someone of your plans. Cell phones do not canyons, rock formations, intaglios, etc. always work in remote areas. Amboy Crater is a cinder cone from an ancient Amboy, CA volcano. The Crater is on BLM land, and has a graded Avoid intense midday Summer sun at Amboy Crater. 2 Historic Route 66 dirt road leading to the base of the crater.
    [Show full text]
  • Background to Historic and Prehistoric Resources of the East Mojave
    BLM LIBRARY Background to Historic and Prehistoric Resources of the East Mojave Desert Region by Chester King and Dennis G. Casebier Archaeological Research Unit University of California, Riverside with sections by Matthew C. Hall and Carol Rector Prepared for the UNITED STATES DEPARTMENT OF INTERIOR BUREAU OF LAND MANAGEMENT California Desert Planning Program 1695 Spruce Street Riverside, California 92507 Contract No. YA-512-CT6-14 May 31, 1976 BLM LIBRARY INCOMING wc RKFLOW CHECKLIST (04/15/2002) TYPE XC RECEIVE DATE I XC/BLM OC WHO HAS SEEN CC AC/AV BC ! DW RECLASS CT NM AUTHORITY BK KG ^ PROBLEM JP website' AA CATEGORY (S) MA (order) MA(recom) USFS/USGS ser:.es RA Priority BLM BOOK REV. BLM EOT Priority NonBIiM PREVIEW OTEER WEBSITE SPECIAL COI CTION \ 1 [ & PRESERVATIC)N • DONATION By 4- *W>m\ e C. 3- Background to Historic and Prehistoric Resources of the East Mojave Desert Region by Chester King and Dennis G. Casebier Archaeological Research Unit University of California, Riverside with sections by Matthew C. Hall and Carol Rector Prepared for the UNITED STATES DEPARTMENT OF INTERIOR BUREAU OF LAND MANAGEMENT California Desert Planning Program 1695 Spruce Street Riverside, California 92507 Contract No. YA-512-CT6-14 May 31, 1976 D 80225 TABLE OF CONTENTS Page TABLE OF CONTENTS i LIST OF ILLUSTRATIONS vi ACKNOWLEDGEMENTS vii INTRODUCTION PART 1: BACKGROUND TO PREHISTORIC RESOURCES OF THE EAST MOJAVE PLANNING UNIT Chester King ETHNOHISTORIC AND ETHNOGRAPHIC BACKGROUND OF THE EAST MOJAVE PLANNING UNIT 3 The Southern Paiute Nation 3 Southern Paiute Tribes 5 Chemehuevi Chiefs 6 Ceremonial Gatherings 7 Bands 8 The Providence Mountain Band 9 Land Use and Settlement 10 Food Preparation and Storage .
    [Show full text]
  • Species Richness and Endemism in the Native Flora of California
    RESEARCH ARTICLE AMERICAN JOURNAL OF BOTANY Species richness and endemism in the native f ora of California 1 Bruce G. Baldwin 2 , Andrew H. Thornhill , William A. Freyman , David D. Ackerly , Matthew M. Kling , Naia Morueta-Holme , and Brent D. Mishler PREMISE OF THE STUDY: California’s vascular f ora is the most diverse and threatened in temperate North America. Previous studies of spatial patterns of Californian plant diversity have been limited by traditional metrics, non-uniform geographic units, and distributional data derived from f oristic descrip- tions for only a subset of species. METHODS: We revisited patterns of sampling intensity, species richness, and relative endemism in California based on equal-area spatial units, the full vascular f ora, and specimen-based distributional data. We estimated richness, weighted endemism (inverse range-weighting of species), and corrected weighted endemism (weighted endemism corrected for richness), and performed a randomization test for signif cantly high endemism. KEY RESULTS: Possible biases in herbarium data do not obscure patterns of high richness and endemism at the spatial resolution studied. High species richness was sometimes associated with signif cantly high endemism (e.g., Klamath Ranges) but often not. In Stebbins and Major’s (1965) main endemism hotspot, Southwestern California, species richness is high across much of the Peninsular and Transverse ranges but signif cantly high endemism is mostly localized to the Santa Rosa and San Bernardino mountains. In contrast, species richness is low in the Channel Islands, where endemism is signif cantly high, as also found for much of the Death Valley region. CONCLUSIONS: Measures of taxonomic richness, even with greater weighting of range-restricted taxa, are insuf cient for identifying areas of signif cantly high endemism that warrant conservation attention.
    [Show full text]
  • Section 5 5.5 Water Resources 5.5.1 Affected Environment
    SECTION 5 5.5 WATER RESOURCES 5.5.1 AFFECTED ENVIRONMENT The project spreading basins and wellfield will be located entirely on Cadiz Inc. land, which includes more than 27,000 acres in the Cadiz and Fenner valleys as shown in Figure 5.5-1. Approximately 1,600 acres of this land have been developed for vineyards, citrus orchards, and various types of row crops. Seven groundwater production wells were installed between 1984 and 1994 to provide irrigation for the agricultural operation using water-conserving drip and micro-spray techniques. Current groundwater use for irrigation averages between approximately 5,000 and 6,000 acre-feet/year. A more comprehensive description of the agricultural operation is provided in Section 5.1. In 1993, San Bernardino County certified a Final Environmental Impact Report (FEIR) and granted various land use approvals for expansion of agricultural operations on the property up to 9,600 acres (URS Consultants, Inc. 1993b). As a component of this approval, the County identified specific groundwater monitoring activities to be undertaken by Cadiz. To comply with these monitoring requirements, the Cadiz Valley Agricultural Development Ground Water Monitoring Plan (GWMP) was developed in cooperation with San Bernardino County to monitor all potential environmental impacts that could result from the agricultural operations. Physiography and Topography The regional watersheds tributary to the Cadiz Project area are defined by a series of mountain ranges and topographic divides that surround Fenner Valley, Orange Blossom Wash, and the Bristol and Cadiz dry lake depressions as shown on Figure 5.5-2. The Fenner Valley watershed, which contributes the principal source of groundwater recharge to the project area, includes all of Fenner Valley and a portion of Lanfair Valley.
    [Show full text]