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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. -
Elmer C. Aldrich
PLANNING MILESTONES FOR THE PARK UNITS AND MAJOR PROPERTIES ASSOCIATED WITH THE CALIFORNIA STATE PARKS SYSTEM July 1, 2010 Planning Division California State Parks P. O. Box 942896 Sacramento, CA 94296-0001 PLANNING MILESTONES FOR THE PARK UNITS AND MAJOR PROPERTIES ASSOCIATED WITH THE CALIFORNIA STATE PARK SYSTEM July 1, 2010 OVERVIEW This document is a compendium providing selected information on the classified units and major unclassified properties which currently are or have in the past been associated with the California State Park System. The main purposes of this compendium are to provide, in a single source: 1. a record of the major milestones and achievements in unit-level land use and management planning which have been accomplished through the years by the Department, with the major accomplishments of the last year summarized in Chapter II; 2. a variety of other information useful to understanding the past history or current status of these units and properties, and of the evolution of unit-level land use and resource management planning in the Department; and 3. The definitive number and the specific identity of those basic classified units and major unclassified properties which constitute the official State Park System as of the date of this report’s publication. As of July 1, 2010, the California State Park System consists of 278 basic classified units and major unclassified properties. These are identified on Lists 1 and 2 in Chapter III. To have data current to July 1, 2010, this total will be the Department’s official figure until the next edition of this report. -
Chemehuevi Valley Groundwater Basin Bulletin 118
Hydrologic Region Colorado River California’s Groundwater Chemehuevi Valley Groundwater Basin Bulletin 118 Chemehuevi Valley Groundwater Basin • Groundwater Basin Number: 7-43 • County: San Bernardino • Surface Area: 273,000 acres (427 square miles) Basin Boundaries and Hydrology This basin underlies Chemehuevi Valley in eastern San Bernardino County. The basin is bounded by Havasu Lake on the east and by nonwater-bearing rocks of the Sacramento Mountains on the north, of the Chemehuevi Mountains on the northeast, of the Whipple Mountains on the southeast, of the Turtle Mountains on the west and south (Bishop 1963). The valley is drained by Chemehuevi Wash to Havasu Lake. Annual average precipitation ranges from about 4 to 6 inches. Hydrogeologic Information Water Bearing Formations Groundwater in the basin is found in alluvium and the Bouse Formation. Alluvium. Holocene age younger alluvium, which is found in washes and the floodplain of the Colorado River, is composed of sand, silt and gravel (Metzger and Loeltz 1973). Older alluvium consists of unconsolidated, fine- to coarse-grained sand, pebbles, and boulders with variable amounts of silt and clay. Bouse Formation. The Pliocene age Bouse Formation is composed of a basal limestone bed overlain by interbedded clay, silt, and sand. Thickness of the formation reaches 254 feet (Metzger and Loeltz 1973). The formation is underlain by locally derived fanglomerate and overlain by alluviums of the Colorado River and its tributaries. Restrictive Structures An unnamed fault crosses a portion of the southern side of the basin (Bishop 1963), but it is not known whether or not this fault impedes groundwater flow in the basin. -
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. -
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. -
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. -
Status and Distribution of the Elf Owl in California
STATUS AND DISTRIBUTION OF THE ELF OWL IN CALIFORNIA MARY D. HALTERMAN, Department of BiologicalSciences, California State University,Chico, California95929 STEPHEN A. LAYMON, Departmentof Forestryand ResourceManagement, 145 Mulford Hall, Universityof California, Berkeley, California94720 MARY J. WHITFIELD, Department of BiologicalSciences, California State University,Chico, California95929 In California,the Elf Owl (Micrathenewhitneyi) has been found only in riparianhabitats and scatteredstands of Saguaro(Carnegiea gigantea) along the lower Colorado River and at a few desert oases (Grinnell and Miller 1944). Although the specieshas never been numerousin California, there hasapparently been a populationdecline. Surveys in 1978 and 1979 located 11 and 6 pairsof Elf Owls, respectively,at two locationsalong the lower Col- orado River (Cardiff1978, 1979). Cardiff's(1978) completerecord of the 28 Elf Owl sightingsmade in California prior to 1978 identified eight locations where the specieshas been found. We gathered10 additionalrecords made since 1979 (Table 1). All recent records were for either Soto Ranch or near Water Wheel Camp. Since 1979, habitatdestruction has continued, resulting in the loss of much of the remainingcottonwood-willow and mesquite bosques(C. Hunter and B. Andersonpers. comm.). This lossis due to the proliferationof tamarisk (Tamarix chinensis),agricultural clearing, bank stabilizationprojects, urbanization, and recentsustained flooding (Laymon and Halterman1987). This lossand itspotential effect on Elf Owlsprompted thissurvey -
Desert Renewable Energy Conservation Plan Proposed Land
DRECP Proposed LUPA and Final EIS CHAPTER III.8. CULTURAL RESOURCES III.8 CULTURAL RESOURCES This chapter presents the Affected Environment for the Land Use Plan Amendment (LUPA) Decision Area and the Desert Renewable Energy Conservation Plan (DRECP) area for cultural resources. These areas overlap, and in the following programmatic discussion are referred to broadly as the “California Desert Region.” More than 32,000 cultural resources are known in the DRECP area in every existing environmental context ⎼ from mountain crests to dry lake beds ⎼ and include both surface and subsurface deposits. Cultural resources are categorized as buildings, sites, structures, objects, and districts (including cultural landscapes and Traditional Cultural Properties) under the federal National Environmental Policy Act (NEPA) and the National Historic Preservation Act (NHPA). Historic properties are cultural resources included in, or eligible for inclusion in, the National Register of Historic Places (NRHP), maintained by the Secretary of the Interior (36 Code of Federal Regulations [CFR] 60.4). See Section III.8.1.1 for more information on federal regulations and historic properties. This chapter discusses three types of cultural resources classified by their origins: prehistoric, ethnographic, and historic. Prehistoric cultural resources are associated with the human occupation of California prior to prolonged European contact. These resources may include sites and deposits, structures, artifacts, rock art, trails, and other traces of Native American human behavior. In California, the prehistoric period began over 12,000 years ago and extended through the eighteenth century until 1769, when the first Europeans settled in California. Ethnographic resources represent the heritage of a particular ethnic or cultural group, such as Native Americans or African, European, Latino, or Asian immigrants. -
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. -
California Floras, Manuals, and Checklists: a Bibliography
Humboldt State University Digital Commons @ Humboldt State University Botanical Studies Open Educational Resources and Data 2019 California Floras, Manuals, and Checklists: A Bibliography James P. Smith Jr Humboldt State University, [email protected] Follow this and additional works at: https://digitalcommons.humboldt.edu/botany_jps Part of the Botany Commons Recommended Citation Smith, James P. Jr, "California Floras, Manuals, and Checklists: A Bibliography" (2019). Botanical Studies. 70. https://digitalcommons.humboldt.edu/botany_jps/70 This Flora of California is brought to you for free and open access by the Open Educational Resources and Data at Digital Commons @ Humboldt State University. It has been accepted for inclusion in Botanical Studies by an authorized administrator of Digital Commons @ Humboldt State University. For more information, please contact [email protected]. CALIFORNIA FLORAS, MANUALS, AND CHECKLISTS Literature on the Identification and Uses of California Vascular Plants Compiled by James P. Smith, Jr. Professor Emeritus of Botany Department of Biological Sciences Humboldt State University Arcata, California 21st Edition – 14 November 2019 T A B L E O F C O N T E N T S Introduction . 1 1: North American & U. S. Regional Floras. 2 2: California Statewide Floras . 4 3: California Regional Floras . 6 Northern California Sierra Nevada & Eastern California San Francisco Bay, & Central Coast Central Valley & Central California Southern California 4: National Parks, Forests, Monuments, Etc.. 15 5: State Parks and Other Sites . 23 6: County and Local Floras . 27 7: Selected Subjects. 56 Endemic Plants Rare and Endangered Plants Extinct Aquatic Plants & Vernal Pools Cacti Carnivorous Plants Conifers Ferns & Fern Allies Flowering Trees & Shrubs Grasses Orchids Ornamentals Weeds Medicinal Plants Poisonous Plants Useful Plants & Ethnobotanical Studies Wild Edible Plants 8: Sources . -
2020 Volume 2
Society for the Conservation of Bighorn Sheep Sheep Sheet - Volume 2 – September 2020 www.desertbighorn.org Before the project began, collection box area in sad shape After the project: a formal, robust spring box Redwood Spring Box Installed at Castle Mine Spring By Debbie Miller Marschke SCBS has been working to improve the natural spring at the Castle Mine location for many years. Mining ruins and a dilapidated cabin remain as evidence that this spring has a history of folks teasing out the precious water from this location. There is always an overgrowth of vegetation at the spring which is proof positive that the spring is active, even if the flow rate is minimal. Bighorn Sheep biologists have GPS data from collared sheep in the mountain range that prove the Bighorn Sheep wander along the backbones of the ridges; occasionally they visit this spring but they mainly depend on the big game guzzlers to the north of this location. Nevertheless, each water location in a mountain range is crucial in the network of water sources available. SCBS crews have dug out and cleared the guzzler intake Johnson screen several times on previous occasions which has been very frustrating because a spring box had never been installed. The water seeps from the entrance of an old mine adit in the side of a hill. The hill face and adit entrance are unstable, and thus dirt caves in and has buried the intake system time and time again. On the weekend of May 15-17, 2020, a modest SCBS strike force sought to make one final but meaningful attempt to boost water output from Castle Mine spring. -
Flora of the Whipple Mountains
$5.00 (Free to Members) VOL. 35, NO. 1 • WINTER 2007 FREMONTIA JOURNAL OF THE CALIFORNIA NATIVE PLANT SOCIETY FLORA OF THE WHIPPLE MOUNTAINS— THE “NOSE” OF CALIFORNIA INVASIVEINVASIVE PLANTSPLANTS IMPACTIMPACT TRADITIONALTRADITIONAL BASKETRY PLANTS NATIVE GRASSES IN THE GARDEN REMEMBERING GRADY WEBSTER BUCKEYEVOLUME 35:1, AS WINTERBONSAI 2007 AN ORCHID IN SAN DIEGO CALIFORNIA NATIVE PLANT SOCIETY FREMONTIA CNPS, 2707 K Street, Suite 1; Sacramento, CA 95816-5113 Phone: (916) 447-CNPS (2677) Fax: (916) 447-2727 VOL. 35, NO. 1, WINTER 2007 Web site: www.cnps.org Email: [email protected] Copyright © 2007 MEMBERSHIP California Native Plant Society Membership form located on inside back cover; dues include subscriptions to Fremontia and the Bulletin Bart O’Brien, Editor Bob Hass, Copy Editor Mariposa Lily . $1,500 Family or Group . $75 Benefactor . $600 International . $75 Beth Hansen-Winter, Designer Patron . $300 Individual or Library . $45 Brad Jenkins, Jake Sigg, and Carol Plant Lover . $100 Student/Retired/Limited Income . $25 Witham, Proofreaders STAFF CHAPTER COUNCIL CALIFORNIA NATIVE Sacramento Office: Alta Peak (Tulare) . Joan Stewart PLANT SOCIETY Executive Director . Amanda Jorgenson Bristlecone (Inyo-Mono) . Sherryl Taylor Development Director/Finance Channel Islands . Lynne Kada Dedicated to the Preservation of Manager . Cari Porter the California Native Flora Dorothy King Young (Mendocino/ Membership Assistant . Christina Sonoma Coast) . Lori Hubbart The California Native Plant Society Neifer East Bay . Elaine P. Jackson (CNPS) is a statewide nonprofit organi- El Dorado . Amy Hoffman zation dedicated to increasing the un- At Large: Kern County . Lucy Clark derstanding and appreciation of Califor- Fremontia Editor . Bart O’Brien Los Angeles/Santa Monica Mtns .