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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. -
Newberry/Dead Mountains Scenic Backcountry Drive the 10-Mile One-Way Drive Is on Bureau of Land Management Public Lands
Newberry/Dead Mountains Scenic Backcountry Drive The 10-mile one-way drive is on Bureau of Land Management public lands. However, it is better to take this as a loop trail (see directions) so you don’t have to backtrack and can see other attractions. Although the road is gravel, it is in good condition and can be navigated by 2-wheel drive sedan vehicles, although high clearance is preferable. This particular scenic drive offers a wide range of vistas. Looking north are the Newberry Mountains with the prominent and sacred Spirit Mountain looming above the horizon. Looking south are the Dead Moun- tains which are also sacred to the native Indian tribes in the area. To the west are the granitic crystal hills with interesting rock formations. To the east is the Colorado River Valley and the high peaks of the Hualapai Range in Arizona as backdrop. The green fields along the Colorado River in this area are part of the Fort Mojave Indian Reservation. The Fort Mojave Indian Reservation covers nearly 42,000 acres in the tri-state area of Arizona, California, and Nevada. The Mojave Indians are Pipa Aha Macav — “The People By The River.” Mojave culture traces the earthly origins of its people to Spirit Mountain. Newberry Mountains Newberry Mountains Prior to the arrival of white settler to the region, the Mojave Indians were prosperous farmers with well- established villages and trade networks that stretched as far away as the Pacific Ocean. In the 16th Century, the time the Spanish arrived in the territory, the Mojave’s were the largest concentration of people in the Southwest. -
Copyright by Emily Bradshaw Marino 2017
Copyright by Emily Bradshaw Marino 2017 The Thesis Committee for Emily Bradshaw Marino Certifies that this is the approved version of the following thesis: Isolating Lithologic Controls on Landscape Morphology in the Guadalupe Mountains, New Mexico and Texas APPROVED BY SUPERVISING COMMITTEE: Supervisor: Joel Johnson Paola Passalacqua David Mohrig Isolating Lithologic Controls on Landscape Morphology in the Guadalupe Mountains, New Mexico and Texas by Emily Bradshaw Marino, B.S. Thesis Presented to the Faculty of the Graduate School of The University of Texas at Austin in Partial Fulfillment of the Requirements for the Degree of Master of Science in Geological Sciences The University of Texas at Austin May 2017 Dedication To my loving parents, Thomas and Lucy Bradshaw, who have always supported me and encouraged me to follow my dreams. Acknowledgements First, I would like to express my sincere gratitude and appreciation to my advisor, Joel Johnson, for his guidance, support, and patience throughout my time at the Jackson School. I would also like to thank my committee members, David Mohrig and Paola Passalacqua for their assistance with writing this thesis. I am grateful for the opportunities I have been given during my time at the University of Texas and I value the efforts of all the faculty and staff I have had the pleasure of working with. I am beholden to the Jackson School of Geosciences for providing support for my studies and fostering an environment of world class research and scientific study. Though my time in the field was short, I am very appreciative of the funding I received to help with my field studies and would like to thank the Jackson School and the Surface and Hydrologic Processes committee for the seed grant award. -
Miocene Low-Angle Normal Faulting and Dike Emplacement, Homer Mountain and Surrounding Areas, Southeastern California and Southernmost Nevada
Miocene low-angle normal faulting and dike emplacement, Homer Mountain and surrounding areas, southeastern California and southernmost Nevada JON E. SPENCER* U.S. Geological Survey, 345 Middlefleld Road, Menlo Park, California 94025 ABSTRACT tions, differed radically from the state of that collectively accommodated as much as 50% stress in the upper plate, as inferred from to 100% extension of upper-plate rocks (Ander- Homer Mountain and surrounding regions fault geometry. Low-angle faulting and east- son, 1971). In many areas, normal faults within are within, or adjacent to, the western part of northeast-west-southwest distension of up- upper-plate rocks merge with, or are truncated a broad region of low-angle normal faults ex- per-plate rocks reflect regional reduction of by, a basal, subhorizontal fault often referred to posed within the lower Colorado River compression in the east-northeast-west- as a "detachment fault" (for example, see Davis trough. During middle Miocene time, upper- southwest direction and associated large- and others, 1980). The term "detachment fault" plate rocks in the Homer, Sacramento, Dead, scale east-northeast-west-southwest crustal is used here to indicate a low-angle normal fault and Newberry Mountains moved eastward or extension. In contrast, concave-upward flex- that formed at a low angle (for example, Wer- northeastward, relative to the lower plate, ure of the lower plate, in response to tectonic nicke and others, 1984; Reynolds and Spsncer, above single or multiple low-angle normal denudation and resultant isostatic uplift, is in- 1985). The interpretation that detachment faults faults. Deposition of coarse clastic sedimen- ferred to have produced local subhorizontal are rooted faults that accommodate crustal ex- tary rocks occurred during extensional fault- compression at shallow crustal levels in the tension (Wernicke, 1981; Howard and John, ing and was accompanied by, and closely lower plate that overwhelmed the regional 1983; Davis and others, 1983; Allmendinger followed by, eruption of basaltic volcanics. -
Welcome to the 27Th Annual Wildflower Hotline, Brought to You by the Theodore Payne Foundation, a Non-Profit Plant Nursery, Seed
Welcome back to the 28th Annual Wildflower Hotline, brought to you by the Theodore Payne Foundation, a non-profit plant nursery, seed source, book store and education center, dedicated to the preservation of wildflowers and California native plants. The glory of spring has really kicked into high gear as many deserts, canyons, parks, and natural areas are ablaze of color – so get out there and enjoy the beauty of California wildflowers. This week we begin at the Santa Rosa and San Jacinto Mountains National Monument in Palm Desert, where the Randall Henderson and Art Smith Trails are ablaze with beavertail cactus (Opuntia basilaris), Arizona lupine (Lupinus arizonicus), little gold poppy (Eschscholzia minutiflora), chuparosa (Justicia californica), brittlebush (Encelia farinosa), desert lavender (Hyptis emoryi), wild heliotrope (Phacelia distans), and apricot mallow (Sphaeralcea ambigua). If you are heading to Palm Springs for the weekend, take a trip along Palm Canyon Dr. where the roadside is radiant with sand verbena (Abronia villosa), Fremont pincushion (Chaenactis fremontii), desert dandelion (Malacothrix glabrata), forget-me-not (Cryptantha sp.), Spanish needle (Palafoxia arida), Arizona Lupine (Lupinus arizonicus), and creosote bush (Larrea tridentata). While in the area check out Tahquitz Canyon, in the Agua Caliente Indian Reservation, off West Mesquite Ave., which is still decorated with desert dandelion (Malacothrix glabrata), pymy golden poppy (Eschscholzia minutiflora), white fiesta flower (Pholistoma membranaceum), California sun cup (Camissonia californica), brown-eyed primrose (Camissonia claviformis), and more. NOTE: This is a 2-mile loop trail that requires some scrambling over rocks. Just north of I-10, off Varner Road, Edom Hill is a carpet of color with Arizona lupine (Lupinus arizonicus), sand verbena (Abronia villosa), Fremont pincushion (Chaenactis fremontii), and croton (Croton californicus), along with a sprinkling of desert sunflower (Geraea canescens) and dyebush (Psorothamnus emoryi). -
Appendix D Building Descriptions and Climate Zones
Appendix D Building Descriptions and Climate Zones APPENDIX D: Building Descriptions The purpose of the Building Descriptions is to assist the user in selecting an appropriate type of building when using the Air Conditioning estimating tools. The selected building type should be the one that most closely matches the actual project. These summaries provide the user with the inputs for the typical buildings. Minor variations from these inputs will occur based on differences in building vintage and climate zone. The Building Descriptions are referenced from the 2004-2005 Database for Energy Efficiency Resources (DEER) Update Study. It should be noted that the user is required to provide certain inputs for the user’s specific building (e.g. actual conditioned area, city, operating hours, economy cycle, new AC system and new AC system efficiency). The remaining inputs are approximations of the building and are deemed acceptable to the user. If none of the typical building models are determined to be a fair approximation then the user has the option to use the Custom Building approach. The Custom Building option instructs the user how to initiate the Engage Software. The Engage Software is a stand-alone, DOE2 based modeling program. July 16, 2013 D-1 Version 5.0 Prototype Source Activity Area Type Area % Area Simulation Model Notes 1. Assembly DEER Auditorium 33,235 97.8 Thermal Zoning: One zone per activity area. Office 765 2.2 Total 34,000 Model Configuration: Matches 1994 DEER prototype HVAC Systems: The prototype uses Rooftop DX systems, which are changed to Rooftop HP systems for the heat pump efficiency measures. -
Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs: Finding Aid
http://oac.cdlib.org/findaid/ark:/13030/tf2p30028s No online items Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs: Finding Aid Finding aid prepared by Jennifer Watts. The Huntington Library, Art Collections, and Botanical Gardens Photo Archives 1151 Oxford Road San Marino, California 91108 Phone: (626) 405-2191 Email: [email protected] URL: http://www.huntington.org © August 1999 The Huntington Library. All rights reserved. Historical Society of Southern photCL 400 volume 2 & volume 3 1 California Collection -- Charles Puck Collection of Negatives a... Overview of the Collection Title: Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs Dates (inclusive): 1864-1963 Bulk dates: 1920s-1950s Collection Number: photCL 400 volume 2 & volume 3 Creator: Puck, Charles, 1882-1968 Extent: 11,400 photographs in 42 boxes (30.29 linear feet) Repository: The Huntington Library, Art Collections, and Botanical Gardens. Photo Archives 1151 Oxford Road San Marino, California 91108 Phone: (626) 405-2191 Email: [email protected] URL: http://www.huntington.org Abstract: The Puck Collection consists of more than 11,000 photographs and negatives both taken and collected by Los Angeles resident and local history enthusiast Charles Puck (1882-1968), which he donated to the Historical Society of Southern California over more than twenty years in the mid-20th century. The photographs date from 1864 to 1963 (bulk 1920s-1950s) and depict buildings, monuments, civic happenings, modes of transportation, flora and fauna, and anything else that captured his particular interests. Puck compiled several scrapbooks on topics such as adobes and buildings of Los Angeles, illustrating them with his photographs and annotating them with historical anecdotes and personal recollections. -
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. -
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 -
Geographic Names
GEOGRAPHIC NAMES CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES ? REVISED TO JANUARY, 1911 WASHINGTON GOVERNMENT PRINTING OFFICE 1911 PREPARED FOR USE IN THE GOVERNMENT PRINTING OFFICE BY THE UNITED STATES GEOGRAPHIC BOARD WASHINGTON, D. C, JANUARY, 1911 ) CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES. The following list of geographic names includes all decisions on spelling rendered by the United States Geographic Board to and including December 7, 1910. Adopted forms are shown by bold-face type, rejected forms by italic, and revisions of previous decisions by an asterisk (*). Aalplaus ; see Alplaus. Acoma; township, McLeod County, Minn. Abagadasset; point, Kennebec River, Saga- (Not Aconia.) dahoc County, Me. (Not Abagadusset. AQores ; see Azores. Abatan; river, southwest part of Bohol, Acquasco; see Aquaseo. discharging into Maribojoc Bay. (Not Acquia; see Aquia. Abalan nor Abalon.) Acworth; railroad station and town, Cobb Aberjona; river, IVIiddlesex County, Mass. County, Ga. (Not Ackworth.) (Not Abbajona.) Adam; island, Chesapeake Bay, Dorchester Abino; point, in Canada, near east end of County, Md. (Not Adam's nor Adams.) Lake Erie. (Not Abineau nor Albino.) Adams; creek, Chatham County, Ga. (Not Aboite; railroad station, Allen County, Adams's.) Ind. (Not Aboit.) Adams; township. Warren County, Ind. AJjoo-shehr ; see Bushire. (Not J. Q. Adams.) Abookeer; AhouJcir; see Abukir. Adam's Creek; see Cunningham. Ahou Hamad; see Abu Hamed. Adams Fall; ledge in New Haven Harbor, Fall.) Abram ; creek in Grant and Mineral Coun- Conn. (Not Adam's ties, W. Va. (Not Abraham.) Adel; see Somali. Abram; see Shimmo. Adelina; town, Calvert County, Md. (Not Abruad ; see Riad. Adalina.) Absaroka; range of mountains in and near Aderhold; ferry over Chattahoochee River, Yellowstone National Park. -
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.