High-Precision Gravity Stations for Monitoring Vertical Crustal Motion in Southern California
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4.3 Cultural Resources
4.3 CULTURAL RESOURCES INTRODUCTION W & S Consultants, (W&S) conducted an archaeological survey of the project site that included an archival record search conducted at the local California Historic Resource Information System (CHRIS) repository at the South Central Coastal Information Center (SCCIC) located on the campus of California State University, Fullerton. In July 2010, a field survey of the 1.2-mile proposed project site was conducted. The archaeological survey report can be found in Appendix 4.3. Mitigation measures are recommended which would reduce potential impacts to unknown archeological resources within the project site, potential impacts to paleontological resources, and the discovery of human remains during construction to less than significant. PROJECT BACKGROUND Ethnographic Setting Tataviam The upper Santa Clara Valley region, including the study area, was inhabited during the ethnographic past by an ethnolinguistic group known as the Tataviam.1 Their language represents a member of the Takic branch of the Uto-Aztecan linguistic family.2 In this sense, it was related to other Takic languages in the Los Angeles County region, such as Gabrielino/Fernandeño (Tongva) of the Los Angeles Basin proper, and Kitanemuk of the Antelope Valley. The Tataviam are thought to have inhabited the upper Santa Clara River drainage from about Piru eastwards to just beyond the Vasquez Rocks/Agua Dulce area; southwards as far as Newhall and the crests of the San Gabriel and Santa Susana Mountains; and northwards to include the middle reaches of Piru Creek, the Liebre Mountains, and the southwesternmost fringe of Antelope Valley.3 Their northern boundary most likely ran along the northern foothills of the Liebre Mountains (i.e., the edge of Antelope Valley), and then crossed to the southern slopes of the Sawmill Mountains and Sierra Pelona, extending 1 NEA, and King, Chester. -
Prn 198803.Pdf
. the mere mention of the name brings forth railroad images larger than life. It wasn't just tracks and trains.It wasn't just an Indiana institution-though it MONON'certainly was that. Oh. my, no. What the Monon was ...well, it was every American railroad. every American hometown. every American underdog rolled into one. Why. the Monon was practically human. Its birth was a cause for . rejoicing. its operation a source of Hoosier pride. And when it died. a thousand legends lived on. Now, legend and fact are woven together in a brand-new, finely crafted illustrated history of the Monon. We take you from beginning to merger into the L&N. from Louisville to French Lick to Indianapolis to Michigan City to Chicago .•. from Hoosierland to hotshot. from 4-4-0 to Century 420. We're proud to announce the creation of Monon-The Hoosier Line by Gary and Stephen Dolzall. This book is in production and will be published by Interurban Press in the Fall of 1987. Its 'edit!o�r=is=;;�=:�; Roaring Fork Railroad Begins Private Car Service. We offer three levels of service: First class, Vistadome and coach starting as low as $99 one-way Denver to Glenwood Springs. Ticket price includes open bar and fine dining in our VistaDiner. Our route over the Continental Divide includes the famous tun nel district and its spectacular views of the Rocky Mountain wilderness. Departs Denver every Saturday through March for Glenwood Springs, Grand Junction and Salt Lake City. Returns each Sunday. CaD (303) 893-8922 collect for reservations and information. -
4.1 Introduction Ocotillo Wind Energy Facility
4.1 Introduction Ocotillo Wind Energy Facility 4.1 Introduction This chapter assesses environmental consequences or impacts that would result from the implementation of the Proposed Action or the alternatives described in Chapter 2. These analyses consider direct, indirect, and cumulative impacts of the Proposed Action and alternatives, including both short-term impacts during construction and decommissioning, and long-term impacts during operations. This chapter also identifies mitigation measures to address adverse impacts and summarizes the residual and unavoidable adverse impacts on an issue-by-issue basis. The scope of the impact analyses presented in this chapter is commensurate with the level of detail for the alternatives provided in Chapter 2, Proposed Action and Alternatives, and the availability and/or quality of data necessary to assess impacts. Baseline conditions for assessing the potential environmental impacts are described in Chapter 3. The methodology for this assessment conforms with the guidance found in the following sections of the Council on Environmental Quality (CEQ) regulations for implementing NEPA: 40 Code of Federal Regulation (CFR) Section 1502.24, Methodology and Scientific Accuracy; 40 CFR Section 1508.7, Cumulative Impact; and 40 CFR Section 1508.8, Effects. The CEQ regulations require agencies to “rigorously explore and objectively evaluate” the impacts of the alternatives. The methodologies used in the impact assessment also conform to the requirements of the CEQA, Public Resources Code Section 21000 et seq.), including the Guidelines for Implementation of the CEQA, Title 14 California Code of Regulations section 15000 et seq. 4.1.1 Analytical Assumptions The following impacts analysis was conducted with the following assumptions: The laws, regulations, and policies applicable to the BLM authorizing ROW grants for renewable energy development facilities would be applied consistently for all action alternatives. -
Gravity Survey of the Western Mojave Desert California
Gravity Survey of the Western Mojave Desert California By DON R. MABEY GEOPHYSICAL FIELD INVESTIGATIONS GEOLOGICAL SURVEY PROFESSIONAL PAPER 316-D A study of the relation of the gravity anomalies to the geology with special reference to the distribution and thickness of the Cenozoic rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1960 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by^the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract._____________________________ 51 Gravity anomalies.________________ 5*? Introduction __________________________ 51 Garlock fault zone.____________ Location and cultural features.______ 51 Randsburg-Harper Lake area__-. Purpose of geophysical investigations. 52 Boron-Kramer Junction area___. 64 Acknowledgments__ ______________ 64: 53 Barstow-Cajon Pass area. ______ 6" Physical and geologic features.__________ 53 Antelope Valley area___________ Physiography and drainage.________ 53 Significance of the gravity anomalies. 6° Geology __________________________ 53 Geologic significance___________ 6^ Gravity survey._______________________ 55 Economic significance____._-__. 7? Fieldwork and reduction of data-____ 55 Conclusions. ___ ___________________ 71 Bouguer anomaly map.____________ 56 Selected references.________________ 71 Problems of interpretation._________ 56 Index_ ___________________________ 7? ILLUSTRATIONS [Plates are in pocket] PLATE 10. Bouguer anomaly and generalized geologic map of the western Mojave Desert. 11. Bouguer anomaly and generalized geologic map of the area in the vicinity of the Kramer borate district. 12. Map showing major gravity trends, faults, and inferred faults in the western Mojave Desert. Pag-? FIQUKE 22. Index map of southern California showing area of this report in relation to the Mojave Desert and other physiographic features_______________-___________________________-___-_-_---_-------_-_-__-____ 52 23. -
Eagle Mountain Pumped Storage Project Draft License Application Exhibit E, Volume 1, Public Information Palm Desert, California
Eagle Mountain Pumped Storage Project Draft License Application Exhibit E, Volume 1, Public Information Palm Desert, California Submitted to: Federal Energy Regulatory Commission Submitted by: Eagle Crest Energy Company Date: June 16, 2008 Project No. 080470 ©2008 Eagle Crest Energy DRAFT LICENSE APPLICATION- EXHIBIT E Table of Contents 1 General Description 1-1 1.1 Project Description 1-1 1.2 Project Area 1-2 1.2.1 Existing Land Use 1-4 1.3 Compatibility with Landfill Project 1-5 1.3.1 Land Exchange 1-5 1.3.2 Landfill Operations 1-6 1.3.3 Landfill Permitting 1-6 1.3.4 Compatibility of Specific Features 1-7 1.3.4.1 Potential Seepage Issues 1-8 1.3.4.2 Ancillary Facilities Interferences 1-9 2 Water Use and Quality 2-1 2.1 Surface Waters 2-1 2.1.1 Instream Flow Uses of Streams 2-1 2.1.2 Water quality of surface water 2-1 2.1.3 Existing lakes and reservoirs 2-1 2.1.4 Impacts of Construction and Operation 2-1 2.1.5 Measures recommended by Federal and state agencies to protect surface water 2-1 2.2 Description of Existing Groundwater 2-1 2.2.1 Springs and Wells 2-3 2.2.2 Water Bearing Formations 2-3 2.2.3 Hydraulic Characteristics 2-4 2.2.4 Groundwater Levels 2-5 2.2.5 Groundwater Flow Direction 2-6 2.2.6 Groundwater Storage 2-7 2.2.7 Groundwater Pumping 2-7 2.2.8 Recharge Sources 2-8 2.2.9 Outflow 2-9 2.2.10 Perennial Yield 2-9 2.3 Potential Impacts to Groundwater Supply 2-9 2.3.1 Proposed Project Water Supply 2-9 2.3.2 Perennial Yield 2-10 2.3.3 Regional Groundwater Level Effects 2-12 2.3.4 Local Groundwater Level Effects 2-15 2.3.5 Groundwater -
Transverse Ranges - Wikipedia, the Free Encyclopedia
San Gabriel Mountains - Field Trip http://www.csun.edu/science/geoscience/fieldtrips/san-gabriel-mts/index.html Sourcebook Home Biology Chemistry Physics Geoscience Reference Search CSUN San Gabriel Mountains - Field Trip Science Teaching Series Geography & Topography The Sourcebook for Teaching Science Hands-On Physics Activities Tour - The route of the field trip Hands-On Chemistry Activities GPS Activity HIstory of the San Gabriels Photos of field trip Internet Resources Geology of the San Gabriel Mountains I. Developing Scientific Literacy 1 - Building a Scientific Vocabulary Plate Tectonics, Faults, Earthquakes 2 - Developing Science Reading Skills 3 - Developing Science Writing Skills Rocks, Minerals, Geological Features 4 - Science, Technology & Society Big Tujunga Canyon Faults of Southern California II. Developing Scientific Reasoning Gneiss | Schist | Granite | Quartz 5 - Employing Scientific Methods 6 - Developing Scientific Reasoning Ecology of the San Gabriel Mountains 7 - Thinking Critically & Misconceptions Plant communities III. Developing Scientific Animal communities Understanding Fire in the San Gabriel Mountains 8 - Organizing Science Information Human impact 9 - Graphic Oganizers for Science 10 - Learning Science with Analogies 11 - Improving Memory in Science Meteorology, Climate & Weather 12 - Structure and Function in Science 13 - Games for Learning Science Inversion Layer Los Angeles air pollution. Åir Now - EPA reports. IV. Developing Scientific Problem Climate Solving Southern Calfirornia Climate 14 - Science Word Problems United States Air Quality blog 15 - Geometric Principles in Science 16 - Visualizing Problems in Science 1 of 2 7/14/08 12:56 PM San Gabriel Mountains - Field Trip http://www.csun.edu/science/geoscience/fieldtrips/san-gabriel-mts/index.html 17 - Dimensional Analysis Astronomy 18 - Stoichiometry 100 inch Mount Wilson telescope V. -
The El Mirage Shear Line"
perature (cooling), a change in the mois ture content (increased dew points), and either a wind shift and/or an increase in the wind speed and increased gustiness of the wind field. Especially in regard to Southern California sea breezes, there is also a marked change in the visibility as the Los Angeles megalopolis leads to "Modified Convergence Lines: degraded visibilities with the sea breeze frontal passage. During the warm-season months along The El Mirage Shear Line" the West Coast of the United States with its Mediterranean Climate, High Pres sure tends to dominate the upper air pat iffering wind speeds and/or wind subsequently establish pressure gradient tern over or just upstream of California directions can result in convergence forces resulting in inland air movement D (See Chart #1: Upper Air 500 Mb Pres of air and, subsequently, the develop along coastlines, sea breeze effects on sure Level; June 11, 2012}. When High ment of lift useful for soaring flight. In coastal plains can result in air movement Pressure dominates the upper air pat previous discussions we have defined well inland from that coastline air mass tern, only small, diurnal or day-to-day convergence lines and given examples displacement. Such is the case of the El changes tend to occur in the mean sea of convergent lift in Sea Breeze Fronts, Mirage Shear Line. During the warm level (MSL) pressure field over South Terrain-induced Convergence Lines season months along the Southern ern California. Intense surface heating in (Tehachapi and Elsinore Shear Lines), California Coast, a sea-breeze typically the deserts of Southern California by the and Terrain-Channeled Convergence develops daily in response to late morn late morning hours results in a lowering Lines (Mono Lake and the Flying ''M" ing heating over the Los Angeles Basin of surface pressure in Mojave Desert due Shear Lines). -
The Secretary of War
35Tl'I CoNGREss, } HOUSE OF REPRESENTATIVES. { Ex. Doc. 2d Session. No. 1 L4. TOPOGRAPHICAL MEMOIR OF THE DEPARTMENT OF THE PACIFIC. FROM THE SECRETARY OF WAR, TRANSM11TING The topographical memoir and report qf Captain T. J. Gram, relative to the Territories qf Oregon and Washington, in the military department ~ of the Pacific. MARCH 3, 1859.-Lo.id on the table, and ordered to be printed. WAR DEPARTMENT, March 3, 1859. SIR: I transmit herewith the report of Captain T. J. Cram, Topo graphical Engineers, on the military department of the Pacific, called for by a resolution of the House of Representatives. The topographical information contained in this report is, to a great extent, published in the reports and maps of the War Department, or is in course of preparation. A large portion of the report is devoted to subjects irrelevant tu its objects, as indicated by the title and the duties of Captain Cram, and contains animadversions upon public functionaries, which are out of place in a topographical communication, and which are, in no)sense, sanctioned or endorsed by this department. Very respectfully, your obedient servant, JOHN B. FLOYD; Secretary~ of War .. Hon. JAMES L. ORR, Speaker of the House of Representatives. 2 TOPOGRAPHICAL MEMOIR OF THE WAR DEPARTMENT, OFFICE OF ExPLORATIONs AND SuRVEYS, Washington, February 24, 1859. SIR: I transmit herewith the military topographical memoir and re port, with maps: on the military department of the Pacific, by Captain T. J. Cram, Topographical Engineers, called for by a resolution of the House of Representatives of January 8. This is the report to which I called the special attention of the War Department in a report dated March 1, 1858. -
Cenozoic Rock Units of the Mojave Desert
CENOZOIC ROCK UNITS OF THE MOJAVE DESERT Thomas W. Dibblee, Jr_ 316 East Mission Street Santa Barbara, California 93101 ABSTRACT The deeply eroded surface of the Pre-Cenozoic basement complex of plutonic and metamorphic rocks of the Mojave Desert is overlain in many parts by Cenozoic sedimentary and volcanic rocks. The oldest are elastic sedimentary rocks of Paleocene-Eocene age, known only along the southwestern and northwestern margins of the western Mojave Desert. These are marine deposits mostly southwest of the San Andreas fault zone, and fluviatile sediments northwest of the Garlock fault zone. Within the Mojave Desert volcanic and sedimentary deposits of early middle Ter- tiary (Oligocene to middle Miocene) age are the oldest and most widespread Ter- tiary rocks. They are extensive in the western and central parts, and present locally in the northern and eastern parts. They are composed primarily of pyro- elastic rocks, and volcanic breccias and flows of rhyolitic to basaltic rocks erupted from many vents and fissures within these parts of the desert terrain. Intercalated with these eruptive rocks are clastic sedimentary rocks composed of agglomerates, fanglomerates and local minor amounts of finer sediments. The age of this assemblage may range from Oligocene to middle Miocene. At one place, a radioactive age (K-A) of 23.5 m.y.b.p. was obtained from rhyolite. All these deposits acumulated on an eroded basement platform in parts of the Mojave Desert region that evolved into depositional basins. The most extensive are in the western and central parts which are designated as the western and central Mojave Desert basins, respectively. -
Staff Report CARB Review of the Mojave Desert AQMD and Antelope
Staff Report CARB Review of the Mojave Desert AQMD and Antelope Valley AQMD Federal 75 ppb Ozone Attainment Plans for the Western Mojave Desert Nonattainment Area Release Date: April 21, 2017 Hearing Date: May 25, 2017 California Environmental Protection Agency OF Air Resources Board Electronic copies of this report are available online at https://www.arb.ca.gov/planning/sip/planarea/mojavesedsip.htm . Alternatively, paper copies may be obtained from the Visitors and Environmental Services Center of the California Air Resources Board, located at 1001 I Street, Sacramento, California 95814, or by contacting CARB’s Office of Communications at (916) 322-2990. For individuals with sensory disabilities, this document is available in Braille, large print, audiocassette, or compact disc. Please contact CARB’s Disability Coordinator at (916) 323-4916 by voice or through the California Relay Services at 711 to place your request for disability services. If you are a person with limited English and would like to request interpreter services, please contact CARB’s Bilingual Manager at (916) 323-7053. This document has been prepared by the staff of the California Air Resources Board. Publication does not signify that the contents reflect the views and policies of the California Air Resources Board, nor do trade names or commercial products constitute endorsement or recommendation for use. For questions, contact: Monica Lewis, Air Pollution Specialist South Coast Air Quality Planning Section California Air Resources Board P.O. Box 2815 Sacramento, CA 95812 Phone: (916) 324-2716 Email: [email protected] Or Carol Sutkus, Manager South Coast Air Quality Planning Section California Air Resources Board P.O. -
Mountain Windstorms Mountains and Lee Waves
3/14/2019 Chapter 17: Mountain Windstorm Mountain Windstorms Downslope windstorms occur along many of the major mountain ranges of the world. In North America, downslope windstorms occur (1) along the east slope of the Rocky Mountain from Alberta to New Mexico, (2) along the east slope of the Sierra Nevada and Cascade Range, (3) on the west slope Dynamics of Downslope Windstorms of San Bernardino, Santa Ana, and San Gabriel Mountains, (4) leeward side of Chinook Windstorms of the Rockies the Alaskan and Chugach mountains in Santa Ana Windstorms of California Alaska. Katabatic Winds The Chinook Wind Event on January 16-17, 1982 Mountains and Lee Waves Chinook winds are usually warm and dry and may exceed 100 knots (115 mph) in the worst storms. When air approaches a mountain, it must rise on the windward side and descend on the leeward side. Chinook winds are violent and are always extremely gusty, with the A series of waves will form downstream of the mountain. winds vary from over 100 to less than 10 miles per hour and back These waves are called lee waves and are commonly observed east of the again in less than a minute. Rockies. 1 3/14/2019 Dynamically-Driven Chinook Winds Factors Affect the Temperature of Chinook Windstorms When the cross-mountain flow Upstream air temperature: Air near the mountain-top is strong upstream of the Rockies can be warm and an inversion is present streamfunction when it originates over the Pacific, or upstream just above the cold when it originates over western mountaintop, the mountain Canada and Alaska. -
Final Data Collection for Rock Source Investigation
SALTON SEA ECOSYSTEM RESTORATION PLAN Final Follow-On Data Collection for Rock Source Evaluation April 2005 Table of Contents Items Page Follow-On Data Collection for Rock Source Evaluation................................................................ 1 Background ........................................................................................................................ 1 Task Objective ................................................................................................................... 3 Site Visits ........................................................................................................................... 3 Mesquite Mine.................................................................................................................... 4 Site Description ..................................................................................................... 4 History........................................................................................................ 4 Site Ownership .......................................................................................... 4 Site Geology .............................................................................................. 4 Existing Infrastructure................................................................................ 6 Availability of Material/Rock....................................................................... 6 Existing Environmental Documentation and Permits/Plans....................... 7 Conceptual Plan to Obtain