The Secretary of War

Total Page:16

File Type:pdf, Size:1020Kb

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. Very respectfully, your obedient servant, A. A. HUMPHREYS, Captain of Topographical Engineers, in cha1·ge . .lJ.frilitary topographical memoir and 1·eport, with maps, -r.- on the United States military department if the Pacific, by Thomas Jefferson Cram, captain Corps if Topograph·ical EngineeTs, chiif topographical engineer, ·department if the Pacific, 1855, '56, '57. PREFACE. This memoir has been drawn up by virtue of orders receiYed by me ·while serving in the department of the Pacific, under the command ,of Major General J. E. Wool, United States army, of which the fol- 1lowing is a copy: HEADQUARTERS DEPARTMENT OF THE PACIFIC, Benicia, California, J1me 20, 1855. 'SIR: The commanding general directs that you prepare a topo­ ~ graphical memoir, or view of the department of the Pacific, and that, . ·for this purpose, you consult such papers as may be on file at these 'headquarters. You will also call upon any officers serving within the department for such information as they may be able to give you iin the execution of these instructions. I am, sir, very respectfully, your obedient servant, E. D. TOWNSEND, Assistant AdJutant General. (Captain T. J. CRAM, Topographical Enginee?·s, Benicia, California. Accordingly, the information herein embodied has been derived- 1. From reports, sketches, journals of marches by officers of the 1ine, containing much that is valuable, and from reports of recon- 1naiseances and maps by topographical engineer officers, as I found them at headquarters, without, however, having been, as it seemed c The maps, not having been. ordered by the Committee on Engraving, have not been ;printed. DEPARTMENT OF TilE PACIFIC. 3 to me., previously digested, arranged, and embodied in a useful shape for pr::~ctical military purposes, before being forwarded to the War Department. 2. From conversations during personal interviews with many officers of the line and of the staff (too many to be here enumerated) who had been serving in various districts of the department, and who seemed to me to have intelligently calculated the resources of the country and various points of the different branches of the military service. 3. From my own personal observations upon the country, and upon the practical operations of the several branches of the service,· during a tour of duty (of from two to three years) in various directions and at various places, and in various surveys and reconnaissances in the department in the years 1855, '56, '57, while in the performance of duties as senior topographical engineer officer, attached to the general staff of the commanding general of the department of the Pacific. In drawing up the memoir and report I have not confined myself simply to the task of reporting topographical information, but have shaped aU in a manner, while rendering much of that kind of informa­ tion in the text and maps, so as also to meet the requisition contained in paragraph 481, Army Regulations; hence the double title of "Me­ moir and Report,'' seen on title page. Therefore: it will be observed that this will contain what may be regar~ed as a report of the military and other operations connected with, or having relation to, the military service, as they came under my own observation; and it will likewise embrace my own views, as well as the views of other officers when relevant, in regard to various points, upon which it will be seen by those having the patience to follow me that I have freely, but I trust respectfully, commented in the ensuing chapters. Not only shall I deem it within the scope of my province to report what I regard as existing evils in the working of the military opera­ tions of the regular army, and of the self-constituted volunteer armies that have been in the field in the department, and of the Indian ser­ vice in its relations with the army, but I shall feel at perfect liberty to report suggestions which, from a source however destitute of pre­ tension~ might, if carried into effect~ remove those evils, to the great benefit of the army service in the department of the Pacific. I.-General description if the military department of the Pacific. This department ineludes within its limits the State of California, the Territories of Oregon, Washington, and Utah, containing 718,361 square miles in surface; to use the language of one of its distinguished commanders~ ':altogether, in size, an empire of itself." Map No. 1 represents its general features, as far as necessary for general description. The military posts, as now located, are named in red letters, and are 21 in number, viz: nine in Califor.ni~, .fo.ur in 4 TOPOGRAPHICAL MEMOIR 0], THE Oregon, eight in Washington, and none in Utah; others may have to be established to meet exigencies. The physical features of this great area, while eminently favorable to secure the Indians and the depre· dating whites .from pursuit, are, in themselves, formidable obstacles to the transit of troops, with the necessary supplies for anything like an extended march into the interior of the country. These physical obstacles consist in numerous ranges of lofty mount· ains, of great extent, with which the whole department is checkered; a comparative deficiency in the number and extent of navigable rivers; the want of sui table natural roads, and the extreme difficulty of making roads, owing to the formidable obstacles presented by the mountains all over the department, and, besides, the denseness of the forests in Oregon and Washington. The only physical feature at all favorable to military movements is the great extent of seacoast navigation, from the post of San Diego to that at Bellingham Bay, an extent of about 1,400 miles, which may be regarded as the sea front of the depart· ment. Fortunately, this extensive front is furnished by nature with good harbors, viz: the Bay of San Diego at the south and the waters of Washington at the north; also one of the best in the world, at an in· termediate point, in the Bay of San Francisco.-(See maps Nos. 7, 16, 2.) This bay, and the other smaller tide-water bays with which it is con· nected by navigable straits and channels, are surrounded by a shore extent of 200 miles; and they are navigable by sail and steam vessels in any direction, and their waters communicate with the ocean by a deep navigable strait, the '' Golden Gate,'' inside of which stands the city of San Francisco.-(See map No. 2.) With these beautiful bays two navigable rivers (the Sacramento and San Joaquin) communicate: the former, from the north, affording steamboat navigation at all stages to Sacramento, 129 miles above San Francisco, and at high stages 150 miles further up; the latter river, coming from the southeast, affording similar navigation to Stockton, 115 miles above San Francisco. The Columbia is the only other river navigable for any extent piercing the ocean front of the department of the Pacific.-(See map 16.) But the circumstances of the bar at its mouth (see map No. 3) will forever preclude it from being a harbor. Nevertheless, this river, navigable, without interruption: up to the Cascades, 183 miles above its mouth, and in several reaches above that, and its tributary, the Willamette, (see map No. 14,) which al~o has navigable reaches sepa· rated by falls, are both important in reference to military lines of communication with the interior of the department. The Straits of Fuca, and Washington waters generally, (see map No. 16,) forming an extent of navigation, by sail or steam, for some hundreds of miles, having connexion with the ocean front of the department, and having several excellent harbors, also possess highly important advantages for military movements interior to this front. Again: the Colorado river of California, though not piercing this ocean front within our own possessions in the department, is never­ theless of military importance, (see map No. 7,) and it is used by us DEPARTMENT OF THE PACIFIC.
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • ROCK ART of the WESTERN MOJAVE DESERT- a VIEW from the FIRST DECADE of the 21St CENTURY
    ROCK ART OF THE WESTERN MOJAVE DESERT- A VIEW FROM THE FIRST DECADE OF THE 21st CENTURY Albert Knight (Santa Barbara Museum of Natural History) Douglas H. Milburn (USDA - Angeles National Forest) Barbara Tejada (California Department of Parks and Recreation) INTRODUCTION This paper provides an overview of the Native Californian rock art found in the western Mojave Desert. Rock art may be defined as “landscape art” that is comprised of painted, engraved, pecked, ground, or incised images on natural rock surfaces (see Whitley 1998:11). The rock art of the region is best known from Mark Q. Sutton’s (1982) Rock Art of the Western Mojave Desert and Albert Knight’s (1993) Rock Art of the Western Mojave Desert: A Reevaluation (see also Knight 1997; Sutton 1988:67-70). These now somewhat dated publications describe the rock art of the western Mojave Desert as comprised of monochrome and polychrome painted images (pictographs), ground pit petroglyphs (cupules), and a few pecked petroglyph panels. This paper is intended to expand, clarify, and, in some cases, correct information found in those reports and, also, to share results of subsequent rock art research. BACKGROUND The Western Mojave Desert The western Mojave Desert is encompassed within an internally draining hydrologic basin formed by the Fremont and Antelope Valleys (Sutton 1988:3). This desert basin is bounded on the north by the Tehachapi and Sierra Nevada Mountains, to the south by the Transverse Mountain Ranges, and to the east by an indistinct topographical divide punctuated by several granitic buttes. Broad environmental zones in the western Mojave Desert are described as valley floors, playas, interior mountains, and foothills/upper slopes of flanking mountain ranges (Sutton 1988:9).
    [Show full text]
  • A Location Guide for Rock Hounds in the United States
    A Location Guide for Rock Hounds in the United States Collected By: Robert C. Beste, PG 1996 Second Edition A Location Guide for Rock Hounds in the United States Published by Hobbit Press 2435 Union Road St. Louis, Missouri 63125 December, 1996 ii A Location Guide for Rock Hounds in the United States Table of Contents Page Preface..................................................................................................................v Mineral Locations by State Alabama ...............................................................................................................1 Alaska.................................................................................................................11 Arizona ...............................................................................................................19 Arkansas ............................................................................................................39 California ...........................................................................................................47 Colorado .............................................................................................................80 Connecticut ......................................................................................................116 Delaware ..........................................................................................................121 Florida ..............................................................................................................122
    [Show full text]
  • 2004 Breaking Up
    Breaking Up Breaking Up the 2004 Desert Symposium Field Trip Robert E. Reynolds, Editor LSA Associates, Inc. with Abstracts from the 2004 Desert Symposium California State University, Desert Studies Consortium Department of Biological Science California State University, Fullerton Fullerton, California 92384 in association with LSA Associates, Inc. 1650 Spruce Street, Suite 500 Riverside, California 92507 April 2004 1 Desert Symposium 2004 Table of Contents Breaking Up! The Desert Symposium 2004 Field Trip Road Guide Robert E. Reynolds and Miles Kenney ................................................................................................................... 3 Latest Pleistocene (Rancholabrean) fossil assemblage from the Silver Lake Climbing Dune site, northeastern Mojave Desert, California Robert E. Reynolds ............................................................................................................................................. 33 Harper Dry Lake Marsh: past, present, and future Brian Croft and Casey Burns ............................................................................................................................... 39 Mojave River history from an upstream perspective Norman Meek ....................................................................................................................................................41 Non-brittle fault deformation in trench exposure at the Helendale fault Kevin A. Bryan ...................................................................................................................................................51
    [Show full text]
  • Gravity Study of the San Gabriel Mountains, By
    Gravity Study of the San Gabriel Mountains, By Laurence A. WoOd Suimitted in Patial Fulfillment of the Requirement for the Degree of Bachelor of Science LINDGREN at the MASSACHUIETTS INSTITUTE OF TECIOLOGY June, 1968 Signature of Author . ... Certified by .. The si Supe-rvisor Accepted by ......... Chairman, Departmental Comittee on Thc3es Room 14-0551 77 Massachusetts Avenue Cambridge, MA 02139 Ph: 617.253.5668 Fax: 617.253.1690 MITLibraries Email: [email protected] Document Services http://libraries.mit.edu/docs DISCLAIMER OF QUALITY Due to the condition of the original material, there are unavoidable flaws in this reproduction. We have made every effort possible to provide you with the best copy available. If you are dissatisfied with this product and find it unusable, please contact Document Services as soon as possible. Thank you. Due to the poor quality of the original document, there is some spotting or background shading in this document. -2- Abstract A gravity study of the San Gabriel Mountains was made. A map of Bouguer anomalies in the area was completed and a profile across the mountains was taken. Calculations of the crustal thickness beneath the Los Angeles basin, the San Gabriel Mountains, and the Eajave tesert were made using the sin x/x method and a method described by Bott. These calculations indicate that there is a crustal thinning under the San Gabriel Mountains to 27 km. Values of 35 and 38 km were obtained for the Los Angeles basin and the IMojave Desert respectively. These results correspond quite closely to seismic determinations of the crustal thickness in this area.
    [Show full text]
  • Precipitation Depth-Duration and Frequency Characteristics for Antelope Valley, Mojave Desert, California
    PRECIPITATION DEPTH-DURATION AND FREQUENCY CHARACTERISTICS FOR ANTELOPE VALLEY, MOJAVE DESERT, CALIFORNIA U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 95-4O56 Prepared in cooperation with LOS ANGELES COUNTY, CALIFORNIA Three-dimensional sketch of average historical storm depths throughout Antelope Valley. View from northeast to southwest. CONTENTS Abstract.................................................................................................................................................................................. 1 Introduction ....................................................................................................................._^ 1 Description of Study Area........................................................................................................................................... 3 Purpose and Scope....................................................................................................................................................... 6 Data Collection.............................................................................................................................................................^ 6 Seasonal Variation in Precipitation........................................................................................................................................ 10 Precipitation Depth-Duration Characteristics........................................................................................................................ 10 Disaggregation
    [Show full text]