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Sediment Management for Southern California Mountians, Coastal Plains and Shoreline. Part D: Special Inland Studies

Brown, William M., III and Taylor, Brent D. and Kolker, Oded C. and Wells, Wade G., II and Palmer, Nancy R. (1982) Sediment Management for Southern California Mountians, Coastal Plains and Shoreline. Part D: Special Inland Studies. Environmental Quality Laboratory Report, 17-D. California Institute of Technology , Pasadena, CA. (Unpublished)

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[img] Image (JPEG) (Plate D1-1: Inland Structures which Affect Sediment Movements in Southern California) - Supplemental Material
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[img] Image (JPEG) (Plate D3-1: Current Vegetation) - Supplemental Material
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[img] Image (JPEG) (Plate D4-1: The Extent and Frequency of Forest, Brush, and Grass Fires in Coastal Stream Basins of Southern California, 1910-1975) - Supplemental Material
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In southern California the natural environmental system involves the continual relocation of sedimentary materials. Particles are eroded from inland areas where there is sufficient relief and, precipitation. Then, with reductions in hydraulic gradient along the stream course and at the shoreline, the velocity of surface runoff is reduced and there is deposition. Generally, coarse sand, gravel and larger particles are deposited near the base of the eroding surfaces (mountains and hills) and the finer sediments are deposited on floodplains, in bays or lagoons, and at the shoreline as delta deposits. Very fine silt and clay particles, which make up a significant part of the eroded material, are carried offshore where they eventually deposit in deeper areas. Sand deposited at the shoreline is gradually moved along the coast by waves and currents, and provides nourishment for local beaches. However, eventually much of this littoral material is also lost to offshore areas. Human developments in the coastal region have substantially altered the natural sedimentary processes, through changes in land use, the harvesting of natural resources (logging, grazing, and sand and gravel mining); the construction and operation of water conservation facilities and flood control structures; and coastal developments. In almost all cases these developments have grown out of recognized needs and have well served their primary purpose. At the time possible deleterious effects on the local or regional sediment balance were generally unforeseen or were felt to be of secondary importance. In 1975 a large-scale study of inland and coastal sedimentation processes in southern California was initiated by the Environmental Quality Laboratory at the California Institute of Technology and the Center for Coastal Studies at Scripps Institution of Oceanography. This volume is one of a series of reports from this study. Using existing data bases, this series attempts to define quantitatively inland and coastal sedimentation processes and identify the effects man has had on these processes. To resolve some issues related to long-term sediment management, additional research and data will be needed. In the series there are four Caltech reports that provide supporting studies for the summary report (EQL Report No. 17). These reports include: EQL Report 17-A Regional Geological History EQL Report 17-B Inland Sediment Movements by Natural Processes EQL Report 17-C Coastal Sediment Delivery by Major Rivers in Southern California EQL Report 17-D -- Special Inland Studies Additional supporting reports on coastal studies (shoreline sedimentation processes, control structures, dredging, etc.) are being published by the Center for Coastal Studies at Scripps Institution of Oceanography, La Jolla, California.

Item Type:Report or Paper (Technical Report)
Additional Information:© 1982 California Institute of Technology. The authors gratefully acknowledge the principal investigators Norman H. Brooks (Caltech) and Douglas L. Inman (Scripps) for their insight in the conception of this project and their generous contributions thereafter. We also wish to acknowledge the generous assistance of Robert C. Y. Koh and Vito A. Vanoni throughout the preparation of this report; and the assistance of William M. Brown (U.S. Geological Survey), David Sarokin, K. T. Shu and Lloyd R. Townley. Support for this project was provided through grants and contracts from: Ford Foundation, Grant No. 795-0092 Los Angeles County Flood Control District, Agreement No. 27272 Orange County Environmental Management Agency Agreement No. 9-42-133-20 United States Geological Survey, Contract No. 14-08-0001-16826 and Grant No. 14-08-000l-G-60S Department of the Army, Corps of Engineers, South Pacific Division, Contract No. DACW 09-77-A-0040 United States Forest Service, Pacific Southwest Forest and Range Experiment Station, Agreement No. 21-587 National Science Foundation, Grant No. ENG-77-10182 Southern Pacific Corporation EQL Discretionary funds In addition, the U.S. Geological Survey and the U.S. Forest Service provided some research personnel to work with the project team at EQL. Finally, the universities, Caltech and University of California, San Diego, provided the institutional framework for conducting the study including especially useful support for initiating this project.
Group:Environmental Quality Laboratory
Funding AgencyGrant Number
Ford Foundation795-0092
Los Angeles County Flood Control District27272
State of California Department of Boating and Waterways9-42-133-20
Army Corps of Engineers, South Pacific DivisionDACW 09-77-A-0040
United States Forest Service21-587
Southern Pacific CorporationUNSPECIFIED
Series Name:Environmental Quality Laboratory Report
Issue or Number:17-D
Record Number:CaltechEQL:EQL-R-17-D
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Usage Policy:You are granted permission for individual, educational, research and non-commercial reproduction, distribution, display and performance of this work in any format.
ID Code:25781
Deposited By: Imported from CaltechEQL
Deposited On:14 Dec 2009
Last Modified:03 Oct 2019 03:09

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