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・ California Coastal National Monument
・ California Coastal National Monument Expansion Act of 2013
・ California coastal prairie
・ California Coastal Records Project
・ California coastal sage and chaparral ecoregion
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・ California Coastal Trail
・ California Code of Civil Procedure
・ California Code of Regulations
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・ California College of Ayurveda
・ California College of the Arts
・ California and Hawaiian Sugar Company
・ California and Nevada Credit Union Leagues
・ California and Nevada Railroad
California Aqueduct
・ California Area Public Library
・ California Area School District
・ California Army National Guard
・ California Art Club
・ California Art Preservation Act
・ California Artificial Stone Paving Co. v. Molitor
・ California Arts Council
・ California Assembly Bill 540 (2001)
・ California Assembly Bill 811 (2008)
・ California Assembly Bill 962 (2009)
・ California Assemblyman's Bill 1535 (Improved Naloxone Access)
・ California Association of Ayurvedic Medicine
・ California Association of Bicycling Organizations
・ California Association of Marriage and Family Therapists


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California Aqueduct : ウィキペディア英語版
California Aqueduct

The Governor Edmund G. Brown California Aqueduct is a system of canals, tunnels, and pipelines that conveys water collected from the Sierra Nevada Mountains and valleys of Northern and Central California to Southern California. The over aqueduct is the principal feature of the California State Water Project.
The Department of Water Resources (DWR) operates and maintains the California Aqueduct, including one pumped-storage hydroelectric plant, Gianelli Power Plant. Gianelli is located at the base of San Luis Dam, which forms San Luis Reservoir, the largest offstream reservoir in the United States.
The Castaic Power Plant, while similar and which is owned and operated by the Los Angeles Department of Water and Power, is located on the northern end of Castaic Lake, while Castaic Dam is located at the southern end.
==Geological context==
The Central Valley of California is surrounded by high mountains that are eroding into the valley itself. The valley is somewhat rebounding from recent ice age interglacial glaciations.
The region is prone to significant earthquakes due to the many faults and fault lines that pass through the region.
The flatness of the valley bottom contrasts with the rugged hills or gentle mountains that are typical of most of California's terrain. The valley is thought to have originated below sea level as an offshore area depressed by subduction of the Farallon Plate into a trench further offshore. The San Joaquin Fault is a notable seismic feature of the Central Valley.
The valley was later enclosed by the uplift of the Coast Ranges, with its original outlet into Monterey Bay. Faulting moved the Coast Ranges, and a new outlet developed near what is now San Francisco Bay.
Over the millennia, the valley was filled by the sediments of these same ranges, as well as the rising Sierra Nevada to the east; that filling eventually created an extraordinary flatness just barely above sea level; before California's massive flood control and aqueduct system was built, the annual snow melt turned much of the valley into an inland sea.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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