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Temecula Basin
Temecula Basin is a sedimentary basin, which along with the Aguanga Basin, is part of the Elsinore Fault Zone, in southwestern Riverside County, California. The Temecula Basin is a basin of down faulted Mesozoic basement rock, overlain by late Cenozoic continental sediments.〔( John F. Mann, Geology of a Portion of the Elsinore Fault Zone, California, Special Report 43, Department of Resources, Division of Mines, San Francisco, October 1955. )〕
==Aquifer==
The Temecula Basin is also a local ground water basin and aquifer in southwestern Riverside County. It is the largest groundwater basin in the San Diego water region.〔(San Diego Region - The Basin Plan ) from waterboards.ca.gov accessed April 26, 2015〕 This aquifer is recharged by precipitation in the valley, underflow and by surface flow from the creeks draining the mountains southern Perris Block in the watershed of Murrieta Creek and Temecula Creek, tributaries of the Santa Margarita River.〔(Gerald A. Waring, UNITED STATES GEOLOGICAL SURVEY Water-Supply Paper 429, Ground Water In The San Jacinto And Temecula Basins, California, Government Printing Office, Washington, 1919 )〕〔( Experiment Station Record, Volume 41, United States. Office of Experiment Stations, United States Agricultural Research Service, U.S. Government Printing Office, 1920., p.785 )〕
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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