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San Francisquito Formation : ウィキペディア英語版 | San Francisquito Formation
The San Francisquito Formation is a geologic formation in northern Los Angeles County, California.〔( Seismo.berkeley.edu: Field Guide to the Punchbowl Fault Zone, at Devil's Punchbowl Los Angeles County Park ); San Andreas Fault Resources; University of California, Berkeley; by Frederick M. Chester; January 1999.〕〔( AAPG Datapages/Archives: "Stratigraphy and Sedimentology of the Type San Francisquito Formation, Southern California" ); Department of Earth Sciences, University of California, Riverside; 1982.〕 Areas where it is exposed include: San Francisquito Canyon of the Sierra Pelona Mountains, and the northwestern side of the Devil's Punchbowl gorge in the San Gabriel Mountains.〔〔 ==Geology== The San Francisquito Formation is from marine deposits of the Late Cretaceous period of the Mesozoic Era, and the Early Paleocene epoch in the Paleogene period of the Cenozoic Era.〔〔 It is overlain by the Punchbowl Formation (east) and Castaic Formation (west), both of the Miocene and Pliocene epochs.〔 It overlies the crystalline San Gabriel Basement Complex.〔 It is found between the San Andreas Fault on its north, and the Devil's Punchbowl Fault on its south.〔〔 The Pliocene epoch Crowder Formation is to the northeast.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「San Francisquito Formation」の詳細全文を読む
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