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Ocotillo Formation : ウィキペディア英語版 | Ocotillo Formation
The Ocotillo Formation is a Pliocene fluvial-alluvial fan geologic formation in the Colorado Desert of Southern California.〔(National Park Service: "The FISH CREEK CANYON ICHNOFAUNA: a PLIOCENE (BLANCAN) Vertebrate Footprint Assemblage from Anza-Borrego Desert State Park, California" ); by Paul Remeika.〕 It occurs in western Imperial County and eastern San Diego County.〔(USGS.gov: "Pleistocene Brawley and Ocotillo Formations: Evidence for initial strike-slip deformation along the San Felipe and San Jacinto fault zonez, Southern California" ); Journal of Geology; by S.M. Kirby, S.U. Janecke, R.J. Dorsey, B.A. Housen, V.E. Langenheim, K.A. McDougall, and A.N. Steeley.〕 ==Geology== The formation overlies the Brawley Formation, and underlies the Palm Spring Formation.
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