Pg. 363 (fig. 150). Mahala sandstone and conglomerate. Shown on structure section as overlying Peculiar shale (new). [Age is late Miocene.]
Recognized locally southwest of Chino fault in San Bernadino Co., southern CA.
Source: Publication; US geologic names lexicon (USGS Bull. 1200, p. 2326-2327).
Pg. 521. Mahala sandstone and conglomerate (in Puento formation). Coarse conglomerate with minor sandstone and sandy shale; perhaps in part Pliocene. Thickness 30 to more than 115 feet. Upper part of Puente. Measured section noted. Recognized in southern California. Age is late Miocene.
Exposed in Slaughter Canyon in southeastern Puente Hills, between Chino and the Santa Ana River, San Bernardino Co., southern CA.
Source: US geologic names lexicon (USGS Bull. 1200, p. 2326-2327).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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