Pg. 363 (fig. 150). Blanco sandstone. Coarse sandstone with some pebble conglomerate. Shown on structure section as underlying Cubierto shale (new) and overlying Papel Blanco 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. 383).
Pg. 521. Blanco sandstone (in Puento formation). Light-colored medium- and coarse-grained sandstone 337 feet thick. 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. 383).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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