Pg. 37, 38, 63. Timber Canyon fanglomerate. Reddish fanglomerate, of [late] Pleistocene age, occurring on top of the ridges and beveling the edges of the upturned marine beds west of Timber Canyon, on north side of Santa Clara Valley. This deposit was formed at base of Santa Paula Peak. Is present in Ventura and Los Angeles basins, southern California.
Source: US geologic names lexicon (USGS Bull. 896, p. 2150).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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