Pg. 450, 512-517. Dip Creek formation. Name proposed for Paleocene beds in central and south Santa Lucia Range. Consists of coarse cobble and boulder conglomerates and coarse to fine-grained arkose sandstones, commonly filled with carbonized plant remains. Thickness about 1,320 feet. Unconformably underlies pre-Vaqueros landlaid redbeds and marine Vaqueros sandstones; overlies Asuncion formation [group]. Age is Paleocene.
Type locality: in west part of sec. 30, T. 25 S., R. 10 E., Adelaida quadrangle, Santa Lucia Range, west-central CA.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1122).
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