Squire Member of Pismo Formation of Hall (1973a) is adopted. Shown on geologic map of Morro Bay South and Port San Luis 7.5' quads, San Luis Obispo Co, CA. Contains LYROPECTEN CERROSENSIS (Gabb). Age is late Pliocene.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Named as uppermost member (of 5) of Pismo Formation. Type section is exposures on south side of Squire Canyon within Pismo syncline [T31S R12E, Pismo Beach 7.5' quad] San Luis Obispo Co, CA. Consists of massive white or gray arkosic sandstone that is fine- to medium-grained, moderately well sorted, soft to hard, and friable. Unconformably overlies Belleview, Edna, or Miguelito Member (all new and of Pismo Formation). Locally overlaps Monterey Formation. Unconformably underlies Pas Robles(?) Formation. Age is late Pliocene based on marine megafossils.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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