[Named] for Stanton Ranch. [Type locality] is "informally defined" to include red andesite flows and flow breccias, and subordinate tuff breccias, conspicuously exposed on steep slopes northwest of Stanton Ranch, Santa Cruz Island, CA. Is second from lowermost member of Santa Cruz Island Volcanics (new). [Authors say Santa Cruz Island Volcanics informally divided into members.] Thickness ranges from 450 to 1300 ft. Conformably overlies Griffith Canyon Member (new); discordantly underlies Devils Peak Member (new) (both of Santa Cruz Island Volcanics). Text states no precise age is available for Santa Cruz Island Volcanics or time span of volcanic rocks, "but entire pile was presumable emplaced within Saucesian Stage of upper Oligocene and lower Miocene," p.94. Age on map shown as Miocene.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Santa Cruz Island Volcanics (Nolf and Nolf, 1969) and its members (ascending): Griffith Canyon, Stanton Ranch, Devils Peak, and Prisoners Harbor are adopted. No ages have been determined for lower part of Santa Cruz Island Volcanics; however volcanic rocks are underlain by probable Saucesian-age San Onofre Breccia (Weaver and Myers, 1969). Shown on generalized geologic sketch map of north-central Santa Cruz Island as of Tertiary age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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