Named for Portuguese Bend on S coast, Palos Verdes Hills, CA. Type region [area]: along Portuguese Canyon [San Pedro 7.5' quad, Los Angeles Co, CA]. Is bentonitic tuff bed at top of lower part of Altamira shale member of Monterey Shale in Palos Verdes Hills. Is 55 ft thick. Is middle Miocene age based on Foraminifera in lower part of Altamira shale member.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Type region [area] redesignated as Klondike Canyon, near Portuguese Bend [San Pedro 7.5' quad, Los Angeles Co, CA] because in Woodring and others (1936) erroneously cited in Portuguese Canyon. Portuguese tuff bed consists of light-colored bentonitic tuff, 55 ft thick in type region. Included at top in measured section of lower part of Altamira shale member of Monterey shale in unnamed canyon .25 mi E of Portuguese Canyon. At Inspiration Point is about 60 ft thick. Probably acted as lubricant for mass of rocks that slid down structural basin and moving seaward overriding lower marine terraces. Shown on map as middle Miocene age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Sample of bentonite containing plagioclase and minor quartz collected on W wall of Klondike Canyon at 325 ft elevation from Portuguese Tuff Bed yielded K-Ar age of 14.5 +/-1.1 Ma on plagioclase.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Portuguese Tuff Bed in Altamira Shale Member of Monterey Formation dated by Turner (1970) at 14.9 +/-1.1 Ma is close to Relizian-Luisian boundary. [All K-Ar ages have been calculated using decay constants recommended by Steiger and Jager (1977).]
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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