K-Ar ages from Palehua member of Waianae Volcanics range from 3.2 to 2.5 Ma.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Named for extensive exposures around settlement of Palehua at South end of Waianae Range, Island of Oahu. Formerly upper member of Waianae Volcanic Series (Stearns, IN Stearns and Vaksvik, 1935) excluding lavas here considered to be part of Kolekole Volcanics. Is youngest member of Waianae Volcanics. Type section is near Palehua [21 deg 23' 58"N, 158 deg 06' 11"W, Schofield Barracks 7.5' quad]; reference section is near Mount Kaala. Is hawaiite with minor alkalic and basalt and mugearite. Is 200 m thick at type. Generally conformably overlies Kamaileunu Member (new) of Waianae Volcanics. Locally as Pohakea Pass, unconformably overlies the Kamaileunu. Unconformably underlies Kolekole Volcanics and Quaternary sedimentary deposits. Hawaiite, having reversed magnetic polarity led to discovery of Kaena Reversed Polarity Subchron within Gauss Normal Polarity Chron dated at 2.85 +/-0.05 Ma (Doell and Dalrymple, 1973)
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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