[Named for] cinder cone, Puu Kilea, at 260 ft above sea level 0.5 mi north of Olowalu [village] on south bank of Olowalu Stream, west Maui. Included as unit of Lahaina volcanic series. Composed of fine-grained nepheline basanite. Is 15 ft thick. Overlies consolidated older alluvial fan of Olowalu Stream. Appears to be as old as 25-foot stand of sea. Stratigraphic section assigns middle(?) and late Pleistocene age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Type locality: Puu Kilea, cinder cone 0.5 mi north of Olowalu village [20 deg 49' 00"N, 156 deg 37' 30"W, Olowalu 7.5' quad] west Maui. Assigned Pleistocene(?) age based on relationship to 25 foot stand of sea.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
K-Ar age on basanite from Kilea cone, Olowalu Canyon is 1.30 +/-0.10 Ma, "a surprisingly old age" p.350
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Kilea Volcanics of Stearns and Macdonald (1942) abandoned as formally named unit and called Kilea flow and cinder cone, informal unit of Lahaina Volcanics. "The single K-Ar age of 1.30 +/-0.10 Ma (Naughton and others, 1980) is considered to be too old on stratigraphic grounds." Lahaina Volcanics is considered to be of Pleistocene age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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