Main mass of Island of Niihau is composed of Paniau volcanic series. Stratigraphic correlation chart gives age as Pliocene and older.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Named for Paniau hill. Type locality at E side of Paniau hill [21 deg 56' 21"N, 160 deg 04' 59"W] forming remnant of shield volcano on Island of Niihau, HI. Composed of thin-bedded vesicular olivine basalts of both aa and pahoehoe type, beds of vitric lapilli ash, and basaltic dikes. Maximum exposed thickness is 1281 ft at type locality. Underlies with erosional unconformity Kiekie volcanic series. Map plate and cross section show overlying sedimentary rocks of recent age inland and in valleys. Age is given as Pliocene(?).
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Paniau Volcanic Series of Stearns (1947) is reduced in rank and renamed Paniau Basalt to reflect composition of basalt. Unpublished K-Ar data for 11 flows of Paniau indicate Miocene and Pliocene age (G.B. Dalrymple, oral commun., 1986).
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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