Hinds, N.E.A., 1930, Geology of Kauai and Niihau: Bernice P. Bishop Museum Bulletin, no. 71, 103 p.
Basaltic lava flows distributed over most of Island of Kauai, Hawaiian Islands. No type locality designated but Waimea conglomerate (new) separates lower Kauai lavas from upper Kauai lavas in Waimea Canyon. Upper Kauai is as much as 4000 ft thick. Unconformably underlies lavas of Koloa volcanic episode. [named for Island of Kauai]
Source: GNU records (USGS DDS-6; Menlo GNULEX).
"Included in what is now known as the Waimea Canyon volcanic series, which see." Assigned Pliocene(?) age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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