Includes all lava flows making up Kalaupapa Peninsula and Mokuhooniki, island off E coast of Island of Molokai, HI. Crater 400 ft deep indents summit of dome. Extent about 4 sq mi and highest point is 405 ft. Base not exposed. Separated from West Molokai volcanic series (new) by erosional unconformity. "Conglomerate overlying basalt on SE side of peninsula seems to be graded to a stand of the sea 25 ft higher." "On this evidence ... is assigned to the late Pleistocene." (p.73)
Source: GNU records (USGS DDS-6; Menlo GNULEX).
"... is named from the leper settlement which is built on this lava. The basalt forms a peninsula 2.5 miles long and 2.5 miles wide." Map shows Kauhako Crater, vent from which unit extruded.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Type locality: Kalaupapa Peninsula [21 deg 11' 33"N, 156 deg 59' 10"W, Kanuakakai quad] Island of Molokai, HI. Covers 6.25 sq mi. Assigned Pleistocene(?) age although text quotes Stearns (1946) ..."is assigned a late Pleistocene age" based on stratigraphic relation to beach deposits.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
K-Ar age on sample of alkalic olivine basalt from Kauhako Crater [Kalaupapa Basalt] on Kalaupapa Peninsula, Island of Molokai, gave 1.24 +/-0.16 Ma.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Varies in composition from basanite to lava transitional between alkalic and tholeiitic basalt. K-Ar ages on basalt samples [of Kalaupapa Basalt] from west wall and south wall of Kauhako Crater and from collapsed lava tube 500 m north of crater range from 0.57 +/-0.025 to 0.344 +/-0.031 Ma.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Kalaupapa Basalt [Stearns and Macdonald, 1947] remained Kalaupapa Volcanics to reflect range of compositions present. Consists of rejuvenated-stage lava of alkalic basalt, basanite, and associated cone. Unconformably overlies East Molokai Volcanics. Is Pleistocene age based on K-Ar ages of 0.57 +/-0.02 to 0.35 +/-0.03 Ma.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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