Named for occurrence at Kalama crater 0.5 NE mi of Koko crater [Koko Head 7.5' quad] Island of Oahu. Included as unit in upper part of Honolulu series. Crater is 50 ft deep. Flow, extending from cone to sea, consists mostly of aa. "May or may not have been part of the same magma that produced the Koko volcanics". (p.153) Underlies several ft of Koko tuff on SW slope of cone. Appears to be Recent age based on lack of emerged reef of Waimanalo stand of sea.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Is lava flow of nepheline basanite with spatter and cinder at its source (Kalama Crater). Thickness unknown but at least 10 ft thick. Base not exposed. Covers area about 0.75 sq mi on south side of Kalama Range 1 to 2 mi southwest of Makapuu Head. No fossils. Believed to be later than Waimanalo stand of sea. Assigned Recent age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
K-Ar ages of nepheline-basanite from Kalama lava of Honolulu Volcanic Series range from 36.1 +/-3.6 ka to 32.4 +/-5.4 ka.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Kalama Volcanics (Stearns, IN Stearns and Vaksvik, 1935) abandoned as formally named unit and called Kalama flow (and associated cone), informal unit of Honolulu Volcanics.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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