[Apparently named for Kaau volcanics]. Also referred to as Palolo Valley mud flow. Is well exposed 1 mi above mouth of Waiomao Stream along private road excavated in 1939 [Island of Oahu]. Consists chiefly of small nodules of Kaau basalt, few bombs and olivine segregations and numerous fragments of Koolau basalt set in gray dirty matrix. No bedding present. Deposit reaches height of 60 ft above adjacent Kaau basalt.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Probably correlative with Kaau volcanics in lower part of Honolulu volcanic series. Locally rests on tuff of Kaau volcanics. Contains few molds of wood fragments but no identifiable fossils. Assigned Pleistocene age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Abandoned as formally named unit and made part of informal unit called Kaau flows (and associated tuff and mudflow deposits) of Honolulu Volcanics.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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