Occurs [Type locality] in glaciated valley of Clear Fork of the Cowlitz River, Lewis Co, WA. Flow forms a broad bench in valley from Coyote Creek to near mouth of Clear Fork, a distance of 8 mi. Composed of very fine textured dacite. Long slender columnar joints, are exposed where flow has been eroded by Clear Fork River. Shown on geologic sketch map of White Pass region. Overlies Ohanapecosh Formation and Russell Ranch Formation. Age is Quaternary.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Shown on geologic strip sketch map from White Pass to La Grande. Described as light gray dacite, splintery to platy jointed, well developed downward tapering and subdividing columns over 60 m tall. Erupted from vent on east flank of Coal Creek Mountain. Is 75 m thick. Age is <40,000(?) and >20,000(?) yr B.P.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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