Named for exposures at Sitkin Point, Little Sitkin Island, Rat Islands group, Aleutian Islands, AK. Shown on geologic map of Little Sitkin Island. Composed of waterlaid pyroclastic material, tuffaceous graywacke, dacite-boulder tuff-breccia, andesitic tuff, and pumiceous tuff. Is more than 450 ft thick. Unconformably overlies Williwaw Cove formation (new); unconformably underlies Double Point dacite (new). Is probably early Quaternary age based on stratigraphic relations.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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