Named for Tugidak Island, AK. Type section designated as exposures along west coast of Tugidak Island, 25 km southwest of Kodiak Island. Is only bedrock unit underlying Tugidak Island; also occurs at north end of Chirikof Island. Consists of interbedded sandstone and siltstone. A 1-m-thick cobble-conglomerate bed occurs about 350 m above base. Thickness at type is approximately 1500 m. On Chirikof Island unit is in fault contact with older rocks; conformably underlies unnamed Pleistocene rocks. Marine fossils identified by F.S. MacNeil (written commun., 1963) are Pliocene age. Age of unit is Pliocene.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Age changed from Pliocene to: late Pliocene and early Pleistocene based on age of fossils.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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