Type section designated along south shore of Cenotaph Island in Lituya Bay, [Mt Fairweather quad] southeastern AK. Consists of unfossiliferous unit about 1250 ft thick characterized by green, red, and purple andesitic volcanic breccia, tuff, and flows interbedded with tuffaceous siltstone, glauconitic sandstone, pebble-cobble conglomerate, and minor coal. Is probably continental and marine. Intertongues with and in part unconformably underlies Topsy Formation (new). Also unconformably underlies Yakataga Formation. Unconformably overlies pre-Tertiary rocks. Larger areas of Cenotaph Volcanics shown on map of Gulf of Alaska and unit in part shown undivided with Topsy Formation. Tentatively assigned post-early Oligocene(?) to pre-middle Miocene age.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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