At base, thick deposits are stratified debris flow. Clasts seem to be monolithologic, and strification seems to be cause by coarse and fine clast banding. Deposit > 100 m. Rotten, old monolithologic (?) debris flow, clasts are sub-angular scoria. Held together by moss. Sample has 1 chunk of coarse, 1 chunk of fine breccia.
Volcanism on Unimak Island, Alaska, USA: a special focus on Shishaldin and Fisher volcanoes
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