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The main reasons for the formation of sediments excess in the coastal zone have been considered to explain the aeolian accumulation of soil close transfer on different types of shores. The grounds are presented for division of a new type of aeolian morpholithogenesis on volcanic shores associated with a large amount of pyroclastic material entering to the wave processing zone during explosive eruptions in the Middle – Late Holocene. It has been established that the age of such dunes correlates with the age of deposits of volcanic pumice and tephra, but it is not concern to well-known periods of high or low sea level.

A new type of aeolian morphogenesis on volcanic shores (Iturup Island, Great Kuril Ridge)