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This paper proposes a observable criteria for identifying gravelly paleotsunami deposits, based on the apparent features of the gravelly deposits of 2011 Tohoku-oki tsunami observed in Sanriku coast area. Compared to other gravelly coast deposits observed in the same area, the gravelly 2011 tsunami deposits distribute far more discretely and rarely form thick gravel deposits on the slopes. Therefore thick gravel layers in sediments might not be the paleotsunami deposits, they might be the paleo coast deposits. However, in case some gravel within thick gravel layers are found in horizon and continue to wide area along to the same horizon, it should be taken into consideration that such gravel layer might be the combination zone of the paleo coast deposits and tsunami deposits.

Proposal on observable Criteria for identifying gravelly Paleotsunami Deposits