Fig. 11From: Washover deposits related to tsunami and storm surge along the north coast of the Shimokita Peninsula in northern JapanLateral correlation of tsunami deposits (TD1–TD5) between coastal outcrops and SKN-GS cores. A–A′ and B–B′ profile lines are shown in Fig. 1c. Vertical exaggeration is 25X. Sketches of SKN-E, SKN-W, and SKN-GS are from Figs. 2, 4, and 5, respectively. Sandy event deposits in orange in SKN-E and SKN-W indicate candidate tsunami deposits, showing relatively strong wave currents among the sandy event deposits in the outcropsBack to article page