Abstract
There are two marine terraces at the northern part of the western coast of Hunka Bay, Hokkaido. The upper terrace deposits have the sediments of sand dune, peat and clay, and they deposited at the same geological time. The sediments of the present coast of Hunka Bay are also sand dune, peat and clay. By the comparison of the terrace and present deposits, the writer considered that the marine terrace deposits were perhaps sedimented under the same circumstance as the present.
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