抄録
Fluvial terraces distributing extensively along the Hidakahorobetsu and Motoura Rivers in
southern Hidaka, Hokkaido were investigated by the tephrochronological and geomorphological
method to reveal their formative periods and processes. Based on the data obtained and on
the river profile sreconstructed from terrace surfaces and the present river-bed, the change in
the river response to sea-level and climatic change during the Late Quaternary was discussed,
focusing on the period from 20 to 60 kyr.B.P.