琉球列島,伊良部島および下地島における完新世"高海水準"地形の再検討〔英文〕

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概要

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• The slightly emerged shore platforms fringing Shimoji Island do not correspond to a higher Holocene sea-level stand, as believed previously, but to differential erosion caused by strong wave action (tsunamis, typhoons). As in the nearby Miyako Island, the sea level reached its present position some 1, 000 to 2, 000 years ago in Shimoji and Irabu Islands, and has remained almost stable since that time. No evidence of higher Holocene sea-level stands can be found.

著者

• 河名 俊男

  Department of Geography, College of Education, University of the Ryukyus

• Pirazzoli Paolo

  CNRS-URA 141, Laboratoire de Gégraphie Physique

関連論文

• 琉球列島,伊良部島および下地島における完新世"高海水準"地形の再検討〔英文〕

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