Four Holocene wave-cut benches uplifted by subduction earthquakes and historical tsunami gravel beds around Koseda coast, northeastern Yakushima Island: A preliminary report.

Shojiro Nakagawa; Hiroyuki Sasaki; Masamichi Omote; Futoshi Nanayama; Nobuo Geshi; Kazuaki Watanabe; HIdeto Naruo; Fukashi Maeno; Tetsuo Kobayashi

doi:10.14863/geosocabst.2014.0_387

The 121st Annual Meeting(2014' Kagoshima)

Session ID : T9-P-2

DOI https://doi.org/10.14863/geosocabst.2014.0_387

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Host: The Geological Society of Japan

T9. Quaternary basin research

Four Holocene wave-cut benches uplifted by subduction earthquakes and historical tsunami gravel beds around Koseda coast, northeastern Yakushima Island: A preliminary report.

*Shojiro Nakagawa, Hiroyuki Sasaki, Masamichi Omote, Futoshi Nanayama, Nobuo Geshi, Kazuaki Watanabe, HIdeto Naruo, Fukashi Maeno, Tetsuo Kobayashi

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Keywords: Yakushima, koseda-seashore, Holocene, wave-cut bench, historical tsunami, tsunami trace

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