Movement history of Tsukinokawachi-landslide caused by heavy rainfall associate with Typhoon 0514, Miyazaki, Japan

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  • 2005年台風14号豪雨で発生した宮崎県槻之河内地すべりの活動履歴
  • 2005ネン タイフウ 14ゴウ ゴウウ デ ハッセイ シタ ミヤザキケン ツキノカワチ ジスベリ ノ カツドウ リレキ

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Many landslides and slope failures triggered by heavy rainfall associated with Typhoon 0514 occurred in Miyazaki, Japan. Tsukinokawachi-landslide is one of the huge landslides distributed in Wanitsuka Mountains formed landslide dam due to 2005heavy rainfall. The slide block of Tsukinokawachi-landslide is overlain by several marker tephra layers such as AT (29cal ka) , K-Ah (7. 3cal ka) and Kr-M (4. 6cal ka) , but not by A-Fm (31cal ka) , A-Iw (45-50ka) and A-Fk (90ka) . These occurrences of tephra layers suggest that former movement of Tsukinokawachi-landslide occurred between 31 and 29 cal ka.

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