Movement history of Tsukinokawachi-landslide caused by heavy rainfall associate with Typhoon 0514, Miyazaki, Japan
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- NISHIYAMA Ken-ichi
- Institute of Socio-Arts and Sciences, Univ. Tokushima
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- KITAMURA Shin-ichi
- NEWJEC Inc
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- NAGAOKA Shinji
- Faculty of Education, Nagasaki Univ.
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- SUZUKI Keizo
- Minamikyushu Univ.
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- TAKAYA Seiji
- Minamikyushu Univ.
Bibliographic Information
- Other Title
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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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Abstract
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.
Journal
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- Journal of the Japan Landslide Society
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Journal of the Japan Landslide Society 48 (1), 39-44, 2011
The Japan Landslide Society
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Details 詳細情報について
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- CRID
- 1390001205201940736
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- NII Article ID
- 10027884594
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- NII Book ID
- AA11837172
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- ISSN
- 18820034
- 13483986
- http://id.crossref.org/issn/13483986
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- NDL BIB ID
- 10995298
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- Text Lang
- ja
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed
