Tephrochronological age estimate of the Nakauchi Landslide in western Tokushima Prefecture, southwest Japan
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概要
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The Nakauchi Landslide is a large-scale collapse-generated landslide in western Tokushima Prefecture, southwest Japan. A slide block deposit is composed of angular granitic huge boulders with minor proportion of sedimentary rocks . The slide block is not overlain by the Aira-Tanzawa Tephra, but by the Kikai-Akahoya Tephra, suggesting that the landslide occurred primarily between 26, 000-29, 000 and 7, 300 cal. BP. Average incision rate of a tributary of the Naka River after the occurrence of landslide is estimated to 0.9-3.4mm/yr.
- 公益社団法人 日本地すべり学会の論文
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