| Project/Area Number |
23540531
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| Research Category |
Grant-in-Aid for Scientific Research (C)
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| Allocation Type | Multi-year Fund |
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| Section | 一般 |
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| Research Field |
Geology
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| Research Institution | Gifu University |
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Principal Investigator |
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| Co-Investigator(Renkei-kenkyūsha) |
SUZUKI Kazuhiro 名古屋大学, 年代測定総合研究センター, 教授 (90111624)
NAKAMURA Toshio 名古屋大学, 年代測定総合研究センター, 教授 (10135387)
KANEDA Heitaro 千葉大学, 理学研究科, 准教授 (30415658)
OHTANI Tomoyuki 岐阜大学, 工学部, 准教授 (20356645)
KATSUTA Nagayoshi 岐阜大学, 教育学部, 准教授 (70377985)
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| Project Period (FY) |
2011 – 2013
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| Project Status |
Completed (Fiscal Year 2013)
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| Budget Amount *help |
¥5,070,000 (Direct Cost: ¥3,900,000、Indirect Cost: ¥1,170,000)
Fiscal Year 2013: ¥390,000 (Direct Cost: ¥300,000、Indirect Cost: ¥90,000)
Fiscal Year 2012: ¥2,210,000 (Direct Cost: ¥1,700,000、Indirect Cost: ¥510,000)
Fiscal Year 2011: ¥2,470,000 (Direct Cost: ¥1,900,000、Indirect Cost: ¥570,000)
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| Keywords | 地すべり / せき止め湖 / 山体重力変形地形 / 地震 / 豪雨 / 紀伊半島 / 越美山系 |
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| Research Abstract |
Kiritani and Koinami villages in Yatsuo town, Toyama city, are located on the flat basins; they were originally dammed-lakes formed by large landslides. The ages of landslides were estimated by 14C ages of wood fragments embedded in the lake sediments and landslide debris, and they indicate that the landslides were triggered by the earthquake, probably the penultimate activity of the Atotsugawa fault. The sackungen in the Etsumi mountains along the Gifu-Fukui prefecture boundary were formed in the warm climate during or after the last glacial prediod. The dammed-lake sediments and the sackungen-basin sediments in the eastern Kii Peninsula recorded events interpreted as earthquakes and heavy rainfalls.
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