Titlebook: Applied Geomorphology for Mitigation of Natural Hazards; Masahiko Oya Book 2001 Springer Science+Business Media Dordrecht 2001 Earthquake.

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Relationships Between Geomorphic Units and Flood Types of River Basins,Japan’s most striking landform is its mountainous region, which includes some plains and intermontane depressions. The Hida, Kiso and Akaishi mountains, respectively called the Northern Japan Alps, Central Japan Alps and Southern Japan Alps, are found in central Honshu. These mountains are high and are surrounded by steep slopes (.).

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Flooding in Semi-Frigid Zones,Hokkaido, Japan’s northernmost main island, is situated between 41°N to 46°N and its climate is marked as Df in the Köppen classification (.). Its rivers have different characteristics from those in Japan’s other main islands of Honshu, Shikoku and Kyushu, which are classified as Cf.

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Differences in Geomorphology and Flooding Between the Left and Right Banks of Rivers Along the MediSituated in the Circum Pacific Orogenic Belt, the Japanese archipelago has significant crustal movement.

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,Estimation of Land Collapse in Japan’s Mountainous and Volcanic Regions,Japan’s mountainous regions (.) were formed by upheaval and plains by depression. . shows the vertical displacement of Japan during the Quaternary Period. Regions were thrust upward, particularly on the island of Honshu.

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Flood Control in Tokyo, Osaka and Nagoya, diluvial terraces and dissected small valleys in the terraces. The diluvial upland has been free from flooding, with the exception of the flood caused by the Kano River Typhoon in 1958. However, the alluvial plains have been inundated numerous times.

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