Geologic Record of Middle-Late Holocene Paleo-tsunamis and Paleo-earthquakes on the Shizuoka Plain and Coastal Lowland of the Southern Izu Peninsula, Central Japan

Author:

KITAMURA Akihisa12,KOBAYASHI Konatsu1

Affiliation:

1. Center for Integrated Research and Education of Natural hazards, Shizuoka University

2. Institute of Geosciences, Shizuoka University

Publisher

Tokyo Geographical Society

Subject

Materials Chemistry

Reference44 articles.

1. Asai, D., Imamura, F., Shuto, N. and Takahashi, T. (1998): Wave height and sediment transport of tsunami caused by AD 1854 Ansei-Tokai Earthquake in Iruma, Izu Peninsula. Journal of Coastal Engineering, 45, 371-375.

2. Clark, K., Cochran, U. and Mazengarb, C. (2011): Holocene coastal evolution and evidence for paleotsunami from a tectonically stable region, Tasmania, Australia. Holocene, 21, 883-895.

3. Danbara, T. and Tsuchi, R. (1975): Crustal movements in the southern Izu Peninsula. Geoscience Reports of Shizuoka University, 1, 27-30.

4. Fujiwara, O., Masuda, F., Sakai, T., Okazaki, H., Saito, A. and Suzuki, T. (1996): Uplifting examined by the late Pleistocene beach deposits in the northern area of the Boso Peninsula, central Japan. Journal of the Sedimentological Society of Japan, 43, 39-46.

5. Fujiwara, O., Hirakawa, K., Kaneko, H., Sugiyama, H. and Takada, K. (2005): Event deposits discovered from the Usami Ruins in Northern Ito City, Shizuoka Prefecture. Program and Abstracts, Japan Association for Quaternary Research, 35, 32-33.

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