Overview
- Editors:
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Fumihiko Imamura
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Disaster Control Research Center, Tohoku University, Aoba, Sendai 980-88, Japan
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Kenji Satake
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Department of Geological Sciences, University of Michigan, Ann Arbor, USA
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Table of contents (27 chapters)
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- Kenji Satake, Fumihiko Imamura
Pages 373-379
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- F. Schindelé, D. Reymond, E. Gaucher, E. A. Okal
Pages 381-408
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- F. I. González, K. Satake, E. F. Boss, H. O. Mofjeld
Pages 409-426
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- D. J. Thomson, L. J. Lanzerotti, C. G. Maclennan, L. V. Medford
Pages 427-440
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- Masayuki Kikuchi, Hiroo Kanamori
Pages 441-453
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- Yoshinobu Tsuji, Hideo Matsutomi, Fumihiko Imamura, Minoru Takeo, Yoshiaki Kawata, Masafumi Matsuyama et al.
Pages 481-524
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- Shaozhong Shi, Alastair G. Dawson, David E. Smith
Pages 525-536
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- Dannie Hidayat, Jeffrey S. Barker, Kenji Satake
Pages 537-554
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- Fumihiko Imamura, Edison Gica, Tomoyuki Takahashi, Nobuo Shuto
Pages 555-568
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- Michael J. Briggs, Costas E. Synolakis, Gordon S. Harkins, Debra R. Green
Pages 569-593
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- Stefano Tinti, Cesare Vannini
Pages 595-619
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- Kuniaki Abe, Masami Okada
Pages 621-631
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- Jean M. Johnson, Yuichiro Tanioka, Kenji Satake, Larry J. Ruff
Pages 633-647
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- Toshihiko Shimamoto, Akito Tsutsumi, Eiko Kawamoto, Masahiro Miyawaki, Hiroshi Sato
Pages 665-691
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- Hiroshi Sato, Toshihiko Shimamoto, Akito Tsutsumi, Eiko Kawamoto
Pages 693-717
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- Yuichi Nishimura, Naomichi Miyaji
Pages 719-733
About this book
The 1993 Southwest Hokkaido Earthquake of Magnitude 7. 9 (July 12, 22: 17 JST) caused serious tsunami disasters in the southwestern part of Hokkaido, particularly on Okushiri Island (a tiny island off the southwest coast of Hokkaido with a population of about 4,500 at the time of earthquake). Of 230 casualties, including 28 missing, about 200 deaths are attributable to the tsunami. We have conducted detailed field surveys of tsunami disasters to learn lessons from this costly natural experiment for the future prevention of similar tsunami disasters. Our field work was conducted in four surveys totaling 39 days. During the first field survey (July 16 through July 21, 1994), we worked mostly on the estimation of the subsidence of Okushiri Island during the earthquake. Hence, our main work on tsunami disasters initiated from the second field survey (July 31 through Aug. 15, 1994). Several groups have conducted detailed surveys of the distribution of tsunami runup height as measured from the level of sea water (TsUJI et al. , 1 994a, b; MATSUTOMI and SHUTO, 1994; GOTO et al. , 1994). Such a precise runup height distribution is essential for characterizing tsunami, including its overall size. Indeed, the height distribution is the fundamental data for inferring earthquake source parameters through the simulation of tsunami generation (TAKAHASHI et al. , 1994; IMAMURA et al. , 1994; TSUJI et al. , 1994a; SATAKE and TANIOKA 1994; ABE, 1994; TANIOKA et al. , in review).
Editors and Affiliations
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Disaster Control Research Center, Tohoku University, Aoba, Sendai 980-88, Japan
Fumihiko Imamura
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Department of Geological Sciences, University of Michigan, Ann Arbor, USA
Kenji Satake