Tsunami Behavior Estimated from Damage to Utility Poles
Author:
Affiliation:
1. Department of Geography, Graduate School of Environmental Studies, Nagoya University
2. Toyohashi City Office
3. Konan City Office
Publisher
Tokyo Geographical Society
Subject
Materials Chemistry
Link
https://www.jstage.jst.go.jp/article/jgeography/124/2/124_124.227/_pdf
Reference23 articles.
1. Abe, T., Goto, K. and Sugawara, D. (2012): Relationship between the maximum extent of tsunami sand and the inundation limit of the 2011 Tohoku-oki tsunami on the Sendai Plain, Japan. Sedimentary Geology, 282, 142-150.
2. Goto, K., Hashimoto, K., Sugawara, D., Yanagisawa, H. and Abe, T. (2014): Spatial thickness variability of the 2011 Tohoku-oki tsunami deposits along the coastline of Sendai Bay. Marine Geology, 358, 38-48.
3. Koarai, M., Okatani, T., Nakano, T. and Kamiya, I. (2011): Geographic characteristics of tsunami flooded area by the Great East Japan Earthquake. Journal of the Geospatial Information Authority of Japan, 122, 97-111.
4. Geospatial Information Authority of Japan (2011): 1:25,000 tsunami flood area overview map.*http://www.gsi.go.jp/kikaku/kikaku40014.html [Cited 2013/01/30].
5. Matsumoto, H. (1981): Sea-level changes during the Holocene and geomorphic development of the Sendai Coastal Plain, northeast Japan. Geographical Review of Japan, 54, 72-85.
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1. Understanding the damage situation of social infrastructures and geographical characteristics in the tsunami anticipated inundation area of the great earthquake along the Nankai Trough etc.;Reports of the City Planning Institute of Japan;2018-06-08
2. Preface for the Special Issue on “Geographical Investigation on the 2011 Great East Japan Earthquake Disaster, Focusing on the Regional Diversity of Tsunamis and Geo-hazards”;Journal of Geography (Chigaku Zasshi);2015
3. Overview of Special Issue: “Geographical Investigation on the 2011 Great East Japan Earthquake Disaster, Focusing on the Regional Diversity of Tsunamis and Geo-hazards”;Journal of Geography (Chigaku Zasshi);2015
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