Evaluation of Tsunami Disasters Caused by the 1923 Great Kanto Earthquake

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY Journal of Disaster Research Pub Date : 2023-09-01 DOI:10.20965/jdr.2023.p0578
Hiroyuki Kaneko
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Abstract

The 1923 Great Kanto Earthquake is one of the earthquakes that have occurred multiple times in the past as part of the Sagami Trough earthquakes. These earthquakes, which occurred at the plate boundary, occurred in 1495 (Meio Earthquake), 1703 (Genroku Earthquake), and again in 1923, causing significant damage to various areas in Kanto, including Tokyo and Yokohama, and it came to be known as the Great Kanto Earthquake. The Sagami Trough earthquakes have consistently brought strong tsunami disasters to various areas in Kanto, extending from the Sagami Bay coast to the Boso Peninsula, and residents along the coast were highly aware of the risk of tsunamis occurring after major earthquakes. Although a tsunami occurred in the Great Kanto Earthquake of 1923, it is believed to have had a wave height approximately half that of the tsunami in the Genroku Earthquake. However, this tsunami destroyed the livelihoods of villages and caused significant damage. In this study, we aim to reexamine historical records related to the tsunami in the Great Kanto Earthquake and objectively evaluate the actual situation of this tsunami disaster.
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1923年关东大地震海啸灾害评价
1923年关东大地震是相模海槽地震中多次发生的地震之一。这些发生在板块边界的地震分别发生在1495年(美奥大地震)、1703年(根室大地震)和1923年,对包括东京和横滨在内的关东地区造成了重大破坏,被称为关东大地震。相模海槽地震一直给关东地区带来强烈的海啸灾害,从相模湾海岸一直延伸到博索半岛,沿海居民高度意识到大地震后发生海啸的风险。尽管1923年关东大地震中发生了海啸,但据信其波高约为根罗库大地震海啸的一半。然而,这场海啸摧毁了村庄的生计,并造成了重大破坏。本研究旨在重新审视关东大地震海啸的相关历史记录,客观评价此次海啸灾害的实际情况。
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来源期刊
Journal of Disaster Research
Journal of Disaster Research GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.60
自引率
37.50%
发文量
113
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