731-748 Tokyo Metropolitan Government. May 2011.
The Great Kanto earthquake was caused by the Kanto faultline which runs south of the city of Tokyo, where the Philippine plate and the Honshu Plate meet.
Hammer, Joshua.
. About 140,000 people fell victim to this earthquake and the fires caused by it. Dai-ichi Sogo building (right) and Maruzen (left), at Kyobashi, c. 1920. The photographs presented in this special online exhibition were taken by August Kengelbacher.They are a courtesy of Peter Kengelbacher. 75 years ago, on 1 September 1923, one of the worst earthquakes in world history hit the Kanto plain and destroyed Tokyo, Yokohama and the surroundings. Sources Referenced.
The Kanda Ogawamachi business district, c. 1920.
Extensive firestorms and even a fire tornado added to the death toll. Anthropological Quarterly 76.4 (Fall 2003). Manseibashi Station, c. 1910.
The 1923 Great Kantō earthquake caused widespread destruction in Chiba Prefecture, most notably in the southernmost part of the Bōsō Peninsula, where 1,300 residents were killed.
In some areas this may have caused the population to become complacent about safety issues, but as Japan is in such a tectonically unstable area they are in a constant state of readiness.
The Great Kantō earthquake (関東大地震, Kantō dai-jishin) struck the Kantō Plain on the main Japanese island of Honshū at 11:58:44 JST (02:58:44 UTC) on Saturday, September 1, 1923.Varied accounts indicate the duration of the earthquake was between four and ten minutes. "The Great Kanto Earthquake and the Massacre of Koreans in 1923: Notes on Japan's Modern National Sovereignty." View of Tokyo after the 1923 Kanto Earthquake and the destruction it caused. Kanda Ogawamachi, after the Great Kanto earthquake, 1923.
The epicenter of the 1923 Great Kanto earthquake was deep beneath Izu Ōshima Island in Sagami Bay.
Shimbashi Station, gutted in the aftermath of the 1923 Great Kanto earthquake. Artist rendition of the great fires that accompanied the Kanto earthquake and the chaos they caused. Manseibashi Station, after the earthquake, 1923.
Its epicentre was situated in the Sagami Bay, 80km south of Tokyo. Previous to the Kanto earthquake of 1923 Tokyo had not been hit since 1853. The Kanto earthquake measured 8.2 on the Richter Scale.
Movements associated with these two tectonic plates triggered the 8.2 magnitude approximate Genroku Earthquake of 1703 and the 7.9 magnitude approximate Great Kantō Earthquake of 1923. “The Great Japan Earthquake of 1923.” Smithsonian.
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