1891 Mino-Owari earthquake

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The Neodani Faultline. The shift in the ground can be seen in the steep ledging through the center of the picture.
The Neodani Faultline. The shift in the ground can be seen in the steep ledging through the center of the picture.

The Mino-Owari Earthquake (美濃尾張地震 Mino Owari Jishin?) was a large earthquake that struck the former provinces of Mino and Owari in the Nōbi Plain area during the Meiji period in Japan. It is also referred to as the Nōbi Earthquake (濃尾地震 Nōbi Jishin) or the Great Nōbi Earthquake (濃尾大地震 Nōbi Daijishin).

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[edit] History

The earthquake struck on October 28, 1891, at 6:38am. Based on the scale of destruction, it has since been estimated to have had a magnitude of 8.0 on the Richter Scale.[1] Its epicenter is believed to have been the Neodani Faultline (35°35’N, 136°20’E), which is located in the present day city of Motosu, Gifu Prefecture. It is believed to be the largest earthquake that has ever occurred whose epicenter is beneath Japanese soil.[1] It is also one of the largest earthquakes in the world's history. When the fault line broke, the height difference between the two sides was approximately six meters.

[edit] Damage

Gifu's Earthquake Memorial Hall dedicated to the victims of the Mino-Owari Earthquake
Gifu's Earthquake Memorial Hall dedicated to the victims of the Mino-Owari Earthquake

Aichi and Gifu prefectures suffered extensive damage. Damage also occurred in the neighboring Shiga and Fukui prefectures. According to records, there were approximately 7,273 deaths and 17,175 casualties, as well as complete destruction of over 140,000 homes. On mountains near the quake's epicenter, all of the trees were knocked down, leaving what is called a "bald mountain." In the city of Gifu and the surrounding areas, fires broke out, causing even more damage. The first newspaper reports described this complete destruction of Gifu by saying that "Gifu has disappeared." Many important structures in Gifu, including Kanō Tenman-gū and Zenkō-ji, were greatly damaged in the resulting fires.

Though the walls of Nagoya Castle and surrounding lodgings from the Edo period were not damaged, modern buildings that were built with Western architectural knowledge subsequently collapsed. The Nagaragawa Iron Bridge and other structures, including brick structures, etc., that were not earthquake-resistant were destroyed. It is because of this earthquake that interest in creating earthquake resistant structures greatly increased.[2]

[edit] Earthquake preparation and remembrance

In Gifu Prefecture, October 28 has been declared "Prefectural Earthquake Disaster Prevention Day" to help residents prepare for earthquakes. Additionally, on the 28th of every month, there is a Buddhist memorial service for all of the earthquake's victims at the Earthquake Memorial Hall.[3]

[edit] Further reading

Gregory Clancey. Earthquake Nation: The Cultural Politics of Japanese Seismicity (Berkeley, Calif.: California University Press, 2006)

[edit] References

  1. ^ a b Mino Earthquake. (Japanese) Tokyo Science Museum. Accessed July 5, 2007.
  2. ^ Gregory Clancey. Earthquake Nation: The Cultural Politics of Japanese Seismicity (Berkeley, Calif.: California University Press, 2006)
  3. ^ Gifu City Walking Map. Gifu Lively City Public Corporation, 2007.

Coordinates: 35°35′″N, 136°20′″E

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