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Japanese 19c Earthquakes

The Ansei Great Earthquakes (Ansei no Dai Jishin) were a series of three major earthquakes that struck Japan during the Ansei era (1854-1860).
The Ansei Tōkai Quake (Ansei Tōkai Jishin) was an 8.4 magnitude earthquake which struck on December 23, 1854. The epicenter ranged from Suruga Bay to the deep ocean, and struck primarily in the Tōkai region, but destroyed houses as far away as in Edo. The accompanying tsunami caused damage along the entire coast from the Bōsō Peninsula in modern-day Chiba prefecture to Tosa province (modern-day Kōchi prefecture).
The Ansei Nankai Quake (Ansei Nankai Jishin) was an 8.4 magnitude earthquake which struck on December 24, 1854. Over 10,000 people from the Tōkai region down to Kyushu were killed.
The Ansei Edo Quake (Ansei Edo Jishin) was a 6.9 magnitude earthquake which struck Edo (modern-day Tokyo) on November 11, 1855. One hundred and twenty earthquakes and tremors in total were felt in Edo in 1854-55. The great earthquake struck after 10 o'clock in the evening; roughly 30 aftershocks continued until dawn. The epicenter was near the mouth of the Arakawa River. Records from the time indicate 6,641 deaths inside the city, and 2,759 injuries; much of the city was destroyed by fire, leading many people to stay in rural inns. Aftershocks continued for twenty days. This quake was a particularly destructive deep thrust quake caused by a giant slab of rock stuck between the Philippine Plate and Pacific Plates.
The Sumida River (Sumida-gawa) is a river which flows through Tokyo, Japan. It branches from the Arakawa River at Iwabuchi and flows into Tokyo Bay. Its tributaries include the Kanda and Shakujii rivers.
What is now known as the "Sumida River" was previously the path of the Arakawa, however towards the end of the Meiji era work was carried out to divert the main flow of the Arakawa to prevent flooding.
The 1858 Hietsu earthquake (Hietsu jishin) took place on April 9, 1858 (according to the old Japanese calendar, Ansei 5-2-26). It occurred on the Atotsugawa Fault, which connects Mount Tate in Toyama Prefecture and the Amō Pass in Gifu Prefecture on the island of Honshū in Japan. Its name includes one kanji from Hida and one from Etchū, the names of the provinces that were in use at the time. The earthquake is estimated to have killed 200–300 people. It also caused the Mount Tonbi Landslide and blocked the upper reaches of the Jōganji River.
The 1894 Meiji Tokyo earthquake (Meiji-Tokyo jishin) was an earthquake which occurred in Tokyo, Japan at 1404 PM on June 20, 1894. It affected downtown Tokyo and neighboring Kanagawa prefecture, especially the cities of Kawasaki and Yokohama. The Meiji Tokyo earthquake had its epicenter in Tokyo Bay, with a magnitude of 6.6 on the Richter Scale. The depth of the 1894 earthquake has not been determined, but it is thought to have occurred within the subducting Pacific Plate under the Kantō region. The death toll was 31 killed and 157 injured.
The Mino-Owari Earthquake (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 (Nōbi Jishin) or the Great Nōbi Earthquake (Nōbi Daijishin).

(Source Wikipedia)