1833 Shōnai earthquake

Coordinates: 38°54′N 139°15′E / 38.9°N 139.25°E / 38.9; 139.25
Source: Wikipedia, the free encyclopedia.
1833 Shōnai earthquake
Local dateDecember 7, 1833 (1833-12-07)
Local time15:00–16:00 JST
Magnitude7.5–7.7 MJMA
Epicenter38°54′N 139°15′E / 38.9°N 139.25°E / 38.9; 139.25[1]
Max. intensityJMA 6+
TsunamiYes
Casualties150 dead

The Shōnai offshore earthquake (Japanese: 庄内沖地震, Hepburn: Shōnai-oki Jishin) occurred at around 14:00 on December 7, 1833. It struck with an epicenter in the Sea of Japan, off the coast of Yamagata Prefecture, Japan. A tsunami was triggered by the estimated MJMA  7.5–7.7 earthquake. One hundred and fifty people were killed and there was severe damage in the prefecture.

Tectonic setting

Main article: Eastern margin of the Sea of Japan

Japan is situated on a

Amurian Plates. Along the island arc's east and southeast coast, subduction of the Pacific and Philippine Sea Plates occur at the Japan Trench and Nankai Trough, respectively. The west coast of Honshu, bordering the Sea of Japan, is a north–south trending convergent boundary.[2] This boundary between the Amurian and Okhotsk Plates is thought to be an incipient subduction zone, consisting of eastward-dipping thrust faults.[3] Convergent tectonics have been occurring in the region since the end of the Pliocene.[4] Earthquakes and tsunamis are produced on thrust faults that form the boundary, with magnitudes in the range of 6.8–7.9. Major earthquakes and tsunamis along this boundary occurred in 1741, 1940, 1964, 1983 and 1993, although the origin of the 1741 tsunami remains open to debate.[5]

Earthquake

The earthquake ruptured the convergent boundary faults of the eastern margin of the Sea of Japan. The rupture zone partially overlaps that of the 1964 earthquake which struck in the same area, although parts of the rupture area extended north. The earthquake had an estimated JMA magnitude (MJMA ) of 7.5–7.7,[6] similar to the 1964 earthquake, while the tsunami magnitude (Mt ) was 8.1. The JMA magnitude was calculated based on the seismic intensities recorded during the earthquake.[7] A seismic gap exist between the rupture areas of the 1833 and 1983 earthquakes, which is capable of generating a magnitude 7.5 earthquake.[3]

Tsunami

The Shōnai coast which was inundated by the 1833 tsunami.

Although its seismic magnitude was estimated to be similar to the 1964 earthquake, it generated taller tsunami waves. It is thought to be one of the largest tsunami in the Sea of Japan. The tsunami reached a height of 7–8 m (23–26 ft) at Kamomoya, Yamagata Prefecture, believed to be close to the earthquake source. Large waves were reported along a 30–50 km (19–31 mi) stretch of coastline. In Kisakata (Akita) and Ajigasawa (Aomori), waves 4–5 m (13–16 ft) struck. The tsunami measured 1–3 m (3 ft 3 in – 9 ft 10 in) in Izumozaki, Niigata. A tall wave measuring 5.3 m (17 ft) washed onto Wajima, Ishikawa. Waves exceeding 5 m (16 ft) was reported from Kamo (8 m (26 ft)) to Fuya (7 m (23 ft)).[7] Waves were described as "strong" in Tsuruoka. It traveled 2.5 km (1.6 mi) upstream.[8] At Sakaiminato, Tottori, the tsunami measured 2.3 m (7 ft 7 in).[9]

Impact

A total of 150 fatalities resulted.

JMA seismic intensity 6 was estimated in an area measuring 80 km (50 mi) in length from Niigata to Yamagata prefectures.[12] Seismic intensity 5 extended 250 km (160 mi) from Niigata to Akita to the Yamagata basin along the Mogami River. Shaking resulted in the partial destruction of Tsuruoka, Oyama, Makisone, Yosida, Okushinden, and Hironoshinden. Generally, damage in the region in proportion to the number of buildings was not great. The greatest damage was reported along the coast. Liquefaction was observed at Matsugasaki, Sado.[13]

See also

References

  1. ^ "日本付近のおもな被害地震年代表" [Japan Historical Earthquakes Representative]. Seismological Society of Japan. Retrieved 20 June 2022.
  2. S2CID 221463717
    .
  3. ^
    S2CID 73567424
    .
  4. doi:10.1016/0040-1951(85)90047-2
    . Retrieved 20 June 2022.
  5. S2CID 55372867
    .
  6. ^
    doi:10.4294/zisin1948.43.2_227
    .
  7. ^
    doi:10.5575/geosoc.2017.0054
    .
  8. ^ Yata, Toshifumi (2014). "一八三三年庄内沖地震における越後の津波到達点と水死者数". 災害・復興と資料. 4: 27–31.
  9. ^ Tsuji, Yoshinobu; Moriya, Takumi; Haga, Yayoi; Imai, Kentaro; Matsuoka, Yuya; Imamura, Fumihiko; Iwase, Hiroyuki; Sato, Masami (2017). "天保四年(1833)出羽沖地震津波の隠岐諸島,および島根半島での津波高" [Heights of the Tsunami of the Tenpo Dewa-Oki Earthquake of December 7th, 1833 on the Coasts of Oki Archipelago and Shimane Peninsula] (PDF). Research Report of Tsunami Engineering (in Japanese). 33: 333–356.
  10. ^ National Geophysical Data Center / World Data Service (NGDC/WDS), Global Historical Tsunami Database (Data Set), NOAA National Centers for Environmental Information
  11. ^ Hatori, Tokutaro (2012). "新潟県〜石川県沿岸の津波累積エネルギー分布" [Distribution of Cumulative Tsunami Energy along the Niigata to Ishikawa Coasts, the Japan Sea] (PDF). Historical Earthquake (in Japanese). 27.
  12. ISBN 978-4-13-060742-1
    .
  13. doi:10.7289/V5TD9V7K
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