[{"@context":"http:\/\/schema.org\/","@type":"BlogPosting","@id":"https:\/\/wiki.edu.vn\/en\/wiki10\/1982-urakawa-earthquake-wikipedia\/#BlogPosting","mainEntityOfPage":"https:\/\/wiki.edu.vn\/en\/wiki10\/1982-urakawa-earthquake-wikipedia\/","headline":"1982 Urakawa earthquake – Wikipedia","name":"1982 Urakawa earthquake – Wikipedia","description":"before-content-x4 From Wikipedia, the free encyclopedia after-content-x4 The 1982 Urakawa earthquake (Japanese: \u6d66\u6cb3\u6c96\u5730\u9707[6]) was a 6.9 earthquake that struck off","datePublished":"2021-06-04","dateModified":"2021-06-04","author":{"@type":"Person","@id":"https:\/\/wiki.edu.vn\/en\/wiki10\/author\/lordneo\/#Person","name":"lordneo","url":"https:\/\/wiki.edu.vn\/en\/wiki10\/author\/lordneo\/","image":{"@type":"ImageObject","@id":"https:\/\/secure.gravatar.com\/avatar\/c9645c498c9701c88b89b8537773dd7c?s=96&d=mm&r=g","url":"https:\/\/secure.gravatar.com\/avatar\/c9645c498c9701c88b89b8537773dd7c?s=96&d=mm&r=g","height":96,"width":96}},"publisher":{"@type":"Organization","name":"Enzyklop\u00e4die","logo":{"@type":"ImageObject","@id":"https:\/\/wiki.edu.vn\/wiki4\/wp-content\/uploads\/2023\/08\/download.jpg","url":"https:\/\/wiki.edu.vn\/wiki4\/wp-content\/uploads\/2023\/08\/download.jpg","width":600,"height":60}},"image":{"@type":"ImageObject","@id":"https:\/\/en.wikipedia.org\/wiki\/Special:CentralAutoLogin\/start?type=1x1","url":"https:\/\/en.wikipedia.org\/wiki\/Special:CentralAutoLogin\/start?type=1x1","height":"1","width":"1"},"url":"https:\/\/wiki.edu.vn\/en\/wiki10\/1982-urakawa-earthquake-wikipedia\/","wordCount":2636,"articleBody":" (adsbygoogle = window.adsbygoogle || []).push({});before-content-x4From Wikipedia, the free encyclopedia (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4The 1982 Urakawa earthquake (Japanese: \u6d66\u6cb3\u6c96\u5730\u9707[6]) was a 6.9 earthquake that struck off the coast of Urakawa, Japan on 11:32 (JST), March 21, 1982.[7][8] The epicenter was 42\u00b006\u2032N 142\u00b036\u2032E\ufeff \/ \ufeff42.1\u00b0N 142.6\u00b0E\ufeff \/ 42.1; 142.6Coordinates: 42\u00b006\u2032N 142\u00b036\u2032E\ufeff \/ \ufeff42.1\u00b0N 142.6\u00b0E\ufeff \/ 42.1; 142.6.[10] The earthquake was the largest earthquake in the history of the region. The earthquake caused 167 injuries and damage in Tomakomai and Sapporo.[11][12] (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4Table of ContentsTectonic setting[edit]Earthquake[edit]Tsunami[edit]References[edit]External links[edit]Tectonic setting[edit]Hokkaido is situated on the Okhotsk Plate in between two main zones of seismicity. To the west, there is a convergent plate boundary with the Amurian Plate. To the east, there exists a subduction zone where the Pacific Plate subducts underneath the Okhotsk. This is accommodated by slip along the Kuril-Kamchatka Trench and the Japan Trench. This earthquake struck as the result of thrust faulting in an area of compression known as the Hidaka Collision Zone. The same tectonic process, caused by the collision between the Eurasian Plate and the Kuril fore-arc uplifts the Hidaka Mountains.Earthquake[edit]At 2:32 UTC or 11:32 local time on the 21st of March, a large earthquake struck off the shore of southern Hokkaido. The 6.9 earthquake caused shaking that reached a maximum Japan Meteorological Agency seismic intensity scale Shindo of 6- and a Modified Mercalli intensity (MMI) of X (Extreme). The event struck at a depth of 44.0\u00a0km (27.3\u00a0mi), and ruptured along the Hidaka Collision Zone. Inferred rupture dimensions were 12\u00a0km (7.5\u00a0mi) by 22\u00a0km (14\u00a0mi) with an average slip of 2.5\u00a0m (8\u00a0ft 2\u00a0in). Aftershocks covered an area of 35\u00a0km (22\u00a0mi) by 25\u00a0km (16\u00a0mi).Tsunami[edit]Teletsunami observations[16]LocationRecorded height (m)Urakawa, Japan1.3Ayukawa, Japan0.6Hachinohe, Japan0.6Shoya, Japan0.3Kuji, Japan0.3Kamaishi, Japan0.2Kushiro, Japan0.2Tsunami from the earthquake was observed around Hokkaido, with varying run-up heights.[16] Urakawa had the highest run-ups with waves reaching up to 1.3\u00a0m (4\u00a0ft 3\u00a0in) high and going up to 3\u00a0m (9.8\u00a0ft) inland.[16] The observations at Hachinohe and Hiroo were much higher than models predicted, however this may be due to the models not taking into account more local topography that could influence wave heights. (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4References[edit]SourcesArita, Kazunori; Ikawa, Takashi; Ito, Tanio; Yamamoto, Akihiko; Saito, Matsuhiko; Nisihida, Yasunori; Satoh, Hideyuki; Kimura, Gaku; Watanabe, Teruo; Ikawa, Takeshi; Kurodo, Toru (1998). “Crustal structure and tectonics of the Hidaka Collision Zone, Hokkaido (Japan), revealed by vibroseis seismic reflection and gravity surveys”. Tectonophysics. 290 (3\u20134): 197\u2013210. Bibcode:1998Tectp.290..197A. doi:10.1016\/S0040-1951(98)00018-3. Retrieved 30 October 2022.Iwasaki, Takaya; Hirata, Naoshi; Suyehiro, Kiyoshi; Kanazawa, Toshihiko; Urabe, Taku; Moriya, Takeo; Shimamura, Hideki (1983). “Aftershock distribution of the 1982 Urakawa-Oki earthquake determined by ocean bottom seismographic and land observations”. Journal of Physics of the Earth. 31 (5): 299\u2013328. doi:10.4294\/jpe1952.31.299. S2CID\u00a0129929201. Retrieved 30 October 2022.Murai, Yoshio; Akiyama, Satoshi; Katsumata, Kei; Takanami, Tetsuo; Yamashina, Tadashi; Watanabe, Tomoki; Cho, Ikuo; Tanaka, Masayuki; Kuwano, Asako; Wada, Naoto; Shimamura, Hideki; Furuya, Itsuo; Zhao, Dapeng; Sanda, Ryohei (14 May 2003). “Delamination structure imaged in the source area of the 1982 Urakawa-oki earthquake”. Geophysical Research Letters. 30 (9): 1490. Bibcode:2003GeoRL..30.1490M. doi:10.1029\/2002GL016459. hdl:2115\/17236. ISSN\u00a00094-8276. S2CID\u00a053499509. Retrieved 30 October 2022.Seno, Tetsuzo; Sakurai, Taro; Stein, Seth (1996). “Can the Okhotsk Plate be discriminated from the North American plate?”. Journal of Geophysical Research: Solid Earth. 101 (B5): 11305\u201311315. Bibcode:1996JGR…10111305S. doi:10.1029\/96JB00532.Suetsugu, Daisuke; Nakanishi, Ichiro (1988). “Re-examination of fault model for the 1982 Urakawa-oki earthquake by analyses of seismic, geodetic, and Tsunami data”. Journal of Physics of the Earth. 36 (2): 53\u201367. doi:10.4294\/jpe1952.36.53. Retrieved 30 October 2022.Zhou, Dapeng; Huang, Zhouchuan; Umino, Norihito; Hasegawa, Akira; Yoshida, Takeyoshi (September 2011). “Seismic imaging of the Amur\u2013Okhotsk plate boundary zone in the Japan Sea”. Physics of the Earth and Planetary Interiors. 188 (1\u20132): 82\u201395. Bibcode:2011PEPI..188…82Z. doi:10.1016\/j.pepi.2011.06.013. Retrieved 30 October 2022.External links[edit]\u2020 indicates earthquake resulting in at least 30 deaths\u2021 indicates the deadliest earthquake of the year (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4"},{"@context":"http:\/\/schema.org\/","@type":"BreadcrumbList","itemListElement":[{"@type":"ListItem","position":1,"item":{"@id":"https:\/\/wiki.edu.vn\/en\/wiki10\/#breadcrumbitem","name":"Enzyklop\u00e4die"}},{"@type":"ListItem","position":2,"item":{"@id":"https:\/\/wiki.edu.vn\/en\/wiki10\/1982-urakawa-earthquake-wikipedia\/#breadcrumbitem","name":"1982 Urakawa earthquake – Wikipedia"}}]}]