The Hietsu earthquake (飛越地震, Hietsu jishin) was a doublet earthquake that took place on April 9, 1858 (according to the old Japanese calendar, February 26, Ansei 5). earthquakes today - recent and latest earthquakes, earthquake map and earthquake information. Especially the catastrophic Tombi Landslide (Tombi-Kuzure) in the Tateyama Caldera, the upstream of the Joganji River, was the largest in the earthquake. Publish_Country=Japan. Microearthquake hypocentre distribution from 1998 January to 2003 October (Ito et al. The 1995 Great Hanshin Earthquake was M7.3 and a maximum of shindo 7, while the 2011 Great East Japan Earthquake was M8.4 and also recorded a maximum of shindo 7. stated in. Journal/Book_names=Report of the Coordinating Committee for Earthquake Prediction. Published: Jun 17, 2010 Publish_year=1985. Ikeya et al. The 1858 Hietsu earthquake, a large inland earthquake (M 7), occurred along the fault. Hietsu Earthquake of April 9, 1858 and the Atotsugawa Fault. It occurred on the Atotsugawa Fault, which connects the Amō Pass in Gifu Prefecture (in the part that was called Hida Province) and Mount Tate in Toyama Prefecture (then known as Etchū Province) on the island of Honshū in Japan. We suggest that the high-velocity body imaged at the western section is an asperity that ruptured in the 1858 Hietsu Earthquake. Identifiers. The 1896 Sanriku earthquake (明治三陸地震, Meiji Sanriku Jishin) was one of the most destructive seismic events in Japanese history. The Atotsugawa fault is one of the most prominent active faults in Japan that caused the 1858 M7.0 Hietsu Earthquake, and is located in the Niigata-Kobe Tectonic Zone (NKTZ) which is a high strain-rate belt identified from GNSS observations. Eventualaj ŝanĝoj en la angla originalo estos kaptitaj per regulaj retradukoj. volume=21. Journal. Sitelinks. 1858 Hietsu earthquake intensity.png 512 × 512; 39 KB. The collapsed mountain body blocked the Joganji River and formed landslide dams. Features of the 1858 Ansei Hietsu Earthquake The Ansei Hietsu Earthquake occurred on mid-night on 9 April 1858. The Hietsu earthquake on April 9, 1858, caused numerous sediment disasters along the Atotsugawa fault system, some of the sediment movements built up landslide dams dams Subject Category: Infrastructure see more details. In 1858 A.D., a big earthquake, named Hietsu Earthquake, with a magnitude 7.0–7.1 occurred along the Atotsugawa Fault (AGF) in the moun-tainous area between Hida Highland and coastal plains around Toyama Bay [e.g. Journal/Book_names=Report of the Coordinating Committee for Earthquake Prediction. Se vi volas enigi tiun artikolon en la originalan Esperanto-Vikipedion, vi povas uzi nian specialan redakt-interfacon. pages=115-119. These dams broke twice during heavy rainfalls in April and in June. On April 9, 1858, a large, magnitude-7.1 earthquake occurred with its epicenter on the Atotsugawa fault, which spans the prefectures of Toyama and Gifu. 319 houses were destroyed and 203 people were killed by … enwiki 1858 Hietsu earthquake; frwiki Séisme de 1858 de Hietsu; Publish_year=1979. Publisher=Geographical Survey … Earth, Planets and Space – Springer Journals. 1858 Hietsu Earthquake In April 1858, a large earthquake of shindo 6 struck the area. Authors=USAMI Tatsuo. Earthquake Research Institute, University of Tokyo. On February 26th (April 9th on the Gregorian Calendar), 1858, a great earthquake with an estimated magnitude of around 7 struck the Hietsu Region. publication date. Talk:1858 Hietsu earthquake. The Hietsu earthquake took place on April 9, 1858 (according to the old Japanese calendar, February 26, Ansei 5). After the occurrence of the 1995 Kobe earthquake, it has been widely recognized that direct measurements in fault zones by drilling. Due to the cumulative effects of these disasters, the reign name was changed in 1860 to usher in a 'clean slate' and better "fortune". 1858 Hietsu earthquake. For the current exhibition, we selected five historical earthquakes to present.The Zenkoji Quake and the 1858 Hietsu Quake represent typical inland earthquakes.The exhibition also presents detailed distributions of seismic intensity in the Edo-Tokyo area for the 1703 Genroku Quake, the 1855 Ansei-Edo Quake, and the 1923 Great Kanto Quake. 2(a), and notable lateral heterogeneous facts along the Atotsugawa fault are summarized in Table 1. volume=33. Most earthquake hypocenters are distributed at the periphery of the high‐velocity bodies. 1 reference. The 1998 Ryukyu Islands earthquake (石垣島南方沖地震, Ishigakijima nanpō-oki jishin) occurred on May 4, 1998, at 08:30 local time (UTC+9) (on May 3 at 23:30 UTC) in the Philippine Sea region with M w 7.5 (USGS) and M7.7 (JMA). The Hietsu Earthquake, with an estimated magnitude of 7.0–7.1, was the last activity on the fault that occurred in 1858 (Research Group of Atotsugawa Fault, 1989). "The Hietsu Earthquake of April 9, 1858 and the Omachi Earthquake of April 23, 1858" (PDF) (in Japanese). 01858-04-09April 9, 1858: 7.0-7.1: Hietsu earthquake: 飛越地震: Hietsu Jishin: Atotsugawa Fault: 000200200–300: 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. Language_of_Text=JA. The crater of Mount Tate-yama was collapsed by the Hietsu earthquake of (M7.0-7.1) in 1858. Text is available under the CC BY-SA 4.0 license; additional terms may apply. This earthquake with a shallow epicenter right below the region was caused by the active Atozugawa Fault running to the west of the Tateyama mountain range. 2. The Hietsu Earthquake of April 9, 1858 and the Omachi Earthquake of April 23, 1858. We present a hypothesis that the extensional stress is caused locally in a transition zone from the fluid-rich aseismic creep zone to the seismogenic zone that is interpreted as an asperity ruptured by the 1858 Hietsu Earthquake (M = 7.0).
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