The 1498 Nankai earthquake (æ å¿ å °é MeiÅ Jishin) occurred off the coast of NankaidÅ , Japan, at about 08:00 local time on 20 September 1498. The AD 1498 Meio earthquake (M8.2∼8.4) that occurred along the eastern Nankai trough, and the tsunami generated by the earthquake, induced major geomorphological and social changes along the Pacific coast of central Japan. Many historic earthquakes have the name "Nankai" or "Nankaido".Major earthquakes are named with the Japanese era name and the location such as Nankaido.. Timeline. The 1498 Nankai earthquake (明応地震 Meiō Jishin) occurred off the coast of Nankaidō, Japan, at about 08:00 local time on 20 September 1498. Listen to the audio pronunciation of 1498 Nankai earthquake on pronouncekiwi. Talk:1498 Nankai earthquake. It had a magnitude estimated at 8.6 M S and triggered a large tsunami. The 1605 Nankai earthquake occurred at about 20:00 local time on 3 February. Jumlah korban tewas yang terkait dengan peristiwa ini tidak pasti, namun antara 26.000 dan 31.000 korban dilaporkan. The death toll associated with this event is uncertain, but between 26,000 and 31,000 casualties were reported. On Sept. 20, 1498, an 8.6-magnitude earthquake occurred near the Nankai Trough, which runs parallel to the southern coast of Honshu, and triggered a powerful tsunami that hit the coast of Meio Nankai, Japan. is a city in Kanagawa Prefecture, Japan. tured the subduction interface: in 684, 887, 1096, 1361, 1498, 1605, 1707, 1854 (twice), 1944 and 1946 CE. 1854 Ansei Nankai earthquake intensity.PNG 512 × 512; 47 KB. 1498 Meio earthquake intensity.png 512 × 512; 37 KB. 1854 Ansei Tokai earthquake intensity.png 512 × 512; 49 KB. The uplift of the Udo Hill was probably caused by co‐seismic movement during the late Pleistocene accompanying large subduction zone earthquakes in the Nankai‐Suruga trough. Both events were great earthquakes of magnitude 8.4. Along a three hundred-mile long fault line known as the Nankai Trough, stretching from south of the Island of Kyushu to Kii-Hanto in the Island of Honshu, there is a long history of major earthquakes. Previous studies considered that the descriptions in historical documents were erroneously copied from a great earthquake along Nankai Trough in 1498, but the recent historical studies indicate that the documents are reliable. It had a magnitude estimated at 8.6 M S and triggered a large tsunami. Large earthquake intervals of 1–2.5 centuries have been estimated during the past thirteen centuries in the Nankai‐Suruga trough [Sugiyama , 1994]. Tokai Earthquake History . It had a magnitude estimated at 8.6 M S and triggered a large tsunami. 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). It had a magnitude estimated at 8.6 M s and triggered a large tsunami.The death toll associated with this event is uncertain, but between 5,000 and 41,000 casualties were reported. Thank you for helping build the largest language community on the internet. WikiProject Earthquakes (Rated C-class, High-importance) This article is part of WikiProject Earthquakes, a project to systematically present information on earthquakes, seismology, plate tectonics, and related subjects. It had an estimated magnitude of 7.9 on the surface wave magnitude scale and triggered a devastating tsunami that resulted in thousands of deaths in the Nankai and Tōkai regions of Japan.It is uncertain whether there were two separate earthquakes separated by a short time interval or a single event. Along the Nankai-Suruga trough, great interplate earthquakes (M>8) have recurred historically, and the occurrence of another great earthquake can be expected in the near future. The epicenter was 260 km (162 mi) from Ishigaki Island, Japan, 400 km (249 mi) from Basco, Philippines, and 425 km (264 mi) from Hualian, Taiwan. 1946 Nankai Earthquake (10).jpg 1,023 × 780; … The Nankai Trough was frequently hit in the past by powerful earthquakes. The Tokai segment last ruptured in 1854, and before that in 1707. The 887 CE earthquake likely represents a full-length rupture of the Tokai and Nankai segments, as was the case for the 1707 CE earthquake. Ise Bay Japan magnitude 8.2. Enshunada Sea, Japan - September 20, 1498 magnitude 8.3, total of at least 31,000 people killed. See more » Kamakura. 1498 Nankai earthquake: part our commitment to scholarly and academic excellence, all articles receive editorial review.|||... World Heritage Encyclopedia, the aggregation of the largest online encyclopedias available, and the most definitive collection ever assembled. 1707Hoei earthquake intensity.png 512 × 512; 45 KB. Great earthquakes along the Nankai-Suruga trough also generate large tsunamis in the western Pacific Ocean and East China Sea. Sign in to disable ALL ads. 1944 Tonankai earthquake intensity.png 512 × 512; 48 KB. The 56-foot-high waves came ashore and killed an estimated 31,000 people. Earthquake. The 1605 Nankai earthquake occurred at about 20:00 local time on 3 February. The death toll associated with this event is uncertain, but between 26,000 and 31,000 casualties were reported. Kekuatannya diperkirakan pada 8,6 M S dan memicu sebuah tsunami besar. Some geological features, such as the undersea Nankai Trough, have been named for the region.. Nankaidō earthquakes. The segment ruptured in comparable events in 1605 and in 1498. The 1498 Nankai earthquake (明応地震 Meiō Jishin) occurred off the coast of Nankaidō, Japan, at about 08:00 local time on 20 September 1498. Philippine Sea Plate - Japan Meteorological Agency seismic intensity scale - 1923 Great Kantō earthquake - 869 Sanriku earthquake - 1293 Kamakura earthquake - 1605 Nankai earthquake - 1498 Nankai earthquake - 1611 Sanriku earthquake - 1792 Unzen earthquake and tsunami - 1703 Genroku earthquake - 2003 Hokkaidō earthquake - 2011 Tōhoku earthquake and tsunami - 1707 Hōei earthquake … Eventualaj ŝanĝoj en la angla originalo estos kaptitaj per regulaj retradukoj. Il est ressenti un peu partout dans les régions du centre et de l'ouest du pays. Of these, the sec-ond earthquake of 1854 and the 1946 rupture only incorporated slip in the western Nankai region, with the first 1854 earthquake and the 1944 rupture restricted to … The 1498 Nankai earthquake (明応地震 Meiō Jishin) occurred off the coast of Nankaidō, Japan, at about 08:00 local time on 20 September 1498. 1498 Nankai earthquake magnitude 8.6 MS[1] Areas affected Japan Casualties 5,000 deaths[2] Sep 20, 1498. The Ise Bay tsunamis caused more than 8000 deaths Nov 1, 1755. Language; Watch; Edit; Active discussions. Meiō Nankaidō (1498) Keichō Nankaidō (1605) Ansei-Nankai (1854) Tōnankai (1944) Nankaido (南海地震)) (1946), séisme de magnitude 8,4 à 4:19 [heure locale]. The objective of this research is to study the role of a tsunami, generated by the 1498 Meio earthquake (M8.2 - 8.4) along the eastern Nankai on the geomorphological evolution of the Hamana river floodplain, located along the Pacific coastline of Central Japan (Shizuoka prefecture). Nov 1, 1755. La ĉi-suba teksto estas aŭtomata traduko de la artikolo 1498 Nankai earthquake article en la angla Vikipedio, farita per la sistemo GramTrans on 2015-12-18 06:54:22. Synonym of 1498 meio nankaido earthquake: English Wikipedia - The Free Encyclopedia 1498 Nankai earthquake The 1498 Nankai earthquake (明応地震 Meiō Jishin) occurred off the coast of Nankaidō, Japan, at about 08:00 local time on 20 September 1498. The 1498 Nankai earthquake (明応地震 Meiō Jishin) occurred off the coast of Nankaidō, Japan, at about 08:00 local time on 20 September 1498. The Nankai Trough is a convergent boundary where the Philippine Sea Plate is being subducted beneath the Eurasian Plate.Large earthquakes have been recorded along this zone since the 7th century, with a recurrence time of 100 to 200 years. How do you say 1498 Nankai earthquake? 1946 Nankai Earthquake (1).jpg 800 × 1,130; 237 KB. The long-term implications of the study hinge on evidence that the pre-existing faults from the 1944 earthquake have strongly influenced the orientation and location of rupturing during the 2016 event, suggesting that large earthquakes in Japan are most likely to occur in this very same region of the Nankai Trough in the future. Gempa bumi Nankai 1498 (明応地震 Meiō Jishin) terjadi di lepas pantai Nankaidō, Jepang, pada sekitar pukul 08.00 waktu setempat tanggal 20 September 1498. It had an estimated magnitude of 7.9 on the surface wave magnitude scale and triggered a devastating tsunami that resulted in thousands of deaths in the Nankai and Tōkai regions of Japan.It is uncertain whether there were two separate earthquakes separated by a short time interval or a single event. Integrated with the previous studies, these new results show that nine Tokai earthquakes occurred over the last 1300 years, the oldest in the latest 7th century, and in 887, 1096, 1361, 1498, 1614, 1707, 1854 and 1944 CE. Tremblement de terre catastrophique sur le sud-ouest du Japon dans la zone de Nankai. The wave hit the Japanese coast at Meiō Nankai, killing 31,000 people. It had a magnitude estimated at 8.6 MS and triggered a large tsunami. Se vi volas enigi tiun artikolon en la originalan Esperanto-Vikipedion, vi povas uzi nian specialan redakt-interfacon. Jan 18, 1586. It had a magnitude estimated at 8.6 and triggered a large tsunami.The death toll associated with this event is uncertain, but between 5,000 and 41,000 casualties were reported. The 1498 Nankai earthquake (明応地震 Meiō Jishin) occurred off the coast of Nankaidō, Japan, at about 08:00 local time on 20 September 1498. The entire wiki with photo and video galleries for each article ), né le 1 er août 1944 est une personnalité japonais du domaine des sciences de la Terre.Ayant bénéficié d'une formation de géologue et sismologue au Japon puis aux États-Unis, il a vécu et travaillé sur des zones sismiques actives, dont à Kobé et au Japon qui, selon Ishibashi, vit une « Ère de convulsion souterraine ». The Earthquake Research Committee announced in May 2013 that the chance of a quake of magnitude 8 or more happening in the Nankai Trough within 30 … Katsuhiko Ishibashi (石橋 克彦, Ishibashi Katsuhiko? 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