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). Our results also suggest that tsunami size was different for each event. Both events were great earthquakes of magnitude 8.4. 20th » The 1498 Nankai earthquake generates a tsunami that washes away the building housing the statue of the Amitābha called Great Buddha at Kōtoku-in in Kamakura, Kanagawa, Japan; since then the Buddha has sat in the open air. Historical Events for September, 1498. The Tokai segment last ruptured in 1854, and before that in 1707. 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. 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. 1498 Meio Nankaido Earthquake and Tsunami: 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. It had a magnitude estimated at 8.6 M … one and a half millennia, 11 tsunamigenic great earthquakes rup-tured the subduction interface: in 684, 887, 1096, 1361, 1498, 1605, 1707, 1854 (twice), 1944 and 1946 CE. The pattern is pretty stark: a Tokai earthquake has happened about every 110 years, plus or minus 33 years. There are three historic earthquakes of M > 8, occurring in 1498, 1707, and 1854, each ruptured the entire Nankai‐Suruga subduction zone up to the eastern end of the Nankai‐Suruga trough for a length of >500 km [Sugiyama , 1994]. Tokai Earthquake History . 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 resultant 8.6-magnitude earthquake triggered a 56-foot-high wave, according to the US National Geophysical Data Center. 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 In addition, there exists no firm evidence of Nankai earthquake corresponding to the 1498 CE Meio Tokai earthquake . The segment ruptured in comparable events in 1605 and in 1498. The 56-foot-high waves came ashore and killed an estimated 31,000 people. 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. 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. Geological coring along the Kekuatannya diperkirakan pada 8,6 M S dan memicu sebuah tsunami besar. The wave hit the Japanese coast at Meiō Nankai… Jumlah korban tewas yang terkait dengan peristiwa ini tidak pasti, namun antara 26.000 dan 31.000 korban dilaporkan. In spite of the intensive investigations along long continuous excavation walls, no trace of the tsunami attributed to 1361 CE Tokai earthquake was found. 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