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In the 1498 event, the earthquake is thought to have ruptured segments C, D and E and possibly A and B. If both parts of the megathrust ruptured, the events were either simultaneous, or close enough in time, to not be distinguished by historical sources.
Aug 24, 2022 · Similarly, the 1498 Meio Tokai earthquake may have been an unpaired event because the occurrence of a 1498 Meio Nankai earthquake is doubtful (e.g., Ishibashi 1998). The average recurrence interval of historical great earthquakes along the Nankai Trough was almost twice as long before the 1361 Shohei (Koan) earthquake as after it (Fig. 1 ), but ...
In the 1498 event, the earthquake is thought to have ruptured segments C, D and E and possibly A and B. If both parts of the megathrust ruptured, the events were either simultaneous, or close enough in time, to not be distinguished by historical sources. +
Oct 28, 2010 · It sits near where several continental and oceanic plates meet in the Pacific Ocean, and in 1498 those plates shifted. The resultant 8.6-magnitude earthquake triggered a 56-foot-high wave,...
Oct 2, 2013 · Earthquakes rupturing the eastern segment are known as Tokai or Tonankai earthquakes and those rupturing the western segment are known as Nankai earthquakes (Usami, 2003). Since the 15th century, a total of seven earthquakes have occurred, very close in time or simultaneously, along the two rupture zones.
- Osamu Fujiwara, Eisuke Ono, Toshifumi Yata, Masatomo Umitsu, Yoshiki Sato, Vanessa M.A. Heyvaert
- 2013
In the 1498 event, the earthquake is thought to have ruptured segments C, D and E and possibly A and B. If both parts of the megathrust ruptured, the events were either simultaneous, or close enough in time, to not be distinguished by historical sources.
In the 1498 event, the earthquake is thought to have ruptured segments C, D and E and possibly A and B. If both parts of the megathrust ruptured, the events were either simultaneous, or close enough in time, to not be distinguished by historical sources.
