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Nankai megathrust earthquakes ( Japanese: 南海トラフ巨大地震, Hepburn: Nankai Torafu Kyodai Jishin) are great megathrust earthquakes that occur along the Nankai megathrust – the fault under the Nankai Trough – which forms the plate interface between the subducting Philippine Sea Plate and the overriding Amurian Plate (part of the Eurasian Plate ), which ...
The Nankai earthquakes ( 南海地震, Nankai jishin) are major megathrust earthquakes that affect the Nankaidō (Southern Sea Circuit) region of Japan, west of the Tōnankai region (Southeastern Sea) and Tōkai region (Eastern Sea), and are caused by ruptures in the Nankai zone of the Nankai megathrust, specifically segments A and/or B.
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What are Nankai megathrust earthquakes?
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The Nankai Trough (南海トラフ, Nankai Torafu, Southern Sea Trough) is a submarine trough located south of the Nankaidō region of Japan 's island of Honshu, extending approximately 900 km (559 mi) offshore. The underlying fault, the Nankai megathrust, is the source of the devastating Nankai megathrust earthquakes, while the ...
In Japan, the Nankai megathrust under the Nankai Trough is responsible for Nankai megathrust earthquakes and associated tsunamis. The largest megathrust event within the last 20 years was the magnitude 9.0–9.1 Tōhoku earthquake along the Japan Trench megathrust.
The Tōnankai earthquakes are major megathrust earthquakes that affect the Tōnankai region (Southeastern Sea) of Japan, between the Tōkai region (Eastern Sea) and Nankaidō (Southern Sea Circuit) region, and are caused by ruptures in the Tōnankai zone of the Nankai megathrust, specifically segments C and/or D.
Anticipated area of the Tokai Earthquake. Nankai, Tōnankai and Tōkai earthquake areas. The Tōkai earthquakes ( Japanese: 東海地震) are major earthquakes that have occurred regularly with a return period of 100 to 150 years in the Tōkai region of Japan. The Tōkai segment has been struck by earthquakes in 1498, 1605, 1707, and ...
The 1946 Nankai earthquake (昭和南海地震 Shōwa Nankai jishin) was a great earthquake in Nankaidō, Japan. It occurred on December 21, 1946, at 04:19 JST (December 20, 19:19 UTC). [1] The earthquake measured between 8.1 and 8.4 on the moment magnitude scale , and was felt from Northern Honshū to Kyūshū .
