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Kantō earthquakes : ウィキペディア英語版 | Kantō earthquakes A is a megathrust earthquake occurring in the Kantō region of Japan that originate from slippage in the Sagami Trough. Kantō earthquakes are thought to occur with a 200-year return period. Only two earthquakes in the Kantō region are thought to be megathrust earthquakes: * 1923 Great Kantō earthquake; most common usage * 1703 Genroku earthquake Other earthquakes in the Kantō region, which may or may not be due to slippage in the Sagami Trough: *The ''Ruijū Kokushi'' mentions an earthquake that struck the area in 818 * 1855 Edo earthquake ==See also==
*Earthquakes in Japan * *Tōkai earthquakes * *Nankai megathrust earthquakes * *Seismicity of the Sanriku coast
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Kantō earthquakes」の詳細全文を読む
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