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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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