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1810 Crete earthquake : ウィキペディア英語版 | 1810 Crete earthquake
The 1810 Crete earthquake occurred at 22:15 on 16 February. It caused great destruction in Heraklion, some damage from Malta to northern Egypt and was felt from central Italy to Syria. 2,000 fatalities were reported from Candia (Heraklion). ==Tectonic setting== The Hellenic arc is an arcuate tectonic feature related to the subduction of the African Plate beneath the Aegean Sea Plate. It is one of the most active seismic zones in western Eurasia and has a history of large earthquakes that also affect Egypt. Large earthquakes with epicenters near Crete and to the north of the island are typically intermediate depth events located at the subducting plate interface. Such events are often M>7, but due to their depths cause relatively little damage for their size, while being very widely felt.
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「1810 Crete earthquake」の詳細全文を読む
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