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Alaska-Aleutian megathrust : ウィキペディア英語版
Alaska-Aleutian megathrust

The Alaska-Aleutian megathrust is a thrust fault that runs for 3,600 km from near Kamchatka in the west to the Gulf of Alaska in the east.
The Alaska-Aleutian megathust system forms the interface between the subducting Pacific Plate and the overriding North American Plate.
Movement on this megathrust plate system has been responsible for several great historical earthquakes including the M 9.2 1964 Alaska earthquake, M 8.7 1965 Rat Islands earthquake and the M 8.6 1957 Andreanof Islands earthquake, each of them triggering large tsunamis.
== References ==

*Earthquake Hazards Program: http://earthquake.usgs.gov/hazards/products/ak/1999/documentation/


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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