Tsunami Generation and Coastal Arrival  
 

An earthquake underwater can create a tremendous sudden displacement of ocean water with a circular surge of energy much like a rock falling into a pond.

These outward spreading waves travel quickly when in open water.

 

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However, arriving at shallow coastal areas their speed slows and their height is magnified greatly by the upward sloping land beneath.

Just before a destructive tsunami wave hits, the water at a coastal area such as the depicted town recedes and exposes tidelands rarely if ever seen.

 
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Animations by Prof. Miho Aoki from the University of Alaska Fairbanks Art Department Program