Tsunami Generation and Coastal Arrival

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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.

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.

Animations by Prof. Miho Aoki from the University of Alaska Fairbanks Art Department Program
Modified from: www.iris.edu/aed/ by A.Newman Wed Oct 31 14:51:38 EDT 2007