Alaska Science Forum

May 9, 1977

 


Seaquakes
Article #164

by T. Neil Davis


This column is provided as a public service by the Geophysical Institute, University of Alaska Fairbanks, in cooperation with the UAF research community. T. Neil Davis is a seismologist at the institute.

What is an earthquake like at sea? Almost universally, reports by people on ships tell of having thought that the ship had run aground. Rumbling, grating sensations and horrifying rattling of ship superstructures are reported. The noises often appear to come mainly from the bottom of the ship, and there is fear that the ship is breaking up.

Evidently, strong earthquake waves traveling below the ocean floor start compressional wave trains (like sound waves in air) that travel upward through the water at a steep angle. Striking the ship bottom, these waves apparently cause no real damage to the ship.

Much more to be feared by seamen traveling near a shore are the giant tsunami waves generated by nearby or distant earthquakes. In 185S, while traveling near Peru, the unfortunate captian of the U. S. gunboat Wateree was forced to abandon ship after a tsunami deposited his vessel on its flat bottom, two miles inland.



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