1700 Cascadia tsunami
(courtesy of Kenji Satake).
This computer-generated image shows the tsunami produced by the great Cascadia earthquake of January 26, 1700, six hours after initiation. The tsunami moved across the Pacific Ocean and produced destructive waves up to several metres high along a 1000-km length of the coast of Honshu in Japan. Much larger waves struck the west coast of North America less than 30 minutes after the shaking stopped. Deposits of this tsunami are preserved in tidal marshes and low-elevation coastal lakes on the Pacific coast. Their distribution provides information on the wave run-up that can be expected from future Cascadia tsunamis.
Hot Springs Cove after the 1964 Alaska tsunami
The tsunami caused $10 million damage (1964 dollars) to coastal communities on Vancouver Island. Port Alberni was hardest hit, but Hot
Springs Cove, Tofino, Ucluelet, and Zeballos also suffered damage. The photo shows the remnants of the village of Hot Springs Cove shortly
after the tsunami struck in the early morning hours of March 28, 1964. Geological traces of much larger tsunamis produced by earthquakes at
the Cascadia subduction zone are preserved in tidal marshes and low-lying coastal lakes on western Vancouver Island. Study of these
deposits provides insights into tsunami hazards and risk on the British Columbia coast. (photo by Charles Ford).
Tsunami sand beneath tidal marsh at Tofino, BC
A layer of clean sand is sharply bounded by peat and mud in a pit dug at a marsh just east of Tofino on the west coast of Vancouver Island. The sand occurs as a sheet that thins and fines landward and contains marine microfossils. It was deposited by a landward surge of seawater at the time of the last great earthquake at the Cascadia subduction zone in A.D. 1700. (photo by John Clague).
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