Stay Curious

SIGN UP FOR OUR WEEKLY NEWSLETTER AND UNLOCK ONE MORE ARTICLE FOR FREE.

Sign Up

VIEW OUR Privacy Policy


Discover Magazine Logo

WANT MORE? KEEP READING FOR AS LOW AS $1.99!

Subscribe

ALREADY A SUBSCRIBER?

FIND MY SUBSCRIPTION
Advertisement

From the Archive: The Tsunami of 1700

Explore how the Cascadia Subduction Zone triggered the Japanese tsunami of 1700, revealing its potential for catastrophic earthquakes.

Newsletter

Sign up for our email newsletter for the latest science news

Sign Up

Editor’s note: This article originally appeared in the January 1996 Discover.

Around midnight on January 27, 1700, Japan’s Pacific coast had an unwelcome visitor. The wintry seas suddenly rose seven feet and more and stayed that way for many hours, washing through houses and flooding rice paddies up and down the coast. The ocean’s long heave was a tsunami—a wave triggered by a seafloor earthquake—but it was modest compared with others in the Japanese records, and the quake itself wasn’t felt in Japan. This past year Kenji Satake of the Geological Survey of Japan reported that he’d figured out why: the Japanese tsunami of 1700, he said, was but a faint signal from a giant earthquake that occurred ten hours earlier and 5,000 miles away in the Pacific Northwest. The farflung wave implies that the quake was one of the largest ever—a magnitude 9 event that must have rocked the ...

Stay Curious

JoinOur List

Sign up for our weekly science updates

View our Privacy Policy

SubscribeTo The Magazine

Save up to 40% off the cover price when you subscribe to Discover magazine.

Subscribe
Advertisement

0 Free Articles