Giant shock rattles ideas about quake behaviour
http://www.nature.com/news/2011/110315/full/471274a.html"This earthquake is a lesson in humility," says Emile Okal, a geophysicist at Northwestern University in Evanston, Illinois, who studies great earthquakes and tsunamis. Few experts had thought that the seismic zone near Sendai, Japan, was capable of producing earthquakes anywhere near as powerful as the magnitude-9.0 shock on 11 March, the largest on record in Japan. Okal and his colleagues want to understand why the event was so much stronger than many people expected — and what it means for seismic risks in Japan and elsewhere around the globe.
The quake happened along a seam in the planet's surface where the Pacific Ocean floor is diving beneath the tectonic plate carrying northern Japan (see 'Collision zone'). That process of subduction triggers the largest earthquakes in the world, such as the magnitude-9.5 Chilean quake in 1960 and the magnitude-9.1 Sumatran quake in 2004. But geophysicists had thought that great subduction-zone earthquakes happened only where younger oceanic crust scrapes its way into the mantle. Older crust, which is cooler and denser, was thought to slide much more readily downward, triggering smaller quakes. And the ocean crust off the northeast part of Japan, having formed about 140 million years ago, is about as old as it can get.
The history of the Sendai region seemed to support that idea. "There has been seismicity but not really great-earthquake seismicity," says Hiroo Kanamori, a seismologist at the California Institute of Technology in Pasadena. In the past few centuries, the subduction zone off the coast of Sendai has generated earthquakes of up to magnitude 8 or so, but nothing as powerful as a 9, which releases 30 times more energy.
Given that history, seismologists in Japan did not consider great earthquakes to be a threat to the Sendai area. And although that region was one of Japan's best-prepared for tsunamis, the high sea walls along much of the coast were built to stop waves far smaller than the 13–15-metre-tall giants that battered the coastline, causing most of the damage and triggering a nuclear crisis.
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Beware the happy talk about the seismic vulnerability of California's San Onefre and Diablo Canyon nuclear plants...
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