This map shows the March 11, 2011, magnitude-9.0 earthquake off Tohoku and 166 aftershocks of magnitude 5.5 and greater until May 20. Warmer color indicates more recent events. Larger symbol indicates greater quake magnitude.
updated 6/22/2011 5:34:57 PM ET 2011-06-22T21:34:57

Seismic monitoring and centuries of experience have given humankind a pretty good idea of what areas are prone to the devastation of earthquakes and tsunamis. But to truly prepare for huge temblors and accompanying tsunamis like the one that ravaged Japan in March, we need to take a closer look at the deep seafloor, according to one geophysicist.

Writing in the journal Nature this week, Georgia Institute of Technology earthquake researcher Andrew Newman argues for an international effort to monitor the deep seafloor for signs of "locked patches" on faults, where two creeping masses of land catch against one another, storing energy until they break, unleashing an earthquake. These monitoring efforts wouldn't predict exactly when earthquakes would happen, but they would help us gauge how large an impending disaster might be, Newman said.

"Essentially, what we need to start being able to do is identify exactly how the offshore environment is really locking up for earthquakes," Newman told LiveScience. "We can see a little bit of that by using data that's just on land. But (we) just don't have the resolution offshore that we need."

Watching the trench
The size of Japan's March 11 quake surprised scientists, who hadn't expected that area of the Japan Trench to generate a magnitude-9.0 temblor. In retrospect, California Institute of Technology geophysicist Hiroo Kanamori told LiveScience's sister site,, in April that GPS monitors along the Japan trench did show signs that large amounts of strain were building along the fault. But for a rare event like the 9.0-magnitude quake, Kanamori said, scientists do not have enough data to assess the hazards.

And Japan is one of the best performers in terms of the number of seismic monitors on the deep seafloor, Newman said.

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Land-based seismic monitoring can capture what's happening on the seafloor out to a distance of about 12 to 24 miles, Newman said. But faults can rupture 125 miles offshore in deep ocean trenches, where monitors are rare. Besides Japan, Newman said, only offshore Peru has significant seafloor monitoring.

With better monitoring, he wrote, scientists can make more accurate predictions about how big an earthquake and ensuing tsunami might be. In Japan's case, for example, the walls around the Fukushima nuclear plant might have been built higher, preventing a nuclear disaster second only to Chernobyl.

Cutting the cost
Monitoring the deep seafloor isn't a simple prospect, however. Right now, ships place transponders on the seafloor and then read the signals, triangulating the transponders' position and any movement since the last check. Just one position check can cost $500,000, Newman wrote, and many data points over time are necessary to determine what a fault is doing.

To expand the undersea seismic network, Newman said, researchers need to develop autonomous sensor systems that will send information back to shore via undersea cables or buoys, negating the need for ships. In the Japan Trench, Newman wrote, another 100 to 400 sensors are needed. For larger networks, scientists could deploy a sensor every 3,100 to 9,300 miles, he said.

Seismic monitoring isn't cheap: The land-based network monitoring the plate boundary along the U.S. West Coast cost $100 million to install and $10 million to maintain each year. But with technological advances, Newman wrote, it should be possible to equip an environment like the Japan Trench with a seismic network for between $5 million and $20 million — a paltry sum compared with the projected $300 billion cost of the Japan disaster.

"It's ambitious," Newman said. "But I don't think it's out of the realm of possibility."

You can follow LiveScience senior writer Stephanie Pappas on Twitter @sipappas. Follow LiveScience for the latest in science news and discoveries on Twitter @livescience and on Facebook.

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