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Scientists used a supercomputer-driven "virtual earthquake" to explore likely ground shaking in a magnitude 9.0 megathrust earthquake in the Pacific Northwest. Peak ground velocities are displayed in yellow and red. The legend represents speed in meters per second (m/s) with red equaling 2.3 m/s. Although the largest ground motions occur offshore near the fault and decrease eastward, sedimentary basins lying beneath some cities amplify the shaking in Seattle, Tacoma, Olympia, and Vancouver, increasing the risk of damage. (Credit: Kim Olsen, SDSU)

EWA BEACH (HawaiiNewsNow) – Scientists say there are parallels between recent earthquakes and ground movement in the Pacific Northwest and what happened in Japan before last year’s devastating quake and tsunami.

The research was discussed over the weekend at the annual meeting of the American Association for the Advancement of Science. Scientists at the Pacific Tsunami Warning Center in Ewa Beach are well aware of the new research.

The disaster in Japan occurred because of stress from the Pacific tectonic plate sliding below Japan. The plates locked together, slowly pushing Japan westward, and then released, resulting in the magnitude 9.0 earthquake and tsunami that killed thousands. Japan moved about ten to 15 feet eastward in the quake.

Scientists said the same thing is now in the works off the coast of British Columbia, Washington and Oregon, as the Juan de Fuca plate moves beneath the Pacific Northwest.

“The Pacific Northwest is being deformed because the plates are locked together, and the shoreline is sinking and the rest of the thing is being bent. We can see that,” said Dr. Gerard Fryer, a geophysicist with the warning center. “It’s just like Japan, only a mirror image.”

According to Fryer, the last big earthquake in the Pacific Northwest happened in January 1700. Like the Japan quake, it also was a magnitude 9.0, and sent a destructive Pacific wide tsunami that reached Japan.

While there has been more ground movement in the northwest, there’s still the question of Read more…