Finding fault -- From Sendai to the San Andreas.
I'm Bob Karson with the discovery files -- new advances in science and engineering from the National Science Foundation.
The magnitude 8.9 Japan earthquake and destructive tsunami cause many to be concerned about whether similar events could occur on our own west coast. Research led by the University of Texas at Austin following the Haiti quake is kind of a "sorta-good-news -- not-so-good-news" kind of thing. The sorta good news is that the San Andreas Fault is a "strike-slip" fault. The two plates are passing each other moving in opposite directions. The Sendai quake occurred on a subduction fault -- one plate riding under the other.
Traditionally, tsunami risk is considered to be higher in these subduction areas because they displace huge amounts of water when they rupture.
Which brings us to the not-so-good-news for the U.S. the research team found that you do not need a large quake to produce a large wake. In strike-slip areas like those around the San Andreas Fault, large tsunamis can occur through "submarine landslides." Sediment slides along the seafloor and displaces the water above it.
The team conducted geological surveys on and off shore around the epicenter of the Haitian earthquake. They found that tsunamis around Haiti are about 10 times more likely to be generated by submarine landslides than previously thought. Meaning higher risk of destructive tsunamis in places near strike-slip faults -- like Kingston, Istanbul, and Los Angeles.
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