Underwater Earthquakes

Topics: Plate tectonics, Earthquake, Transform fault Pages: 4 (1085 words) Published: February 28, 2011
David Kelleher
Geophysicists Discover Slippery Secret Of Weaker
Underwater Earthquakes


In December 2004, an underwater earthquake triggered a string of tsunamis along the Indian Ocean with devastating effects. Now, scientists have found ways nature is preventing some deep ocean earthquakes and save lives. Strong underwater earthquakes start off silent -- until their tsunami waves roar on shore, destroying property and lives. But now, geophysicists and oceanographers have found a break in studying sea floor faults. Faults aren't one continuous line. Instead, they are broken up into sections and the edges of the faults are full of cracks as the earth's crust on both sides of the fault slides past each other. "Large scale earthquakes don't occur on the sea faults," explains Patricia Gregg, graduate student from M.I.T. and Woods Hole Oceanographic Institution Joint Program in Oceanography in Woods Hole, Mass. Molten rock -- or magma -- from under-sea volcanoes lubricates the fault, reducing the amount of friction that could cause another earthquake. By analyzing data collected by sea vessels, they discovered volcanic activity may be weakening fault lines. The hot rock could be serving as a geological lubricant, making the fault line more malleable. Less friction means less of a quake. "So, the scale of the earthquake is smaller because the volcanism warms up the fault line and makes it more difficult to break rocks," Gregg says. "Our ultimate purpose is to forecast earthquakes on land because earthquakes cause so much damage and kill so many people," says Jian Lin, Ph.D., senior scientist in the Department of Geology & Geophysics at Woods Hole Oceanographic Institution. By understanding what happens below the Earth's surface, geophysicists are hoping to be able to send a warning to those above-ground. The researchers say it is easier to study fault lines below sea level. They are simple...
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