http://news.yahoo.com/s/time/20100113/wl_time/08599195328400Haiti Earthquake Was the 'Big One' Says Top Seismologist
By EBEN HARRELL / LONDON 7 mins ago
The British Geological Survey in Edinburgh has been one of the leading geoscience research centers in the world since its founding in 1835. To understand more about the 7.0-magnitude earthquake that devastated Haiti on Tuesday, TIME spoke with one of the survey's seismologists, Roger Musson, about the science behind the seismic event.
What sort of earthquake was this?
An earthquake is the sudden release of energy along a fault line in the earth's crust as rocks break in response to stress. There are three types, and they depend on the sort of movement along the fault. This was what we call a strike-slip, or transform, earthquake, where one side of the fault slides horizontally past the other one.(See pictures of the devastating earthquake in Haiti.)
Which fault produced this earthquake?
It is rather baroquely called the Enriquillo-Plaintain Garden fault. It is a major plate boundary fault and is analogous to the San Andreas fault in California. It starts around the southern border between Haiti and the Dominican Republic and runs west until it reaches Jamaica.
Was it the most destructive type of earthquake?
A thrust earthquake, in which one side of the fault goes up, is the type that produces truly enormous events like the Sumatra earthquake of 2004. But strike-slip faults often run through populated areas, so they can be the most damaging to humans.(Read "Haiti Death Toll May Be in the Thousands.")
People talk about waiting for the Big One in California. Was this a similar earthquake for this fault?
This was the Big One. The fault has been more or less locked for 200 years. Seismologists were unsure as to whether it would produce one Big One or several smaller ones. We seem to have the answer.
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