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Earthquakes typically occur along fault lines, areas where two sections of the Earth's crust grind past each other. When decades or centuries of accumulated stress become too great at a fault boundary, the land gives way, causing an earthquake. The first sign that the Enriquillo fault might not be to blame in the Haiti quake came when geologists didn't find any surface disturbance along the east-west fault. Instead, data pointed to new, unknown fault because an area north of the Enriquillo fault had been forced upward and to the south, Calais said. The new findings are based on surface observations in the devastated region around Port-au-Prince, global positioning system measurements and other observations and data. Calais presented the research Tuesday at a meeting of the American Geophysical Union in Foz do Iguacu, Brazil. In 2008, he warned that growing stresses in southern Haiti had left the Enriquillo fault ripe for up to a magnitude 7.2 quake. He said this week that the information then wasn't conclusive enough to say whether those stresses were building up along the Enriquillo fault, or some other fault.
[Associated
Press;
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