The devastating earthquake that rocked Haiti in January was unleashed by a previously undetected fault line — not the well-known one initially blamed, according to an analysis of new data.
Its unclear how dangerous the new, unmapped fault might be or how it’s discovery changes the overall earthquake hazard risk for Haiti, said Eric Calais, a professor of geophysics at Purdue University in Indiana, who presented the findings this week at a scientific conference in Brazil.
The analysis shows that most, if not all, of the geologic movement that caused January’s magnitude 7.0 earthquake occurred along the newly uncovered fault, not the well-documented Enriquillo fault, he said
That suggests Haiti’s seismic zone is far more complex than scientists had anticipated, but the new fault’s profile, including the possibility that it merges with the Enriquillo fault at some depth, won’t be known until the region is intensively studied.
“If there are other faults capable of producing earthquakes besides the Enriquillo and this new one, we need to know about them. We need to go after them,” Calais said.
At the time of the quake, Haiti had no seismic stations. Researchers who flocked to the Caribbean nation have since installed about 10 stations.
Bruce Presgrave, a geophysicist with the US Geological Survey, said the discovery is the sort of revelation that often comes to light after big earthquakes, when scientists descend on quake-ravaged sites to conduct intensive research.
“It’s part of the learning process of science,” he said.
“They’re doing detailed studies of the area that aren’t possible in the hours following the quake.”
Presgrave declined to comment on the specifics of the analysis because he had not reviewed it.
Earthquakes typically occur along fault lines, areas where two sections of the Earth’s crust grind against 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 for the Haiti quake came when geologists didn’t find any surface disturbance along the east-west fault. Instead, data pointed to a 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 on 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.
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