Exactly What Happens to the Ground at a Fault Line?

A special observatory 2 miles underground plus a great aerial photo illustrate why the earth trembles like it did in Haiti.

By Janet Fang
May 13, 2010 12:00 AMMay 5, 2023 2:32 PM

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Faults are breaks in the earth’s crust where adjacent sections, or plates, have moved relative to each other. When a lot of slippage happens all at once, the result is a major earthquake, like the one that struck Haiti in January along the Enriquillo-Plantain Garden Fault, which runs in an east/west direction across the Caribbean. North of that fault a piece of crust called the Gonave Platelet is advancing westward, while the Caribbean Plate south of the fault is grinding to the east at a rate of about one-third inch per year. This side-by-side motion defines what is known as a strike-slip fault. (The Yushu earthquake in Tibet on April 13 was also the result of strike-slip movement, but the huge Chilean earthquake in February was instead a subduction event, where one plate slips under another.) 

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