How did this devastation happen? The truth is, scientists do not exactly know; however, after researchers spent weeks gathering geologic data and putting together theories, they started to form an idea of how these quakes took place. According to the U.S. Geological Survey, the two earthquakes are known as a doublet because they happened nearly at the same place. In this case, the quake with the stronger magnitude of 7.5 would be the main shock, while the one with a magnitude of 7.2 would be the foreshock. However, as Brandon Bishop, a seismologist at Saint Louis University, said: “Most doublets don’t occur quite this close together in time. Delays of hours to a few days are much more common.” The reason for this peculiar phenomenon was that the first quake created seismic waves that convulsed an adjacent locked section of the fault, causing it to break, therefore creating the second quake.
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