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Each of them moves at a different speed and in its own direction, which makes predicting seismic activity in such areas extraordinarily difficult. The Tehuantepec earthquake happened just offshore, within the Cocos plate, at a depth of approximately 37 miles.The plate tectonics here get complicated, but essentially the oceanic Cocos plate slides underneath the North American continental plate, dipping some 50 degrees.The magnitude of the main event was so great that it reactivated numerous shallow faults, triggering a seemingly endless series aftershocks: the release of energy accumulated over decades.
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Scientists know remarkably little about how this subduction, as it’s called, affects seismicity – not here, and not in other regions with similarly complex topography.
In this part of the Mexican Pacific coast there is also what’s called a “triple-junction zone,” meaning that the boundaries of three tectonic plates intersect here – in this case, the Cocos, North America and Caribbean plates.
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In the pre-Hispanic epoch, inhabitants of the country’s central zone reported on earthquakes in their “códices,” or indigenous records, attributing the shaking to the wrath of their gods.