USGs

This morning, a 7.1 magnitude earthquake struck Belize and Honduras, resulting a few fatalities and some property damage.

Paul Earl, a seismologist with the United States Geological Survey, told Popsci.com that the quake emanated from the Swan Island Transform fault, a strike-slip fault not unlike the San Andreas fault in California. Both the location -- 80 miles off shore -- and the type of fault helped minimize the destruction caused by the event.

We know this much: Earthquakes strike along faults—fractures in the planet’s crust where plates of rock are thrust into a sort of geological gridlock. The difference between a tremor and an earth-shattering 8.0-plus-magnitude quake depends on whether the plates slip when the tension between them is still relatively low or if they snap after enduring millennia of mounting strain.

Calculating exactly when this might happen, however, is no easy feat.