Reacción a "7.7 magnitude earthquake strikes Myanmar"

Large earthquakes in this region are rare but not unknown, the last similar event being in 1956, more or less beyond living memory. This means that buildings are unlikely to be designed against seismic forces, and therefore are more vulnerable when an earthquake like this occurs, resulting in more damage and higher casualties. The ultimate cause of the earthquake is the northward movement of the Indian Plate, which produces a tearing effect along N-S trending vertical faults.