As rescue and recovery efforts continue to ramp-up in earthquake-ravaged Myanmar, new details about how the geologic setting amplified the disaster are beginning to emerge.
The March 28 magnitude 7.7 earthquake that rocked through Southeast Asia collapsed buildings, dams and bridges, and killed at least 2,700 people. The rupture occurred along several hundred kilometers of a roughly 1,400-kilometer-long fault known as the Sagaing Fault. The epicenter of the event was just 10 kilometers beneath Earth’s surface and occurred near the Myanmar city of Mandalay.
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