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The technical data provided by the U.S. Geological Survey paints a terrifying picture of why the destruction was so absolute. The epicenter was pinpointed in a rugged, high-altitude region along the China–Myanmar border, but the true danger lay in the quake’s depth—or lack thereof. Striking at a shallow depth of roughly 10 kilometers, the energy released was not absorbed by the earth’s mantle but was instead thrust directly upward and outward with a ferocity that intensified the surface shaking tenfold. In seismic terms, a shallow quake of this magnitude is the “worst-case scenario” for human settlements. The lateral movement was so extreme that it bypassed the structural integrity of even the most modern reinforcements, while the older, historic brick-and-mortar villages of the region stood no chance against the earth’s sudden, violent rhythm.