Violent. Damage considerable in specially-designed structures. Buildings shifted off foundations; ground cracked.
MMI is the Modified Mercalli Intensity scale — what people actually feel. This estimate is derived from magnitude alone; real shaking varies with depth, distance and local soil. The official USGS ShakeMap is the authoritative source.
Strong earthquake. Felt by everyone. Furniture moves, plaster falls, weak chimneys break. Many run outdoors. Standing is difficult near the epicenter.
Considerable damage to ordinary buildings, partial collapse of older or non-reinforced structures. Well-built buildings sustain slight damage.
Intermediate-depth events (70–300 km) attenuate more before reaching the surface, so a given magnitude is typically felt over a wider but weaker area than a shallow quake of the same size.
This earthquake released roughly 6.31e+13 joules of seismic energy — about 1.00× the Hiroshima atomic bomb.
Caveat: bomb energy is concentrated at a single point in microseconds; seismic energy radiates outward through Earth's crust over many seconds. The comparison is for relative scale only.
QuakeNear.Me aggregates feeds from multiple seismic networks. For the official record, including any updates to magnitude, ShakeMap, Did-You-Feel-It reports and aftershock sequences, see the upstream agency's event page.
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