Very strong. Difficult to stand. Damage negligible in well-built structures, considerable in poorly-built ones.
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.
Light earthquake. Felt indoors by many, outdoors by a few. Hanging objects swing, dishes rattle, parked cars rock noticeably.
No structural damage expected. May knock light items off shelves at the epicenter.
Deep earthquakes (over 300 km) occur within subducting tectonic slabs. They can be felt over very large areas but rarely cause surface damage — energy spreads out by the time it reaches the surface.
This earthquake released roughly 7.08e+11 joules of seismic energy — about 11.24 thousandths of a Hiroshima 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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