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A powerful magnitude 6.8 earthquake struck the Central Mid‑Atlantic Ridge on 13th October 2026 at 12:23 UTC, according to the United States Geological Survey (USGS). The quake originated at a shallow depth of 10 km, which typically results in stronger shaking near the rupture zone.
Although this seismic event occurred far from populated coastlines, earthquakes of this size are scientifically important due to the tectonic processes that shape the Mid‑Atlantic Ridge — one of the longest and most active underwater mountain chains on Earth.
The Mid‑Atlantic Ridge marks the boundary between several major tectonic plates, including the North American, South American, African, and Eurasian plates. These plates are slowly pulling apart, creating new oceanic crust through a process known as seafloor spreading.
Earthquakes in this region are common, but events approaching magnitude 7.0 highlight periods of increased tectonic stress release along the ridge’s central segment.
Because the earthquake occurred deep in the Atlantic Ocean, no damage or casualties were reported. However, shallow earthquakes of this size can produce strong local shaking along the ridge and are closely monitored by global seismic networks.
No tsunami alerts were issued. Mid‑ocean earthquakes can generate tsunamis under specific fault motions, but this event did not trigger any warnings or advisories.
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