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A magnitude 5.5 earthquake struck the Southern East Pacific Rise on 12th July 2026, occurring at a shallow depth of 11 km beneath the ocean floor. The event was recorded at 07:29 UTC, with global seismic networks confirming tectonic movement along this fast‑spreading mid‑ocean ridge.
The Southern East Pacific Rise is located deep in the southeastern Pacific Ocean, far from any populated areas. Earthquakes in this region are typically associated with seafloor spreading, where tectonic plates gradually pull apart and magma rises to form new oceanic crust. Because of its remote location, seismic activity here rarely poses any risk to coastal communities.
Although moderate in strength, the earthquake was easily detected by monitoring stations worldwide. No tsunami warnings were issued, and there were no reports of damage or impact, as the nearest landmasses are thousands of kilometres away.
This event contributes to the ongoing tectonic activity along the East Pacific Rise, a key area for understanding how oceanic plates evolve and how seismic energy is released along spreading centres.
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