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A magnitude 5.7 earthquake struck the Drake Passage on 24th July 2026 at 23:10 UTC, occurring at a shallow depth of 10 km. The event was detected by global seismic networks and drew attention due to its location in one of the most remote and geologically active marine corridors in the Southern Ocean.
The Drake Passage lies between the southern tip of South America and Antarctica, an area known for strong ocean currents and frequent tectonic movement. Because of its remote position, no damage or impact to populated areas has been reported.
The earthquake was recorded by multiple international agencies, including the USGS and regional monitoring centres. Although the event occurred far from inhabited regions, scientists routinely track seismic activity in the Drake Passage due to its role in the interaction between major tectonic plates.
The shallow depth of the quake means the seismic waves were strong near the epicentre, but given the oceanic location, the effects were limited to the surrounding waters.
The Drake Passage sits near the boundary between the Scotia Plate, the Antarctic Plate, and the South American Plate. This complex tectonic environment produces regular seismic activity, ranging from moderate to strong events.
Earthquakes in this region are typically associated with plate movement and crustal deformation beneath the ocean floor. While they rarely pose a threat to human settlements, they contribute valuable data to ongoing geological research.
Seismologists note that aftershocks may occur following an event of this magnitude, though they are expected to be minor and confined to the oceanic region. Monitoring will continue over the next several days.
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