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Location:
Magnitude:
7.4
Time:
19 Aug 2016 07:32:22
Depth:
10.0
There are 3 swarms found nearby.
2016
PS20160819.1(31.5km)
19 Aug
1 day 20 hours
26 earthquakes
PS20160822.1(58.4km)
22 Aug
21 hours
6 earthquakes
PS20160902.1(47.3km)
1 Sep
17 hours
5 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

The 2016 Magnitude 7.4 Earthquake in the South Georgia Island Region

On August 19, 2016, at 07:32 UTC, a magnitude 7.4 earthquake struck the South Georgia Island region in the South Atlantic Ocean. The event occurred at a shallow depth of 10 kilometers, classifying it as a significant seismic occurrence within a tectonically active zone. South Georgia Island lies along the boundary between the South American and Scotia plates. This area forms part of the broader Scotia Arc system, where complex interactions between continental and oceanic plates generate frequent seismic activity. The nearby South Sandwich Trench represents a subduction zone, contributing to the region's elevated earthquake risk. Shallow-depth events like the 2016 quake often result from thrust faulting or strike-slip motion along these plate margins. Seismicity in the South Georgia region reflects ongoing plate convergence and transform faulting. Historical records indicate multiple large-magnitude earthquakes tied to the Scotia Plate's motion relative to surrounding plates. Since 2000, the area has experienced notable strong events, with the 2016 magnitude 7.4 quake standing as a prominent example at the epicentral location. The 2016 earthquake's parameters align with typical characteristics of South Atlantic seismicity. Its shallow focus increased the potential for felt shaking across remote island stations and oceanographic monitoring sites, though the sparsely populated nature of the region limited direct human impacts. Post-event analysis confirmed no major tsunami generation, consistent with the event's tectonic setting away from high-displacement subduction interfaces. Geological studies of the Scotia Arc highlight its evolution through Cenozoic plate reorganization, with South Georgia representing a continental fragment detached from South America. This history underscores persistent seismic hazards driven by relative plate velocities of several centimeters per year.

References

USGS Earthquake Catalog Global CMT Project NOAA National Centers for Environmental Information