Mag 6.0 - 124km ENE of Codrington, Barbuda

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A magnitude 6.0 earthquake struck 124 km ENE of Codrington, Barbuda, on March 19, 2016, at a depth of 32 km. The region has a history of significant seismic activity, with the last major interplate event occurring in 1787, causing widespread destruction. Notable earthquakes in the area include the 1946 M8.0 Samana earthquake and the 1943 M7.6 Mona Passage earthquake, both resulting from shallow thrust faults. The motion between the North American and Caribbean plates is primarily accommodated by left-lateral strike-slip faults, particularly the Enriquillo-Plantain Garden Fault system. Concerns about potential subsequent stronger earthquakes in the region have been raised, highlighting the area's seismic risk.
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http://earthquake.usgs.gov/earthquakes/eventpage/us20005azy#general_region

2016-03-19 11:26:34 (UTC)
Location: Lat. 17.991 °N, Long. 60.700 °W
Depth: 32.0 km (19.9 mi)

The last probable interplate (thrust fault) event here occurred on May 2, 1787 and was widely felt throughout the island with documented destruction across the entire northern coast, including Arecibo and San Juan. Since 1900, the two largest earthquakes to occur in this region were the August 4, 1946 M8.0 Samana earthquake in northeastern Hispaniola and the July 29, 1943 M7.6 Mona Passage earthquake, both of which were shallow thrust fault earthquakes. A significant portion of the motion between the North America plate and the Caribbean plate in this region is accommodated by a series of left-lateral strike-slip faults that bisect the island of Hispaniola, notably the Septentrional Fault in the north and the Enriquillo-Plantain Garden Fault in the south.

Activity adjacent to the Enriquillo-Plantain Garden Fault system is best documented by the devastating January 12, 2010 M7.0 Haiti strike-slip earthquake, its associated aftershocks and a comparable earthquake in 1770.
I wonder if there will be subsequent and stronger events - sooner than later.
 
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