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Caribbean Sea
1692 06 07 - Jamaica Fatalities 2,000
1787 05 02 - Puerto Rico - M 8.0
1843 02 08 - Leeward Islands - M 8.3 Fatalities 5,000
1867 11 18 - Puerto Rico Region
1907 01 14 - Kingston, Jamaica - M 6.5 Fatalities 1,000
1918 10 11 - Mona Passage - M 7.5 Fatalities 116
1946 08 04 - Samana, Dominican Republic - M 8.0 Fatalities 100
1969 12 25 - Guadeloupe, Leeward Islands - M 7.2
1974 10 08 - Leeward Islands - M 7.5
2004 11 21 - Leeward Islands - M 6.3 Fatalities 1
2004 12 14 - Cayman Islands Region - M 6.8
2006 09 10 - Gulf of Mexico - M 5.8
2007 11 29 - Martinique Region, Windward Islands - M 7.4 Fatalities 1
The location and focal mechanism of the earthquake are consistent with the event having occurred as left-lateral strike slip faulting on the Enriquillo-Plaintain Garden fault system. This fault system accommodates about 7 mm/y, nearly half the overall motion between the Caribbean plate and North America plate.
The Enriquillo-Plaintain Garden fault system has not produced a major earthquake in recent decades. The EPGFZ is the likely source of historical large earthquakes in 1860, 1770, 1761, 1751, 1684, 1673, and 1618, though none of these has been confirmed in the field as associated with this fault.
People in the large Western Quebec seismic zone have felt small earthquakes and suffered damage from larger ones for three centuries. The two largest damaging earthquakes occurred in 1935 (magnitude 6.1) at the northwestern end of the seismic zone, and in 1732 (magnitude 6.2) 450 km (280 mi) away at the southeastern end of the zone where it caused significant damage in Montreal. Earthquakes cause damage in the zone about once a decade. Smaller earthquakes are felt three or four times a year.