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2010 Haiti Earthquake


USGS Haiti Earthquake Data

Magnitude
7.0
Date-Time
  • Tuesday, January 12, 2010 at 21:53:10 UTC
  • Tuesday, January 12, 2010 at 04:53:10 PM at epicenter
  • Time of Earthquake in other Time Zones
Location
18.457°N, 72.533°W
Depth
13 km (8.1 miles) set by location program
Region
HAITI REGION
Distances
25 km (15 miles) WSW of PORT-AU-PRINCE, Haiti
130 km (80 miles) E of Les Cayes, Haiti
150 km (95 miles) S of Cap-Haitien, Haiti
1125 km (700 miles) SE of Miami, Florida
Location Uncertainty
horizontal +/- 3.4 km (2.1 miles); depth fixed by location program
Parameters
NST=312, Nph=312, Dmin=143.7 km, Rmss=0.93 sec, Gp= 25°,
M-type=teleseismic moment magnitude (Mw), Version=9
Source
USGS NEIC (WDCS-D)
Event ID
us2010rja6

USGS Haiti Earthquake Summary

Felt Reports

Severe damage and casualties in the Port-au-Prince area. Felt throughout Haiti and the Dominican Republic, in Turks and Caicos Islands, southeastern Cuba, eastern Jamaica, in parts of Puerto Rico and the Bahamas, and as far as Tampa, Florida and Caracas, Venezuela.

Tectonic Summary

The January 12, 2010, Haiti earthquake occurred in the boundary region separating the Caribbean plate and the North America plate. This plate boundary is dominated by left-lateral strike slip motion and compression, and accommodates about 20 mm/y slip, with the Caribbean plate moving eastward with respect to the North America plate.

Haiti occupies the western part of the island of Hispaniola, one of the Greater Antilles islands, situated between Puerto Rico and Cuba. At the longitude of the January 12 earthquake, motion between the Caribbean and North American plates is partitioned between two major east-west trending, strike-slip fault systems -- the Septentrional fault system in northern Haiti and the Enriquillo-Plantain Garden fault system in southern Haiti.

The location and focal mechanism of the earthquake are consistent with the event having occurred as left-lateral strike slip faulting on the Enriquillo-Plantain Garden fault system. This fault system accommodates about 7 mm/y, nearly half the overall motion between the Caribbean plate and North America plate.

 
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