The 2009 Swan Islands earthquake occurred on May 28 at 02:24:45 AM local time with a moment magnitude of 7.3 and a maximum Mercalli intensity of VII (Very strong). The epicenter was located in the Caribbean Sea, 64 kilometres (40 mi) northeast of the island of Roatán, 19 miles northeast of Port Royal, Isla de Bahias, 15 miles northwest of Isla Barbaretta, and 130 kilometres (81 mi) north-northeast of La Ceiba.[2] Three aftershocks followed the earthquake within magnitude 4 range.[3]
Analysis of geodetic and seismic data indicated that up to 1 meter of slip occurred across a 250-km-long fault rupture. Although the epicenter was located far off the coast of Central America, the long rupture contributed to severe damage in Honduras. The earthquake ruptured a segment of plate boundary immediately east of the 1976 earthquake rupture on the Motagua Fault.[6]
The earthquake caused at least seven fatalities, 40 injuries, and more than 130 collapsed or damaged buildings across northern Honduras.[2] Two important bridges and a number of levees and port terminals were also seriously damaged.[7] In the Guatemalan department of Izabal, 35 buildings were destroyed and 80 were damaged. In Belize, at least 5 buildings were also destroyed and 25 were damaged. In Roatan, one home was damaged and one injury occurred.[2][8] The earthquake caused an estimated $37 million worth of damage, and electricity, Internet and telephone connections were cut throughout the majority of Honduras.[9]
A tsunami watch was put into effect by the Pacific Tsunami Warning Center for Honduras, Guatemala, and Belize and was discontinued 90 minutes after the earthquake occurred.[4]
^Belarbi, A., Luna, R., Applegate, K., Calderon, H., Rivera, O., Lopez, L.A. and Rodriguez, R., 2009. The M7.3 Honduras Earthquake of May 28, 2009, EERI Special Earthquake Report, 1–4
Graham, S. E.; Demets, C.; Deshon, H. R.; Rogers, R.; Maradiaga, M. Rodriguez; Strauch, W.; Wiese, K.; Hernandez, D. (2012), "GPS and seismic constraints on the M = 7.3 2009 Swan Islands earthquake: Implications for stress changes along the Motagua fault and other nearby faults", Geophysical Journal International, 190 (3): 1625–1639, Bibcode:2012GeoJI.190.1625G, doi:10.1111/j.1365-246X.2012.05560.x