2000 Banggai Islands earthquake
On 4 May 2000 at 12:21 WITA, a earthquake struck off the coast of Banggai Islands Regency, Central Sulawesi, Indonesia, which was followed by a damaging local tsunami. The earthquake and tsunami killed at least 54 people and injured 270 others, with most of the damage and casualties occurring in the Banggai Islands.
Tectonic setting
The Banggai region of Sulawesi lies within the complex area of interaction between the Pacific, Philippine Sea, Australian and Eurasian plates. The Banggai Islands themselves form part of the Banggai-Sula microcontinent, which collided with eastern Sulawesi during the Neogene, with a thrust fault boundary along the southeastern edge of the Eastern arm. The northern margin of the Banggai-Sula block has been interpreted as a continuous southward moving thrust zone, but seismic reflection data and high-resolution multibeam bathymetry show little sign of thrusting, with evidence instead of a zone of dextral strike-slip faulting.Earthquake
The earthquake had an initial estimated magnitude of 7.6, 7.5, 6.7 and a recalculated magnitude of 7.5. By 31 December 2000, 84 aftershocks exceeding were detected by the USGS, with the strongest one measuring and occurring on 5 May. These aftershocks mainly occurred south and southwest of the epicenter, with many having epicenters located directly beneath the islands of Peleng and Banggai, unlike the offshore mainshock.The focal mechanism is consistent with strike-slip faulting on either a northwest-southeast trending sinistral fault or a southwest-northeast trending dextral fault. A rupture area of x was estimated, extending from Bangkulu Island to the Molucca Sea near the Gulf of Tomini, with a maximum slip of near the hypocenter. The observed source time function gives a 30 second duration for the earthquake, with the greatest phase of seismic moment release occurring about five seconds after initiation.