Note:This page contains AI-generated content for informational and entertainment purposes only. It may contain inaccuracies. Raw event data is from USGS and EMSC. All statistics, lists, and derived information are generated by this site. Full disclaimerFound an error?
Location:
Magnitude:
7.5
Time:
5 Mar 2002 21:16:09
Depth:
31.0
M 7.0+:
There are 4 swarms found nearby.
2002
PS20020306.1(46.3km)
5 Mar
22 hours
6 earthquakes
2010
PS20100723.1(97.5km)
23 Jul
13 hours
11 earthquakes
2026
S20260128.1(74.6km)
27 Jan
1 day 15 hours
41 earthquakes
PS20260127.1(65.4km)
27 Jan
1 day 7 hours
15 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

The 2002 Mindanao Earthquake and Regional Seismicity

Mindanao, the southernmost major island of the Philippines, lies within one of the world's most tectonically active zones. The island sits at the boundary between the Philippine Sea Plate and the Sunda Plate, where oblique convergence drives subduction along the Philippine Trench to the east and the Cotabato Trench to the west. These features, combined with the left-lateral Philippine Fault that bisects the island, produce frequent moderate-to-large earthquakes. On 5 March 2002 at 21:16 local time, a magnitude 7.5 earthquake struck central Mindanao at a depth of 31 km. The event originated within the complex fault network of the region and was felt across much of the southern Philippines. Ground shaking reached intensity VII on the Modified Mercalli scale in several provinces, causing damage to buildings and infrastructure. No major tsunami was generated, consistent with the earthquake's inland epicenter and focal depth. Since 2000, Mindanao has experienced several other strong events. A magnitude 7.6 earthquake occurred on 23 July 2010 approximately 99 km from the 2002 epicenter, located 61 km west of Bantogon. Both events underscore the persistent seismic hazard associated with the Philippine Fault and nearby subduction interfaces. Geologically, Mindanao features a collage of volcanic arcs, ophiolite complexes, and sedimentary basins shaped by millions of years of plate interaction. The island's crust records multiple episodes of arc magmatism and collision, contributing to its elevated topography and active fault systems. Ongoing convergence at rates of 6–8 cm per year maintains high strain accumulation along major structures. Seismic monitoring by the Philippine Institute of Volcanology and Seismology (PHIVOLCS) and international networks continues to track activity, supporting improved hazard assessment and building-code enforcement. The 2002 and 2010 events highlight the importance of preparedness in this rapidly deforming region.

References

USGS Earthquake Catalog PHIVOLCS Seismic Reports