Seismic Swarm PS20140530.1: Analysis of Activity Near Cortes, Philippines
The seismic swarm designated PS20140530.1 occurred on 30 May 2014 in the central Philippines, centered approximately 70 km east-northeast of Cortes in Bohol province. The sequence began at 15:26 UTC and concluded at 20:37 UTC, encompassing a total duration of five hours and eleven minutes. During this interval, six earthquakes were recorded, with magnitudes ranging from 4.5 to 5.7 and focal depths between 8 km and 18 km.
The events unfolded as follows: the initial shock at 15:26:14 registered magnitude 5.7 at 14 km depth, followed by a magnitude 5.1 event at 16:36:21 (10 km depth). Subsequent activity included a magnitude 4.5 at 17:06:09 (8 km), magnitude 5.3 at 17:41:25 (12 km), magnitude 5.0 at 17:53:07 (18 km), and a final magnitude 5.0 at 20:37:55 (10 km). All events clustered tightly in both time and space, characteristic of swarm behavior without a dominant mainshock-aftershock pattern.
The Philippines occupies a tectonically active segment of the Pacific Ring of Fire, where convergence between the Philippine Sea Plate and the Eurasian Plate drives subduction along the Philippine Trench and associated fault systems. Bohol island lies near the western edge of the Philippine Fault Zone and the Cotabato Fault system, regions historically prone to moderate seismic swarms due to crustal stresses from oblique subduction and strike-slip motion. Depths in the 8–18 km range align with typical shallow crustal seismicity in this setting.
Historical records since 1 January 2000 indicate only three prior swarms in the immediate region: one in 2009 and two in 2012. This low frequency underscores the episodic nature of swarm activity amid ongoing plate-boundary deformation. A notable regional event was the magnitude 7.6 earthquake on 2 December 2023, located 19 km east of Gamut and 91 km from the 2014 swarm center, highlighting the potential for larger ruptures along nearby structures.
Such swarms provide valuable data for understanding stress transfer and fault interactions in subduction-influenced crust. Continued monitoring by networks such as PHIVOLCS supports improved hazard assessment in this high-seismicity archipelago.
References
SeismoSight internal swarm classification PS20140530.1
USGS earthquake catalog (regional tectonics and historical events)