Seismic Swarm PS20050806.1 Near San Julian, Philippines
On August 6, 2005, a seismic swarm designated PS20050806.1 occurred 38 km east of San Julian in Eastern Samar, Philippines. The sequence began at 11:58 and concluded at 13:08, encompassing five earthquakes within one hour and nine minutes. This event cluster reflects typical tectonic activity in a highly active subduction setting.
The individual events unfolded as follows. The first registered at 11:58:44 with magnitude 5.0 at 28 km depth. A second event occurred at 12:40:34 with magnitude 5.2 at 1 km depth. Immediately afterward, at 12:40:37, a magnitude 5.5 earthquake struck at 28 km depth. Two additional events followed: a magnitude 5.0 at 13:01:27 (28 km depth) and a magnitude 4.7 at 13:08:07 (28 km depth). The tight temporal spacing and varying focal depths highlight the swarm’s clustered nature without a dominant mainshock.
Eastern Samar lies within the Philippine Mobile Belt, where the Philippine Sea Plate subducts westward beneath the Sunda Plate along the Philippine Trench. This convergent margin drives frequent seismicity across the archipelago. The trench reaches depths exceeding 10,000 m offshore Samar, generating intermediate-depth earthquakes along the Wadati-Benioff zone. Shallow crustal faults, including strands of the Philippine Fault system that traverse the islands, further contribute to seismic hazard. Historical records document repeated moderate-to-large events in the Samar region, consistent with ongoing plate convergence at rates of approximately 6–8 cm per year.
Swarm sequences such as PS20050806.1 commonly arise from stress transfer along pre-existing faults or fluid migration within the crust. The presence of both shallow and intermediate-depth events suggests possible interaction between the subducting slab and overlying crustal structures. No volcanic association is indicated for this particular swarm, aligning instead with purely tectonic processes characteristic of the Philippine subduction zone.
Seismic monitoring in the Philippines has improved substantially since 2005 through expanded networks operated by the Philippine Institute of Volcanology and Seismology (PHIVOLCS). Updated hazard assessments continue to emphasize the elevated risk along the eastern seaboard of Samar due to its proximity to the trench. The 2005 swarm, while modest in scale, underscores the persistent potential for clustered activity that can precede or accompany larger tectonic episodes.
References
USGS Earthquake Catalog PHIVOLCS Seismic Reports Global CMT Catalog