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:
Period:
31 Aug 2012 13:05:15 - 1 Sep 2012 23:55:34 (1 day 10 hours 50 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
33
4 swarms found nearby.
2012
PS20120831.1(24.9km)
31 Aug
19 hours
15 earthquakes
4 Sep
14 hours
9 earthquakes
2019
PS20190208.1(103.0km)
8 Feb
9 hours
7 earthquakes
PS20190426.1(97.9km)
26 Apr
15 hours
9 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Earthquake Swarm S20120901.1: Seismic Activity Northeast of Santa Monica, Philippines

The Philippines lies within the tectonically active Pacific Ring of Fire, where the Philippine Sea Plate subducts beneath the Eurasian Plate along the Philippine Trench. This convergence drives frequent seismicity across the archipelago, particularly in eastern Mindanao and the Visayas. The region near Santa Monica experiences ongoing deformation associated with the Philippine Fault system and subsidiary strike-slip structures that accommodate oblique convergence.

Swarm S20120901.1 was recorded 103 km northeast of Santa Monica. The sequence began at 13:05 on 31 August 2012 and concluded at 23:55 on 1 September 2012, lasting 34 hours and 50 minutes. During this interval, 33 earthquakes were registered, with magnitudes ranging from 4.1 to 4.9 and focal depths between 20 km and 44 km. The events clustered tightly in both space and time, characteristic of swarm behavior rather than a classic mainshock-aftershock sequence.

Initial activity on 31 August featured several events of magnitude 4.8–4.9 at approximately 35 km depth within the first two hours. Subsequent shocks maintained similar depths until late in the day, when a pair of magnitude 4.9 events occurred at 40 km and 44 km. Depths shallowed modestly on 1 September, with the final notable events reaching 22 km. No single dominant mainshock exceeded the surrounding activity, supporting classification as a swarm.

Such swarms in the Philippine setting often reflect fluid migration or aseismic slip along faults within the mobile belt. The 2012 sequence represents the sole swarm documented in the catalog since 1 January 2000, underscoring the episodic nature of clustered seismicity in this segment of the subduction margin.

Seismic monitoring by the Philippine Institute of Volcanology and Seismology (PHIVOLCS) and global networks provides the primary data for these events. Continued instrumentation upgrades since 2012 have improved detection thresholds across eastern Mindanao, enhancing future swarm characterization.

References

PHIVOLCS Earthquake Catalog
USGS Earthquake Hazards Program
Global Centroid Moment Tensor Project