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Location:
Period:
8 Feb 2019 11:55:07 - 8 Feb 2019 21:09:58 (9 hours 14 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
7
11 swarms found nearby.
2012
PS20120831.1(82.7km)
31 Aug
19 hours
15 earthquakes
S20120901.1(103.0km)
31 Aug
1 day 10 hours
33 earthquakes
PS20120904.1(94.5km)
4 Sep
14 hours
9 earthquakes
2014
PS20140530.1(56.6km)
30 May
5 hours
6 earthquakes
PS20140531.1(57.1km)
31 May
1 hours
9 earthquakes
2018
PS20181029.1(150.9km)
29 Oct
7 hours
5 earthquakes
2019
PS20190426.1(31.2km)
26 Apr
15 hours
9 earthquakes
2023
PS20231202.1(122.4km)
2 Dec
5 days 19 hours
107 earthquakes
PS20231212.1(149.0km)
11 Dec
14 hours
5 earthquakes
PS20231224.1(176.4km)
23 Dec
15 hours
5 earthquakes
2024
PS20240803.1(196.4km)
2 Aug
5 hours
7 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Earthquake Swarm PS20190208.1: Seismic Activity Near Pilar, Philippines

On 8 February 2019, a notable earthquake swarm designated PS20190208.1 occurred 42 km ENE of Pilar in the Philippines. The sequence began at 11:55 and concluded at 21:09, spanning 9 hours and 14 minutes. During this period, seven earthquakes were recorded, with magnitudes ranging from 4.6 to 5.9 and focal depths primarily at 10–20 km.

The events unfolded as follows: the initial shock measured 5.9 at 20 km depth, followed by subsequent tremors of 5.0, 5.2, 5.0, 4.6, 5.0, and a final 5.0 magnitude event. All but the first occurred at 10 km depth. This swarm reflects clustered seismic energy release typical of the tectonically active Philippine region.

The Philippines lies within the Pacific Ring of Fire, where the Philippine Sea Plate subducts beneath the Eurasian Plate along the Philippine Trench. This convergence drives frequent seismicity and volcanism. The area east of Pilar, in the Bicol Peninsula, experiences stress accumulation along segments of the Philippine Fault and associated secondary structures. Historical records indicate that such swarms represent episodic releases rather than isolated mainshock-aftershock sequences.

Since 2000, six earthquake swarms have been documented in the vicinity. Earlier episodes occurred in 2012 (three swarms), 2014 (two swarms), and 2018 (one swarm). These patterns suggest recurring strain accommodation in the crust, influenced by both regional plate motion and local fault interactions.

Swarm activity of this nature often correlates with fluid migration or minor stress perturbations along faults, though no direct link to volcanic unrest at nearby Mayon Volcano has been established for this event. Depths of 10–20 km place the hypocenters within the brittle upper crust, consistent with the regional tectonic regime.

Continued monitoring by national seismic networks remains essential for assessing whether similar clusters may recur. The 2019 swarm underscores the dynamic nature of Philippine seismicity and the importance of preparedness in tectonically active zones.

References

SeismoSight internal swarm classification records
PHIVOLCS seismic bulletins
USGS earthquake catalog (regional tectonics)