Location:
Period:
8 Apr 2017 07:07:56 - 8 Apr 2017 08:36:35 (1h 28m)
Volcanoes in 100km radius:
Earthquakes:
5
4 swarms found nearby.
2008
PS20080927.1(80.8km)
27 Sep
5 minutes
5 earthquakes
2020
S20200112.1(36.6km)
12 Jan
1 day 18 hours
45 earthquakes
S20200113.1(37.4km)
12 Jan
2 days 12 hours
35 earthquakes
2022
PS20220314.1(189.1km)
13 Mar
1 day 10 hours
7 earthquakes
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Seismic Swarm PS20170408.1 Near Talahib Payap, Philippines

On 8 April 2017, a seismic swarm designated PS20170408.1 was recorded 1 km SSW of Talahib Payap in the Philippines. The sequence began at 07:07 and concluded at 08:36 local time, encompassing five earthquakes within 1 hour and 28 minutes. This event provides a focused example of clustered seismic activity in a tectonically active archipelago.

The recorded events unfolded as follows. The initial shock at 07:07:56 registered magnitude 5.5 at a depth of 10 km. Two minutes later, at 07:09:23, a magnitude 5.9 event occurred at 14 km depth. Subsequent activity included two magnitude 5.0 earthquakes at 07:29:09 (10 km depth) and 07:29:15 (60 km depth), followed by a magnitude 4.7 shock at 08:36:35 (10 km depth). Depths remained predominantly shallow, consistent with upper-crustal faulting.

The Philippines occupies a complex tectonic setting at the convergence of the Philippine Sea Plate and the Eurasian Plate. Subduction along the Philippine Trench and Manila Trench drives regional deformation, while strike-slip faults such as the Philippine Fault accommodate lateral motion. The swarm location lies within the southern Luzon block, where interactions between these plates and local volcanic systems produce frequent moderate-magnitude events.

Historical records indicate limited swarm-type sequences in the area since 2000. Only one prior swarm has been documented, occurring in 2008. This scarcity highlights that clustered activity without a dominant mainshock remains uncommon relative to isolated tectonic earthquakes in the same corridor.

Swarm events like PS20170408.1 typically reflect fluid migration, stress transfer along minor faults, or volcanic unrest rather than a single large rupture. The rapid succession of comparable magnitudes, absence of a clear foreshock-mainshock-aftershock pattern, and concentration within a narrow time window align with these mechanisms. Depths between 10 km and 60 km suggest involvement of both shallow crustal structures and slightly deeper transitional zones.

Ongoing monitoring by national agencies continues to track microseismicity in southern Luzon. Updated catalogs through 2023 confirm that moderate swarms remain infrequent, reinforcing the value of detailed analysis for refining local hazard models.

References

Philippine Institute of Volcanology and Seismology (PHIVOLCS) seismic bulletins, 2017–2023.
USGS Earthquake Catalog, regional events 2000–2023.
SeismoSight internal swarm classification records.