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Location:
Period:
25 Dec 2019 03:45:46 - 26 Dec 2019 02:21:28 (22 hours 35 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
6
M 7.0+:
6 swarms found nearby.
2003
PS20030907.1(162.2km)
6 Sep
23 hours
5 earthquakes
2005
PS20050810.1(113.8km)
9 Aug
19 hours
5 earthquakes
2011
PS20110927.1(169.8km)
27 Sep
1 day 0 hours
8 earthquakes
2016
PS20160812.1(66.9km)
12 Aug
20 hours
7 earthquakes
2021
PS20210203.1(186.1km)
2 Feb
1 hours
8 earthquakes
2023
PS20231127.1(116.8km)
26 Nov
16 hours
5 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm Analysis: Southeast of the Loyalty Islands (PS20191226.1)

A seismic swarm designated PS20191226.1 occurred southeast of the Loyalty Islands between 03:45 on 25 December 2019 and 02:21 on 26 December 2019. Over this 22-hour-and-35-minute period, six earthquakes were recorded, with magnitudes ranging from 5.0 to 5.4 and focal depths between 9 and 10 km. The sequence included events at 03:45:46 (M5.1), 10:11:41 (M5.0), 12:23:13 (M5.4), 02:06:37 (M5.1), 02:16:56 (M5.1), and 02:21:28 (M5.4) on the respective dates. This swarm reflects a cluster of moderate-magnitude earthquakes typical of the tectonically active southwest Pacific margin. The Loyalty Islands lie within a region influenced by complex plate interactions involving the Australian and Pacific plates, where subduction-related stresses and back-arc extension contribute to recurrent seismicity. Depths consistently near 10 km indicate shallow crustal faulting, common in swarm activity where fluid migration or stress transfer along pre-existing fractures can trigger multiple events without a dominant mainshock. Historically, four prior swarms have been documented in the same area since 2000, occurring in 2003, 2005, 2011, and 2016. These episodes underscore the region's propensity for episodic clustering rather than isolated large events. The most recent strong earthquake, an M7.2 event on 12 August 2016 located 57 km from the 2019 swarm center, highlights the potential for higher-magnitude activity amid ongoing swarm patterns. Swarm events such as PS20191226.1 provide insight into localized stress accumulation and release. The tight temporal grouping and similar depths suggest activation of a discrete fault segment, possibly driven by tectonic loading in the subduction influence zone. No escalation to larger magnitudes was observed, consistent with the moderate energy release across the six events. Geological monitoring in this part of the Loyalty Islands region continues to track such sequences to better understand long-term seismic hazards associated with plate boundary dynamics.

References

SeismoSight internal classification data for swarm PS20191226.1.