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Location:
Period:
10 Feb 2021 12:24:21 - 12 Feb 2021 20:55:16 (2 days 8 hours 30 minutes)
Volcanoes in 100km radius:
Earthquakes:
91
M 7.0+:
15 swarms found nearby.
2001
PS20010228.1(185.5km)
28 Feb
15 hours
7 earthquakes
2003
PS20030907.1(67.8km)
6 Sep
23 hours
5 earthquakes
2008
PS20081123.1(93.1km)
22 Nov
17 hours
5 earthquakes
2009
PS20090116.1(162.8km)
16 Jan
12 hours
6 earthquakes
PS20090119.1(116.5km)
18 Jan
1 day 10 hours
6 earthquakes
2011
PS20110927.1(46.1km)
27 Sep
1 day 0 hours
8 earthquakes
2016
PS20160812.1(177.0km)
12 Aug
20 hours
7 earthquakes
2018
PS20180829.1(188.8km)
29 Aug
9 hours
7 earthquakes
2021
PS20210203.1(41.1km)
2 Feb
1 hours
8 earthquakes
PS20210214.1(12.0km)
13 Feb
1 day 23 hours
14 earthquakes
2022
PS20220331.1(145.5km)
30 Mar
1 day 16 hours
16 earthquakes
2023
PS20230519.1(106.1km)
19 May
1 day 15 hours
44 earthquakes
S20230519.1(82.9km)
19 May
1 day 22 hours
34 earthquakes
PS20230523.1(121.8km)
22 May
11 hours
6 earthquakes
2026
PS20260713.1(44.0km)
13 Jul
14 hours
6 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm PS20210210.1 Southeast of the Loyalty Islands

The seismic swarm PS20210210.1 occurred southeast of the Loyalty Islands in the southwestern Pacific Ocean. It began at 12:24 on 10 February 2021 and concluded at 20:55 on 12 February 2021, spanning 56 hours and 30 minutes. During this period, 91 earthquakes were recorded.

The swarm initiated with a magnitude 6.1 event at 12:24 on 10 February at a depth of 11 km. Subsequent activity included multiple events exceeding magnitude 5.0, with peaks at magnitudes 7.7 and 6.3. Depths predominantly ranged between 8 km and 17 km, though isolated deeper events reached 68 km and 80 km. The sequence featured 14 events of magnitude 6.0 or greater, concentrated primarily on 10 February.

This activity aligns with the broader tectonic framework of the region. The Loyalty Islands lie along the Loyalty Ridge, where the Australian Plate interacts with the Pacific Plate near the New Hebrides subduction zone. Subduction-driven compression and associated faulting produce recurrent seismicity, often manifesting as swarms rather than isolated mainshock-aftershock sequences.

Historical records indicate nine such swarms in the area since 1 January 2000. These occurred in 2001, 2003, 2008, 2009 (two swarms), 2011, 2016, 2018, and 2021. The 2021 event included a magnitude 7.7 earthquake located 19 km from the swarm center, consistent with the largest recorded magnitude in the dataset since 2000.

Swarm patterns in this setting typically reflect fluid migration or episodic slip along pre-existing faults within the overriding plate. Depths in the 10–15 km range suggest activation within the upper crust, influenced by the regional stress field from plate convergence rates of approximately 5–7 cm per year.

The February 2021 swarm contributed to ongoing monitoring of seismic hazards in the Loyalty Islands region, where moderate-to-large events remain a characteristic feature of the tectonic environment.

References

USGS Earthquake Catalog (earthquake.usgs.gov)
Global CMT Catalog (globalcmt.org)
Geoscience Australia Seismology (ga.gov.au)