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Location:
Period:
4 Mar 2021 20:24:14 - 5 Mar 2021 23:48:28 (1 day 3 hours 24 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
21
M 7.0+:
31 swarms found nearby.
2003
PS20030930.1(56.1km)
29 Sep
1 day 16 hours
7 earthquakes
PS20031002.1(58.8km)
2 Oct
23 hours
6 earthquakes
2005
PS20051208.1(57.8km)
7 Dec
5 hours
5 earthquakes
2006
PS20060331.1(36.0km)
31 Mar
1 day 8 hours
23 earthquakes
PS20060405.1(88.0km)
4 Apr
1 day 3 hours
10 earthquakes
PS20060501.2(192.2km)
1 May
19 hours
5 earthquakes
2008
PS20080929.1(81.0km)
29 Sep
8 hours
5 earthquakes
PS20081005.1(58.0km)
4 Oct
1 day 11 hours
7 earthquakes
PS20081212.1(117.5km)
12 Dec
5 hours
5 earthquakes
2011
PS20110706.1(86.6km)
6 Jul
5 days 11 hours
52 earthquakes
2012
PS20120128.1(59.6km)
28 Jan
2 hours
10 earthquakes
2014
PS20140623.1(55.8km)
23 Jun
1 day 0 hours
27 earthquakes
S20140624.1(52.5km)
23 Jun
1 day 11 hours
41 earthquakes
PS20140701.1(23.4km)
30 Jun
22 hours
5 earthquakes
2016
PS20160204.1(57.2km)
4 Feb
8 hours
5 earthquakes
2019
PS20190616.1(115.3km)
15 Jun
3 days 8 hours
21 earthquakes
PS20190621.1(95.4km)
20 Jun
1 day 1 hours
7 earthquakes
2020
PS20200118.1(112.0km)
18 Jan
17 minutes
5 earthquakes
2021
PS20210304.2(51.1km)
4 Mar
4 days 4 hours
107 earthquakes
PS20210306.1(187.3km)
6 Mar
18 hours
10 earthquakes
PS20210316.1(73.2km)
15 Mar
17 hours
5 earthquakes
PS20210406.1(59.0km)
5 Apr
15 hours
6 earthquakes
PS20210407.1(131.1km)
7 Apr
15 hours
9 earthquakes
PS20210427.1(67.6km)
26 Apr
1 day 14 hours
10 earthquakes
PS20210429.1(69.2km)
29 Apr
19 hours
8 earthquakes
PS20210725.1(24.1km)
25 Jul
8 hours
5 earthquakes
2022
PS20220129.1(49.0km)
29 Jan
2 hours
7 earthquakes
2023
PS20230424.1(62.3km)
23 Apr
1 day 12 hours
7 earthquakes
PS20230613.1(91.7km)
13 Jun
23 hours
7 earthquakes
2024
PS20240531.1(68.9km)
31 May
7 hours
5 earthquakes
PS20241016.1(135.0km)
15 Oct
1 day 8 hours
7 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm PS20210304.3 in the Kermadec Islands Region

The Kermadec Islands region lies along the Kermadec-Tonga subduction zone, where the Pacific Plate subducts westward beneath the Australian Plate. This convergent margin produces one of the most seismically active environments on Earth, forming the Kermadec Trench and an associated volcanic arc. Subduction occurs at rates of approximately 5–7 cm per year, generating frequent earthquakes at shallow to intermediate depths as well as occasional great events exceeding magnitude 8.

Seismic swarm PS20210304.3 began at 20:24 on 4 March 2021 and ended at 23:48 on 5 March 2021, spanning 27 hours and 24 minutes. Twenty-one earthquakes were recorded during this interval. Magnitudes ranged from 4.9 to 5.8, with the majority occurring at depths of 10 km and one event at 11 km. The swarm followed the magnitude-8.1 mainshock of 4 March 2021 by several hours and was located 53 km from that event’s epicenter.

The sequence comprised the following events (times in UTC):
4 March 2021 – 20:24:14 (M5.1), 22:32:54 (M5.1), 22:33:45 (M5.8), 23:11:17 (M5.4), 23:28:29 (M4.9), 23:37:09 (M5.6);
5 March 2021 – 00:54:37 (M5.2), 00:58:27 (M5.6), 03:18:46 (M5.1), 07:23:16 (M5.4), 07:23:18 (M5.4), 15:00:46 (M5.0), 15:34:13 (M5.0), 19:34:53 (M5.5), 20:20:43 (M5.3), 20:26:35 (M5.8), 20:45:08 (M5.0), 20:52:41 (M5.1), 21:47:20 (M5.0), 22:34:50 (M5.1), 23:48:28 (M5.0).

Since 1 January 2000, nineteen swarms have been documented in the same region. These occurred in the years 2003 (two), 2005 (one), 2006 (three), 2008 (three), 2011 (one), 2012 (one), 2014 (three), 2016 (one), 2019 (two), 2020 (one), and 2021 (one).

Strong earthquakes (M ≥ 7.0) recorded since 2000 within roughly 100 km of the swarm center include:
M7.1 on 24 April 2023 (92 km distant);
M7.0 on 16 March 2023 (66 km distant);
M8.1 on 4 March 2021 (53 km distant);
M7.6 on 6 July 2011 (77 km distant);
M7.0 on 29 September 2008 (83 km distant).

The repeated occurrence of both swarms and great earthquakes underscores the persistent strain accumulation and release along this rapidly converging plate boundary. Continued monitoring remains essential for understanding short-term clustering and long-term seismic hazard in the Kermadec arc.

References

USGS Earthquake Catalog (earthquake.usgs.gov)
GNS Science New Zealand seismic reports
Global CMT Catalog (globalcmt.org)