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Location:
Period:
2 Nov 2024 04:54:45 - 4 Nov 2024 16:28:57 (2 days 11 hours 34 minutes)
Volcanoes in 100km radius:
Kama'ehuakanaloa(10km), Kilauea(63km), Mauna Loa(81km)
Earthquakes:
59
6 swarms found nearby.
2001
10 Sep
3 days 13 hours
50 earthquakes
2005
7 Dec
3 days 11 hours
117 earthquakes
2017
S20170629.1(10.7km)
29 Jun
2 days 9 hours
51 earthquakes
2020
11 May
3 days 16 hours
131 earthquakes
2021
S20210205.1(24.4km)
4 Feb
25 days 20 hours
475 earthquakes
S20211216.1(11.2km)
15 Dec
2 days 7 hours
38 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20241102.1 Near Naalehu, Hawaii

A seismic swarm designated S20241102.1 was recorded 42 km east-southeast of Naalehu on Hawaii’s Big Island. The sequence began at 04:54 on 2 November 2024 and concluded at 16:28 on 4 November 2024, spanning 59 hours and 34 minutes. During this interval, 59 earthquakes were registered.

The events clustered at shallow depths between 4 km and 13 km, with the majority occurring between 9 km and 11 km. Magnitudes ranged from 1.3 to 4.3. The largest shock, magnitude 4.3, struck at 22:05 on 2 November at a depth of 5 km. Other notable events included a magnitude 3.9 at 09:49 on 2 November (11 km depth) and a magnitude 3.8 at 00:33 on 3 November (10 km depth). Activity showed two distinct peaks on 2 November, followed by a gradual decline through 4 November.

This swarm occurred within the tectonically active south flank of Kilauea volcano. The region experiences frequent seismicity driven by magma movement, gravitational spreading of the volcanic edifice, and slip along the basal decollement fault. Depths recorded in the swarm align with the typical range for both volcanic-tectonic and shallow crustal events in this sector.

Since 1 January 2000, six comparable swarms have been documented in the same area: one each in 2001, 2005, 2017, and 2020, and two in 2021. These episodes illustrate the recurring nature of clustered seismicity linked to ongoing volcanic and flank dynamics.

The November 2024 swarm fits the established pattern of short-duration, moderate-magnitude sequences that release strain without producing significant surface deformation or eruptive activity. Continued monitoring remains essential given the proximity to populated coastal communities and the potential for larger flank earthquakes.

References

  • SeismoSight internal swarm classification S20241102.1
  • Hawaiian Volcano Observatory seismic catalogs (historical swarm records)