Seismic Swarm S20241220.1 Near Pāhala, Hawaii
A seismic swarm designated S20241220.1 occurred south of Pāhala on the Island of Hawaii, beginning at 04:26 on 19 December 2024 and concluding at 23:41 on 20 December 2024. Over 43 hours and 15 minutes, the sequence produced 42 earthquakes. Magnitudes ranged from 1.2 to 2.9, with the majority falling between 1.5 and 2.5. Focal depths clustered tightly around 28–34 km, indicating a consistent source volume beneath the Kaʻū district.
The swarm initiated with a magnitude-2.0 event at 30 km depth. Activity intensified during the evening of 19 December, including a magnitude-2.9 shock at 34 km. Subsequent events maintained similar depths while showing a gradual decline in rate through 20 December, ending with a magnitude-1.9 event at 29 km. This pattern is characteristic of volcanic or magmatic swarm sequences, in which numerous events of comparable size occur without a single dominant mainshock.
Pāhala lies on the southern flank of Kīlauea volcano within the active volcanic zone of the Big Island. The region experiences persistent seismicity driven by magma movement, flank slip along the décollement, and crustal stresses associated with the Hawaiian hotspot. Earthquakes at 25–35 km depth commonly reflect processes near the base of the volcanic edifice or within the underlying oceanic crust.
Seismic swarms have been recurrent in this area since at least 2000. Records document 110 swarms through 2024, with notable increases in frequency after 2018. Annual counts rose from single digits in the early 2000s to 22 swarms in 2023 and 13 in 2024. These episodes frequently accompany inflation or deflation cycles at Kīlauea and Mauna Loa, underscoring the link between swarm activity and magmatic recharge.
The December 2024 swarm fits within this established framework. Its duration, magnitude distribution, and depth range align with previously observed swarms south of Pāhala. No surface deformation or eruptive activity has been associated with this particular sequence, consistent with many past non-eruptive swarms in the same locale.
Continued monitoring by the Hawaiian Volcano Observatory remains essential. Swarms in this region can precede changes in volcanic unrest, although most remain isolated seismic events without immediate hazard implications.
References
- U.S. Geological Survey Hawaiian Volcano Observatory reports on Kīlauea seismicity
- SeismoSight internal swarm catalog (S20241220.1 parameters)
- Historical swarm statistics compiled from USGS earthquake archives, 2000–2024