Seismic Swarm S20240209.1: Analysis of Activity Near Pāhala, Hawaii
Seismic swarm S20240209.1 occurred 15 km east-southeast of Pāhala on Hawaii's Big Island. The sequence began at 16:14 on 8 February 2024 and concluded at 10:00 on 13 February 2024, spanning 113 hours and 45 minutes. A total of 200 earthquakes were recorded during this period.
The first 100 events displayed magnitudes ranging from 1.5 to 5.8. Depths clustered predominantly between 28 km and 37 km, with a notable subset occurring at or near 0 km depth. Key events included a magnitude 5.8 earthquake at 20:06 on 9 February at 36 km depth, accompanied by several magnitude 3.0–3.4 aftershocks within minutes. Earlier activity featured smaller events around magnitude 2.0–2.7 at depths near 30 km. The sequence showed a concentration of events on 9 February, with repeated pairs of similar-timed quakes at varying depths.
This swarm aligns with patterns observed in Hawaii's volcanic systems, where seismic activity frequently results from magma movement, crustal stress changes, and fault interactions along the island's south flank. Pāhala lies in a region influenced by the active Kīlauea and Mauna Loa volcanoes, part of the Hawaiian hotspot chain. The underlying geology features oceanic crust overlying a mantle plume, producing frequent basaltic eruptions and associated seismicity. Depths around 30 km correspond to the lower crust and upper mantle transition zone, where magma reservoirs often trigger swarms through pressurization or dike propagation.
Historical records since 2000 indicate 31 prior swarms in the area. These occurred in 2014 (1 swarm), 2015 (2), 2017 (1), 2018 (4), 2019 (2), 2020 (7), 2021 (3), 2022 (2), 2023 (8), and 2024 (1). Such recurrent activity underscores the dynamic nature of Hawaii's volcanic flank, where slow slip events and microseismicity are common.
The February 2024 swarm's mix of deep and shallow events suggests complex interactions between magmatic and tectonic processes. No significant surface deformation or eruptive activity was directly linked in available monitoring summaries, though continued vigilance remains essential in this high-hazard zone.
References
- SeismoSight internal swarm classification database (S20240209.1 parameters and event list).
- USGS Hawaiian Volcano Observatory geological summaries on Big Island seismicity and hotspot volcanism.