Seismic Swarm S20201205.1 Near Honaunau-Napoopoo, Hawaii
A seismic swarm designated S20201205.1 was recorded beginning at 17:44 on 4 December 2020 and concluding at 07:35 on 10 December 2020, approximately 20 km east of Honaunau-Napoopoo on the Island of Hawaii. Over 133 hours and 50 minutes, the sequence produced 110 earthquakes. Analysis of the first 100 events reveals predominantly shallow activity, with focal depths ranging from -3 km to 4 km and magnitudes between 0.6 and 4.0. The initial event reached magnitude 4.0 at 4 km depth, followed by numerous events clustered between 1.0 and 3.3 in magnitude during the first two days. Later stages showed a decline in larger events, with most registering below magnitude 2.0.
The region lies on the western flank of the Big Island, where the Hawaiian hotspot has built a volcanic edifice through successive shield volcanoes. Honaunau-Napoopoo sits within the South Kona district, influenced by the ongoing evolution of Mauna Loa and Kilauea. Seismicity here commonly arises from magma migration, crustal adjustment, and fault slip along the Hilina and Kealakekua fault systems. Depths recorded in the swarm align with typical upper-crustal volcanic processes in Hawaii, where events often occur within the first few kilometers beneath the surface.
Historical records indicate that seismic swarms are recurrent in this setting. Since 2000, eleven such swarms have been documented in the broader area, occurring in 2004 (four events), 2006 (one), 2015 (two), 2016 (one), 2017 (two), and 2020 (one). These episodes reflect the dynamic interplay between volcanic loading and tectonic stress release characteristic of the Hawaiian Islands.
Patterns within the December 2020 swarm include repeated low-magnitude aftershocks following the initial magnitude-4.0 event, with many events exhibiting negative depths suggestive of near-surface or slightly elevated sources relative to the reference datum. Activity intensified on 5 and 8 December, featuring several events above magnitude 2.5, before tapering. Such sequences contribute to ongoing monitoring of volcanic unrest and help refine models of crustal deformation in Hawaii's active volcanic zones.
References
USGS Earthquake Catalog
Hawaii Volcano Observatory reports
Hawaiian Volcano Observatory geological summaries