M 7.2; 2023 Sand Point, Alaska Earthquake; (16 Jul 2023) (71km from the swarm center)
M 7.6; 2020 Sand Point, Alaska Earthquake; (19 Oct 2020) (33km from the swarm center)
Seismic Swarm PS20201019.2: Analysis of Activity Near Sand Point, Alaska
The seismic swarm PS20201019.2 occurred in the tectonically active region 119 km south-southeast of Sand Point, Alaska, within the Aleutian subduction zone. This setting arises from the convergence of the Pacific Plate and the North American Plate, where the Pacific Plate subducts northwestward at rates of 6–7 cm per year. The interaction generates frequent earthquakes, volcanic activity along the Aleutian arc, and associated seismic swarms due to stress transfer along the megathrust interface and crustal faults.
The swarm initiated at 20:54 UTC on 19 October 2020 with a magnitude 7.6 event at 28 km depth and concluded at 01:17 UTC on 21 October 2020. Over 28 hours and 23 minutes, 12 earthquakes were recorded. The sequence included a magnitude 5.7 event at 22 km depth shortly after the mainshock, followed by additional events ranging from magnitude 3.9 to 5.9 at depths between 12 km and 30 km. Notable shocks comprised magnitudes 5.7 (26 km), 5.0 (16 km), 5.2 (22 km), 5.5 (26 km), 5.1 (27 km), 5.9 (30 km), 5.6 (12 km), and two final magnitude 5.1 events at 22 km and 18 km.
This activity aligns with the broader historical pattern of the region. Since 1 January 2000, ten seismic swarms have been documented near Sand Point, with prior episodes in 2007 (one swarm) and 2011 (two swarms), followed by seven in 2020. The 2020 swarm occurred amid a period of elevated seismicity that also featured strong earthquakes, including a magnitude 7.6 event on 19 October 2020 located 33 km from the swarm center, a magnitude 7.2 event on 16 July 2023 at 71 km distance, and a magnitude 7.3 event on 16 July 2025 at 59 km distance.
Such swarms reflect episodic stress release in a subduction environment prone to both mainshock-aftershock sequences and clustered swarm behavior. Depths in the 12–30 km range indicate activity within the overriding plate and near the plate interface, consistent with the regional geology shaped by prolonged subduction since the Mesozoic era.
References
SeismoSight internal classification data for swarm PS20201019.2 and regional statistics.