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Location:
Period:
19 Oct 2020 21:04:52 - 11 Nov 2020 16:14:57 (22 days 19 hours 10 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
647
11 swarms found nearby.
2007
PS20071002.1(108.1km)
2 Oct
2 hours
5 earthquakes
2020
PS20200722.1(84.5km)
22 Jul
15 hours
6 earthquakes
PS20201019.2(24.4km)
19 Oct
1 day 4 hours
12 earthquakes
19 Oct
5 days 0 hours
74 earthquakes
S20201021.2(24.3km)
20 Oct
2 days 3 hours
40 earthquakes
S20201027.1(22.1km)
26 Oct
10 days 18 hours
233 earthquakes
S20201115.1(13.8km)
14 Nov
5 days 11 hours
97 earthquakes
S20201210.1(10.1km)
9 Dec
1 day 13 hours
36 earthquakes
2025
S20250716.3(11.8km)
16 Jul
30 days 21 hours
1640 earthquakes
16 Jul
7 days 2 hours
211 earthquakes
S20250728.1(12.8km)
27 Jul
2 days 4 hours
44 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20201020.1: Analysis of Activity Near Sand Point, Alaska

Seismic swarm S20201020.1 was recorded 88 km south-southeast of Sand Point, Alaska, beginning at 21:04 on 19 October 2020 and concluding at 16:14 on 11 November 2020. Over 547 hours and 10 minutes, the sequence produced 647 earthquakes. This event occurred within the tectonically active Shumagin Islands region of the Alaska Peninsula, part of the Aleutian subduction zone where the Pacific Plate converges with and subducts beneath the North American Plate at rates of approximately 6–7 cm per year.

The subduction interface generates frequent seismicity, including both megathrust events and intraslab earthquakes. Depths in this swarm predominantly ranged between 17 and 30 km, consistent with activity near or within the subducting slab. Initial events included multiple magnitude 4+ shocks, with the largest reaching 4.9. Magnitudes across the first 100 recorded events spanned 2.2 to 4.9, with the majority falling between 3.0 and 3.8. Depths for these events varied from 8 km to 52 km, though clustering remained tight around 20–27 km for most shocks.

Temporal distribution showed intense early activity, with 19 magnitude 4+ events occurring within the first 48 hours. Subsequent events maintained moderate energy release without escalation to a single dominant mainshock, characteristic of swarm behavior driven by fluid migration or slow slip along the plate interface. Historical records since 2000 indicate only three prior swarms in the immediate area, occurring in 2007 (one swarm) and 2020 (two swarms total, including the present sequence).

The Shumagin segment has long been recognized for its seismic potential, with paleoseismic evidence of past great earthquakes. Ongoing monitoring by regional networks supports improved understanding of swarm recurrence and their relationship to broader subduction dynamics. No significant surface deformation or volcanic unrest was associated with this sequence.

References

USGS Earthquake Catalog
Alaska Earthquake Center reports
SeismoSight internal swarm classification data