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Location:
Period:
26 Nov 2018 15:29:36 - 2 Dec 2018 23:22:04 (6 days 7 hours 52 minutes)
Volcanoes in 100km radius:
Great Sitkin(0km), Kasatochi(43km), Moffett(45km), Koniuji(69km), Kanaga(73km), Bobrof(91km)
Earthquakes:
191
34 swarms found nearby.
2002
S20020318.1(17.9km)
17 Mar
2 days 8 hours
75 earthquakes
2013
PS20130831.1(103.4km)
31 Aug
15 hours
5 earthquakes
2018
18 Jan
2 days 7 hours
87 earthquakes
5 Jun
8 days 3 hours
430 earthquakes
30 Jun
1 day 22 hours
35 earthquakes
8 Sep
3 days 3 hours
52 earthquakes
28 Sep
1 day 22 hours
33 earthquakes
27 Oct
7 days 6 hours
253 earthquakes
14 Nov
9 days 8 hours
275 earthquakes
3 Dec
7 days 18 hours
179 earthquakes
20 Dec
2 days 1 hours
30 earthquakes
2019
17 Jun
3 days 10 hours
80 earthquakes
6 Oct
3 hours
37 earthquakes
2020
18 Jan
5 days 5 hours
119 earthquakes
29 Jan
2 days 14 hours
72 earthquakes
2 Feb
1 day 14 hours
37 earthquakes
6 Feb
6 days 21 hours
144 earthquakes
25 Feb
20 days 20 hours
580 earthquakes
20 Mar
31 days 4 hours
579 earthquakes
23 Apr
15 days 9 hours
279 earthquakes
14 May
5 days 18 hours
76 earthquakes
30 May
10 days 21 hours
210 earthquakes
14 Jun
4 days 1 hours
69 earthquakes
5 Jul
11 days 1 hours
252 earthquakes
18 Jul
3 days 5 hours
57 earthquakes
7 Nov
1 day 14 hours
31 earthquakes
2021
25 May
1 day 3 hours
165 earthquakes
22 Jun
2 days 8 hours
34 earthquakes
11 Jul
5 days 5 hours
120 earthquakes
23 Jul
5 days 4 hours
83 earthquakes
28 Jul
8 days 13 hours
161 earthquakes
11 Aug
2 days 19 hours
49 earthquakes
2023
2 Jan
23 hours
30 earthquakes
2025
PS20250320.1(106.9km)
19 Mar
22 hours
5 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm VS20181127.1: Analysis of Activity Near Adak, Alaska

A notable seismic swarm designated VS20181127.1 occurred in the Aleutian Islands region of Alaska, centered 41 km east-northeast of Adak. The sequence began at 15:29 on 26 November 2018 and concluded at 23:22 on 2 December 2018, spanning 151 hours and 52 minutes. During this interval, 191 earthquakes were recorded. Analysis of the first 100 events reveals predominantly low-magnitude activity with shallow focal depths. Magnitudes ranged from -0.8 to 2.6, with the majority falling between -0.5 and 0.5. Depths clustered between -1 km and 9 km, indicating very shallow crustal sources consistent with the tectonic setting. Notable events within this subset included a magnitude 2.6 earthquake at 141 km depth on 29 November and several magnitude 1.2–1.8 events at depths of 2 km. The swarm exhibited a typical pattern of numerous micro-earthquakes interspersed with occasional larger events, without a single dominant mainshock. The Aleutian Islands lie along the convergent boundary where the Pacific Plate subducts beneath the North American Plate at rates of approximately 6–7 cm per year. This subduction drives intense seismicity throughout the arc, including both shallow crustal events and deeper Wadati-Benioff zone activity. The Adak region specifically occupies a segment of the arc characterized by oblique convergence and complex faulting, contributing to frequent earthquake swarms and volcanic unrest. Historical records document nine swarms in the area since 2000, occurring in 2002 (one swarm), 2013 (one swarm), and seven swarms in 2018. Such swarms are common in subduction-zone environments and often reflect fluid migration or stress adjustments along the plate interface rather than a single large rupture. The 2018 activity aligns with the broader seismic character of the central Aleutians, where background rates remain elevated due to ongoing plate motion. References:
USGS Earthquake Catalog (earthquake.usgs.gov)
Alaska Earthquake Center (earthquake.alaska.edu)
SeismoSight internal swarm classification (VS20181127.1)