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Location:
Period:
31 Mar 2015 16:38:05 - 1 Apr 2015 12:53:18 (20 hours 15 minutes)
Volcanoes in 100km radius:
Earthquakes:
26
11 swarms found nearby.
2003
PS20030317.1(106.6km)
17 Mar
5 hours
7 earthquakes
PS20031117.1(65.8km)
17 Nov
1 day 5 hours
18 earthquakes
2005
14 Jun
14 hours
7 earthquakes
14 Jun
23 hours
36 earthquakes
2006
PS20060708.1(101.7km)
8 Jul
9 hours
10 earthquakes
15 Aug
1 day 7 hours
101 earthquakes
PS20060826.1(85.0km)
26 Aug
47 minutes
6 earthquakes
2007
PS20071219.1(100.9km)
19 Dec
19 hours
12 earthquakes
2012
15 Aug
1 day 7 hours
86 earthquakes
2014
PS20140623.2(111.7km)
23 Jun
1 day 3 hours
11 earthquakes
2020
PS20200126.1(51.2km)
26 Jan
18 hours
8 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20150401.2: Earthquake Activity West of Adak, Alaska

Seismic swarm S20150401.2 occurred approximately 297 km west-southwest of Adak, Alaska, in the central Aleutian Islands. The sequence began at 16:38 UTC on 31 March 2015 and concluded at 12:53 UTC on 1 April 2015, spanning 20 hours and 15 minutes. During this period, 26 earthquakes were recorded, with magnitudes ranging from 1.7 to 4.1 and focal depths between 7 km and 30 km.

The swarm initiated with two magnitude-2.2 events at depths of 20 km and 18 km. Activity intensified several hours later, producing four events of magnitude 3.9–4.1 between 18:19 and 18:37 UTC on 31 March. Subsequent events remained predominantly below magnitude 3.0, although additional magnitude-3.9 and 3.8 shocks occurred at 22:53 UTC and 23:39 UTC. Depths showed modest variation, clustering most frequently between 13 km and 25 km.

The Aleutian Islands occupy a tectonically active subduction zone where the Pacific Plate converges with and descends beneath the North American Plate at rates exceeding 6 cm per year. This setting generates frequent intermediate-depth seismicity and occasional volcanic activity along the arc. Adak and the surrounding Andreanof Islands lie within a region characterized by complex faulting and repeated moderate-magnitude earthquake sequences.

Historical records indicate that ten earthquake swarms have been identified in the same general area since 1 January 2000. These occurred in 2003 (two swarms), 2005 (two), 2006 (three), 2007 (one), 2012 (one), and 2014 (one). Swarm sequences in this segment of the arc typically consist of low-to-moderate magnitude events distributed over hours to days, consistent with the pattern observed in S20150401.2.

The 2015 swarm displayed classic swarm characteristics: rapid onset, clustered timing, absence of a single dominant mainshock, and relatively shallow focal depths. Such sequences are commonly attributed to fluid migration or localized stress adjustments within the overriding plate or along the plate interface.

References

  • USGS Earthquake Catalog (earthquake.usgs.gov)
  • Alaska Earthquake Center, University of Alaska Fairbanks
  • SeismoSight internal swarm classification records