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Location:
Period:
7 May 2017 23:01:53 - 11 May 2017 09:02:49 (3 days 10 hours)
Volcanoes in 100km radius:
Gareloi(33km), Tanaga(40km), Takawangha(44km), Bobrof(79km), Kanaga(96km)
Earthquakes:
165
14 swarms found nearby.
2006
PS20060708.1(69.2km)
8 Jul
9 hours
10 earthquakes
PS20060826.1(76.1km)
26 Aug
47 minutes
6 earthquakes
2007
PS20071219.1(73.2km)
19 Dec
19 hours
12 earthquakes
2008
VS20080416.1(30.0km)
15 Apr
3 days 6 hours
89 earthquakes
2012
S20120927.1(24.6km)
26 Sep
10 days 9 hours
594 earthquakes
S20121018.1(29.2km)
17 Oct
3 days 8 hours
60 earthquakes
2013
21 Jan
3 days 11 hours
62 earthquakes
2017
S20170501.2(24.3km)
30 Apr
23 days 10 hours
1627 earthquakes
S20170508.2(23.2km)
8 May
3 days 22 hours
59 earthquakes
S20170527.1(10.5km)
26 May
18 days 7 hours
298 earthquakes
2018
S20180927.1(15.3km)
27 Sep
1 day 9 hours
40 earthquakes
2019
S20190909.1(22.7km)
9 Sep
1 day 19 hours
112 earthquakes
2020
PS20200126.1(111.8km)
26 Jan
18 hours
8 earthquakes
2023
13 Jun
1 day 7 hours
40 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20170508.1: Analysis of Activity Near Adak, Alaska

A notable earthquake swarm, designated S20170508.1, occurred approximately 127 km west-southwest of Adak, Alaska, in the central Aleutian Islands. The sequence began at 23:01 UTC on 7 May 2017 and concluded at 09:02 UTC on 11 May 2017, spanning 82 hours and producing 165 recorded events. This swarm reflects the intense tectonic activity characteristic of the region. Analysis of the first 100 events reveals a concentration of shallow seismicity. Magnitudes ranged from 2.5 to 4.5, with the largest event (M4.5) occurring at 22:22 on 8 May at a depth of 10 km. Depths varied between 1 km and 21 km, though the majority clustered near 10 km. Activity intensified on 8 May, featuring multiple events above M3.5 within a short window, including a cluster between 17:10 and 17:30 UTC. Subsequent days showed a gradual decline, with events becoming less frequent and generally smaller after 9 May. The temporal pattern indicates a classic swarm progression driven by fluid migration or stress transfer rather than a single mainshock-aftershock sequence. The Aleutian Islands lie along the convergent boundary where the Pacific Plate subducts beneath the North American Plate at rates exceeding 6 cm per year. This subduction generates the Aleutian megathrust and associated volcanic arc, producing frequent earthquakes at depths from shallow crustal levels to over 200 km. The central Aleutians, including the area near Adak, experience elevated seismicity due to the oblique convergence and complex slab geometry. Historical records document numerous swarms in this segment, consistent with episodic slip or magmatic processes. Since 2000, eight swarms have been identified in the immediate region, occurring in 2006 (two swarms), 2007, 2008, 2012 (two swarms), 2013, and 2017. These events underscore the persistent seismic hazard in the central Aleutians, where monitoring supports tsunami and volcanic risk assessment.

References

USGS Earthquake Hazards Program, Aleutian Arc tectonics overview. Alaska Earthquake Center regional seismicity reports.