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Location:
Period:
14 Jun 2006 04:22:54 - 2 Jul 2006 23:29:48 (18 days 19 hours 6 minutes)
Volcanoes in 100km radius:
Kiska(28km), Segula(65km), Davidof(78km), Buldir(92km), Little Sitkin(93km)
Earthquakes:
1106
6 swarms found nearby.
2003
PS20030317.1(106.4km)
17 Mar
5 hours
7 earthquakes
2006
PS20060614.1(16.7km)
14 Jun
1 hours
5 earthquakes
S20060614.1(11.9km)
14 Jun
1 day 1 hours
136 earthquakes
S20060614.3(20.5km)
14 Jun
3 days 7 hours
62 earthquakes
2014
PS20140623.2(88.6km)
23 Jun
1 day 3 hours
11 earthquakes
2021
10 Jul
1 day 12 hours
37 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Earthquake Swarm S20060614.2 Near Attu Station, Alaska

The Aleutian Islands form a volcanic arc in the northern Pacific Ocean, resulting from the subduction of the Pacific Plate beneath the North American Plate along the Aleutian Trench. This tectonic setting produces frequent seismic activity, including earthquake swarms, as stress accumulates and releases along the megathrust fault and associated crustal structures. The region near Attu Station, the westernmost community in the United States, lies approximately 282 km east-southeast of the swarm epicenter and experiences elevated seismicity due to its position on the convergent margin. Swarm S20060614.2 began at 04:22 on 14 June 2006 and concluded at 23:29 on 2 July 2006, spanning 451 hours and 6 minutes. During this interval, 1,106 earthquakes were recorded. Analysis of the first 100 events reveals a rapid onset with several events exceeding magnitude 4.0 within the initial hours, followed by a progressive decline in both frequency and magnitude. Depths predominantly ranged between 4 km and 40 km, consistent with activity in the upper crust and near the plate interface. The largest events reached magnitudes of 4.9, 4.8, and 4.7, occurring early in the sequence on 14 June, while later events clustered around magnitudes 2.2 to 3.4. This pattern indicates a typical swarm evolution driven by fluid migration or aseismic slip rather than a single mainshock-aftershock sequence. Seismic swarms in the Aleutians have been documented since at least 2000, with only two recorded prior to and including this event: one in 2003 and the 2006 swarm itself. Such episodes highlight the region's capacity for clustered seismicity without producing large destructive earthquakes, although they contribute to ongoing hazard assessment for the remote island communities and maritime traffic. The Aleutian subduction zone remains one of the most active tectonic boundaries on Earth, with continuous monitoring by regional seismic networks providing critical data for understanding plate-boundary processes.

References

USGS Earthquake Catalog Alaska Earthquake Center historical records