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Location:
Period:
23 Jun 2014 21:16:16 - 1 Jul 2014 17:29:31 (7 days 20 hours 13 minutes)
Volcanoes in 100km radius:
Davidof(20km), Little Sitkin(23km), Segula(28km), Kiska(60km), Semisopochnoi(87km)
Earthquakes:
135
12 swarms found nearby.
2003
PS20030317.1(73.0km)
17 Mar
5 hours
7 earthquakes
PS20031117.1(74.1km)
17 Nov
1 day 5 hours
18 earthquakes
2006
PS20060614.1(88.6km)
14 Jun
1 hours
5 earthquakes
2014
PS20140623.2(15.9km)
23 Jun
1 day 3 hours
11 earthquakes
23 Jun
26 days 6 hours
992 earthquakes
S20140624.4(22.7km)
23 Jun
6 days 8 hours
79 earthquakes
S20140624.5(21.2km)
23 Jun
2 days 11 hours
33 earthquakes
2021
S20210622.3(21.8km)
22 Jun
1 day 2 hours
48 earthquakes
VS20211210.1(27.0km)
9 Dec
2 days 12 hours
55 earthquakes
2022
VS20220126.1(21.4km)
25 Jan
3 days 9 hours
91 earthquakes
S20220605.1(16.1km)
4 Jun
4 days 0 hours
74 earthquakes
2024
VS20240610.1(23.0km)
9 Jun
3 days 5 hours
85 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm Activity in the Rat Islands, Aleutian Islands, Alaska

The Rat Islands region of the western Aleutian arc in Alaska lies along the convergent boundary where the Pacific Plate subducts beneath the North American Plate. This tectonic setting produces frequent seismicity, including both shallow crustal events and intermediate-depth earthquakes within the subducting slab. The arc segment is characterized by high volcanic and seismic activity as part of the circum-Pacific Ring of Fire, with historical large-magnitude ruptures documented along the plate interface.

Swarm S20140624.3 was recorded in this region, commencing at 21:16 on 23 June 2014 and concluding at 17:29 on 1 July 2014. Over 188 hours and 13 minutes, a total of 135 earthquakes were detected. Analysis of the first 100 events reveals a sequence dominated by intermediate-depth earthquakes, with focal depths predominantly between 100 km and 140 km. Magnitudes ranged from 1.4 to 4.9, with the largest event reaching 4.9 on 24 June 2014. Early activity included several events above magnitude 4.0 clustered within the first 24 hours, followed by a gradual decline in both frequency and maximum magnitude. A few shallower events, including depths near 0 km and 4–6 km, appeared later in the sequence, though the majority remained consistent with slab-related seismicity.

This swarm represents one of five documented seismic swarms in the Rat Islands area since 2000. Prior episodes occurred in 2003 (two swarms) and 2006 (one swarm), with two additional swarms recorded in 2014. Such swarms typically reflect episodic stress release within the subducting lithosphere rather than mainshock-aftershock sequences driven by a single large rupture.

The 2014 activity aligns with the long-term pattern of clustered intermediate-depth seismicity observed throughout the Aleutian subduction zone. Continued monitoring by regional seismic networks remains essential for distinguishing swarm behavior from potential precursory signals associated with larger interface earthquakes.

References
USGS Earthquake Catalog (earthquake.usgs.gov)
Alaska Earthquake Center, University of Alaska Fairbanks
Global CMT Catalog for focal mechanism data