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Location:
Period:
1 Jun 2003 11:24:24 - 13 Jun 2003 00:50:39 (11 days 13 hours 26 minutes)
Volcanoes in 100km radius:
Earthquakes:
108
M 7.0+:
25 swarms found nearby.
2002
23 Oct
1 day 18 hours
37 earthquakes
S20021103.1(24.7km)
2 Nov
123 days 19 hours
7093 earthquakes
S20021104.2(15.9km)
3 Nov
19 days 3 hours
621 earthquakes
S20021105.2(29.5km)
4 Nov
16 days 23 hours
418 earthquakes
S20021108.1(18.7km)
7 Nov
1 day 2 hours
42 earthquakes
S20021110.1(11.4km)
9 Nov
1 day 17 hours
53 earthquakes
S20021111.1(28.1km)
10 Nov
1 day 16 hours
49 earthquakes
12 Nov
1 day 14 hours
71 earthquakes
S20021125.1(29.2km)
24 Nov
3 days 20 hours
81 earthquakes
S20021126.1(24.9km)
25 Nov
1 day 2 hours
30 earthquakes
S20021201.1(27.4km)
30 Nov
6 days 3 hours
158 earthquakes
S20021211.1(29.2km)
10 Dec
4 days 4 hours
122 earthquakes
S20021220.2(29.8km)
20 Dec
3 days 6 hours
135 earthquakes
S20021225.1(13.5km)
24 Dec
5 days 15 hours
113 earthquakes
S20021227.1(15.1km)
26 Dec
7 days 19 hours
98 earthquakes
S20021229.1(29.7km)
28 Dec
9 days 5 hours
191 earthquakes
2003
S20030101.1(24.7km)
1 Jan
2 days 1 hours
49 earthquakes
6 Jan
4 days 21 hours
72 earthquakes
S20030203.1(29.6km)
2 Feb
3 days 0 hours
42 earthquakes
S20030223.2(27.3km)
22 Feb
1 day 14 hours
31 earthquakes
S20030307.1(17.7km)
6 Mar
26 days 8 hours
396 earthquakes
S20030316.1(29.8km)
15 Mar
1 day 20 hours
37 earthquakes
2 Apr
23 days 4 hours
248 earthquakes
13 Jul
20 days 18 hours
166 earthquakes
7 Aug
6 days 18 hours
95 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Analysis of Swarm S20030602.2: Denali Region, Alaska

Earthquake swarm S20030602.2 occurred approximately 74 km east-southeast of McKinley Park in Alaska's Denali region. The sequence initiated at 11:24 on 1 June 2003 and concluded at 00:50 on 13 June 2003, spanning 277 hours and 26 minutes. During this interval, 108 events were recorded, with the first 100 events providing detailed insight into the swarm's temporal and magnitude distribution.

The events exhibited low to moderate magnitudes, predominantly between 0.8 and 2.4, with the majority under 2.0. Depths remained shallow, ranging from 0 to 25 km, consistent with crustal activity in the area. Temporal clustering was evident, with higher event rates on 2 June and 8 June, including several magnitude 2.0+ shocks. Notable peaks included a 2.4 magnitude event on 5 June at 10 km depth and multiple 2.2 magnitude occurrences on 7–8 June at depths of 1–5 km. Overall, the swarm displayed a typical swarm pattern of numerous small events without a dominant mainshock.

The Denali region lies within the Alaska Range, influenced by the complex interaction between the Pacific and North American plates. The Denali Fault, a major right-lateral strike-slip structure, accommodates significant lateral motion and has hosted major historical ruptures. The 2002 Denali Fault earthquake, magnitude 7.9 on 3 November, occurred just 10 km from the swarm center, highlighting the fault's ongoing activity. Post-2002 aftershock sequences and subsequent swarms indicate continued stress adjustment along fault segments.

Since 1 January 2000, 23 swarms have been documented in the region, with 16 occurring in 2002 and 7 in 2003. These swarms reflect episodic release of strain in a tectonically active zone characterized by both strike-slip and thrust faulting. Depths under 25 km align with the brittle upper crust where most seismicity concentrates.

This swarm underscores the Denali area's persistent microseismicity. Monitoring such sequences aids in understanding fault behavior following large events like the 2002 earthquake. Continued observation remains essential for assessing regional seismic hazards.

References

Alaska Earthquake Information Center (AEIC)
U.S. Geological Survey Earthquake Hazards Program
SeismoSight internal swarm classification records