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