Seismic Swarm S20080603.1: Analysis of Activity Near El Centro, California
Seismic swarm S20080603.1 occurred in the Imperial Valley of southern California, centered 4 km south-southwest of El Centro. The sequence began at 23:52 UTC on 2 June 2008 and concluded at 11:34 UTC on 7 June 2008, spanning 107 hours and 42 minutes. During this interval, 54 earthquakes were recorded.
The events clustered at focal depths predominantly between 13 and 16 km, with isolated shallower and deeper occurrences ranging from 5 km to 19 km. Magnitudes remained modest, peaking at 2.9 on 3 June at 12:51:45 UTC. Other notable events included multiple shocks of magnitude 2.8 on 3 June and several of magnitude 2.5–2.6 distributed across the first three days. The majority of activity concentrated within the first 48 hours, after which event rates declined steadily.
This swarm fits the regional pattern of the Imperial Valley, part of the Salton Trough. The trough formed through oblique extension at the Pacific–North America plate boundary, where the San Andreas Fault system transitions into the Gulf of California rift. Right-lateral strike-slip motion along the Imperial and Brawley faults, combined with localized spreading centers beneath the Salton Sea, produces frequent earthquake swarms rather than isolated mainshock-aftershock sequences. Crustal temperatures are elevated due to recent volcanism and high heat flow, which may facilitate swarm behavior through fluid migration and aseismic slip.
Historical records maintained by SeismoSight indicate four prior swarms in the immediate area since 1 January 2000, occurring in 2000 (one swarm), 2003 (two swarms), and 2005 (one swarm). These episodes share similar magnitude ranges and durations, underscoring the recurrent nature of clustered seismicity in this portion of the Imperial Valley.
The 2008 swarm produced no reported damage or felt reports beyond light shaking near the epicentral zone, consistent with its maximum magnitude. Continued monitoring of the Brawley Seismic Zone remains important given its proximity to critical infrastructure and population centers.
References
SeismoSight internal swarm catalog (S20080603.1 parameters and historical swarm statistics).
United States Geological Survey Earthquake Hazards Program regional tectonic summaries for the Imperial Valley.