Seismic Swarm S20100602.1: Analysis of Earthquake Activity Near Ocotillo, California
Seismic swarm S20100602.1 was recorded from 02:49 on 2 June 2010 to 20:52 on 10 June 2010, centered 12 km NNE of Ocotillo, California. Over 210 hours and 3 minutes, the event sequence produced 98 earthquakes. This swarm exemplifies clustered seismic activity typical of the tectonically dynamic Salton Trough region.
The sequence initiated with low-magnitude events around 1.4 to 1.6 at depths of 8 km. Early peaks included two magnitude 2.9 shocks on 2 June at depths of 9 km and 3 km. Subsequent activity featured frequent events between magnitudes 1.0 and 2.0, with depths ranging from 0 km to 11 km. Notable later events encompassed a magnitude 2.7 on 5 June at 8 km depth and a magnitude 2.6 on 7 June at 8 km depth. The swarm concluded with smaller events near magnitude 1.0 to 1.3. Depths predominantly clustered between 3 km and 9 km, indicating shallow crustal involvement.
Ocotillo lies within the Imperial Valley portion of the Salton Trough, a pull-apart basin formed by oblique extension along the Pacific-North American plate boundary. The area experiences distributed faulting associated with the San Andreas system, including the Coyote Creek, Superstition Hills, and Elsinore faults. High heat flow and sedimentary infill contribute to elevated seismicity rates. Historical records show recurrent swarm activity linked to fluid migration and stress transfer in this extensional regime.
Since 1 January 2000, eleven swarms have occurred in the vicinity. Prior episodes took place in 2005 (1 swarm), 2008 (1 swarm), 2009 (3 swarms), and 2010 (6 swarms). These patterns align with the region's history of episodic unrest rather than isolated mainshock-aftershock sequences.
Geological context reveals ongoing rifting that connects the Gulf of California to the San Andreas Fault. The 2010 swarm postdated the April 2010 El Mayor-Cucapah earthquake, suggesting possible triggering through regional stress adjustments. Depths under 11 km reflect brittle failure in the upper crust above ductile lower layers influenced by magmatic and hydrothermal processes.
This swarm underscores the importance of continuous monitoring in tectonically active basins. Data from the sequence provide insights into fault interactions and precursory signals for larger events along the plate boundary.
References
SeismoSight internal swarm classification records.
US Geological Survey earthquake catalog for Imperial County, California.
California Geological Survey regional fault maps and Salton Trough tectonic summaries.