Seismic Swarm VS20130516.1: Analysis of Activity Near Calipatria, California
An earthquake swarm designated VS20130516.1 occurred 10 km northwest of Calipatria in California's Imperial Valley. The sequence began at 01:29 on 16 May 2013 and concluded at 23:02 on 21 May 2013, spanning 141 hours and 33 minutes. During this interval, 135 earthquakes were recorded. The Imperial Valley lies within the Salton Trough, a tectonically active pull-apart basin formed by the interaction of the San Andreas and San Jacinto fault systems. This region experiences frequent seismic swarms driven by right-lateral strike-slip faulting, geothermal fluid migration, and crustal extension associated with the Pacific-North America plate boundary.
Analysis of the first 100 events reveals predominantly shallow hypocenters between 0 and 7 km depth, consistent with activity in the brittle upper crust. Magnitudes ranged from 0.2 to 3.5, with the largest event (M3.5) occurring at 03:07 on 17 May 2013 at 1 km depth. Early activity on 16 May featured numerous events below M1.0, followed by a gradual increase in both rate and magnitude on 17 May. No single dominant mainshock was evident; instead, the sequence displayed the classic swarm pattern of clustered, similar-sized events without a clear aftershock decay.
The swarm's location places it within the Brawley Seismic Zone, where historical data document repeated swarm episodes linked to the same fault network. Since 1 January 2000, 57 swarms have been identified in the region, distributed across years as follows: 2000 (1), 2001 (1), 2002 (1), 2003 (3), 2004 (1), 2005 (3), 2008 (5), 2009 (11), 2010 (13), 2011 (4), 2012 (11), and 2013 (3). These episodes underscore the area's persistent seismic productivity, often occurring without producing damaging ground motions due to their modest magnitudes and shallow but localized sources.
Geological conditions in the Salton Trough include thick sedimentary fill overlying thinned continental crust, with active geothermal fields enhancing pore-pressure changes that can trigger swarm-like seismicity. Updated regional monitoring by the Southern California Seismic Network continues to track such activity, confirming that swarms remain a characteristic feature of Imperial Valley tectonics rather than isolated anomalies.
- USGS Earthquake Catalog (earthquake.usgs.gov)
- Southern California Seismic Network reports
- SeismoSight internal swarm classification VS20130516.1