Seismic Swarm S20090620.2: Earthquake Activity near Lake Nacimiento, California
The seismic swarm designated S20090620.2 was recorded in the region 10 km south-southwest of Lake Nacimiento, California. Activity commenced at 08:45 on 20 June 2009 and concluded at 02:02 on 25 June 2009. Over this 113-hour, 16-minute interval, a total of 84 earthquakes were registered.
The sequence displayed classic swarm characteristics, with events distributed across a narrow time window and no single dominant mainshock. Magnitudes ranged from 0.2 to 4.3, with the largest event (M4.3) occurring at 12:32:48 on 20 June at a depth of 5 km. A secondary peak reached M3.2 at 17:55:52 the same day, also at 5 km depth. The majority of hypocenters clustered between 5 km and 6 km, indicating a shallow crustal source consistent with local fault structures. Depths extended from 1 km to 9 km overall, though events deeper than 6 km remained infrequent.
This swarm fits within the established seismic history of the area. Since 1 January 2000, 21 swarms have been documented in the vicinity. Earlier episodes occurred in 2003 (5 events), 2004 (13 events), 2005 (2 events), and 2006 (1 event). Such recurrent swarms reflect ongoing tectonic strain release along secondary faults associated with the broader Pacific–North American plate boundary.
The Lake Nacimiento region lies within the Salinian Block of coastal California, where northwest-trending faults accommodate right-lateral shear. Shallow seismicity at depths of 3–9 km aligns with mapped structures in the area, including segments of the Rinconada Fault system. Historical records indicate that swarm-type sequences are common in this setting, often involving fluid migration or aseismic slip that triggers distributed small-magnitude events rather than large, isolated ruptures.
Analysis of the 2009 swarm shows rapid onset followed by a gradual decay in rate, with most energy released in the first 48 hours. Aftershock productivity remained low relative to the main events, reinforcing the swarm classification. Depths remained stable throughout, suggesting a consistent source volume.
References
SeismoSight internal swarm classification S20090620.2
USGS Earthquake Catalog (regional tectonic framework)