Seismic Swarm S20200213.1: Analysis of Activity Near Ridgecrest, California
Seismic swarm S20200213.1 was recorded in the Ridgecrest region of California, beginning at 12:31 on 12 February 2020 and concluding at 10:57 on 18 February 2020. The sequence lasted 142 hours and 26 minutes, during which 159 earthquakes were detected at a location 14 km ENE of Ridgecrest. This activity occurred within the Eastern California Shear Zone, a tectonically active area characterized by northwest-trending strike-slip faults that accommodate a portion of the Pacific-North American plate boundary motion.
Analysis of the first 100 events reveals predominantly low-magnitude seismicity. Magnitudes ranged from -0.6 to 2.4, with the majority falling between 0.0 and 1.5. The largest events in this subset reached 2.3 and 2.4. Depths were shallow, concentrated between 1 km and 11 km, consistent with brittle failure in the upper crust. Temporal distribution showed clustering in the initial hours, followed by a gradual decline, typical of swarm behavior where no single mainshock dominates.
The Ridgecrest area lies near the intersection of the Garlock Fault and the Little Lake Fault Zone. These structures have produced historical seismicity, including the significant 2019 Ridgecrest Earthquake Sequence. That sequence featured a magnitude 7.1 mainshock on 6 July 2019, located 14 km from the center of swarm S20200213.1. The 2019 events highlighted the region's capacity for large earthquakes and extensive aftershock sequences.
Historical records since 2000 indicate 25 swarms in the vicinity, with notable concentrations in 2019 (19 swarms) and additional activity in 2013, 2015, and 2020. Swarm S20200213.1 represents one of four documented in 2020. Such recurrent swarms reflect ongoing strain accumulation and release along local fault networks in the Mojave Desert block.
This swarm underscores the persistent seismic hazard in the Ridgecrest area, where shallow crustal earthquakes can occur in clusters without a clear triggering mainshock. Continued monitoring supports improved understanding of fault interactions in the shear zone.
References
USGS Earthquake Catalog (historical seismicity and 2019 Ridgecrest sequence details)
SeismoSight internal swarm classification records (S20200213.1 parameters and event list)