Seismic Swarm S20200208.1 Near Searles Valley, California
Seismic swarm S20200208.1 was recorded 13 km SSW of Searles Valley, California. The sequence began at 09:12 on 7 February 2020 and concluded at 05:08 on 9 February 2020, spanning 43 hours and 55 minutes. During this interval, 44 earthquakes were registered. Magnitudes remained predominantly low, ranging from negative values to a peak of 2.8, with the majority falling between 0.0 and 1.6. Focal depths clustered between 0 km and 11 km, indicating shallow crustal activity typical of the region.
The swarm exhibited a classic pattern of clustered, low-magnitude events without a dominant mainshock, consistent with swarm behavior observed in tectonically active zones. Event timing showed initial activity on 7 February with several events above magnitude 1.0, followed by sustained lower-magnitude occurrences through 8 February, and a final notable event of magnitude 2.8 on 9 February.
The Searles Valley region lies within the Eastern California Shear Zone, a broad area of distributed right-lateral strike-slip faulting that accommodates a portion of the Pacific-North American plate boundary motion. This zone features numerous northwest-trending faults and is subject to ongoing deformation. The local geology includes Quaternary alluvium, lacustrine deposits from ancient Searles Lake, and surrounding basement rocks of Mesozoic age. The area experiences elevated seismic hazard due to its position between the San Andreas Fault system to the west and the Basin and Range province to the east.
Historical records since 2000 document 29 swarms in the vicinity, with notable concentrations in 2019 (23 swarms) and additional episodes in 2013, 2015, and 2020 (four swarms total). These recurrent swarms reflect persistent microseismicity along minor faults and fractures. The July 2019 Ridgecrest earthquake sequence, highlighted by a magnitude 7.1 mainshock located 11 km from the swarm center, significantly altered local stress conditions and likely contributed to subsequent seismic episodes, including this 2020 swarm.
Such swarms provide insight into post-mainshock relaxation processes and fluid migration within the crust. Continued monitoring remains essential given the region's demonstrated capacity for both swarm activity and larger events.
References
SeismoSight internal swarm classification S20200208.1
USGS Earthquake Catalog and regional fault database
California Geological Survey seismic hazard reports