Seismic Swarm S20191016.2 Near Searles Valley, California
Searles Valley lies in the Mojave Desert of southern California, within the Eastern California Shear Zone. This tectonically active region features multiple northwest-trending strike-slip faults that accommodate right-lateral shear between the Pacific and North American plates. The Garlock Fault, a major left-lateral structure, bounds the area to the north and influences local stress regimes. Seismic swarms are common here due to fluid migration and fault interactions in the shallow crust.
The swarm designated S20191016.2 began at 10:39 on 15 October 2019 and concluded at 10:11 on 18 October 2019. It occurred 14 km south-southwest of Searles Valley and produced 108 earthquakes over 71 hours and 31 minutes. Analysis of the first 100 events reveals predominantly low-magnitude activity. Magnitudes ranged from -0.3 to 2.8, with the majority between 0.5 and 1.6. Depths were shallow, concentrated between 1 km and 9 km, consistent with brittle failure in the upper crust.
Temporal distribution showed peak rates during the first 24 hours, followed by a gradual decline. Early events included several above magnitude 1.5, such as the 2.2 at 00:44 on 16 October and the 2.7 at 22:27 on the same day. Later events remained below magnitude 2.0. Depth variations stayed consistent, rarely exceeding 11 km, indicating a compact source volume.
This swarm aligns with regional patterns observed since 2000, during which 13 swarms have occurred. Prior episodes were recorded in 2013 (one swarm) and 2019 (twelve swarms), underscoring elevated activity that year. Such sequences typically reflect aseismic slip or pore-pressure changes rather than mainshock-aftershock sequences.
References
SeismoSight internal swarm classification S20191016.2
USGS regional fault database for Mojave Desert
California Geological Survey seismic history reports