Seismic Swarm S20190909.2: Analysis of Activity Near Searles Valley, California
Seismic swarm S20190909.2 was recorded in the Searles Valley region of California, beginning at 14:13 on 8 September 2019 and concluding at 03:53 on 10 September 2019. Over 37 hours and 40 minutes, 47 earthquakes were detected, with magnitudes ranging from 0.5 to 2.2 and focal depths between 1 and 11 km. The events clustered approximately 14 km southwest of Searles Valley, an area situated in the Mojave Desert within San Bernardino County.
The swarm exhibited typical characteristics of clustered seismicity, with the largest event reaching magnitude 2.2 at a depth of 6 km early in the sequence. Subsequent activity included multiple events of magnitude 1.0–1.9 distributed across shallow to mid-crustal depths, indicating possible involvement of local fault structures and fluid-related processes. Depths predominantly fell between 3 and 9 km, consistent with brittle failure in the upper crust of this tectonically active zone.
Searles Valley lies within the Eastern California Shear Zone, a broad region of distributed right-lateral strike-slip deformation that accommodates a portion of the Pacific-North America plate motion. The local geology consists of Quaternary alluvial deposits, playa sediments associated with Searles Lake, and underlying basement rocks of Mesozoic age. This setting experiences recurrent seismic activity due to its position between the San Andreas Fault system to the west and the Basin and Range province to the east. Historical records show that earthquake swarms have occurred periodically in the vicinity, reflecting stress adjustments along minor faults rather than mainshock-aftershock sequences driven by a single large rupture.
Since 2000, eight swarms have been identified in the area, with notable occurrences in 2013 (one swarm), 2015 (one swarm), and six swarms in 2019. These episodes underscore the persistent low-to-moderate level of background seismicity in the region, often linked to tectonic loading and occasional magmatic or hydrothermal influences at depth.
The 2019 swarm fits within this pattern of episodic clustering, providing data for refining models of fault interaction in the shear zone. No significant surface rupture or damage was associated with these events, as expected given the modest magnitudes.
References
- United States Geological Survey Earthquake Catalog
- California Geological Survey Regional Fault Maps
- SeismoSight internal swarm classification records