Seismic Swarm S20190812.1 Near Trona, California: Geological Context and Event Analysis
The seismic swarm designated S20190812.1 occurred approximately 17 km south of Trona in San Bernardino County, California. This sequence began at 00:05 UTC on 12 August 2019 and concluded at 06:08 UTC on 15 August 2019, spanning 78 hours and 3 minutes. During this period, 50 earthquakes were recorded, providing a detailed snapshot of localized crustal activity in the region.
The Trona area lies within the Searles Valley, part of the Mojave Desert's tectonically active landscape. This zone forms a transition between the Eastern California Shear Zone and the Basin and Range Province, where northwest-trending strike-slip faults accommodate dextral shear between the Pacific and North American plates. The Garlock Fault, located nearby to the north, and segments of the San Andreas system influence regional strain accumulation. Historical deformation has produced both strike-slip and normal faulting, with Quaternary sediments overlying crystalline basement rocks that facilitate shallow seismicity.
Seismic swarms in this setting often reflect fluid migration or aseismic slip along fault networks rather than mainshock-aftershock sequences. The 2019 activity aligns with patterns observed in prior events, underscoring the area's persistent low-to-moderate seismicity. Since 2000, three swarms have been documented in the vicinity, with one occurring in 2013 and two in 2019.
Analysis of the S20190812.1 sequence reveals predominantly small-magnitude events. The largest recorded shocks reached 2.4 on 12 August at 19:36:14 UTC (depth 10 km) and 2.2 on both 14 August at 18:32:30 UTC (depth 7 km) and 15 August at 06:08:18 UTC (depth 4 km). Most events clustered between magnitudes 0.6 and 2.1, with depths ranging from 1 km to 14 km. Shallower events (under 5 km) were frequent during the initial 24 hours, while deeper activity (8–14 km) appeared sporadically on 13–15 August. Temporal distribution showed peak rates on 12 August, with 32 events, followed by a decline to 13 events on 13–14 August and 5 on 15 August.
These characteristics indicate a compact source volume consistent with swarm behavior in the Eastern California Shear Zone. No damage or felt reports were associated with the sequence, typical for events below magnitude 3.0 in this sparsely populated desert terrain.
The swarm's timing followed the major July 2019 Ridgecrest sequence by roughly one month, suggesting possible stress triggering across nearby fault strands, though direct causal links remain under study by regional networks.
References
- United States Geological Survey Earthquake Catalog (earthquake.usgs.gov)
- California Geological Survey, Regional Fault and Seismic Hazard Reports
- SeismoSight internal swarm classification database