Seismic Swarm S20200516.2: Analysis of Activity Near Mina, Nevada
Seismic swarm S20200516.2 occurred 24 km south-southeast of Mina, Nevada, in western Mineral County. The sequence began at 11:17 UTC on 15 May 2020 and concluded at 09:53 UTC on 16 May 2020, spanning 22 hours and 36 minutes. During this interval, 26 earthquakes were recorded, with magnitudes ranging from 1.7 to 4.6.
The largest events included two magnitude 4.6 earthquakes, one at 11:17 on 15 May at a depth of 8 km and another at 04:12 on 16 May at 5 km depth. Additional notable shocks reached magnitude 3.7 at 17:49 on 15 May (5 km depth) and magnitude 3.5 at 17:25 the same day (10 km depth). Depths throughout the swarm clustered between 0 and 16 km, consistent with shallow crustal faulting typical of the region. The sequence displayed a pattern of initial larger events followed by smaller aftershocks, with activity tapering toward the end of the period.
This swarm forms part of recurring seismic episodes in the Mina area. Since 2000, eight swarms have been documented in the immediate vicinity, occurring in 2003 (two events), 2013 (two events), 2014 (one event), and 2020 (three events). Such clustering suggests episodic release of strain along local fault networks rather than isolated mainshock-aftershock sequences.
The Mina region lies within the Walker Lane belt of western Nevada, a zone of distributed right-lateral shear and extension that accommodates a significant portion of Pacific-North America relative plate motion. The local geology is dominated by Basin and Range normal faults superimposed on earlier Mesozoic and Cenozoic structures. Quaternary fault scarps and volcanic rocks indicate ongoing tectonic activity, with the area experiencing moderate seismicity driven by northwest-directed extension and shear.
Historical records show that Mineral County and adjacent regions have hosted damaging earthquakes, underscoring the potential for larger events amid swarm activity. The 2020 swarm aligns with this tectonic framework, where fluid migration or aseismic slip may trigger clustered seismicity along favorably oriented faults.
Further monitoring by regional seismic networks continues to refine understanding of strain accumulation in this portion of the Walker Lane.
References
USGS Earthquake Catalog
Nevada Seismological Laboratory records
SeismoSight internal swarm classification database