Seismic Swarm S20190619.1: Analysis of Activity Near Sun Valley, Nevada
Seismic swarm S20190619.1 was recorded 2 km southeast of Sun Valley, Nevada, beginning at 04:06 on 19 June 2019 and concluding at 09:43 on 20 June 2019. Over 29 hours and 37 minutes, the sequence produced 103 earthquakes. Analysis of the first 100 events reveals predominantly low-magnitude activity, with values ranging from -0.5 to 1.8. Depths clustered between 3 km and 10 km, indicating shallow crustal sources consistent with regional faulting patterns.
The sequence initiated with microseismic events near magnitude 0.0, followed by a gradual increase in both frequency and peak magnitudes around 07:21. Notable events included a magnitude 1.7 at 07:23 and another at 08:39, both at 8 km depth. Later activity featured a magnitude 1.8 at 13:56 on 19 June. The distribution shows episodic bursts separated by quieter intervals, a hallmark of swarm behavior rather than a mainshock-aftershock sequence.
Sun Valley lies within the Basin and Range Province of western Nevada, where active normal faulting accommodates ongoing east-west crustal extension. The region forms part of the northern Walker Lane belt, a zone of distributed shear and transtension that transfers motion between the Pacific and North American plates. This tectonic setting produces frequent small earthquakes and occasional swarms along Quaternary faults. Historical records document elevated seismicity rates in the Reno-Sun Valley area, driven by the same extensional regime responsible for regional basin formation.
Since 1 January 2000, 36 swarms have occurred in the vicinity. Annual counts include single swarms in 2003, 2004, 2010, and 2017; seven in 2008; two in 2012; eight in 2013; five in 2014; four in 2015 and 2018; and two in 2016. These episodes underscore persistent swarm activity linked to fluid migration and fault interactions within the extensional stress field.
The 2019 swarm aligns with this established pattern, exhibiting similar magnitude ranges and depth distributions. Such events rarely produce surface rupture or significant damage but contribute valuable data on local stress conditions and fault connectivity. Continued monitoring supports improved characterization of seismic hazard in this rapidly urbanizing portion of northern Nevada.
References
- USGS Earthquake Catalog (earthquake.usgs.gov)
- Nevada Seismological Laboratory historical records
- SeismoSight internal swarm classification data