Seismic Swarm S20160805.1: Analysis of Activity Near Hawthorne, Nevada
An earthquake swarm designated S20160805.1 occurred 32 km SSW of Hawthorne, Nevada, registering 205 events over 127 hours and 22 minutes from 14:00 on 4 August 2016 to 21:23 on 9 August 2016. This sequence reflects typical swarm behavior in the region, with events clustered in time and space without a dominant mainshock. Analysis of the first 100 events reveals predominantly low-magnitude activity. Initial events on 4 August began with magnitudes between 0.3 and 1.0 at depths of 8–12 km. Activity intensified on 5 August, including a magnitude 2.7 event at 9 km depth and a magnitude 1.7 event at 8 km. Depths remained consistent, averaging around 9–10 km, with occasional shallower occurrences near 4–7 km. On 6 August, notable events reached magnitudes of 2.5, 2.1, 1.6, and 1.4, all at depths of 7–11 km. Negative magnitudes appeared sporadically, indicating microseismicity, while the overall pattern showed a gradual decline in frequency after the peak period. The swarm aligns with historical patterns in the area. Since 2000, 18 swarms have been documented near Hawthorne, with notable clusters in 2011 (7 swarms), 2006 (3 swarms), and 2015 (3 swarms). Earlier episodes occurred in 2001, 2004, and 2013. These recurrent swarms underscore ongoing seismic unrest without progression to larger, damaging earthquakes. The Hawthorne region lies in western Nevada within the Basin and Range Province, where extensional tectonics drive normal faulting along north-trending structures. This setting forms part of the broader Walker Lane belt, accommodating right-lateral shear between the Pacific and North American plates. Crustal extension here produces frequent small earthquakes and occasional swarms, often at depths of 5–15 km, consistent with the observed event distribution. Updated regional monitoring confirms persistent low-level seismicity tied to these faults. Such swarms provide valuable data for understanding stress accumulation in the province. Continued observation supports hazard assessment in this tectonically active zone.
References
SeismoSight internal swarm classification records.
USGS Earthquake Hazards Program regional tectonic summaries.
Nevada Seismological Laboratory historical earthquake database.