Seismic Swarm S20160321.1 Near Hawthorne, Nevada
Seismic swarm S20160321.1 occurred 22 km east-southeast of Hawthorne, Nevada, beginning at 07:37 UTC on 21 March 2016 and concluding at 13:37 UTC on 7 April 2016. Over 414 hours, the swarm produced 779 earthquakes. This sequence is consistent with the region's tectonic setting within the Walker Lane belt, a zone of distributed right-lateral shear and extension that accommodates a portion of the Pacific-North America plate motion.
The first 100 events provide a representative view of swarm behavior. The sequence initiated with a magnitude 4.3 earthquake at 9 km depth. Subsequent events were predominantly smaller, with magnitudes clustered below 1.0 and focal depths mostly between 2 km and 5 km. Several events reached magnitudes of 2.0–3.4, including a 3.3 quake at 5 km depth and a 3.4 event at 4 km depth. Depths ranged from surface-near (0 km) to a maximum of 9 km, reflecting brittle failure within the shallow crust typical of Basin and Range normal faulting.
Hawthorne lies in Mineral County within the western Great Basin. The area experiences active extensional tectonics driven by northwest-directed shear along the Walker Lane and associated normal faults. Historical records document recurrent seismic swarms in this corridor, often linked to fluid migration or aseismic slip on favorably oriented faults. Since 2000, twelve swarms have been identified in the immediate vicinity, with notable activity in 2014 (four swarms) and 2015 (four swarms).
Swarm characteristics—high event rates, absence of a single dominant mainshock, and shallow focal depths—align with patterns observed in other Walker Lane sequences. The 2016 swarm's duration of roughly 17 days and total event count fall within the range documented for prior episodes in the same locale.
References
- SeismoSight internal swarm catalog (S20160321.1 parameters)
- USGS Earthquake Catalog (regional tectonics and historical context)