Seismic Swarm S20161211.1: Analysis of Activity Near Pahrump, Nevada
Seismic swarm S20161211.1 occurred approximately 49 km north-northwest of Pahrump, Nevada, between 04:07 on 10 December 2016 and 07:33 on 14 December 2016. Over 99 hours and 26 minutes, the swarm produced 49 earthquakes, with magnitudes ranging from -0.8 to 1.5 and focal depths primarily between 1 and 12 km. This event provides a clear example of clustered microseismicity in the region.
The sequence began with low-magnitude events near 3–8 km depth on 10 December, followed by a cluster of slightly larger events around 19:00–21:00 that included the swarm’s peak magnitude of 1.5 at 21:28. Subsequent activity on 11–13 December remained subdued, with most events below magnitude 0.0 and depths stabilizing near 9–11 km. The final recorded event on 14 December reached magnitude -0.5 at 1 km depth. Depths showed modest variation early in the swarm before converging around 10 km, consistent with shallow crustal faulting.
This swarm fits into a broader pattern of seismic activity documented since 2000. Thirty-nine swarms have occurred in the same area, with notable concentrations in 2000 (5 swarms), 2002 (7), 2008 (6), and 2009 (4). Activity has continued at lower rates in later years, including two swarms in 2016 prior to S20161211.1. Such recurrence indicates persistent, low-level strain release along local structures.
The Pahrump area lies within the southern Basin and Range province, where east-west extension drives normal faulting and distributed seismicity. Regional tectonics reflect interaction between the Sierra Nevada block to the west and stable North American interior to the east. Historical earthquakes in this portion of Nevada have generally remained small, with swarms serving as the dominant mode of energy release rather than mainshock-aftershock sequences.
Ongoing monitoring by regional seismic networks continues to track similar clusters, aiding in the characterization of background rates and potential precursors to larger events. The 2016 swarm underscores the value of dense instrumentation for resolving fine-scale migration of activity at depths of 1–12 km.
References
- SeismoSight internal swarm catalog (S20161211.1 parameters and historical statistics)
- USGS Earthquake Hazards Program regional tectonic summaries for the Basin and Range province