Seismic Swarm S20001020.1: Analysis of Activity Near Pahrump, Nevada
SeismoSight recorded seismic swarm S20001020.1 beginning at 22:03 on 19 October 2000 and concluding at 17:58 on 22 October 2000. The sequence unfolded 48 km NNW of Pahrump, Nevada, spanning 67 hours and 55 minutes with a total of 98 earthquakes.
Event magnitudes ranged from -0.3 to 3.4, with the largest shock occurring at 14:02 on 20 October at a depth of 4 km. Depths clustered primarily between 0 and 8 km, indicating shallow crustal sources typical of the region’s extensional regime. The swarm exhibited a rapid onset followed by a gradual decline in frequency, consistent with fluid-driven or stress-triggered sequences rather than a single mainshock-aftershock pattern.
The Pahrump area lies within the southern Basin and Range province, where northwest-directed extension along normal and strike-slip faults accommodates tectonic strain between the Sierra Nevada and the stable North American interior. Historical seismicity in this portion of Nye County reflects ongoing deformation along the Death Valley–Furnace Creek fault system and related structures. Instrumental records since 2000 document two swarms in the immediate vicinity, with S20001020.1 representing the earliest.
This swarm’s temporal distribution shows peak activity within the first 24 hours, after which event rates decreased steadily. Most events remained below magnitude 2.0, underscoring the low-energy character of the sequence while still providing valuable data on local fault behavior and crustal permeability.
Continued monitoring of similar sequences contributes to refined hazard assessments for nearby communities and infrastructure. The shallow focal depths observed reinforce the importance of incorporating swarm statistics into probabilistic seismic models for the western Great Basin.
References
- SeismoSight internal swarm classification database
- USGS Earthquake Catalog (regional tectonic framework)