Seismic Swarm S20020526.1: Analysis of Microearthquake Activity Near Beatty, Nevada
Seismic swarm S20020526.1 was recorded beginning at 11:46 on 25 May 2002 and concluding at 14:15 on 6 June 2002. The events were located 45 km ESE of Beatty, Nevada. Over a duration of 290 hours and 28 minutes, a total of 136 earthquakes were registered. This swarm represents one of several documented seismic episodes in the region since 2000.
The study area lies within the Basin and Range Province of southwestern Nevada, where extensional tectonics dominate. Normal faulting along range-bounding structures accommodates regional crustal stretching. Historical seismic data indicate recurrent swarm activity linked to fluid movement within fault zones rather than large mainshock-aftershock sequences. Since 1 January 2000, eight swarms have occurred in the vicinity, with five events recorded in 2000 and three in 2002.
Examination of the first 100 events reveals predominantly low-magnitude activity. Magnitudes ranged from -0.6 to 2.9, with the majority falling below 0.5. Depths clustered between 7 and 10 km, consistent with shallow crustal processes in the area. The initial event at magnitude -0.5 occurred at 2 km depth, followed shortly by a magnitude 2.9 shock at 9 km. Subsequent events maintained shallow focal depths, suggesting brittle failure within the upper crust.
Temporal distribution shows peak activity during the first 48 hours, with events occurring at intervals of minutes to hours. Later phases exhibited longer quiescence periods. Notable larger events included a magnitude 2.3 shock on 26 May at 8 km depth and a magnitude 1.1 event on 28 May at 9 km depth. Negative magnitudes dominated the catalog, reflecting the swarm's microseismic character.
Geological context supports swarm-style seismicity. The Beatty region features Quaternary fault scarps and proximity to volcanic centers associated with the southwestern Nevada volcanic field. Such settings facilitate episodic fluid pressure changes that trigger diffuse earthquake clusters without significant surface rupture.
This swarm aligns with prior regional patterns of low-energy seismic release. Continued monitoring remains essential for understanding long-term strain accumulation in the Basin and Range Province.
References
SeismoSight internal swarm classification database USGS Earthquake Catalog (regional historical data)