Seismic Swarm S20180522.1 Near Cold Springs, Nevada
A seismic swarm designated S20180522.1 occurred 7 km west-southwest of Cold Springs, Nevada, on 22 May 2018. The sequence began at 03:43 UTC and concluded at 19:36 UTC, spanning 15 hours and 53 minutes. During this interval, 26 earthquakes were recorded.
The events exhibited very low magnitudes, ranging from -0.3 to 0.8. Depths varied between 4 km and 15 km, with the majority concentrated between 4 km and 8 km. Activity remained sporadic in the morning hours before intensifying in the early afternoon, with multiple events clustered around 16:00–16:18 UTC. The swarm displayed no dominant mainshock, consistent with swarm-type behavior driven by distributed stress release rather than a single large rupture.
The Cold Springs area lies in western Nevada within the Basin and Range Province. This extensional tectonic regime features active normal faulting and distributed crustal deformation. Regional seismicity arises from ongoing extension between the Sierra Nevada and the stable North American interior, with numerous Quaternary faults capable of producing small to moderate earthquakes. Historical records indicate persistent microseismicity in the vicinity, often manifesting as short-lived swarms.
Since 1 January 2000, 24 swarms have been documented in the region. Notable years include 2013 (7 swarms), 2008 (6 swarms), and 2011 (5 swarms). Earlier activity occurred in 2005, 2010, 2012, and 2014. These repeated swarm episodes reflect the area’s structural complexity and sensitivity to minor stress perturbations.
The 2018 swarm fits the established pattern of low-magnitude, shallow-to-mid-crustal activity. Such sequences typically last hours to days and rarely produce felt shaking or surface rupture. Continued monitoring supports improved understanding of fault interactions in this portion of the Walker Lane transition zone.
Data for this analysis derive from internal SeismoSight classifications. Geological context is drawn from standard references on Basin and Range tectonics.