Seismic Swarm S20250420.2 Near Goldfield, Nevada: Characteristics and Regional Context
Seismic swarm S20250420.2 was recorded 38 km south of Goldfield, Nevada, commencing at 18:54 on 19 April 2025 and concluding at 08:30 on 22 April 2025. Over 61 hours and 35 minutes, the sequence produced 49 earthquakes. Magnitudes ranged from 0.3 to 2.3, with the largest event occurring at 07:20 on 21 April. Focal depths were predominantly shallow, between 0 and 9 km, consistent with activity in the upper crust.
The swarm exhibited a typical pattern of clustered, low-magnitude events without a dominant mainshock. Early activity on 19–20 April included events of magnitude 1.0–2.1 at depths of 2–9 km. Activity intensified on 20 April with multiple events above magnitude 1.0, followed by a gradual decline. On 21 April, the sequence peaked with the magnitude 2.3 event and several others near magnitude 2.0 at depths around 4–5 km. The final events on 22 April were smaller, below magnitude 1.6. This temporal distribution reflects the episodic nature common in swarm sequences.
The Goldfield area lies in Esmeralda County within the Basin and Range Province. The region experiences extensional tectonics driven by normal and strike-slip faulting along the Walker Lane belt, which accommodates a portion of Pacific–North American plate boundary deformation. Historical earthquake swarms in this setting are frequently linked to fluid movement along pre-existing faults rather than magmatic processes.
Since 1 January 2000, 23 swarms have occurred in the same vicinity. These events cluster in specific years: one each in 2000, 2001, 2002, 2004, 2005, 2006, 2011, 2012, 2017, 2019, 2020 and 2021; two each in 2007, 2010 and 2015; and four in 2024. The current swarm continues this pattern of recurrent, moderate activity, underscoring persistent crustal stress release in the Goldfield region.
Such swarms contribute to the broader seismic hazard assessment for central Nevada. Although individual events remain small, their frequency indicates ongoing fault interactions that warrant continued monitoring by regional seismic networks.
References
- SeismoSight internal swarm classification database (S20250420.2 parameters and historical statistics).
- USGS Earthquake Catalog (regional tectonic framework for Esmeralda County, Nevada).