Seismic Swarm S20140821.1: Analysis of Activity Near Hebgen Lake, Montana
Seismic swarm S20140821.1 occurred approximately 4 km east-southeast of Hebgen Lake Estates in Montana, registering 40 earthquakes between 18:36 on 20 August 2014 and 22:47 on 21 August 2014. The sequence lasted 28 hours and 11 minutes, with events exhibiting magnitudes ranging from -0.8 to 2.0 and focal depths between 2 km and 12 km. The majority of events clustered at depths of 8–12 km, consistent with shallow crustal seismicity typical of the region.
Hebgen Lake lies within the Intermountain Seismic Belt, a zone of active tectonism extending from Montana into Idaho and Utah. This belt marks the transition between the stable North American craton and the extensional Basin and Range province, where normal faulting accommodates regional strain. The 1959 Hebgen Lake earthquake, magnitude 7.3, remains the largest historical event in the immediate area and produced significant surface rupture along the Hebgen Lake fault. Ongoing small-magnitude activity reflects continued slip on distributed faults within this extensional regime.
Earthquake swarms in this setting often arise from fluid migration or aseismic slip transients rather than mainshock-aftershock sequences driven by static stress transfer. The 2014 swarm displayed a typical pattern: an initial cluster of events on 20 August followed by a more energetic phase on 21 August, including the largest event of magnitude 2.0 at 06:48. Negative magnitudes indicate microseismicity detectable only by sensitive local networks, highlighting the swarm’s low overall energy release.
Historical records document 51 swarms in the Hebgen Lake region since 2000, with notable concentrations in 2000 (7 swarms), 2008 (6 swarms), 2013 (6 swarms), and 2014 (3 swarms). These recurrent swarms underscore the area’s persistent seismic productivity, driven by its position near the Yellowstone volcanic system’s northwestern margin. Although no direct link to magmatic processes has been established for individual swarms, the broader tectonic framework allows for episodic release of accumulated strain through swarm-like sequences.
Monitoring by regional seismic networks continues to refine understanding of fault interactions and swarm statistics, supporting improved hazard assessment for nearby communities and infrastructure.
References
USGS Earthquake Hazards Program – Hebgen Lake region seismicity reports
Montana Bureau of Mines and Geology – Intermountain Seismic Belt studies
Published literature on the 1959 Hebgen Lake earthquake and Basin and Range extension