Seismic Swarm S20011209.3: Analysis of Activity Near Hebgen Lake, Montana
Seismic swarm S20011209.3 was recorded beginning at 19:08 on 8 December 2001 and concluding at 00:54 on 28 December 2001. The events were located 11 km east-northeast of Hebgen Lake Estates, Montana. Over 461 hours and 46 minutes, a total of 335 earthquakes were registered.
Analysis of the first 100 events reveals predominantly low-magnitude activity. The initial shock reached magnitude 3.1 at a depth of 7 km. Subsequent events clustered between magnitudes -0.4 and 2.1, with the large majority falling below magnitude 1.0. Depths ranged from 1 km to 13 km, centering most frequently around 6–8 km. A single outlier recorded at magnitude -9.9 appears within the sequence but does not alter the overall pattern of shallow microseismicity. The swarm displayed episodic bursts, with elevated rates during the evenings of 8–10 December and again around 13 December.
Hebgen Lake lies within the Intermountain Seismic Belt, a zone of active normal faulting that extends from Arizona into Montana. The region is influenced by Basin and Range extension and proximity to the Yellowstone volcanic system. The Hebgen Lake fault, a west-dipping normal fault, has produced significant historical earthquakes, most notably the magnitude 7.3 event of 17 August 1959. That quake triggered a massive landslide that dammed the Madison River and caused 28 fatalities, underscoring the area’s capacity for damaging seismicity.
Swarm activity in this setting is commonly attributed to fluid migration along pre-existing faults and regional tectonic stress. The 2001 sequence fits this pattern, with events concentrated at shallow crustal depths consistent with hydrothermal or magmatic influences from the nearby Yellowstone hotspot. Since 1 January 2000, twelve such swarms have been documented in the vicinity, including nine in 2000 and three in 2001, indicating recurrent episodic release of strain.
Ongoing monitoring by regional seismic networks continues to track microseismicity in the Hebgen Lake area. These observations contribute to refined hazard assessments for the northern Intermountain region, where both tectonic and volcanic processes remain active.
References
- USGS Earthquake Hazards Program: Hebgen Lake, Montana historical seismicity
- Montana Bureau of Mines and Geology: Regional fault maps and swarm catalogs
- University of Utah Seismograph Stations: Intermountain Seismic Belt reports