Magnitude 2.2 - 24 miles E of Coldfoot
March 25, 2024 23:10:20 AKDT (March 26, 2024 07:10:20 UTC)
67.2181°N 149.2726°W Depth 6.1 miles (9 km)
This event has been reviewed by a seismologist
- 26 miles (42 km) SE of Wiseman
- 47 miles (76 km) NE of Pump Station #5
- 68 miles (110 km) E of Bettles
- 78 miles (126 km) W of Venetie
- 79 miles (128 km) NW of Beaver
- 83 miles (134 km) S of Pump Station #4
- 84 miles (136 km) N of Stevens Village
- 91 miles (147 km) SE of Anaktuvuk Pass
- 95 miles (154 km) N of Pump Station #6
- 102 miles (165 km) NE of Allakaket
- 113 miles (183 km) S of Pump Station #3
- 170 miles (275 km) N of Fairbanks
- Magnitude type: Ml2
- Event type: earthquake
Tectonic Setting of the Brooks Range
Seismicity in the Brooks Range is characterized by intraplate earthquakes associated with mountain building and crustal reorganization. A broad earthquake band extends from northeast of the Brooks Range toward the Beaufort Sea. Earthquake source mechanisms comprise a mixture of strike-slip and normal faulting events, indicative of north-northwest compression and northeast extension. A magnitude 6.4 earthquake on August 12, 2018 located 43 miles (69 km) south of Kaktovik was the largest earthquake ever recorded north of the Brooks Range. It produced an energetic aftershock sequence that continues to this day. In 2019, a vigorous swarm sequence began in the Purcell Mountains. More than 9,000 earthquakes have been recorded as part of this swarm through the end of 2021, including five earthquakes with magnitudes larger than 5. At present, this swarm continues, though at a decreased activity level.
