Magnitude 1.7 - 23 miles SW of Allakaket
May 31, 2025 19:48:16 AKDT (June 1, 2025 03:48:16 UTC)
66.3473°N 153.2606°W Depth 0.0 miles (0 km)
This event has not been reviewed by a seismologist
- 35 miles (56 km) NE of Hughes
- 58 miles (94 km) SW of Bettles
- 78 miles (126 km) SW of Pump Station #5
- 88 miles (142 km) N of Tanana
- 99 miles (160 km) NE of Huslia
- 104 miles (168 km) W of Pump Station #6
- 105 miles (170 km) SW of Coldfoot
- 105 miles (170 km) NW of Rampart
- 106 miles (171 km) E of Kobuk
- 113 miles (183 km) E of Shungnak
- 113 miles (183 km) SW of Wiseman
- 190 miles (308 km) NW of Fairbanks
- Magnitude type: Ml
- 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.
