Magnitude 2.6 - 46 miles SW of Kaktovik
September 12, 2022 13:15:35 AKDT (September 12, 2022 21:15:35 UTC)
69.5203°N 144.3902°W Depth 4.5 miles (7 km)
This event has been reviewed by a seismologist
- 101 miles (163 km) N of Arctic Village
- 101 miles (163 km) E of Pump Station #2
- 107 miles (173 km) SE of Deadhorse
- 107 miles (173 km) SE of Prudhoe Bay
- 112 miles (181 km) SE of Pump Station #1
- 119 miles (192 km) NE of Pump Station #3
- 145 miles (235 km) NE of Pump Station #4
- 181 miles (293 km) N of Venetie
- 185 miles (299 km) NW of Old Crow
- 188 miles (304 km) E of Umiat
- 199 miles (322 km) N of Chalkyitsik
- 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.