Magnitude 2.2 - 47 miles S of Kaktovik
June 19, 2019 18:07:16 AKDT (June 20, 2019 02:07:16 UTC)
69.4662°N 144.1153°W Depth 2.7 miles (4 km)
This event has been reviewed by a seismologist
- 99 miles (160 km) N of Arctic Village
- 108 miles (175 km) E of Pump Station #2
- 114 miles (184 km) SE of Deadhorse
- 114 miles (184 km) SE of Prudhoe Bay
- 120 miles (194 km) SE of Pump Station #1
- 124 miles (201 km) NE of Pump Station #3
- 149 miles (241 km) NE of Pump Station #4
- 178 miles (288 km) NW of Old Crow
- 180 miles (291 km) N of Venetie
- 195 miles (316 km) N of Chalkyitsik
- 195 miles (316 km) E of Umiat
- 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.