Magnitude 2.2 - 21 miles N of Mt. Gareloi
March 26, 2024 11:15:34 AKDT (March 26, 2024 19:15:34 UTC)
52.0765°N 178.6241°W Depth 84.1 miles (136 km)
This event has been reviewed by a seismologist
- 24 miles (38 km) NW of Tanaga Volcano
- 51 miles (82 km) W of Bobrof Island
- 63 miles (102 km) W of Kanaga Volcano
- 76 miles (123 km) E of Semisopochnoi Island
- 81 miles (131 km) W of Mt. Moffett
- 85 miles (137 km) W of Adak
- 87 miles (141 km) W of Mt. Adagdak
- 106 miles (171 km) W of Great Sitkin Island
- 108 miles (175 km) E of Amchitka
- 127 miles (205 km) E of Little Sitkin Pass
- 130 miles (210 km) E of Davidof Island
- Magnitude type: Ml2
- Event type: earthquake
Tectonic Setting of the Aleutian Islands
The Aleutian Arc marks the region where the Pacific Plate subducts into the mantle beneath the North American Plate. It is a seismically active region, evidenced by the thousands of earthquakes occurring each year. Since 1900, this region has hosted several major megathrust earthquakes, including the 1957 M8.6 in the Andreanof Islands, the 1965 M8.7 in the Rat Islands, the 1986 M7.9 and the 1996 M7.9 in the Andreanof Islands, and the 2003 M7.8 in the Rat Islands. Together they have ruptured the entire length of the megathrust boundary in this region. Another notable source of seismicity in the arc is the zone 6-9 miles (10-15 km) wide of intermediate-depth earthquakes within the subducting Pacific Plate, known as the Wadati-Benioff Zone. The largest recorded intermediate-depth earthquake in this region was the 2014 M7.9 Little Sitkin event. A third source of seismicity in this region are shallow earthquakes associated with volcanic processes and crustal faults within the overriding North American Plate. They occur regularly and may produce vigorous aftershock or swarm-like sequences.