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Magnitude 4.4 - 33 miles W of Attu
February 24, 2023 03:15:56 AKST (February 24, 2023 12:15:56 UTC)
53.1086°N 172.4998°E Depth 17.8 miles (28 km)
This event has been reviewed by a seismologist
- 73 miles (118 km) W of Shemya Is
- 152 miles (246 km) W of Buldir Island
- 153 miles (248 km) W of Buldir Is
- 225 miles (364 km) W of Kiska Volcano
- 248 miles (402 km) W of Segula Peak
- 258 miles (418 km) W of Davidof Island
- 260 miles (421 km) W of Little Sitkin Pass
- 289 miles (468 km) E of Bering Is, Komandorsky
- 295 miles (478 km) NW of Amchitka
- 309 miles (501 km) W of Semisopochnoi Island
- 378 miles (612 km) W of Mt. Gareloi
- Magnitude type: Mb2
- Event type: earthquake
Tectonic Setting of the Aleutian Islands
The world's largest earthquakes originate along convergent plate boundaries such as the Aleutian megathrust. Starting in 1938, a series of three great earthquakes ruptured the subduction zone along its entire length from the Alaska Peninsula to the western Aleutians with the exception of a small gap near the Shumagin Islands. The sequence began with a M8.2 earthquake southwest of Kodiak Island. A M8.6 in the Andreanof Islands followed in 1957, and the sequence concluded with the Rat Islands M8.7 in 1965. The Shumagin Gap still has not ruptured, but GPS observations suggest that little strain has built up in this region.
Another notable source of seismicity in the arc are the intermediate depth earthquakes within the subducting Pacific Plate, known as the Wadati-Benioff zone. The largest recorded earthquake of this kind was the 2014 M7.9 Little Sitkin event. Shallow earthquakes associated with volcano processes and crustal faults within the overriding North American plate occur regularly and may produce vigorous aftershock or swarm-like sequences.