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Magnitude 7.9 - 23 miles S of Bobrof Island
June 9, 1996 20:03:35 AKDT (June 10, 1996 04:03:35 UTC)
51.5820°N 177.604°W Depth 20.5 miles (33 km)
This event has been reviewed by a seismologist
- 30 miles (48 km) SW of Kanaga Volcano
- 31 miles (50 km) SE of Tanaga Volcano
- 44 miles (71 km) SW of Mt. Moffett
- 45 miles (72 km) SW of Adak
- 52 miles (84 km) SW of Mt. Adagdak
- 53 miles (85 km) E of Mt. Gareloi
- 71 miles (115 km) SW of Great Sitkin Island
- 98 miles (158 km) SW of Kasatochi Island
- 99 miles (160 km) W of Atka Pass
- 114 miles (184 km) W of Koniuji Island
- 118 miles (191 km) W of Mt. Sergief
- Magnitude type: Mw2
- Event type: N/A
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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.