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Volcano Mountain M3.5 | Alaska Earthquake Center

Volcano Mountain M3.5 | Alaska Earthquake Center

 


6 Nov 2024 12:26:58 AKST (6 Nov 2024 21:26:58 UTC)51.2945°N 177.7902°W, depth 21.9 miles (35 km)

This event has not been reviewed by a seismologist

45 miles (72 km) S of Bobrov Island, 51 miles (82 km) SW of Kanaga Volcano, 55 miles (89 km) SE of Mount Gariloi, 63 miles (102 km) SW of Adak, 63 miles (102 km) SW Mount Moffett, 70 miles (113 km) southwest of Mount Adagdak 89 miles (144 km) southwest of Grand Sitkin Island 114 miles (184 km) southwest of Atka Pass 115 miles (186 km) southwest of Kasatochi Island 121 miles (196 km) East of Semisopochnoi Island 130 miles (210 km) southwest of Kuniyogi Island Force type: Ml2 Event type: Tectonic earthquake Setting: Aleutian Islands

The Aleutian Arc represents the region where the Pacific Plate subducts into the mantle beneath the North American Plate. It is a seismically active area, as evidenced by the thousands of earthquakes that occur every year. Since 1900, this area has hosted several major earthquakes, including the 1957 M8.6 in the Andrianof Islands, the 1965 M8.7 in the Rat Islands, the 1986 M7.9 and 1996 M7.9 in the Andrianof Islands, and the 2003 M7 8. In the Rat Islands. Together they tore up the entire length of the large thrust boundary in this area. Another notable source of earthquakes in the arc is the 6-9 mile (10-15 km) wide zone of moderate-depth earthquakes within the subducting Pacific plate, known as the Wadati-Benioff zone. The largest medium depth earthquake recorded in this region was the 2014 M7.9 Little Sitkin event. The third source of earthquakes in this region is shallow earthquakes associated with volcanic processes and crustal faults within the overriding North American plate. They occur regularly and may produce strong aftershocks or swarm-like sequences.

Sources

1/ https://Google.com/

2/ https://earthquake.alaska.edu/event/024eaosqg4

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