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Onalaska M3.5 | Alaska Earthquake Center

Onalaska M3.5 | Alaska Earthquake Center


2 Dec 2025 08:35:13 AKST (2 Dec 2025 17:35:13 UTC) 53.3400°N 165.94°W Depth 13.7 miles (22 km)

This event has not been reviewed by a seismologist

45 miles (72 km) southeast of Dutch 50 miles (81 km) south of Akutan Pass 55 miles (89 km) south of Akutan 55 miles (89 km) southeast of Makushin Volcano 91 miles (147 km) east of Okmok Caldera 95 miles (154 km) southeast of Bogoslof Island 97 miles (157 km) southwest of Westdale Peak 108 miles (175 km) east Mount Reshchennoi 112 miles (181 km) southwest of Fisher Caldera 115 miles (186 km) east of Mount Vsevedov 124 miles (201 km) east of Nikolsky Force Type: ML 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 earthquake in the Andrianof Islands, the 1965 M8.7 earthquake in the Rat Islands, the 1986 M7.9 earthquake and the 1996 M7.9 earthquake in the Andrianof Islands, and the 2003 M7.8 earthquake 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/ak2025xshgdp

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