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Onalaska M3.7 | Alaska Earthquake Center

Onalaska M3.7 |  Alaska Earthquake Center

 


Apr 16, 2024 12:33:07 AKDT (Apr 16, 2024 20:33:07 UTC)52.4799°N 166.2355°W Depth 0.2 mi (0 km)

This event has not been reviewed by a seismologist

98 miles (158 km) S of Dutch 101 miles (163 km) S of Makushin Volcano 103 miles (167 km) SE of Okmok Caldera 107 miles (173 km) SE of Mt. Access 109 miles (176 km) south from Akutan Pass 112 miles (181 km) east from Mt. Vsevidof 115 miles (186 km) east of Nikolsky 116 miles (188 km) south of Akutan 125 miles (202 km) southeast of Bogoslov Island 150 miles (243 km) east of Kagamel Island 153 miles (248 km) east of Uliaga Island Size Type: Ml2 Type Event: Seismic-tectonic setting of the 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 large 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 M7.9 in the Andrianof Islands. 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/0244xalw4y

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