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mountain. M3.1 Chariot | Alaska Earthquake Center

mountain. M3.1 Chariot | Alaska Earthquake Center

 


13 Nov 2024 07:56:18 AKST (13 Nov 2024 16:56:18 UTC)51.3094°N 178.4884°W, depth 20.6 miles (33 km)

This event has not been reviewed by a seismologist

42 miles (68 km) S of Tanaga Volcano, 61 miles (98 km) SSW of Bobrov Island, 71 miles (115 km) SSW of Kanaga Volcano, 86 miles (139 km) SSW of Mount Moffett, 88 miles (142 km) S West of Adak, 93 miles (150 km) southeast of Semisopochnoi Island 94 miles (152 km) southwest of Mount Adaghdak 109 miles (176 km) east of Amchitka 114 miles (184 km) southwest of Great Sitkin Island 140 miles (226 km) south W of Kasatochi Island 141 miles (228 km) W of Atka PassMagnitude Type: Ml2 Event Type: Tectonic Earthquake in 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 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/024em6rc8h

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