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Amchitka M2.8 | Alaska Earthquake Center

Amchitka M2.8 |  Alaska Earthquake Center


23 February 2024 7:16:28 PM AEST (24 February 2024 04:16:28 UTC) 51.3137°N 179.2965°E Depth 25.5 miles (41 km)

This event has not been reviewed by a seismologist

46 miles (74 km) south of Semisopochnoi Island 59 miles (95 km) southeast of Little Sitkin Pass 61 miles (98 km) southeast of Davidoff Island 70 miles (113 km) southeast of Segula Peak 88 miles (142 km) west of Mt. Gareloi 91 miles (147 km) southeast of Kiska Volcano 117 miles (189 km) west of Tanaga Volcano 146 miles (236 km) west of Bobrov Island 158 miles (256 km) west of Kanaga Volcano 161 miles (261 km) southeast of Boulder Island 161 miles (261 km) ) ) southeast of Boulder IslandForce type: Ml2Event 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.




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