Oakenrick Drill M2.2 | Alaska Earthquake Center

5 November 2024, 11:32:10 AEST (5 November 2024, 20:32:10 UTC) 57.8859°N 156.2245°W, depth 80.3 miles (130 km)

This event has not been reviewed by a seismologist

19 miles (30 km) north of Mount Ugašek, 37 miles (59 km) southwest of Mount Martin, 41 miles (66 km) southwest of Magic Mountain, 43 miles (69 km) north of Kjalagvik Creek, 47 miles (76 km) southwest Novarupta, 48 miles (77 km) southeast of Igek 48 miles (77 km) southwest of Trident Volcano 52 miles (84 km) southwest of Mount Greggs 54 miles (87 km) southwest of Mount Katmai 55 miles (89 km) northeast of Pilot Point 57 miles (92 km) S of King Salmon 141 miles (228 km) W of Kodiak Force Type: Ml2 Event Type: Tectonic Earthquake Setting of the Alaska Peninsula Earthquakes in the Alaska Peninsula region are produced by various tectonic features: (1) Thrust The Great Aleutian is the source of the strongest earthquakes in the region. More recent examples include the 2020 M7.8 Simeonof earthquake beneath the Shumagin Islands and the 2021 M8.2 Chignik earthquake southwest of Kodiak Island. While these recent earthquakes did not produce devastating tsunamis, previous tsunamis have been documented in the historical records of Russian communities and in recently discovered ancient tsunami deposits. (2) Moderate-depth earthquakes (less than 20 miles/32 km) occur in the Wadati-Benioff zone, where the subducting Pacific plate dips into the mantle beneath the North American plate. This region extends along the Aleutian Arc, the Alaska Peninsula, and Cook Inlet. In the Alaska Peninsula region, seismic activity subsides to a depth of about 150 miles (241 km), reflecting the lower extension of the Pacific Plate. The Aleutian-Alaska Wadati-Benioff region produces thousands of earthquakes every year, most of them too deep and too small to be felt. The most notable examples of these earthquakes are the M7.0 events of 1999 and the M6.9 Kodiak Island events of 2001. Both earthquakes caused damage and disruption to the city of Kodiak and other communities on the island. (3) Crustal earthquakes in this region can be attributed to the Kodiak Escarpment fault zone and to the volcanic arc. In 1912, a series of M7+ earthquakes were associated with the Novarupta eruption, which was the largest volcanic eruption of the 20th century worldwide.

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