False pass M2.8 | Alaska Earthquake Center

20 Jun 2024 18:41:56 AKDT (21 Jun 2024 02:41:56 UTC)54.2665°N 162.6127°W, depth 11.9 miles (19 km)

This event has not been reviewed by a seismologist

54 miles (87 km) southeast of Roundtop Mountain 56 miles (90 km) south of Frosty Peak 56 miles (90 km) southeast of Isanotski Peaks 56 miles (90 km) south of King Cove 64 miles (103 km) south of Cold Bay 64 miles ( 103 km) Southeast of Shishaldin Volcano 65 miles (105 km) South of Mount Dutton 75 miles (121 km) South of Emmons Lake 77 miles (124 km) East of Fisher Caldera 82 miles (132 km) South of Amak Island 84 miles (136 km) East Westdale Peak 160 miles (259 km) E of Dutch Force Type: Ml2 Event Type: Tectonic Earthquake Setting Alaska Peninsula Earthquakes in the Alaska Peninsula area are produced by various tectonic features: (1) The large Aleutian thrust is the source of the strongest earthquakes in 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 Harbor. In the Alaska Peninsula region, seismic activity subsides at a depth of approximately 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 area 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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