Kaguyak Crater M1.8 | Alaska Earthquake Center

August 16, 2024 11:56:04 AKDT (August 16, 2024 19:56:04 UTC)58.4717°N 153.85°W Depth 56.9 miles (92 km)

This event has not been reviewed by a seismologist.

16 miles (25 km) east of Devils Office 18 miles (29 km) east of Kokak Volcano 20 miles (32 km) east of Mount Stellar 22 miles (35 km) south of Mount Forbeck 22 miles (35 km) east of Mount Denison 29 miles (47 km) southwest of Mount Douglas 32 miles (51 km) east of Mount Snowy 42 miles (68 km) east of Mount Katmai 46 miles (74 km) east of Mount Griggs 48 miles (77 km) east of Trident Volcano 49 miles (79 km) east of Novarupta 71 miles (115 km) northwest of Kodiak 234 miles (379 km) southwest of Anchorage Magnitude: ML2 Event Type: Earthquake Tectonic Environment of the Alaska Peninsula Earthquakes in the Alaska Peninsula are caused by various tectonic features: (1) The Aleutian Islands' massive thrust The source of the region’s most powerful earthquakes. More recent examples include the 2020 7.8-magnitude Semyonov earthquake under the Shumagin Islands and the 2021 8.2-magnitude Chizhnik earthquake southwest of Kodiak Island. While these recent earthquakes did not produce destructive waves, previous tsunamis have been documented in historical records of Russian communities and in recently discovered ancient tsunami deposits. (2) Earthquakes occur at intermediate depths (less than 20 miles/32 km) in the Wadati-Benioff Zone, where the subducting Pacific Plate descends into the mantle beneath the North American Plate. This zone extends along the Aleutian Arc, the Alaska Peninsula, and Cook Inlet. In the Alaska Peninsula, earthquakes subside at a depth of about 150 miles (241 km), reflecting the Pacific Plate’s downward extension. The Aleutian-Alaska Wadati-Benioff region produces thousands of earthquakes each year, most of which are too deep and small to be felt. Notable examples of these earthquakes include the 1999 magnitude 7.0 Kodiak Island earthquake and the 2001 magnitude 6.9 earthquake. 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 the volcanic arc. In 1912, a series of magnitude 7.0 earthquakes were associated with the eruption of Novarupta, the largest volcanic eruption worldwide in the 20th century.

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