M1.6 Griggs Mountain | Alaska Earthquake Center

August 20, 2024 21:35:27 AKDT (August 21, 2024 05:35:27 UTC)58.6646°N 155.1172°W Depth 88.0 miles (142 km)

This event has not been reviewed by a seismologist.

27 miles (43 km) north of Mount Katmai28 miles (45 km) north of Novarupta28 miles (45 km) northwest of Mount Snowy29 miles (47 km) northwest of Mount Denison30 miles (48 km) north of Trident Volcano31 miles (50 km) northwest of Kokak Volcano31 miles (50 km) northwest of Mount Stellar32 miles (51 km) northwest of Devil's Disc33 miles (53 km) north of Mount Magic35 miles (56 km) north of Mount Martin38 miles (61 km) west of Kaguyak Crater116 miles (188 km) northwest of Kodiak252 miles (408 km) southwest of AnchorageMagnitude: ML2Event Type: EarthquakeTectonic Setting of the Alaska PeninsulaEarthquakes in the Alaska Peninsula are produced by various tectonic phenomena Characteristics: (1) The Aleutian Islands' massive thrust is a source of For the most powerful earthquakes in the region. 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) Moderate-depth earthquakes (less than 20 miles/32 km) occur 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 about 150 miles (241 km) deep, 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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