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Iliamna Volcano M1.6 | Alaska Earthquake Center

Iliamna Volcano M1.6 | Alaska Earthquake Center

 


August 10, 2024 03:52:00 AKDT (August 10, 2024 11:52:00 UTC)60.1503°N 153.2088°W Depth 77.7 miles (125 km)

This event has not been reviewed by a seismologist.

28 miles (45 km) southwest of Redoubt Volcano 38 miles (61 km) east of Port Ellsworth 40 miles (64 km) northeast of Pedro Bay 54 miles (87 km) northwest of Anchor Point 54 miles (87 km) west of Ninilchik 55 miles (89 km) north of Augustine Volcano 58 miles (94 km) east of Nondalton 63 miles (102 km) west of Clam Gulch 65 miles (105 km) northeast of Iliamna 65 miles (105 km) northeast of New Halen 68 miles (110 km) northwest of Homer 134 miles (217 km) southwest of Anchorage 166 miles (269 km) north of Kodiak Magnitude: ML2 Event Type: Earthquake Status: South Alaska Seismic contamination in south-central Alaska results from a number of different tectonic features. (1) The most powerful earthquakes in south-central Alaska are generated by the massive fault that marks the contact between the subducting Pacific and North American plates. The 1964 Great Alaska Earthquake, which measured 9.2 on the Richter scale and remains the second largest earthquake ever recorded, originated beneath Prince William Sound. (2) Intermediate-depth earthquakes (less than 20 miles/32 km) occur in the Wadati-Benioff Zone, where the subducting quiescent plate descends into the mantle beneath the North American plate. This zone extends along the Aleutian Arc, the Alaska Peninsula, and Cook Inlet, and terminates beneath the foothills of northern Alaska. In south-central Alaska, these earthquakes attenuate at depths of about 140 miles (225 km), reflecting the downward extension of the quiescent plate. The 2016 M7.1 Enniskin and 2018 M7.1 Anchorage earthquakes are the two most recent notable intermediate-depth events. Both have caused significant ground shaking in the south-central region and have resulted in structural damage to buildings and infrastructure. (3) Crustal earthquakes in this region can be attributed to three main sources: the faults and folds of the Cook Inlet Basin, the Castle Mountain fault, and a broad band of spreading earthquakes extending from northern Cook Inlet to the Denali fault. The geologic structures mapped in upper Cook Inlet are capable of generating strong earthquakes. The April 1933 M6. 9 earthquake, which caused significant damage in Anchorage, appears to have occurred on such a structure. The Castle Mountain fault, which runs 25 miles (40 km) north of Anchorage, exhibits geologic evidence of Holocene deflection and generated the 1984 M5. 6 Sutton earthquake. The spreading zone of earthquakes between Cook Inlet and the Denali fault may represent a deformation zone between the Bering Plate to the west and the southern Alaska Block to the east. This vast earthquake zone includes a series of strong thrust faults, and a 7.0 magnitude earthquake in 1943 may have originated in this area.

Sources

1/ https://Google.com/

2/ https://earthquake.alaska.edu/event/024a8zpb1m

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