Iliamna Volcano M1.7 | Alaska Earthquake Center

July 4, 2024 10:32:46 AKDT (July 4, 2024 18:32:46 UTC)60.1043°N 153.0672°W Depth 78.2 miles (126 km)

This event has not been reviewed by a seismologist.

29 miles (47 km) southwest of Redoubt Volcano 42 miles (68 km) northeast of Pedro Bay 43 miles (69 km) east of Port Ellsworth 48 miles (77 km) west of Ninilchik 49 miles (79 km) northwest of Anchor Point 53 miles (85 km) north of Augustine Volcano 58 miles (94 km) west of Clam Gulch 62 miles (100 km) northwest of Homer 62 miles (100 km) east of Nondalton 64 miles (103 km) west of Kasilof 65 miles (105 km) northwest of English Bay 132 miles (214 km) southwest of Anchorage 162 miles (262 km) north of Kodiak Magnitude: ML2 Event Type: Earthquake Mode South Alaska Landforms in south-central Alaska occur as a result of a number of different tectonic features. (1) The strongest earthquakes in south-central Alaska are generated by the massive thrust 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 under Prince William Sound. (2) Intermediate-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, and terminates beneath the foothills of northern Alaska. In south-central Alaska, these earthquakes taper off at depths of about 140 miles (225 km), reflecting the downward extension of the Pacific 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: faults and folds in 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.

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