Whittier M1.6 | Alaska Earthquake Center

August 26, 2024 18:27:50 AKDT (August 27, 2024 02:27:50 UTC)60.7936°N 148.9175°W Depth 0.0 miles (0 km)

This event has not been reviewed by a seismologist.

13 miles (21 km) southeast of Girdwood 26 miles (42 km) east of Hope 26 miles (42 km) northeast of Moose Pass 38 miles (61 km) northeast of Cooper Landing 41 miles (66 km) southeast of Fort Richardson 42 miles (68 km) southeast of Eagle River 43 miles (69 km) southeast of Elmendorf Air Force Base 44 miles (71 km) southeast of Anchorage 45 miles (72 km) southeast of Chugiak 51 miles (82 km) north of Seward 56 miles (90 km) south of Palmer 241 miles (390 km) northeast of Kodiak 282 miles (457 km) south of Fairbanks Magnitude: ML2 Event Type: Earthquake South Alaska Tectonic Mode Earthquakes in south-central Alaska are caused by 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 zone between the subducting Pacific and North American plates. The 1964 Great Alaska Earthquake of magnitude 9.2, still 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 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: 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.

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