Earthquake Hits Alaska Peninsula Area
On November 12, 2024, a seismic event was recorded at 03:04 AKST (12:04 UTC) with a magnitude type of Ml2, located at coordinates 54.4760°N latitude and 161.6177°W longitude, at a depth of 15.6 miles (25 km). This event was situated approximately 55 miles southeast of Mt. Dutton and 61 miles south of Emmons Lake.
The earthquake has not yet been reviewed by a seismologist, and details regarding its impact remain limited. Notable geographic landmarks nearby include Frosty Peak, Cold Bay, and Pavlof Volcano, among others in the region.
- 55 miles (89 km) SE of Mt. Dutton
- 61 miles (98 km) S of Emmons Lake
- 63 miles (102 km) SE of Frosty Peak
- 66 miles (107 km) SE of Cold Bay
- 66 miles (107 km) S of Pavlof Volcano
- 68 miles (110 km) S of Pavlof Sister
- 74 miles (119 km) SW of Sand Point
- 76 miles (123 km) E of False Pass
- 82 miles (132 km) S of Mt. Dana
- 82 miles (132 km) E of Roundtop Mountain
- 87 miles (141 km) E of Isanotski Peaks
- 202 miles (327 km) E of Dutch
Tectonic Setting of the Alaska Peninsula
The Alaska Peninsula region experiences seismicity due to various tectonic features, including the Aleutian megathrust, which is responsible for the strongest earthquakes in the area. Notable past events include the 2020 M7.8 Simeonof Earthquake and the 2021 M8.2 Chignik Earthquake. Though these did not cause tsunamis, previous events have resulted in documented tsunamis in Russian historical records. The Wadati-Benioff Zone, where the Pacific Plate subducts beneath the North American Plate, accounts for much of the intermediate depth seismicity in this region. Various crustal seismic activities arise from local fault zones and volcanic arcs, indicative of the area’s dynamic geological landscape.
Source
Photo credit earthquake.alaska.edu