M2.3 Magnitude Earthquake | Alaska Earthquake Center

27 Jun 2024 08:25:12 AKDT (27 Jun 2024 16:25:12 UTC)61.2002°N 140.4881°W, depth 7.5 mi (12 km)

This event has not been reviewed by a seismologist

82 miles (132 km) east of McCarthy 86 miles (139 km) southeast of Chisana 95 miles (154 km) northeast of Icy Bay 103 miles (167 km) northeast of Cape Yakataga 104 miles (168 km) west of Haines Junction 115 miles (186 km) km) SE Nabesna 118 miles (191 km) N of Yakutat 129 miles (209 km) SE of Mount Wrangel 130 miles (210 km) S of North Road 132 miles (214 km) E of Chitina 149 miles (241 km) SE of Tetlin 291 miles (471 km) NW Juneau Type Magnitude: Ml2 Event Type: Tectonic Earthquake Setting of the Yakutat Massif The Yakutat Massif is the latest addition to the complex of accreted terranes that make up southern Alaska. The microplate was transported northward along marginal-parallel transform faults, including the Queen Charlotte and Fairweather faults. Eventually, the microplate encountered the southern Alaska continental margin, where continued collision created complex seismic interactions resulting in a highly active seismic belt. Two major earthquakes in 1899 (M8.1 and M8.2) rearranged the terrain in the Yakutat Bay area, resulting in uplift of up to 40 feet and land subsidence of 6 feet. Another notable event in this region was the 1958 M7.7 Lituya Bay earthquake, which ruptured from the head of Yakutat Bay along the entire Fairweather Fault. This earthquake triggered a massive landslide that crashed into Lituya Bay, creating a 1,720-foot tsunami wave. The last major earthquake in the area was the M7.4 Saint Elias earthquake in 1972. In the offshore area, the most prominent structures are the transition fault separating the Yakutat microplate from the Pacific plate and the northern Gulf of Alaska fault zone. A series of powerful earthquakes in the Gulf of Alaska, including M7.7 in 1987 and M7.8 in 1988, produced large ground motions that were felt along the entire coast of southeastern and southern Alaska. The transition fault is not known to have produced large earthquakes except for the 1973 M6.7 event along the southeastern end of the fault. This area has a high level of seismic activity, with hundreds of earthquakes recorded each year, most of which are shallow and located within the 50-mile-wide coastal zone.

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