Klukwan M2.2 | Alaska Earthquake Center

July 28, 2024 14:03:52 AKDT (July 28, 2024 22:03:52 UTC)59.0244°N 137.0961°W Depth 3.1 miles (5 km)

This event has not been reviewed by a seismologist.

60 miles (97 km) west of Hines 64 miles (103 km) northwest of Elfin Bay 65 miles (105 km) northwest of Gustavus 70 miles (113 km) southwest of Skagway 80 miles (129 km) northwest of Pelican 87 miles (141 km) northwest of Hoonah 99 miles (160 km) east of Yakutat 108 miles (175 km) northwest of Juneau 110 miles (178 km) northwest of Douglas 110 miles (178 km) northwest of Tenakee Springs 120 miles (194 km) south of Hines Junction Magnitude: ML 2 Event Type: Earthquake Yakutat Block Placement The Yakutat microplate is the latest addition to the stacked terrane that makes up southern Alaska. The microplate has moved north along parallel transform faults, including the Queen Charlotte and Fairweather faults. Eventually, the microplate encountered the southern Alaska continental margin, where the ongoing collision creates complex seismic interactions that result in a highly active earthquake belt. Two major earthquakes in 1899 (M8.1 and M8.2) rearranged the terrain in the Yakutat Bay area, causing uplift of up to 40 feet and subsidence of 6 feet. Another notable event in this area was the 1958 Lituya Bay earthquake of magnitude 7.7, which erupted from the head of Yakutat Bay along the entire Fairweather Fault. This earthquake triggered a massive landslide that struck Lituya Bay, generating a 1,720-foot tsunami. The most recent major earthquake in the area was the 1972 St. Elias earthquake of magnitude 7.4. Offshore, the transition fault separating the Yakutat microplate from the Pacific Plate and the northern Gulf of Alaska fault zone are the most well-known structures. A series of powerful earthquakes in the Gulf of Alaska, including a magnitude 7.7 earthquake in 1987 and a magnitude 7.8 earthquake in 1988, have caused significant ground motions that have been felt along the entire coast of southeastern and southern Alaska. The transition fault is not known to have produced major earthquakes except for a magnitude 6.7 event in 1973 along the southeastern end of the fault. This area has a high level of background seismicity, 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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