Klocoin M1.9 | Alaska Earthquake Center

9 Mar 2024 22:37:44 AKST (10 Mar 2024 07:37:44 UTC)59.0089°N 136.5919°W, depth 0.9 mi (1 km)

This event has not been reviewed by a seismologist

44 miles (71 km) west of Haines 52 miles (84 km) northwest of Gustavus 55 miles (89 km) southwest of Skagway 57 miles (92 km) north of Elvin Cove 74 miles (119 km) north of Pelican 75 miles (121 km) north West of Hoonah 92 miles (149 km) northwest of Juneau 94 miles (152 km) northwest of Douglas 99 miles (160 km) northwest of Tenaki Springs 116 miles (188 km) east of Yakutat 118 miles (191 km) southwest of White Horse Size Type : Ml2 Event Type: Yakutat Block Tectonic Earthquake The Yakutat Microplate is the latest addition to the collection of accreted landforms 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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