Ice Bay M1.9 | Alaska Earthquake Center

11 Feb 2024 02:28:51 AKST (11 Feb 2024 11:28:51 UTC)60.2535°N 141.1635°W, depth 5.5 mi (8 km)

This event has not been reviewed by a seismologist

45 miles (72 km) east of Cape Yakataga 70 miles (113 km) northwest of Yakutat 95 miles (154 km) southwest of Burwash Landing 101 miles (163 km) southeast of McCarthy 128 miles (207 km) west of Haines Junction 135 miles (218 km) km) S of Chisana 140 miles (226 km) SE of Chitina 154 miles (249 km) SE of Mount Wrangel 158 miles (256 km) E of Cordova 158 miles (256 km) SE of Pumping Station #12,159 miles (257 km) S East of Nabesna 273 miles (442 km) northwest of Juneau, 302 miles (489 km) east of Anchorage Magnitude Type: Ml2 Event Type: Tectonic Earthquake Setting The Yakutat Block The Yakutat Microplate is the latest addition to the complex of accreted landforms that make up the South 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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