Carealabat M1.3 | Esau is the place of e from CERE

Mar Mar, 2025 02:29:54 Akdt (Mar Mar, 2025 10:29:54 UTC) 60.4959 ° N 143.0787 ° w depth 2.2 miles (3 km)

This event was not reviewed by an earthquake

61 miles (98 km) northwest of the iceberg 65 miles (105 km) from McCarthy83 mile (134 km) SE from Chitina91 mile (147 km) E from Cordova97 Miles (157 km) SE of Pump Station #12100 miles (162 km) SE from Thompson 109 miles) Valdez119 Miles (192 km) S of Christ124 mile (201 km) E from Tatitlek125 mile (202 km) SE from Copper Center133 mile (215 km) NW from Yakeutat235 Miles (381 km) E of Menorage340 Miles (551 km) yakutat blackthe yakutat Microplate is the latest addition to the accumulated terrain that forms southern Alaska. Microscopic panels were moved north along the parallel transformation of the margin, including Queen Charlotte and Feroywat's mistakes. In the end, the fine panels faced the continental margin of South Alaska, where the constant collision creates complex reactions of earthquakes from a very active seismic belt. Two great earthquakes in 1899 (M8.1 and M8.2) rearranged the ground shapes in the Yakotat Bay area, which led to up to 40 feet of height and 6 feet of land landing. Another noticeable event in this area was the 1958 M7.7 Bay earthquake, which was torn from the head of the Yakotat Bay along the fully Ferroeer error. This earthquake caused a huge ground collapse that was shattered in the Bay of Litoya, creating a rise in the 1720 feet tsunami. The last main earthquake in the region was the 1972 Saint Elias earthquake. In the external region, the most prominent structures are the transitional error that separates the Yakutat micro -plate from the Pacific Painting and the Northern Gulf cracking area in Alaska. A series of strong earthquakes in the Bay of Alaska, including M7.7 in 1987 and M7.8 in 1988, produced large ground movements along the coast of southeast and southern Alaska. It is not known that the transition error has produced major earthquakes except for the M6.7 event in 1973 along the southeastern end of the error. This area has a high level of background earthquakes, where hundreds of earthquakes are registered every year, most of which are shallow and located in the coastal area of ​​50 miles.

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