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Martin M0.8 Mountain | The Alaska Center for the earthquake

Mar Mar, 2025 08:25:39 Akdt (Mar 24, 2025 16:25:39 UTC) 58.1362 ° N 155.5614 ° w depth 1.2 miles (1 km)
This event was not reviewed by an earthquake
12 miles (19 km) from Mageik17 Mountain (27 km) SW from Novarupta18 mile (29 km) of the volcano Trading 23 miles (37 km) SW from MT. Griggs24 miles (38 km) SW from MT. (72 km) SW from MT. Denison45 Miles (72 km) from MT. Ugashik47 Miles (76 km) SW from MT. Stellar49 Miles (79 km) SW from Kukak Volcano118 Miles (191 km) from Kodiak290 miles (470 km) SW of the anchor is produced by the Alaska Peninsula in the Alaska Peninsula through different tectonic features: (1) The huge allemayyan is the most powerful source of earthquakes in the region. The latest examples include the SimeonOF 2020 M7.8 earthquake under the Shuagin Islands and the Chignik Southwest Southwest earth Recent discovery. (2) Earthquakes of the intermediate depth (less than 20 miles/32 km) occur in the Wadati Beniof area, where the exterior Pacific plate descends towards the scarf located below the North American plate. This area extends along the geo -bow, Alaska Peninsula, and Cook Entrance. In the Alaska Peninsula, earthquakes give up about 150 miles (241 km), reflecting the DOP extension of the quiet plate. The Aleutian-Alaska Wadati-Benioff produces thousands of earthquakes every year, most of them are very deep and very small. The most prominent examples of these earthquakes are the events of Kodiak Island of 1999 M7.0 and 2001 M6.9. Both earthquakes caused damage and disruption of the city of Kodiak and other societies on the island. (3) Cortexal earthquakes in this area can be attributed to the Codak Rift area and to the volcanic arc. In 1912, a series of M7+ earthquakes was associated with the Novarupta explosion, which was the largest volcanic eruption in the twentieth century around the world.
Sources 2/ https://earthquake.alaska.edu/event/0253tja6ke The mention sources can contact us to remove/changing this article |
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