Redoubt Volcano M2.0 | The Alaska Center for the earthquake

April 5, 2025 17:38:49 Akdt (April 6, 2025 01:38:49 UTC) 60.3399 ° N 153.3224 ° w depth 86.6 miles (140 km)

This event was not reviewed by an earthquake

23 miles (37 km) N from Iliamna Volcano35 Miles (56 km) E from Port Alsworth 47 miles (76 km) NE from Pedo Bay58 Miles (94 km) NE from Nondalton 60 Miles (97 km) W from Ninilchik65 mile (105 km) Nw of Ascor Point67 Miles (from the volcano Augustine 68 miles (110 km) NE from ILIAMNA69 Miles (111 km) NE from Newhalen70 Miles (113 km) from Kasilof130 mile (210 km) SW from Anchorage179 mile Various tectonic features. Miss/32 km) in the Wadati-Benioff area, where the hidden pictured plate is descended towards the scarf at the bottom of the North American plate. In southern and central Alaska, these earthquakes abandoned a depth of about 140 miles (225 km), reflecting the DOP extension of the Pacific Painting. Seismological M7.1 M7.1 2018 and 2018 M7.1 Anchorage are the latest noticeable in -depth events. They both produced a major shaking in the south and caused structural damage to buildings and infrastructure. (3) Al -Qalimiya earthquakes in this region can be attributed to three main sources: the errors and troops of the cooking entrance basin, the rift of the mountain of the castle, and the wide division of the widespread earthquakes that extend from the northern cooking entrance to the error of the dinary. The geological structures in the upper cooking entrance are able to generate strong earthquakes. The M6.9 earthquake appears to be in April 1933, which caused great damage to Marsa, occurring in such a structure. Mountain Castle, which passes 25 miles (40 km) north of Marsa, is a geological guide on Holosin's removal and the generation of Sutton 1984 M5.6 earthquake. The widespread area of ​​earthquakes between the entrance to Cook and the error of the Denali distortion between the BERING microbes to the west and the southern mass in Alaska to the east. This wide area of ​​earthquakes includes a series of most often payment errors, and the 1943 M7.0 earthquake may have arisen in this band.

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