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The very active year started its major activity with a magnitude 8.6 earthquake in Alaska in March. This event was one of the largest on record in the United States and was followed by an energetic aftershock sequence which resulted in 6 aftershocks measuring greater than magnitude 7.0. Mongolia was affected by the strong 1957 Mongolia earthquake.
The earthquake struck southern Mongolia at 11:37:53 local time on December 4, 1957. Rupture was complex, with multiple scenarios proposed. The original hypothesis was that the earthquake occurred along the strike-slip Bogd fault and ruptured for 560 km (350 mi), [1] however, the more recently adopted conclusion is that there was a 250–300 km (160–190 mi) [15] long strike-slip rupture at a ...
The 1957 Abant earthquake occurred at 8:33am on 26 May, in Turkey. The earthquake had an estimated surface-wave magnitude of 7.1 and a maximum felt intensity of IX (Violent) on the Mercalli intensity scale, causing 52 fatalities and 101 injuries. Five thousand homes were damaged as a result of the earthquake. [3] [4]
UTC time: 1957-03-22 19:44:22: ISC event: 886234: USGS-ANSSComCat: Local date: March 22, 1957 (): Local time: 11:44:22 PST [1]: Magnitude: 5.7 M w [1]: Depth: 15 km (9.3 mi) [1] Epicenter: 1]: Type: Oblique-slip: Areas affected: San Francisco Bay Area Northern California United States: Total damage: $1 million [2]: Max. intensity: MMI VII (Very strong) [2]: Peak acceleration: 0.18 g [3 ...
The first earthquake hit at 21:17 hours local time on April 24, 1957, and lasted 25 seconds having a magnitude of 7.1 on the moment magnitude scale; a stronger second quake occurred at 04:26 hours on April 25; this one lasted for 60 seconds and had a magnitude of 7.3.
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The 1957 Andreanof Islands earthquake occurred at 04:22 local time on March 9 with a moment magnitude estimated at 8.6 and a maximum Modified Mercalli intensity of VIII (Severe). It occurred south of the Andreanof Islands group, which is part of the Aleutian Islands arc.
The earthquake's rupture dimensions was an area of fault estimated at 50 km (31 mi) by 25 km (16 mi). It was the second largest instrumentally recorded earthquake in the Alborz, behind the 1990 Manjil–Rudbar earthquake (M w 7.3). The earthquake's fault plane solution indicates it occurred along a northwest–southeast trending reverse fault.