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This is a list of earthquakes in 1957. Only magnitude 6.0 or greater earthquakes appear on the list. Lower magnitude events are included if they have caused death, injury or damage. Events which occurred in remote areas will be excluded from the list as they wouldn't have generated significant media interest. All dates are listed according to ...
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 earthquake ruined almost the entire city, with 90% of buildings being damaged. [6] Thanks to the strict evacuation order of the district governor Nazif Okuş after the first quake, the number of dead remained at only 19 for the city and the villages around with a total population of around 60,000.
A Minecraft server is a player-owned or business-owned multiplayer game server for the 2011 Mojang Studios video game Minecraft. In this context, the term "server" often refers to a network of connected servers, rather than a single machine. [ 1 ]
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]
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.
The Guerrero seismic gap is a ca. 200 km long segment of the subduction interface, which has not had a large earthquake since the 1911 event. Although several slow earthquakes have been observed in that time interval, an earthquake in the range M 7.9–8.0 could still be expected within the Guerrero gap. [6]