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The North Anatolian Fault (NAF; Turkish: Kuzey Anadolu Fay Hattı) is an active right-lateral strike-slip fault in northern Anatolia, and is the transform boundary between the Eurasian plate and the Anatolian sub-plate. The fault extends westward from a junction with the East Anatolian Fault at the Karliova triple junction in eastern Turkey ...
UTC time: 1939-12-26 23:57:23: ISC event: 902291: USGS-ANSSComCat: Local date: 27 December 1939 (): Local time: 1:57:23 a.m. Magnitude: 7.8 M w [1]: Depth: 20 km (12 mi) [1] Epicenter: 1]: Fault: North Anatolian Fault: Type: Strike-slip: Areas affected: Erzincan Province Turkey: Total damage: 116,720 buildings were seriously damaged: Max. intensity: MMI XII (Extreme) [2]: Tsunami: 0.53 m (1 ft ...
The 1999 Düzce event is the most recent in a sequence of large earthquakes that have affected the North Anatolian Fault, starting towards the eastern end with the 1939 Erzincan earthquake, then propagating towards the west with events in 1942, 1943, 1944, 1951, 1957, 1967 and finally the 1999 İzmit event. At its western end the North ...
The Sürgü-Çardak Fault is an east–west striking 160 km (99 mi) long fault that runs north of the EAF. It branches away from the EAF west of Çelikhan and extends westwards to Göksun. [ 21 ] Comprising two segments; the Sürgü Fault runs 70 km (43 mi) between Çelikhan and Nurhak; the Çardak Fault runs 90 km (56 mi) between Nurhak and ...
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Local date: 17 August 1668: Local time: Late morning: Magnitude: 7.8–8.0 M s: Epicentre: 1]: Fault: North Anatolian Fault: Type: Strike-slip: Areas affected: North Anatolia, Ottoman Empire: Max. intensity: MMI IX (Violent) [1]: Foreshocks: Yes : Aftershocks: Continued for 6 months : Casualties: 8,000 dead: Northern Anatolia was struck by a large earthquake on 17 August 1668 in the late ...
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