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  2. North Anatolian Fault - Wikipedia

    en.wikipedia.org/wiki/North_Anatolian_Fault

    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 ...

  3. 1668 North Anatolia earthquake - Wikipedia

    en.wikipedia.org/wiki/1668_North_Anatolia_earthquake

    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 ...

  4. 1943 Tosya–Ladik earthquake - Wikipedia

    en.wikipedia.org/wiki/1943_Tosya–Ladik_earthquake

    The earthquake occurred on the North Anatolian Fault, which is a fault line around 1500 km long, right-lateral, strike-slip plate boundary fault between the Eurasian plate and the Anatolian Plate that travels across the northern section of Turkey. Large earthquakes measuring 7+ magnitudes on the North Anatolian fault in the 1900s have ruptured ...

  5. List of earthquakes in Turkey - Wikipedia

    en.wikipedia.org/wiki/List_of_earthquakes_in_Turkey

    Much of the country lies on the Anatolian sub-plate, a small plate bounded by two major strike-slip fault zones, the North Anatolian Fault and East Anatolian Fault. The western part of the country is also affected by the zone of extensional tectonics in the Aegean Sea caused by the southward migration of the Hellenic arc.

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  7. Karlıova triple junction - Wikipedia

    en.wikipedia.org/wiki/Karlıova_Triple_Junction

    The Karlıova triple junction is found where the east–west trending North Anatolian Fault intersects the East Anatolian Fault coming up from the southwest, and is ~700 km distant from the Maras triple junction. Because each arm of the junction is a transform fault (F), the Karlıova triple junction is an F-F-F type junction. [clarification ...

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  9. 1999 Düzce earthquake - Wikipedia

    en.wikipedia.org/wiki/1999_Düzce_earthquake

    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 ...