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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 ...
The East Anatolian Fault (EAF; Turkish: Doğu Anadolu Fay Hattı) is a ~700 km long major strike-slip fault zone running from eastern to south-central Turkey. It forms the transform type tectonic boundary between the Anatolian sub-plate and the northward-moving Arabian plate . [ 1 ]
These are the North Anatolian Fault Zone, which forms the present-day plate boundary of Eurasia near the Black Sea coast, and the East Anatolian Fault Zone, which forms part of the boundary of the North Arabian plate in the southeast. As a result, Turkey lies on one of the world's seismically most active regions. [citation needed]
She continued: “The recent earthquakes in East Anatolia have occurred on the East Anatolian Fault and the nearby faults where three tectonic plates meet, what is called a triple junction: the ...
The devastating 2023 Turkey–Syria earthquakes occurred along the active East Anatolian Fault at a strike-slip fault where the Arabian plate is sliding past the Anatolian plate horizontally. [4] [5] According to the American Museum of Natural History, the Anatolian transform fault system is "probably the most active in the world". [6]
Map of the Anatolian sub-plate, showing the location of the East Anatolian Fault. Central southern Turkey and northwestern Syria are affected by the interaction between three tectonic plates; the African plate, Arabian plate and Anatolian sub-plate.
The earthquake in Turkey that killed more than 3,100 people and set off a series of aftershocks ruptured just over 11 miles beneath the earth’s surface.
Turkey is a seismically active area within the complex zone of collision between the Eurasian plate and both the African and Arabian plates.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.