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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 ]
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 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]
A combined diagram of the Aegean and Anatolian plates. The southern margin of the Hellenic arc is shown, which is the trend line of the faults separating the arc and the Hellenic Trench. The body of the arc is the chain called the outer Hellenides, which includes west Peloponnesus, Crete, Rhodes, southwestern Turkey, and all the islands between.
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Pontic Mountains (in Turkish, Kuzey Anadolu Dağları, meaning North Anatolian Mountains) range along the southern coast of the Black Sea in northern Turkey Kaçkar Mountains form the eastern end of the Pontic Mountains; Köroğlu Mountains (Northwest Anatolia) Yıldız Mountains (Istranca or Strandzha) are in the European part of Turkey and in ...
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]
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 ...