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  2. East Anatolian Fault - Wikipedia

    en.wikipedia.org/wiki/East_Anatolian_Fault

    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 ]

  3. 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 ...

  4. Anatolian sub-plate - Wikipedia

    en.wikipedia.org/wiki/Anatolian_sub-plate

    Anatolian plate. The Anatolian sub-plate [1] [2] is a continental tectonic plate that is separated from the Eurasian plate and the Arabian plate by the North Anatolian Fault and the East Anatolian Fault respectively. Most of the country of Turkey is located on the Anatolian plate. [3]

  5. Geology of Turkey - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Turkey

    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]

  6. Hellenic arc - Wikipedia

    en.wikipedia.org/wiki/Hellenic_arc

    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.

  7. Why was the Turkey-Syria earthquake so bad? - AOL

    www.aol.com/news/explainer-why-turkey-syria...

    The epicentre was about 26 km east of the Turkish city of Nurdagi at a depth of about 18 km on the East Anatolian Fault. During the 20th century, the East Anatolian Fault yielded little major ...

  8. 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 ...

  9. Beyond magnitude: A shallow earthquake hammered Turkey - AOL

    www.aol.com/beyond-magnitude-shallow-earthquake...

    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. Beyond magnitude: A shallow earthquake ...