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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 ]
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 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 ...
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 magnitude 7.8 earthquake that struck Turkey and Syria on Monday is likely to be one of the deadliest this decade, seismologists said, with a more than 100 km (62 miles) rupture between the ...
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 ...
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]
Turkey's longest and most active geological fracture, the North Anatolian Fault, runs through the southern foot of Mount Ilgaz. [3] The entire region features valleys, slopes and peaks of different characters. Additionally, it has geomorphological structure with a high-level landscape speciality. [1]