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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 northern edge is a transform boundary with the Eurasian plate, forming the North Anatolian Fault zone (NAFZ). Eurasian and Anatolian plates Research indicates that the Anatolian plate is rotating counterclockwise as it is being pushed west by the Arabian plate, impeded from any northerly movement by the Eurasian plate. [ 8 ]
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 ...
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.
The African plate is subducting under the Aegean plate at a rate of about 40 mm/year, causing shallow earthquakes near the fault and deeper earthquakes near the Greek volcanic arc. [8] Some seismic activity is a result of the extension of the plate, which creates east–west trending faults that can slip and cause earthquakes. [9]
During the 20th century, the East Anatolian Fault yielded little major seismic activity. ... Eleven minutes after the initial quake, the region was hit by a 6.7-magnitude aftershock. A 7.5 ...
[2] [3] Ridges like the Mid-Atlantic ridge form at a divergent plate boundary. They are located deep underwater and very difficult to study. Scientists know less about ocean ridges than they do the planets of the solar system. [4] There is another triple junction where the Eurasian plate meets the Anatolian sub-plate and the Arabian plate.