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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 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.
The Anatolian sub-plate is currently being squeezed by the collision of the Eurasian plate with the Arabian plate in the East Anatolian Fault Zone. [ 5 ] [ 6 ] The boundary between the North American plate and the Eurasian plate in the area around Japan has been described as "shifty". [ 7 ]
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 ...
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 northern plains are delimited in the west by the Scandinavian Mountains and the mountainous parts of the British Isles. The southern mountainous region is bounded by the Mediterranean Sea and the Black Sea. Major shallow water bodies submerging parts of the northern plains are the Celtic Sea, the North Sea, the Baltic Sea and the Barents Sea.