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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]
This process is still at work today as the African plate converges with the Eurasian plate and the Anatolian sub-plate escapes towards the west and southwest along strike-slip faults. 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 ...
The geology of Europe is varied and complex, and gives rise to the wide variety of landscapes found across the continent, from the Scottish Highlands to the rolling plains of Hungary. Europe's most significant feature is the dichotomy between highland and mountainous Southern Europe and a vast, partially underwater, northern plain ranging from ...
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 ]
The Keryneia Terrane occupies the northern margin of Cyprus, stretching from Cape Kormakitis in the west to Cape Andreas in the east. The terrane is a sequence of Permian to recent sediments. [ 3 ] The carbonate rocks are divided into the Dhikomo, the Hilarion and the Sykhari Formation.
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 ...
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.