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The Aegean Sea plate (also called the Hellenic plate or Aegean plate) is a small tectonic plate located in the Eastern Mediterranean under Southern Greece and western Turkey. Its southern edge is the Hellenic subduction zone south of Crete , where the African plate is being swept under the Aegean Sea plate. [ 1 ]
Adriatic plate, also known as the Apulian plate – A small tectonic plate in the Mediterranean; Aegean Sea plate, also known as Hellenic plate – A small tectonic plate in the eastern Mediterranean Sea; Anatolian plate – Continental tectonic plate comprising most of the Anatolian Peninsula (Asia Minor) Azores microplate [7] [8]
From the standpoint of plate tectonics, the ongoing northward drive of the African Plate into the Eurasian Plate in the Mediterranean basin is the most prominent aspect of the European scene today. The pressure exerted by the African plate is the overall cause of the rise of the Pyrenees, the Alps and the Carpathian Mountains.
Obduction zones occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction. [citation needed]
Tectonic plates in Turkey; the Anatolian sub-plate, the African plate, the Arabian plate, and the Eurasian plate. Except for a relatively small portion of its territory along the Syrian border that is a continuation of the Arabian plate , Turkey geologically is part of the great Alpide belt that extends from the Atlantic Ocean to the Himalaya ...
In the western Mediterranean, the relative motions of the Eurasian and African plates produce a combination of lateral and compressive forces, concentrated in a zone known as the Azores–Gibraltar Fault Zone. Along its northeast margin, the African plate is bounded by the Red Sea Rift where the Arabian plate is moving away from the African plate.
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