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The Mediterranean Sea (/ ËŒ m É› d ɪ t É™ ˈ r eɪ n i É™n / MED-ih-tÉ™-RAY-nee-É™n) is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Southern Europe and Anatolia, on the south by North Africa, on the east by the Levant in West Asia, and on the west almost by the Morocco–Spain border.
Aegean Sea Plate. The Aegean Sea Plate (also called the Hellenic Plate or Aegean Plate) is a small tectonic plate located in the eastern Mediterranean Sea 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]
Mediterranean basin. In biogeography, the Mediterranean Basin (/ ˌmɛdɪtəˈreɪniən / MED-ih-tə-RAY-nee-ən), also known as the Mediterranean Region or sometimes Mediterranea, is the region of lands around the Mediterranean Sea that have mostly a Mediterranean climate, with mild to cool, rainy winters and warm to hot, dry summers, which ...
Pelso Plate – Small tectonic unit in the Pannonian Basin in Europe. Timor Plate – Microplate in Southeast Asia carrying the island of Timor and surrounding islands. Tisza Plate – Tectonic microplate, in present-day Europe. Juan de Fuca Plate – Small tectonic plate in the eastern North Pacific – 250,000 km 2.
A Mediterranean climate (/ ËŒ m É› d ɪ t É™ ˈ r eɪ n i É™n / MED-ih-tÉ™-RAY-nee-É™n), also called a dry summer climate, described by Köppen as Cs, is a temperate climate type that occurs in the lower mid-latitudes (normally 30 to 44 north and south latitude).
t. e. Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικÏŒς (tektonikós) 'pertaining to building') [1] is the scientific theory that Earth 's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago. [2][3][4] The model builds on the concept of continental ...
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