African tectonic plate in the context of "Anatolian plate"

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⭐ Core Definition: African tectonic plate

The African plate, also known as the Nubian plate, is a major tectonic plate that includes most of the continent of Africa (except for its easternmost part) and the adjacent oceanic crust to the west and south. It also includes a narrow strip of Western Asia along the Mediterranean Sea, including much of Israel and Lebanon. It is bounded by the North American plate and South American plate to the west (separated by the Mid-Atlantic Ridge); the Arabian plate and Somali plate to the east; the Eurasian plate, Aegean Sea plate and Anatolian plate to the north; and the Antarctic plate to the south.

Between 60 million years ago and 10 million years ago, the Somali plate began rifting from the African plate along the East African Rift. Since the continent of Africa consists of crust from both the African and the Somali plates, some literature refers to the African plate as the Nubian plate to distinguish it from the continent as a whole.

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African tectonic plate in the context of Maltese archipelago

The geography of Malta is dominated by water. Malta is an archipelago of coralline limestone, located in Southern Europe, but like most of Sicily sits on the African tectonic plate in the Mediterranean Sea. Malta is 81 kilometres (50 mi) south of Sicily, Italy, and nearly 300 km (190 mi) north (Libya) and northeast (Tunisia) of Africa. Although Malta is located farther south than Tunis and some other cities in North Africa, it is not the Southernmost point of Europe. Only the three largest islands – Malta, Gozo and Comino – are inhabited. Other (uninhabited) islands are: Cominotto, Filfla and the St. Paul's Islands. The country is approximately 316 km (122 sq mi) in area. Numerous bays along the indented coastline of the islands provide harbours. The landscape of the islands is characterised by high hills with terraced fields. The capital is Valletta.

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