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The Eurasian plate is a tectonic plate that includes most of Eurasia (a landmass consisting of the traditional continents of Asia and Europe), with the notable exceptions of the Arabian Peninsula, the Indian subcontinent, and the area east of the Chersky Range in eastern Siberia.
These plates are often grouped with an adjacent principal plate on a tectonic plate world map. For purposes of this list, a microplate is any plate with an area less than 1 million km 2 . Some models identify more minor plates within current orogens (events that lead to a large structural deformation of Earth's lithosphere ) like the Apulian ...
Clickable map of Europe, showing the standard convention for its continental boundary with Asia. (see boundary between Asia and Europe for more information). Legend: blue = Contiguous transcontinental states; green = Sometimes considered European but geographically outside Europe's boundaries.
The boundary between Asia and Europe is unusual among continental boundaries because of its largely mountain-and-river-based characteristics north and east of the Black Sea. Asia and Europe are considered separate continents for historical reasons; the division between the two goes back to the early Greek geographers.
Banda Sea triple junction – Point where three tectonic plates meet; Boso triple junction – The meeting point of the Okhotsk Plate, the Pacific plate, and the Philippine Sea plate; Bouvet triple junction – Meeting point of three tectonic plates; Chile triple junction – Place where the South American, Nazca and Antarctic tectonic plates meet
See List of extinct countries, empires, etc. and Former countries in Europe after 1815 for articles about countries that are no longer in existence. See List of countries for other articles and lists on countries. Wikimedia Commons includes the Wikimedia Atlas of the World. Entries available in the atlas. General pages
Major shallow water bodies submerging parts of the northern plains are the Celtic Sea, the North Sea, the Baltic Sea and the Barents Sea. 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 vast majority of the world's active volcanoes occur along plate boundaries, with the Pacific plate's Ring of Fire being the most active and widely known. Some volcanoes occur in the interiors of plates, and these have been variously attributed to internal plate deformation [15] and to mantle plumes.