Geologists generally agree that the following tectonic plates currently exist on Earth's surface with roughly definable boundaries. Tectonic plates are sometimes subdivided into three fairly arbitrary categories: major (or primary) plates, minor (or secondary) plates, and microplates (or tertiary plates).[1]
Major plates
Map showing Earth's principal tectonic plates and their boundaries in detail
These plates comprise the bulk of the continents and the Pacific Ocean. For purposes of this list, a major plate is any plate with an area greater than 20 million km2.
Earth:Antarctic Plate – Major tectonic plate containing Antarctica and the surrounding ocean floor – 60,900,000 km2
Earth:Eurasian Plate – Tectonic plate which includes most of the continent of Eurasia – 67,800,000 km2
Earth:Indo-Australian Plate – A major tectonic plate formed by the fusion of the Indian and the Australian plates (sometimes considered to be two separate tectonic plates) – 58,900,000 km2
Earth:Australian Plate – Major tectonic plate separated from Indo-Australian Plate about 3 million years ago – 47,000,000 km2
Earth:Indian Plate – Minor plate that separated from Gondwana – 11,900,000 km2
Earth:North American Plate – Large tectonic plate including most of North America, Greenland and part of Siberia – 75,900,000 km2
Earth:Pacific Plate – Oceanic tectonic plate under the Pacific Ocean – 103,300,000 km2
Earth:South American Plate – Major tectonic plate which includes most of South America and a large part of the south Atlantic – 43,600,000 km2
Minor plates
These smaller plates are often not shown on major plate maps, as the majority of them do not comprise significant land area. For purposes of this list, a minor plate is any plate with an area less than 20 million km2 but greater than 1 million km2.
Earth:Yangtze Plate – Small tectonic plate carrying the bulk of southern China
Microplates
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 km2. Some models identify more minor plates within current orogens (events that lead to a large structural deformation of Earth's lithosphere) like the Apulian, Explorer, Gorda, and Philippine Mobile Belt plates.
[2] One study has theorized that microplates may be the basic elements of which the crust is composed.
[3]
African Plate
Earth:Lwandle Plate – Mainly oceanic tectonic microplate off the southeast coast of Africa
Earth:Rovuma Plate – One of three tectonic microplates that contribute to the Nubian Plate and the Somali Plate
Antarctic Plate
Earth:Shetland Plate – Tectonic microplate off the tip of the Antarctic Peninsula
In the history of Earth, many tectonic plates have come into existence and have over the intervening years either accreted onto other plates to form larger plates, rifted into smaller plates, or have been crushed by or subducted under other plates.
The following is a list of ancient cratons, microplates, plates, and terranes which no longer exist as separate plates. Cratons are the oldest and most stable parts of the continental lithosphere, and shields are exposed parts of them. Terranes are fragments of crustal material formed on one tectonic plate and accreted to crust lying on another plate, which may or may not have originated as independent microplates: a terrane may not contain the full thickness of the lithosphere.
African Plate
Earth:Atlantica – Ancient continent formed during the Proterozoic about 2 billion years ago
Earth:Congo Craton – Precambrian craton that with four others makes up the modern continent of Africa (Angola, Cameroon, Central African Republic, Democratic Republic of Congo, Gabon, Sudan, and Zambia)
Earth:Saharan Metacraton – Large area of continental crust in the north-central part of Africa (Algeria)
Earth:Tanzania Craton – Old and stable part of the continental lithosphere in central Tanzania (Tanzania)
Earth:West African Craton – One of the five cratons of the Precambrian basement rock of Africa that make up the African Plate (Algeria, Benin, Burkina Faso, Côte d'Ivoire, Gambia, Ghana, Guinea, Guinea Bissau, Liberia, Mali, Mauritania, Morocco, Nigeria, Senegal, Sierra Leone, and Togo)
Earth:Avalonia – Microcontinent in the Paleozoic era (Canada, Great Britain, and United States)
Earth:Churchill Craton – Northwest section of the Canadian Shield from southern Saskatchewan and Alberta to northern Nunavut (Canada)
Earth:Farallon Plate – Ancient oceanic plate that has mostly subducted under the North American Plate (split into the Cocos, Explorer, Juan de Fuca, Gorda Plates, Nazca Plate, and Rivera Plates)
Laurentian Craton, also known as North American Craton – A large continental craton that forms the ancient geological core of the North American continent (Canada and United States)
Cordani, U.G.; Cardona, A.; Jiménez, D.M.; Dunyl, L.; Nutman, A.P. (2003). "Geochronology of Proterozoic basement from the Colombian Andes: Tectonic history of remnants from a fragmented Grenville Belt". 10o Congreso Geológico Chileno. pp. 1–10.