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African Plate

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Article Genealogy
Parent: Atlantic Ocean Hop 3
Expansion Funnel Raw 108 → Dedup 39 → NER 26 → Enqueued 23
1. Extracted108
2. After dedup39 (None)
3. After NER26 (None)
Rejected: 1 (not NE: 1)
4. Enqueued23 (None)
Similarity rejected: 4
African Plate
African Plate
Alataristarion · CC BY-SA 4.0 · source
NameAfrican Plate
TypeTectonic plate
Area km230000000
Movement directionnorthward, rotating clockwise
Movement speed2–3 cm/yr
StatusActive

African Plate

The African Plate is a major lithospheric plate comprising much of the continent of Africa, parts of the Mediterranean Sea, and portions of the South Atlantic Ocean; it underlies nations such as Algeria, Nigeria, Egypt, South Africa, and Kenya. It interacts with neighboring plates including the Eurasian Plate, North American Plate, South American Plate, Indian Plate, Arabian Plate, and Scotia Plate and influences phenomena recorded by institutions like the United States Geological Survey, the British Geological Survey, and the Institut de Physique du Globe de Paris. Research on the plate informs projects at universities such as University of Cape Town, Université de Montpellier, Massachusetts Institute of Technology, and agencies including the European Space Agency and the National Aeronautics and Space Administration.

Overview

The plate covers the continental crust of Sahara Desert countries and the cratons of West African Craton and Kaapvaal Craton plus offshore margins like the Gabon Basin and the Benguela Current margin; its motion is constrained by paleomagnetic studies from the Geological Society of America and seismic tomography by the International Seismological Centre. Satellite geodesy from Global Positioning System networks and missions like GRACE and Envisat document its present-day kinematics, while historical maps in the British Museum and collections at the Smithsonian Institution preserve records of exploration relevant to its coastal geology.

Tectonic Boundaries and Plate Interactions

Boundaries include divergent margins such as the East African Rift, transform systems like the Dead Sea Transform, and convergent zones beneath the Mediterranean Sea where the plate contacts the Eurasian Plate and the Anatolian Plate. The southern margin interacts with the Scotia Plate and the South American Plate along the Mid-Atlantic Ridge, and the eastern margin abuts the Arabian Plate near the Gulf of Aden and Red Sea. Historic subduction episodes involved terranes now juxtaposed in orogenic belts like the Atlas Mountains and the Zagros Mountains, studied by researchers from institutions including the Royal Society and the Max Planck Society.

Geology and Structure

The lithosphere includes ancient shields such as the Sahara Metacraton and the Congo Craton overlain by Proterozoic and Phanerozoic basins like the Taoudeni Basin and the Karoo Basin. Crustal architecture features cratonic roots sampled in boreholes documented by the Geological Survey of Egypt and geophysical surveys run by companies like Schlumberger and BP. Mantle processes are investigated using data from the Seismological Society of America and shear-wave studies at the European Seismological Commission, revealing plume candidates beneath hotspots such as Réunion, Ile de la Réunion, and Mount Kilimanjaro.

Geological History and Evolution

The plate's assembly involved Precambrian collisions forming shields and sutures preserved in regions like the Man Shield and the Tanzania Craton, followed by breakup events tied to the dispersal of Pangaea and the opening of the South Atlantic Ocean. Cenozoic rifting created the East African Rift System and the Afar Triple Junction, linked to paleoenvironmental changes studied in cores housed at the Natural History Museum, London and through isotope analyses at Scripps Institution of Oceanography. Tectonic episodes that shaped the plate are recorded alongside global events such as the Cretaceous–Paleogene extinction event and the Eocene–Oligocene extinction event.

Seismicity and Volcanism

Seismic activity occurs along rifts and transform faults producing events recorded by networks like the Global Seismographic Network and the African Seismological Commission. Notable historic earthquakes impacted cities such as Mogadishu, Marrakesh, Cairo, and Addis Ababa and are cataloged by the International Seismological Centre. Volcanism includes stratovolcanoes and shield volcanoes exemplified by Mount Nyiragongo, Mount Cameroon, Ol Doinyo Lengai, and the Ethiopian Highlands associated with mantle upwelling studied by groups at the African Academy of Sciences and the United Nations Office for Disaster Risk Reduction.

Geomorphology and Surface Features

Surface expression comprises rift valleys like the Great Rift Valley, plateaus such as the Ethiopian Plateau, deserts including the Sahara, river systems like the Nile River, Congo River, and Zambezi River, and lake basins such as Lake Tanganyika and Lake Malawi. Coastal features include the Gulf of Guinea and the Mozambique Channel shaped by sea-level changes chronicled in records from the Intergovernmental Panel on Climate Change and sediment archives at the Woods Hole Oceanographic Institution.

Economic Resources and Human Impact

The plate hosts mineral provinces exploited by companies like Rio Tinto, Anglo American, De Beers, and Barrick Gold producing diamonds from the Kimberley fields and gold from the Witwatersrand Basin; hydrocarbon basins include the Niger Delta, Egyptian Nile Delta, and the Congo Basin with exploration by TotalEnergies and ExxonMobil. Groundwater resources in the Nubian Sandstone Aquifer System and mineral-rich manganese deposits in the Kalahari Basin support societies in capitals like Pretoria, Lagos, Nairobi, and Cairo, while environmental impacts are addressed by organizations such as United Nations Environment Programme and World Wildlife Fund.

Category:Tectonic plates