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Upper Karoo

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Upper Karoo
NameUpper Karoo
LocationSouthern Africa
Subdivision typeCountries
Subdivision nameBotswana; Namibia; South Africa; Zimbabwe; Zambia; Mozambique; Angola

Upper Karoo

The Upper Karoo is a highland plateau region of southern Africa characterized by semi-arid savanna, escarpments and sedimentary basins lying across parts of Botswana, Namibia, South Africa, Zimbabwe and fringes of Zambia and Mozambique; it links the Kalahari Basin to the Great Escarpment and the East African Rift. The region has been central to studies by institutions such as the University of Cape Town, the Natural History Museum, London, the Smithsonian Institution, the South African National Biodiversity Institute and the Botswana Department of Geological Survey. The Upper Karoo's landscapes are referenced in works by geologists like Alexander DuToit, paleontologists such as Robert Broom, and explorers including David Livingstone and Henrietta Stockdale.

Geography and Boundaries

The plateau extends from the Kalahari Desert margins through the Molopo River catchment to the foot of the Drakensberg and adjoins the Zambezi River headwaters, forming transitional zones with the Kalahari Basin, the Zambezi Basin, the Okavango Delta, the Limpopo Basin and the Namib Desert. Major towns and cities near or within the region include Upington, Kimberley, Gaborone, Francistown, Bulawayo, Lusaka and Maputo, while protected areas and parks touching the plateau include Kgalagadi Transfrontier Park, Hwange National Park, Etosha National Park and Kruger National Park. Transport corridors such as the Cape Town–Harare Road, the Trans-Kalahari Corridor, the Limpopo Railway and regional airfields at Maun Airport and Upington Airport mediate flows between the plateau and coastal ports like Walvis Bay and Durban.

Geology and Stratigraphy

The Upper Karoo overlies the Karoo Supergroup sedimentary succession, with stratigraphic units correlated with the Beaufort Group, Stormberg Group, Drakensberg Group and underlying Dwyka Group glacial deposits; magmatism associated with the Karoo-Ferrar Flood Basalts and the Drakensberg Group influences the plateau's basalt caprock. Economic geology intersects with discoveries at the Sishen mine, Modikwa Mine, and stratigraphic research performed by the Council for Geoscience (South Africa), the Botswana Geoscience Institute and the Geological Survey of Namibia. Fossiliferous horizons within the Karoo Supergroup yielded taxa described by Harry Seeley, Richard Owen, Cecil Rhodes-era collectors, and later revisions by Anusuya Chinsamy-Turan and J. W. Kitching.

Climate and Hydrology

The climate is semi-arid to subhumid with seasonal rainfall gradients influenced by the Intertropical Convergence Zone, the Benguela Current and the Agulhas Current; climate records are monitored by national services including the South African Weather Service, the Botswana Meteorological Services and the Zimbabwe Meteorological Services. Major rivers and drainage features include the Molopo River, the Shashe River, tributaries of the Limpopo River, and ephemeral channels feeding the Okavango Delta and endorheic pans such as Makgadikgadi Pan, with water management projects linked to agencies like the Limpopo Watercourse Commission and the OKACOM initiative. Paleoclimate reconstructions using cores and isotopes have been developed by researchers at the University of the Witwatersrand, the Max Planck Institute for Chemistry, and the University of Oxford.

Ecology and Vegetation

Vegetation mosaics encompass miombo woodlands near Zambia, combretum-dominated savanna, Kalahari sandveld shrublands and riparian gallery forests associated with Acacia and Baikiaea species; biodiversity surveys have been conducted by the IUCN, the World Wildlife Fund, BirdLife International and national conservation agencies. Faunal assemblages span endemic and migratory species recorded in inventories by the South African National Biodiversity Institute and the Botswana Predator Conservation Trust and include mammals such as African elephant, plains zebra, springbok, gemsbok, lion and leopard, as well as avifauna documented by The Peregrine Fund and BirdLife Zimbabwe.

Human History and Archaeology

Archaeological records reveal Middle Stone Age and Later Stone Age occupations with lithic industries, rock art systems and pastoralist transitions investigated by teams from the British Museum, University of the Witwatersrand, University of Botswana and the National Museum of Namibia. Ethnohistoric and colonial interactions involved groups and polities such as the Tswana, Ndebele (Zimbabwe), San people, Batswana chiefdoms, and episodes linked to the Mfecane, Bechuanaland Protectorate administration, European explorers like David Livingstone and missionary networks including London Missionary Society. Heritage sites and stratified cave deposits have been curated and published by institutions such as the McGregor Museum, Iziko South African Museum and the National Museums and Monuments of Zimbabwe.

Economy and Land Use

Land use practices combine extensive livestock ranching, wildlife tourism, mining, and irrigated agriculture around floodplains; commercial enterprises include firms like Debswana, mining operations supplying the Johannesburg Stock Exchange supply chain, and tourism operators servicing routes between Victoria Falls and Cape Town. Conservation and development intersect in cooperative initiatives by the Peace Parks Foundation, African Parks, bilateral programmes with the European Union and multilateral funding from the World Bank and African Development Bank focused on sustainable land management, transfrontier parks, and water resource projects.

Category:Geography of Southern Africa