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Central African Plateau

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Central African Plateau
NameCentral African Plateau
Other namesCameroon Plateau; Adamawa Plateau (partial)
LocationCameroon; Central African Republic; Chad; Republic of the Congo (northern); Sudan (southern fringes); Democratic Republic of the Congo (northeastern edge)
Coordinates6°N 18°E
Area km2800000
Elevation m500–1400
Highest pointMount Cameroon (adjacent highlands)

Central African Plateau is an extensive highland region occupying much of central Africa between the Sahel and the Congo Basin. The plateau forms a broad, gently undulating surface that influences the courses of major rivers such as the Chari River, Logone River and upper reaches of the Congo River, and shapes the boundaries of states like Cameroon and the Central African Republic. The plateau’s elevation, geology and climate have produced distinct ecosystems used by peoples including the Fang people, Fulani people, and Sara people.

Geography

The plateau extends from the foothills of the Adamawa Mountains and the Cameroonian Highlands eastward toward the borderlands of Sudan and the Democratic Republic of the Congo, encompassing parts of Cameroen North Region and Mbéré Department, as well as Bamingui-Bangoran and Vakaga Prefecture in the Central African Republic. Principal cities on or near the plateau include Garoua, Maroua, Moundou, and N'Djamena (on the plateau’s western approaches). Surrounding physiographic features include the Adamawa Plateau, the Borkou-Ennedi-Tibesti Region, the Lake Chad Basin, and the Congo Basin. Drainage divides send water north toward the Chari River and Lake Chad and south to the Sangha River and Ubangi River tributaries of the Congo River. The plateau’s soils, plateaus, and escarpments shaped historic routes such as those used by explorers like Paul Du Chaillu and colonial administrations including French Equatorial Africa.

Geology and Formation

The plateau is underlain by Precambrian crystalline basement rocks related to the Gondwana assembly and later modified during the Pan-African orogeny. Volcanism associated with the Cameroon Volcanic Line and Miocene uplift produced basaltic flows and lateritic caps overlapping older schists and gneisses. Rift-related faulting linked to the East African Rift system and intraplate stress created mesas, inselbergs and faults that influenced drainage toward the Chari and Congo catchments. Sedimentary sequences deposited in the Lake Chad Basin and the Congo Basin record fluctuating Pleistocene paleoenvironments studied by researchers at institutions such as the French National Centre for Scientific Research and the Smithsonian Institution. Economic geology includes laterite-hosted iron and manganese and basement-controlled gold occurrences explored by companies like Randgold Resources and state entities such as Société Nationale des Hydrocarbures variants.

Climate and Hydrology

The plateau experiences a gradient from tropical wet-and-dry climates in the south (monsoon-influenced) to semi-arid climates in the north (Sudano-Sahelian), modulated by elevation that brings cooler nights and increased precipitation relative to adjacent lowlands. Seasonal migration of the Intertropical Convergence Zone controls rainy seasons that feed the Chari-Logone system and ephemeral tributaries of the Sangha River. Groundwater in crystalline basement aquifers supports wells and boreholes sunk by development projects funded by World Bank and African Development Bank initiatives. Historic hydrological events—flooding of the Logone and low flows in the Chari River—have impacted populations during episodes recorded by agencies like UNICEF and World Health Organization.

Ecology and Vegetation

Vegetation varies from wooded savanna and miombo-like woodlands in southern sectors to open sahelian grasslands and isolated montane forest patches on the plateau’s higher ridges. Flora includes species associated with Guineo-Congolian and Sudano-Zambezian domains, with trees such as Isoberlinia doka, Vitellaria paradoxa (shea), and gallery forests hosting Entandrophragma cylindricum and Milicia excelsa where riverine conditions permit. Fauna historically included large mammals like African elephants, roan antelope, and lions, and supports endemic and migratory bird species that attract ornithologists from institutions including the British Ornithologists' Union and the National Audubon Society for studies of SahelCongo Basin avifaunal links.

Human Settlement and Land Use

Indigenous peoples such as the Sara people, Gbaya people, Mbororo, and Baka people have practiced shifting cultivation, agro-pastoralism, and transhumant pastoralism across the plateau. Colonial-era land policies by French Equatorial Africa and postcolonial administrations in Cameroon and the Central African Republic reshaped settlement patterns, encouraging urban centers like Garoua and transport corridors linking to colonial railheads and roads to Douala and Brazzaville. Contemporary land uses include subsistence farming of millet, sorghum, and cassava; pastoralism by groups linked to the Fulani people; commercial cattle ranching; and peri-urban agriculture supplying markets in N'Djamena and Yaoundé. Conflicts over land tenure and grazing rights involve actors such as the African Union and regional bodies like the Economic Community of Central African States.

Economy and Natural Resources

The plateau contains agricultural zones producing sorghum, millet, groundnuts, cotton, and cashew nuts marketed via companies like Cargill and regional cooperatives. Mineral prospects include iron ore, gold, and manganese targeted by firms such as Glencore and national mining agencies. Forestry resources in gallery woodlands and patches of rainfed forest support timber extraction by enterprises linked to certification schemes from the Forest Stewardship Council; charcoal production supplies urban energy markets. Hydropower potential on plateau rivers has been proposed in projects evaluated by African Development Bank and International Finance Corporation, while oil explorations in basins adjacent to the plateau have involved multinational corporations like TotalEnergies and ExxonMobil.

Conservation and Environmental Issues

Environmental pressures include deforestation for agriculture and fuelwood, soil erosion on cultivated slopes, and biodiversity loss exacerbated by poaching networks tied to international trafficking monitored by Interpol and conservation NGOs such as World Wildlife Fund and Conservation International. Protected areas and reserves—some managed in partnership with the United Nations Environment Programme and national park authorities like Cameroon National Parks Authority—aim to conserve endemic species and watershed integrity. Climate change models from the Intergovernmental Panel on Climate Change project shifts in rainfall regimes, raising concern among development agencies and local communities relying on NGO programs from organizations like FAO and UNDP. Cross-border conservation initiatives involve corridors linking plateau habitats to the Congo Basin and seek financing through mechanisms such as the Green Climate Fund and REDD+ pilots.

Category:Plateaus of Africa