Hydrogeology of Cameroon
Much of the textual information on this page was taken from the chapter on Cameroon in the report ‘Groundwater in North and West Africa’ (UN 1988). Other sources are referenced individually below. Some of the following information is outdated. If you have more recent information on the hydrogeology of Cameroon, please get in touch.
- 1 Compilers
- 2 Terms and conditions
- 3 Geographical Setting
- 4 Geology
- 5 Hydrogeology
- 6 Groundwater Status
- 7 Groundwater use and management
- 8 References
- 9 Return to the index pages
Dr Kirsty Upton and Brighid Ó Dochartaigh, British Geological Survey, UK
Please cite this page as: Upton & Ó Dochartaigh, 2016.
Bibliographic reference: Upton, K. & Ó Dochartaigh, B.É. 2016. Africa Groundwater Atlas: Hydrogeology of Cameroon. British Geological Survey. Accessed [date you accessed the information]. http://earthwise.bgs.ac.uk/index.php/Hydrogeology_of_Cameroon
Terms and conditions
The Africa Groundwater Atlas is hosted by the British Geological Survey (BGS) and includes information from third party sources. Your use of information provided by this website is at your own risk. If reproducing diagrams that include third party information, please cite both the Africa Groundwater Atlas and the third party sources. Please see the Terms and Conditions for more information.
Cameroon is in central-west Africa with a western coast on the Gulf of Guinea, and Lake Chad at its northernmost extent. Its geography includes a coastal plain, which extends 15 to 150 km inland; the south Cameroon plateau which rises from the coastal plain to more than 600 m; the Cameroon chain of mountains, hills and plateaus that extends from Mount Cameroon on the coast(Cameroon's highest point at 4,095 m) almost to Lake Chad on the northern border; the Adamawa Plateau in the centre of the country, with an average elevation of 1,100 m; and a northern lowland region which extends from the edge of the Adamawa Plateau to Lake Chad, with an elevation of around 300 m.
|Estimated Population in 2013*||22,253,959|
|Rural Population (% of total) (2013)*||46.8%|
|Total Surface Area*||472,710 sq km|
|Agricultural Land (% of total area) (2012)*||20.6%|
|Border Countries||Nigeria, Chad, the Central African Republic, Equatorial Guinea, Gabon, the Republic of the Congo.|
|Annual Freshwater Withdrawal (2013)*||966.4 Million cubic metres|
|Annual Freshwater Withdrawal for Agriculture (2013)*||76.3%|
|Annual Freshwater Withdrawal for Domestic Use (2013)*||16.7%|
|Annual Freshwater Withdrawal for Industry (2013)*||7.1%|
|Rural Population with Access to Improved Water Source (2012)*||51.9%|
|Urban Population with Access to Improved Water Source (2012)*||94.1%|
* Source: World Bank
The climate varies across the country, controlled by topography. The upland areas have a mild climate with high rainfall. The coast is hot and very wet, with only a short dry season. The plateau areas show distinct wet and dry seasons, with lower rainfall than the coastal region. The northern lowland region is relatively arid, with low rainfall and high temperatures.
These maps and graphs were developed from the CRU TS 3.21 dataset produced by the Climatic Research Unit at the University of East Anglia, UK. For more information see the climate resource page.
|The main rivers in the south of the country are the Ntem, Nyong, Sanaga, and Wouri, which flow southwestward or westward into the Gulf of Guinea. The Dja and Kadéï drain southeastward into the Congo River. In the north, the Bénoué River flows north and west into the Niger. The Logone flows northward into Lake Chad, which Cameroon shares with three neighbouring countries.|
|The coastal plain and southern plateau is dominated by equatorial rainforest. The upland regions have highland forest type vegetation. The dominant land cover in the northern lowland region is savanna scrub and grass.
This section provides a summary of the geology of Cameroon. More information is available in the report Groundwater in North and West Africa: Cameroon (1988) (see References section, below).
The geology map shows a simplified version of the geology at a national scale (see the Geology resources page for more details).
|Mesozoic, Cenozoic and Quaternary Sedimentary|
|Douala coastal basin||Cretaceous to Quaternary||Composed mainly of Cretaceous marine sandstones and limestones, which are 1000 to 2000 m thick. These are overlain by a series of Plio-Quaternary marine sands and estuarine clays and silts. The two aquifers are separated by mudstones of the Nkappa formation.|
|Lake Chad basin||Cretaceous to Quaternary||The Lake Chad basin contains three main geological units: a upper Quaternary-Lower Pliocene series; the Tertiary Continental Terminal; and the lower Cretaceous series of the Hamadien Continental and the Continental Intercalaire (GWP 2013).|
|Garoua basin||Cretaceous-Tertiary||A lower series of clays and sandstones in the southeast, and an upper series of sandstones in the west of the basin. This is the equivalent of the Bima sandstone of the Upper Benue basin in Nigeria (Mafany and Fantong 2006).|
|Koum, Babouri-Figuil, Mayo Oulo, Mayo Sorawel, Mamfé, Bamusso and Djerem basins||These are smaller sedimentary basins. Some - eg Mamfé - contain evaporites.|
|Volcanic massifs from the Adamaoua to the Atlantic||Various ages||There are a series of parallel faults running northeast/southwest, with displacements that can reach 1000 m, and associated with large volcanic massifs of various ages and compositions. These are dominantly basalts, with occasional intermediate to acidic phonolites, trachytes and rhyolites, and some loose pyroclastic and tuffaceous ash on the flanks of the volcanic centres.|
|Lower Dja series and others||Upper Precambrian||This is generally un-metamorphosed, and made up of tillites with sandstones and schist intersected by granitic intrusions (the Lower Dja series).|
|Middle Precambrian||Found in the southeast, and north of the Adamaoua, around Poli, this is made up of a series of schists-amphibolites with intercalations of quartzitic sandstones and phyllites.|
|Lower Precambrian||A complex of granites, micaschists and migmatites.|
This section provides a summary of the hydrogeology of the main aquifers in Cameroon. More information is available in the report Groundwater in North and West Africa: Cameroon (1988) (see References section, below).
The hydrogeology map shows a simplified version of the type and productivity of the main aquifers at a national scale (see the Hydrogeology Map resource page for more details).
Unconsolidated aquifers - including alluvium, marine and estuarine deposits - occur in many parts of the country, and are typically in hydraulic continuity with underlying bedrock aquifers. They are described in the relevant sections below.
Sedimentary - Intergranular & Fracture Flow
|Named Aquifers||Period||General Description||Water quality|
|Douala basin||Tertiary-Quaternary||The main aquifer in this basin is the unconsolidated Plio-Quaternary sands, which form an upper and a lower aquifer, separated by a clay layer. The uppermost sandy layer is hydraulically connected with brackish waters in the Wouri estuary, and saline waters of the coastal wetlands. Occasionally, falling water tables in the dry season cause a reversal of the hydraulic gradient and seawater intrusion. The deeper aquifer is confined by the intervening clays, which is widely used for industry and domestic supplies in Douala (Mafany and Fantong 2006). Boreholes are between 60 and 200 m deep (UN 1988).
The deeper Cretaceous sandstones also form an important aquifer, hydraulically separated from the overlying Plio-Quaternary by mudstones. This aquifer is not vulnerable to saline intrusion (Mafany and Fantong 2006).
|Groundwater in the upper Plio-Quaternary aquifer is typically of Na-Cl type and brackish. Groundwater in the deeper confined Plio-Quaternary aquifer is dominated by Na-HCO3 and Ca-HCO3 types, with typically good quality.
Groundwater in the deeper Cretaceous sandstone aquifer is dominated by K/Na-HCO3 types, and typically of good quality. It is used to supplement the domestic and industrial water demand of Douala (Mafany and Fantong 2006).
|Garoua basin||Cretaceous-Tertiary||These sandstones form a productive aquifer, with permeabilities of around 8 to 80 m/day; transmissivities of 300 to 1700 m²/day; and a storage coefficient of 0.025. Boreholes are typically between 40 and 200 m deep.||Largely acidic groundwater, with pH from 4 to 7. Very high fluoride concentrations are seen in the southwest of the basin, causing dental fluorosis (Mafany and Fantong 2006).|
|Lake Chad Basin Aquifer||Cretaceous to Quaternary||The Lake Chad basin aquifer contains three main aquifer units: a upper Quaternary-Lower Pliocene series; the Tertiary Continental Terminal; and the lower Cretaceous series of the Hamadien Continental and the Continental Intercalaire (GWP 2013). The basin is shared by Chad, Niger, the Central African Republic, Nigeria, Cameroon, Algeria, Sudan and Libya.
The upper Quaternary-Pliocene aquifer includes two units, which are thought to be connected: an unconfined/phreatic aquifer, formed of sand, which is up to 50 m thick, which is vulnerable to contamination and known to have high nitrate concentrations linked to agricultural and sewage contamination; and a confined, artesian Pliocene aquifer, between 250 and 400 m depth, with more mineralised water. Artesian pressure is being reduced, possibly due to over pumping. Recharge occurs to the confined aquifer only in limited areas (GWP 2013).
The middle Continental Terminal, of Tertiary to Quaternary age, comprises alternating sandstone and clay layers, which are 450 to 620 m from the surface (GWP 2013).
Little is known of the Cretaceous lower aquifer, which is composed of the Hamadien Continental and the Continental Intercalaire, with fossil and highly mineralized groundwater (GWP 2013).
|Small sedimentary basins - including Hama Kossou, Babouri-Figuil, Sorawel, Mayo Oulo and Mamfé||Cretaceous||These basins generally form low to moderately productive aquifers, capable of borehole yields of up to 5 m³/hour. Many springs occur. Abstraction boreholes in the Hama Kossou, Babouri-Figuil and Mayo Oulo basins are typically between 120 and 180 m deep.||Groundwater quality is generally good. The local presence of evaporites in the Mamfé basin leads to groundwaters of sodium-chloride composition (Mafany and Fantong 2006).|
|Named Aquifers||Period||General Description||Water quality|
|Various ages||Volcanic centres form moderately to highly productive fractured/weathered aquifers. Many springs emerge from hill slopes, some of them thermal (Mafany and Fantong 2006).||Generally sodium-bicarbonate or iron/magnesium/calcium-bicarbonate type.|
|Named Aquifers||Period||General Description||Water quality|
|Metamorphic crystalline basement||Precambrian||Crystalline rocks cover most of Cameroon, sometimes covered with alluvium and other unconsolidated deposits, and laterite. They typically form small, local aquifers, limited to areas where the rock has been fractured and weathered to increase its permeability. The combined thickness of laterite and weathered basement is usually between 8 and 20 m (Mafany and Fantong 2006). Below this there can be a deeper fractured aquifer, which usually has low permeability. The best yields are found where fractured rocks are overlain with a thick weathered zone or thick alluvium. Borehole yields are usually 1 to 3 m³/hour, in the region of the Mandara mountains, but can rarely reach 30 m³/hour in places in the Kribi region, associated with large faults (UN 1988||Groundwater usually has low mineral content, with total dissolved solids rarely exceeding 300 mg/l, and conductivities generally between 30 and 350 uS/cm. The water is usually of magnesium-carbonate type (Mafany and Fantong 2006).|
Of the 322 billion cubic meters of total available water resources, groundwater constitutes 21% (57 billion cubic meters) of this resource (Ako Ako et al. 2009; Sigha-Nkamdjou et al. 1998). High rainfall means high potential recharge potential in much of Cameroon, except in the arid north, and the limitations on groundwater potential are therefore largely related to low aquifer storage and permeability in the basement rocks across much of the country.
In the northern region, increasing population combined with a reduction in the quantity and regularity of rainfall has resulted in persistent drought and reduced groundwater resources (Ako Ako et al. 2009).
Most groundwater in Cameroon is of good natural inorganic quality. The least mineralised overall is groundwater in basement aquifers; the most mineralised is found in volcanic aquifers, apart from the mineralised springs in the Mamfé basin, related to evaporites. Groundwater from the volcanics is widely used by the bottled water industry. Some groundwater in deeper aquifers contains low oxygen and corresponding high iron and even hydrogen sulphate gas (Mafany and Fandong 2006).
However, much of the shallow groundwater is vulnerable to contamination. Shallow coastal aquifers are subject to seawater intrusion. There is no evidence for widespread inorganic contamination of groundwaters, even in urban areas, but there is widespread bacteriological contamination of shallow groundwater in urban areas, such as Yoaundé and Douala, derived from domestic, industrial and hospital waste (Mafany and Fandong 2006).
Groundwater use and management
The rural population largely relies on groundwater for water supply, through springs, hand dug wells, and boreholes equipped with hand pumps (Ako Ako et al. 2009).
Some urban centres widely use groundwater, including Douala.
The Ministry of Mines, Energy and Water (Ministère des Mines, de l’Énergie et de l’Eau), has responsibility for water supply and sanitation in both rural areas and towns through the Directorate of Directorate of Water (DE: Direction de l’Eau). In recent years, the former National Water Supply Company of Cameroon (SNEC: Société Nationale des Eaux du Cameroun) has been privatised with the creation of the Cameroon Water Utilities Corporation (CAMWATER) with responsibility for public water supplies in urban areas; and the responsibility for the construction and management of rural wells and boreholes has been transferred to communes (AMCOW 2011).
In northeast Chad, the Lake Chad basin aquifer is shared with neighbouring countries. A number of agreements and cooperative activities exist between these countries (e.g Alker 2008).
For further information about transboundary aquifers, please see the Transboundary aquifers resources page
The following references provide more information on the geology and hydrogeology of Cameroon.
These, and others, can be accessed through the Africa Groundwater Literature Archive
Alker M. 2008. The Lake Chad Basin Aquifer System: a case study for the research project 'Transboundary groundwater management in Africa'. German Development Institute.
AMCOW. 2011. Water Supply and Sanitation in Cameroon. Water and Sanitation Program.
GWP (Global Water Partnership). 2013. The Lake Chad Basin Aquifer System. Transboundary Groundwater Fact Sheet, compiled by F Bontemps.
Mafany GT and Fantong WY. 2006. Groundwater quality in Cameroon and its vulnerability to pollution. In: Groundwater quality in Africa, ed. Y Xu and B Usher, Taylor and Francis/Balkema, Rotterdam, pp 47-55
United Nations. 1988. Groundwater in North and West Africa: Cameroon. United Nations Department of Technical Cooperation for Development and Economic Commission for Africa, Natural Resources/Water Series No. 18, ST/TCD/5.