Hydrogeology of Central African Republic

Africa Groundwater Atlas >> Hydrogeology by country >> Hydrogeology of the Central African Republic

Most of the textual information on this page was taken from the chapter on the Central African Republic in the report‘Groundwater in North and West Africa’ (UN 1988). This information is outdated. If you have more recent information on the hydrogeology of the Central African Republic, please get in touch.

Compilers

Dr Kirsty Upton and Brighid Ó Dochartaigh, British Geological Survey, UK

Geographical Setting

Map of the Central African Republic (For more information on the datasets used in the map see the geography resources section)

General

The Central African Republic has a low relief formed by erosion, with occasional inselbergs forming isolated higher areas of ground. In the northeast and northwest of the country are small two mountain ranges which rise to over 1,300 m. A ridge of high ground between the two mountain ranges forms a boundary between the Lake Chad basin to the north, and the Congo basin to the south.

Estimated Population in 2013*	4,616,417
Rural Population (% of total) (2013)*	60.5%
Total Surface Area*	622,980 sq km
Agricultural Land (% of total area) (2012)*	8.2%
Capital City	Bangui
Region	Central Africa
Border Countries	Chad, Sudan, South Sudan, the Democratic Republic of the Congo, the Republic of the Congo, Cameroon
Annual Freshwater Withdrawal (2013)*	72.5 Million cubic metres
Annual Freshwater Withdrawal for Agriculture (2013)*	0.6%
Annual Freshwater Withdrawal for Domestic Use (2013)*	82.9%
Annual Freshwater Withdrawal for Industry (2013)*	16.6%
Rural Population with Access to Improved Water Source (2012)*	54.4%
Urban Population with Access to Improved Water Source (2012)*	89.6%

* Source: World Bank

Climate

The Central African Republic has a tropical to semi-arid climate, with average annual rainfall ranging from 1,700 mm in the south to 700 mm in the north. There are two wet seasons, the main one in August-September and the smaller one in May-June.

Average temperatures range from about 23 degrees in the south to 26 degrees in the north, with a larger seasonal variation in temperatures in the north. Calculated evaporation potential ranges from 1,500 mm/year in the south to over 1,900 mm/year in the north.

• 
  Koppen Geiger Climate Zones
• 
  Average Annual Precipitation
• 
  Average Temperature

For further detail on the climate datasets used see the climate resources section.

Surface water

The north of the country is part of the Lake Chad basin, with sometimes ephemeral rivers draining to the Chari and the Logone, both of which flow into Chad and to Lake Chad. The south is part of the Congo basin, and the main rivers are the Obangui and the Sangha, and their tributaries, which are largely perennial.

Surface Water Map of the Central African Republic (For more information on the datasets used in the map see the surface water resources section)

Soil

Most soils are plinthosols, ferrasols or arenosols, with some acrisols. Soil Map of the Central African Republic (For map key and more information on the datasets used in the map see the soil resources section)

Land cover

The south of the country is dominated by evergreen tropical forest. Much of the central part of the country is dominated by decidous forest and grassland. In the north, the dominant land cover is mostly shrubland.

Land Cover Map of the Central African Republic (For map key and more information on the datasets used in the map see the land cover resources section)

Geology

This section provides a summary of the geology of the Central African Republic. More information is available in the report ‘Groundwater in North and West Africa’ (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).

Another geology map is available in the report by Chirico et al.. 2010.

Summary

Most of the country is underlain by crystalline metamorphic Precambrian basement rocks of the African shield.

Younger rocks cover only about a quarter of the country, mainly in the west and north, and smaller areas in the far south. They include Mesozoic sandstone formations; Tertiary sandstone formations; and Quaternary lacustrine and alluvial deposits.

Geological Environments

Key Formations	Period	Lithology
Quaternary unconsolidated
Lacustrine and alluvial deposits	Quaternary	Neo-Chadian (part of the Lake Chad basin series) formations of lacustrine origin with thick layers of recent clays. Alluvium in river valleys. Deposits in the depressions and swampy areas of the Sangha basin.
Phanerozoic sedimentary
Tertiary	Banbio sandstone	In the north are ferruginous sandstones, sands and cuirasses forming the edge of the Lake Chad basin. In the south are silicified sandstones, sands and loess of the Congo basin, including the Banbio sandstone.
Cretaceous	Carnot and Mouka Ouadda sandstones; small outcrops in north	Thick continental sedimentary sequences resting in angular disconformity on the basement complex. The Carnot Sandstones are fluvio-lacustrine detrital formations probably largely of Cretaceous age, which stretch over an area of more than 40 000 km² in the the western part of the country, comprised of a succession of conglomerates, sandstones and argilites which can reach 300 m in thickness (Censier 1990).
Palaeozoic		The two major Paleozoic formations are the Mambéré Formation in the west of the country, and the Kombélé Formation in the east, both of glacial origin (Censier et Lang 1992, Chirico et al. 2010). The Mambéré Formation is a tillite composed of both basal and flow tills as well as reworked glacial deposits derived from sandstone, conglomeratic sandstone, and siltstone that occur in continuous beds, lenses, and isolated blocks. The Kombélé Formation is a conglomeratic-sandstone-tillite composed of glacial outwash sediments. Both the Mambéré and the Kombélé formations generally range in thickness from 30 to 50 m and are unconformably overlain by Cretaceous sandstone formations (Chirico et al. 2010).
Crystalline Basement
Intrusive rocks	Proterozoic	Discontinuous basic intrusions, including large masses of batholithic granite (e.g. the Bouar plateau and Mt Yade) and doloritic veins (e.g. upstream of Bangui and Nola region).
	Proterozoic	Not extensively metamorphosed. These rocks overlie the base complex and are subdivided into three units: - an upper unit with a series of schists, quartzites, limestones and sandstones; - a middle unit consisting mainly of carbonate formations with a glacial conglomerate at the base; and - a lower unit represented by quartzites alternating with sericitic schists.
Granitic-gneissic basement	Archean	A base complex subdivided into two groups: an upper group formed of quartzites and schists; and a lower group formed of gneisses, micaschists, amphibolites, granulites, migmatites and anatectic granites.

Hydrogeology

This section provides a summary of the hydrogeology of the main aquifers in the Central African Republic. More information is available in the report ‘Groundwater in North and West Africa’ (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 Aquifer properties resource page for more details).

Unconsolidated

Named Aquifers	Period	General Description	Water quality

Sedimentary - Intergranular Flow

Named Aquifers	Period	General Description	Water quality

Sedimentary - Intergranular & Fracture Flow

Named Aquifers	Period	General Description	Water quality

Sedimentary - Fracture Flow

Named Aquifers	Period	General Description	Water quality

Basement

Named Aquifers	Period	General Description	Water quality

Groundwater use and management

Transboundary aquifers

For further information about transboundary aquifers, please see the Transboundary aquifers resources page

References

The following references provide more information on the geology and hydrogeology of the Central African Republic.

These, and others, can be accessed through the Africa Groundwater Literature Archive EDIT THE LINK TO CORRECT COUNTRY!!

Censier C. 1990. Characteristics of Mesozoic fluvio-lacustrine formations of the western Central African Republic (Carnot Sandstones) by means of mineralogical and exoscopic analyses of detrital material. Journal of African Earth Sciences Vol.10, Issues 1-2, pp 385-398.

Censier C et Lang J. 1992. La formation glaciaire de la Mambéré (République Centrafricaine), Reconstitution paléogéographique et implications à l’échelle du Paléozoïque africain. Geologische Rundschau, Vol.81, No. 3, pp 769-789

Chirico PG, Barthélémy F and Ngbokoto FA. 2010. Alluvial Diamond Resource Potential and Production Capacity Assessment of the Central African Republic. Prepared in cooperation with the Bureau de Recherches Géologiques et Minières and the Direction Générale des Mines under the auspices of the U.S. Department of State; Scientific Investigations Report 2010–5043.

United Nations. 1988. Groundwater in North and West Africa: Central African Republic. United Nations Department of Technical Cooperation for Development and Economic Commission for Africa. Natural Resources/Water Series No.18, ST/TCD/5.

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