Hydrogeology of Gambia
- 1 Authors
- 2 Terms and conditions
- 3 Geographical Setting
- 4 Geology
- 5 Hydrogeology
- 6 Groundwater Status
- 7 Groundwater use and management
- 8 References
Landing Bojang, Department of Water Resources, The Gambia
Giran Corr, RC Engineering / NIRAS, The Gambia
Kirsty Upton, Brighid Ó Dochartaigh, British Geological Survey, UK
Please cite this page as: Bojang, Corr, Upton & Ó Dochartaigh, 2016.
Bibliographic reference: Bojang, L., Corr, G., Upton, K. & Ó Dochartaigh, B.É. 2016. Africa Groundwater Atlas: Hydrogeology of the Gambia. British Geological Survey. Accessed [date you accessed the information]. http://earthwise.bgs.ac.uk/index.php/Hydrogeology_of_Gambria
Terms and conditions
The Gambia is the smallest country in Africa. It borders the Atlantic Ocean to the west, and is otherwise entirely surrounded by the country of Senegal. The majority the country comprises the floodplain of the Gambia River, which originates in Guinea before flowing through Senegal and through the Gambia to the sea. The country is therefore generally very flat, ranging from 0 to <100 m above sea level.
|Estimated Population in 2013*||1,849,285|
|Rural Population (% of total)*||42%|
|Total Surface Area*||10,120 sq km|
|Agricultural Land (% of total area)*||60%|
|Annual Freshwater Withdrawal (2013)*||91 Million cubic metres|
|Annual Freshwater Withdrawal for Agriculture*||43%|
|Annual Freshwater Withdrawal for Domestic Use*||37%|
|Annual Freshwater Withdrawal for Industry*||19%|
|Rural Population with Access to Improved Water Source*||84%|
|Urban Population with Access to Improved Water Source*||94%|
* Source: World Bank
The climate of the Gambia is largely classified as tropical savannah, apart from the central north region which transitions into hot, arid steppe. There is little spatial variation in average annual precipitation and temperature, other than a slight reduction in rainfall in the central north region.
Gambia has a very distinct wet season between June and October, and is relatively dry from November to April. The wet season is relatively hot compared to the cooler dry season.
More information on average rainfall and temperature for each climate zone in Gambia can be found on the Gambia Climate Page.
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 Gambia is dominated by the perennial Gambia River, which flows along the entire length of the country from the border with Senegal in the east to its discharge point to the Atlantic Ocean to the west.
The Department of Water Resources is responsible for river flow gauging, and currently monitors the Gambia River close to its discharge point to the Atlantic Ocean.
|Soils across the floodplain of the Gambia River are dominantly Gleysols, which are highly important for agriculture.
Lixisols in the north of the country are associated with fine-grained weathered parent material, and natural savannah or open woodland vegetation.
More acidic Acrisols are found in the coastal region. This soil type is common in the wetter parts of Africa, and is generally deficient in nutrients.
Regosols, which cover a significant area inland, are reflective of the largely unconsolidated underlying geological deposits.
This section provides a summary of the geology of the Gambia.
The geology map on this page shows a simplified version of the geology at a national scale (see the geology resource page for more details).
|Unconsolidated Sedimentary Deposits||Quaternary||Unconsolidated deposits of Quaternary age crop out across the whole country. They consist of Holocene aeolian sands/silts and alluvial clays, underlain by Pleistocene sandy clays and Pliocene fine-medium grained sands which contain varying amounts of silt, clay and laterites.||The Holocene deposits are typically up to 20 m thick, while the underlying Pleistocene and Pliocene deposits have thicknesses of around 20 and 30 m, respectively.|
|Mauritania/Senegal Basin Sedimentary||Cretaceous-Tertiary||Loosely consolidated deposits, variously of fluvial, lacustrine and marine origin. These Cretaceous and Tertiary deposits are part of the Mauritania/Senegal sedimentary basin, which formed as a result of the breakup of Gondwana in the late Palaeozoic/early Mesozoic.
The Tertiary sediments are largely composed of shales and marly limestones. These can be subdivided into 4 main units:
(1) Miocene shales and marly fine sands with subordinate limestones;
(2) Oligocene marly limestones, which are of limited extent;
(3) Eocene shales and marly limestones with bands of flint near the base;
(4) Paleocene limestones interbedded with dark grey marls.
Below this are two sequences of Cretaceous loosely consolidated sediments. The younger sediments, of Maestrichtian age, are composed of fine to coarse grained sandstones, with subordinate grey-black shales, phosphatic nodules and lignite bands. The older Cretaceous sediments (of Campanian age) consist of grey clays and marls interbedded with fine calcareous sandstones, dolomite limestones, and lignite bands.
|The Tertiary sediments have a total thickness of around 180 m. The Maestrichtian sediments are typically around 200 m thick while the underlying Campanian sediments are >500m thick.|
This section provides a summary of the hydrogeology of the main aquifers in the Gambia. More information is available in the references listed at the bottom of this page. Many of these references can be accessed through the Africa Groundwater Literature Archive.
The hydrogeology map on this page 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).
There are two main aquifers in the Gambia: the upper Quaternary unconsolidated sands comprise a shallow sand aquifer (SSA), which is an important aquifer throughout the Gambia. The deeper Cretaceous sediments form a deep sandstone aquifer (DSA). More detail can be seen below.
|Named Aquifers||General Description||Water quantity issues||Water quality issues||Recharge|
|Shallow Sand Aquifer (SSA)||The shallow sand aquifer (SSA) is composed predominantly of fine to coarse sand, and is found and exploited across the extent of Gambia. It can be subdivided into 2 units: the phreatic aquifer, which comprises the Holocene sediments, and the semi-confined aquifer, which comprises the underlying Pliocene sediments. The two aquifers are separated by a 15-30 m clay-silt layer which allows limited hydraulic connection between them.
Yields are generally in the range of 1-30 l/s and can be greater than 30 l/s in the most productive areas.
Hydraulic conductivity and transmissivity generally ranges from 5-30 m/d and 100-10000 m²/d, respectively.
Storage is generally between 10-4 and 10-2.
The SSA typically varies from 5-25 m thick and the water table may sit between 4 and 50 m below ground level. Boreholes are generally drilled to depths of 35-100 m.
|Groundwater abstraction is significantly less than recharge and water levels fully recover during the wet season.||There are no major groundwater quality issues. Isolated instances of elevated iron concentrations have been reported.||When mean annual precipitation is above 900 mm, recharge is generally in the range of 250 – 300 mm. This is a result of direct infiltration.|
|Deep Sandstone Aquifer (DSA)||The deep sandstone aquifer (DSA) comprises mainly unconsolidated sands and loosely consolidated sandstones, typically at depths of 250-450m. Groundwater in the DSA is confined, and is very old water of 'fossil' origin, between 4000 and 40000 years old. Exploitation of the DSA would require deep boreholes (up to 380 m), and potential yields have been estimated at 40 l/s.||Storage in the DSA has been estimated at 650,000 M cubic metres, of which only 80,000 M cubic metres is thought to be potable.||In the east of Gambia, groundwater in the DSA is potable, but in the west the old confined groundwater is typically highly mineralised, with total dissolved solids in the range 1000 to 2000 mg/l, and fluoride concentrations between 2 and 5 mg/l. If required, highly mineralised water in the western parts of the DSA could be abstracted and mixed with groundwater from the SSA at a ratio of 2:1 to expand the exploitable water resources of Gambia.||There is no appreciable modern recharge to the DSA.|
Groundwater abstraction from the main unconsolidated aquifer (SSA) is less than average annual recharge. Total groundwater availability could be significantly increased by exploiting the DSA.
Groundwater use and management
The national water supply in Gambia is derived entirely from groundwater.
The following groundwater abstractions are currently known: 207 boreholes with hand pumps, 260 boreholes with solar pumping systems, 84 boreholes with electric pumping systems, and 1634 hand dug wells with hand pumps (Department of Water Resources).
The Department of Water Resources is responsible for the development, utilisation and protection of groundwater in Gambia. They issue permits, which are required for both borehole drilling and groundwater abstraction.
The National Water and Electricity Company (NAWEC) is mandated to provide water supply in the Greater Banjul Area and surrounding provinces.
The Department of Water Resources established a network of 38 groundwater level and quality monitoring boreholes in 2014. These are distributed across Gambia and are equipped with automatic data loggers. The recorded groundwater level observations are collected every 3 months, and the data is stored in the GeOdin database in the Department of Water Resources.
The same network is used to monitor groundwater quality.
Other references relating to the hydrogeology of the Gambia can be found in the Africa Groundwater Literature Archive.
Whyte WJ and Russell TS. 1988. Geological and Mineral Map of The Republic of The Gambia. Ministry of Economic Planning and Industrial Development.
Whyte WJ and Russell TS. 1988. Geological Survey of The Gambia. Ministry of Local Government and Lands
1983. Groundwater Resources of The Gambia, Preliminary Report. April 1983
Ceesay S and Humphreys H. 1987. Groundwater Survey Phase I.