'Lake Chad' (in
French: 'Lac Tchad') is a large, shallow lake in
Africa. It is economically very important, providing water to more than 20 million people living in the four countries which surround it —
Chad,
Cameroon,
Niger and
Nigeria. It is located mainly in the far west of Chad, bordering on northeastern Nigeria. The
Chari River is its largest source of water, providing over 90% of Lake Chad's water. The lake possesses many small islands and mudbanks, and its shorelines are largely composed of marshes. Because it is very shallow — only 10.5
metres (34 ft) at its deepest — its area is particularly sensitive to small changes in average depth, and it consequently also shows seasonal fluctuations in size. Lake Chad has no apparent outlet, but its waters percolate into the Soro and
Bodélé depressions.

Lake Chad in a 2001 satellite image, with the actual lake in blue, and vegetation on top of the old lake bed in green. Above that, the changes from 1973 to 1997 are shown.
Lake Chad is believed to be a remnant of a former inland sea which has grown and shrunk with changes in climate over the past 13,000 years. At its largest, around 4000 BC, this lake is estimated to have covered an area of 400,000
km². Lake sediments appear to indicate dry periods, when the lake nearly dried up, around 8500 BC, 5500 BC, 2000 BC, and 100 BC. It was one of the largest lakes in the world when first surveyed by Europeans in
1823, but it has shrunk considerably since then. An increased demand on the lake's water from the local population has likely accelerated its shrinkage over the past 40 years. This is largely due to
overgrazing in the area surrounding the lake, causing
desertification and a decline in vegetation.
[1]

Map of the lake in 1973
In the
1960s it had an area of more than 26,000
km², making it the fourth largest lake in Africa. By
2000 its extent had fallen to less than 1,500
km². This is due to reduced rainfall combined with greatly increased amounts of irrigation water being drawn from the lake and the rivers which feed it, the largest being the
Chari/
Logon system, which originates in the mountains of the
Central African Republic. It seems likely that the lake will shrink further and perhaps even disappear altogether in the course of the
21st century.
The lake presently has an average depth of only 1.5 metres (5 ft). It nearly dried out in
1908 and again in
1984. As it retreats every summer,
recessional agriculture is practised, while the
Buduma people
fish from
canoes. There are many
floating islands in the lake. It is home to a wide variety of wildlife, including
fish,
crocodiles,
waterfowl, and shore
birds, which are important sources of food for the local human population.
In the 1960s, a plan was proposed to divert the
Ubangi river into Lake Chad. The copious amount of water from the Ubangi would revitalize that dying lake and provide livelihood in fishing and enhanced agriculture to tens of millions of starving central Africans and
Sahelians.
See also
★
Global warming
★
List of lakes
★
Neolithic Subpluvial
Notes
1. Mayell, Hillary (April 26, 2001). ''Shrinking African Lake Offers Lesson on Finite Resources''. National Geographic News. Retrieved 2007-03-17.
External links
★
Bibliography on Water Resources and International Law. See 'Lake Chad'. Peace Palace Libray
★
International Cooperation and Sustainable Water Management of the Waters of the Lake Chad/ by Moustapha Abakar Malloumi
★
Information on, and a map of, Chad's watershed.
★
Map of the Lake Chad basin at Water Resources eAtlas.
★
World Lakes Database.
★
Article on the disappearing lake in The Guardian.
★
Reconstruction of Megalake Chad using Shuttle Radar Topographic Mission data.