| Lake
Chad |
|
| Cameroon
/ Nigeria / Niger / Chad, Africa |
| |
| Surface area
1,350 km² |
| Average depth
1.5 m |
| Max. depth 11
m |
| Shore length
650 km |
| |
|
Coordinates:
13° 0' 0 N, 14° 0' 0 E
|
Aerial
photos of lake Chad-1973-2001
[1] |
Lake Chad (in French
Lac Tchad) is a historically large,
shallow lake in Africa, whose size
has varied greatly over the centuries.
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 gave its name
to the country of Chad. The name Chad
is a local word meaning "large
expanse of water," in other words
simply "lake."
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,
(approx. 154,000 sq miles). 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.
A 2001 study published in the Journal
of Geophysical Research blamed the
lake's retreat largely on overgrazing
in the area surrounding the lake,
causing desertification and a decline
in vegetation. According to CNN senior
producer, A. Chris Gajilan, "the
United Nations Environment Programme
says that about half of the lake's
decrease is attributable to human
water use such as inefficient damming
and irrigation methods. The other
half of the shrinkage is due to shifting
climate patterns. Anada Tiega of the
Lake Chad Basin Commission blames
climate change for 50 to 75 percent
of the water's disappearance."
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/Logone
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 (4.9 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. [2]