Chad

Relief and drainage

In its physical structure Chad consists of a large basin bounded on the north, east, and south by mountains. Lake Chad, which represents all that remains of a much larger lake that covered much of the region in earlier geologic periods, is situated in the center of the western frontier; it is 922 feet (281 meters) above sea level. The lowest elevation of the basin is the Djourab Depression, which is 573 feet (175 meters) above sea level.

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In the early Holocene Epoch, possibly until as recently as 7,000 years ago, the lake stood at a level of about 1,100 feet (335 meters) above sea level, or some 180 feet (55 meters) higher than today, and was as much as 550 feet (170 meters) deep. At that stage Mega-Chad, as it has been called, occupied an area of some 130,000 square miles (336,700 square km) and overflowed southward via the present-day Kébi River and then over the Gauthiot Falls westward to the Benue River and the Atlantic Ocean. Older dune systems, flooded by Mega-Chad, form linear islands in the present lake and extend hundreds of miles to the east, the interdunal hollows being occupied by diatomites and other lake sediments.

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The mountains that rim the basin include the volcanic Tibesti Massif to the north (of which the highest point is Mount Koussi, with an elevation of 11,204 feet [3,415 meters]), the sandstone peaks of the Ennedi Plateau to the northeast, the crystalline rock mountains of the Ouaddaï (Wadai) region to the east, and the Oubangui Plateau to the south. The semicircle is completed to the southwest by the mountains of Adamawa and Mandara, which lie mostly beyond the frontier in Cameroon and Nigeria.

Chad’s river network is virtually limited to the Chari and Logone rivers and their tributaries, which flow from the southeast to feed Lake Chad. The remaining Chad waterways are either seasonal or are of insignificant size. The Chari, which arises from headstreams in the Central African Republic to the south, is later joined from the east by the Salamat Wadi and from the west by the Ouham River, its largest tributary. After entering an ill-defined area of swampland between Niellim and Dourbali, it flows through a large delta into Lake Chad. The Chari is about 750 miles (1,200 km) in length and has a flow that normally varies between 600 and 12,000 cubic feet (17,000 to 340,000 liters) per second, according to the season. The Logone, which for some of its course runs along the Cameroon frontier, is formed by the junction of the Pendé and Mbéré rivers; its flow varies between 170 and 3,000 cubic feet (4,800 and 85,000 liters) per second, and its course is more than 600 miles (965 km) long before it joins the Chari at N’Djamena. The level of Lake Chad fluctuates according to the flow of these rivers, as well as according to the degree of precipitation, evaporation, and seepage. The droughts of the 1970s and early ’80s in the Sahel region of western Africa reduced the lake to record low levels. By 1985 it had been reduced to a pool, immediately to the north of the Chari–Logone mouth, occupying about 1,000 square miles (2,600 square km). The size of the lake continued to decline, and in the early 21st century, the area was typically about 580 square miles (1,500 square km).

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Soils

Several types of soil formation occur in Chad, apart from the sand of the desert zone and the sheer rock of the mountainous areas. On the south side of Lake Chad the soils are derived from clayey deposits that accumulated on the floor of Mega-Chad. Along the seasonally flooded banks of the Chari and Logone rivers and the Salamat Wadi, hydromorphic (waterlogged) soils occur. Tropical iron-bearing soils, red in color, are found on the exposed folds and mounds of the Ouaddaï region’s upland slopes. In the area north of Lake Chad, subarid soils are characteristic, except in the depressions that occur between the dunes on the shores of Lake Chad, where hydromorphic soils liable to salinization are found.