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The sources of the Congo are in the highlands and mountains of the East Africa Rift, as well as Lake Tanganyika and Lake Mweru, which feed the Lualaba River, which then becomes the Congo below Boyoma Falls. The Congo flows generally west from Kisangani just below the falls, then gradually bends southwest, passing by Mbandaka, joining with the Ubangi River, and running into the Pool Malebo (Stanley Pool). Kinshasa and Brazzaville are on opposite sides of the river at the Pool, then the river narrows and falls through a number of cataracts in deep canyons (collectively known as the Livingstone Falls), running by Matadi and Boma, and into the sea at the small town of Muanda. The mouth of the Congo was visited in 1482 by the Portuguese Diogo Cão, and in 1816 a British expedition went up as far as Isangila. Henry Morton Stanley was the first European to navigate along the river's length and report that the Lualaba was not a source of the Nile as had been suggested. Nearly the entire Congo is readily navigable, and with railways now bypassing the three major falls, much of the trade of central Africa passes along it, including copper, palm oil (as kernels), sugar, coffee, and cotton. The river is also potentially valuable for hydroelectric power, and the Inga facility below Pool Malebo is the first to exploit the river. Tributaries, in order going upstream:
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da:Congofloden de:Kongo (Fluss) eo:Kongo (rivero) fr:Congo (fleuve) nl:Congo (rivier) pl:Kongo (rzeka) pt:Rio Congo sl:Kongo (reka) sv:Kongofloden zh:刚果河 |
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