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Congo River

(Formerly also Zaire River)

A river of central Africa flowing about 4,666 km (2,900 mi) north, west, and southwest through the Democratic Republic of the Congo (formerly Zaire) to the Atlantic Ocean. Its remotest tributaries rise in northern Zambia. For much of its latter course the river forms the border between the Democratic Republic of the Congo and the Republic of the Congo.

 

 
 

River, west-central Africa. Rising in Zambia as the Chambeshi and flowing 2,900 mi (4,700 km) through the Democratic Republic of the Congo to the Atlantic Ocean, it is the second longest river in Africa. It flows through three contrasting regions: the upper Congo, characterized by lakes, waterfalls, and rapids; the middle Congo, with seven cataracts known as Boyoma (Stanley) Falls; and the lower Congo, which divides into two branches forming a vast lake area called the Malebo (Stanley) Pool.

For more information on Congo River, visit Britannica.com.

 
(kŏng') or Zaïre ('ēr, zäēr') , great river of equatorial Africa, c.2,720 mi (4,380 km) long, formed by the waters of the Lualaba River and its tributary, the Luvua River, and flowing generally N and W through Congo (Kinshasa) to the Atlantic Ocean.

Course

The second longest river of Africa and one of the longest in the world, the Congo River drains c.1,425,000 sq mi (3,690,750 sq km) including all of Congo (Kinshasa) and parts of Congo (Brazzaville), Cameroon, Central African Republic, Burundi, Tanzania, Zambia, and Angola. The Lualaba River, considered to be the upper Congo River, rises in SE Congo (Kinshasa), flows north over rapids and falls to Bukama, and thence across a vast plain and through a series of marshy lakes (Kabwe, Kabele, Upemba) to receive the Luvua River at Ankoro. The Luvua River has its most remote source in the Chambeshi River, which rises in N Zambia and flows southwest into swamps around Lake Bangweulu; it emerges from the swamps as the Luapula River, continues N along the Congo (Kinshasa)–Zambia border into Lake Mweru, exits from there as the Luvua River, and continues NW to the Lualaba River. A third major headstream is the Lukuga River, which drains from Lake Tanganyika and joins the Lualaba River near Kabalo. From Kabalo, the Lualaba River flows N to Kisangani in a varied course marked by a deep and narrow gorge (the Gates of Hell) below Kongolo, a navigable stretch from Kasongo to Kibombo, a section of rapids and falls from Kibombo to Kindu, a shallow but navigable section from Kindu to Ubundu, and a section of seven cataracts—known as Boyoma Falls—between Ubundu and Kisangani that marks the end of the Lualaba and the beginning of the Congo River proper.

Below Kisangani, the Congo flows west and southwest, in a great curve unbroken by falls or rapids for about 1,090 mi (1,750 km) to Kinshasa. For most of its middle section the Congo is from 4 to 10 mi (6.4–16.1 km) wide, with many islands and sandbars. Because its many large tributaries (including the Lomami, Kasai, Lulonga, Ubangi, Aruwimi, Itimbiri, and Mongala rivers) drain areas with alternating rainy seasons on either side of the equator, the Congo has a fairly constant flow throughout the year. Between Bolobo and Kwamouth the Congo narrows in width to between 1 mi and 11/2 mi (1.6–2.4 km) but, c.350 mi (560 km) from its mouth, widens to form lakelike Pool Malebo, on which Kinshasa and Brazzaville are located. From the western end of Pool Malebo, the Congo descends 876 ft (267 m) in a series of 32 rapids, known as Livingstone Falls, to the port of Matadi.

Below Matadi (83 mi/134 km inland) the Congo is navigable by oceangoing vessels and, despite such hazards as the whirlpools of the Devil's Cauldron, shifting sandbars, and sharp bends in the river, forms one of the largest natural harbors in Africa. The river is tidal to Boma, c.60 mi (100 km) upstream. The Congo River enters the Atlantic Ocean between Banana Point, Congo (Kinshasa), and Sharks Point, Angola, and dredging is required to keep a navigable channel open. The river is continued offshore by a c.500-mi-long (800-km) submarine canyon that is c.4,000 ft (1,220 m) deep.

Economic Importance

With railroads to bypass major falls (Matadi-Kinshasa; Kisangani-Ubundu; Kindu-Kongolo), the Congo River and its tributaries form a system of navigable waterways c.9,000 mi (14,480 km) long, along which move much of central Africa's copper, palm-oil kernels, cotton, sugar, and coffee. The chief ocean port is Matadi, with its associated oil port, Ango Ango; the chief river ports are Kinshasa and Kisangani. River steamers operate throughout the year between Kinshasa and Kisangani. The Congo River is Africa's largest potential source of hydroelectric power; the most valuable site is along Livingstone Falls, where the first phase of the Inga Power Project has been completed. In spite of government initiatives, hydroelectric power is underdeveloped.

The Congo river basin encompasses the world's second largest contiguous rain forest, surpassed only by that of the Amazon. The region is biologically diverse, and a huge watershed. The forest is threatened by illegal logging and the poaching of large mammals (especially for the bushmeat trade), but two summits (1999, 2005) that brought together the nations of the basin have committed its participants to forest conservation and have led to the establishment of wildlife preserves.

European Exploration

The mouth of the Congo River was visited (1482) by Diogo Cão, the Portuguese navigator. It became known as the Zaïre River (a corruption of the local name Mzadi meaning “great water”) and was later referred to as the Congo River (for the Kongo kingdom located near its mouth); it was called Zaïre River by the government of Zaïre (now Congo [Kinshasa]) from 1971 to 1997. The Congo's lower course was traced upstream as far as Isangila by a British force under Capt. J. K. Tuckey in 1816, and its upper headwaters by the missionary David Livingstone, who followed the Lualaba River to Nyangwe in 1871. The journalist Henry Stanley traveled from Nyangwe to Isangila and on to Boma during his great transcontinental journey (1874–77), thus proving the headwaters to be tributaries of the Congo River, and not sources of the Nile as hypothesized by Livingstone.

Bibliography

See H. Winternitz, East Along the Equator: A Journey up the Congo and into Zaïre (1987).


 
Geography: Congo River

River of central Africa, flowing through Democratic Republic of Congo to the Atlantic Ocean.

  • One of the world's longest rivers, it is Africa's largest potential source of electric power.
  • Explored separately but simultaneously by the missionary David Livingstone and the journalist Henry Stanley, the Congo was the site of their proverbial encounter. (See “Dr. Livingstone, I presume?”)

 
Wikipedia: Congo River
Congo River
Congo River near Maluku
Congo River near Maluku
Mouth Atlantic Ocean
Basin countries Democratic Republic of the Congo, Central African Republic, Republic of the Congo
Length 4,700 km (2,922 mi)
Avg. discharge 41,800 m³/s (1,476,376 ft³/s)
Basin area 3,680,000 km² (1,420,848 mi²)

The Congo River (for a time known as Zaire River) is the largest river in Western Central Africa. Its overall length of 4,700 km (2,922 miles) makes it the second longest in Africa (after the Nile). The river and its tributaries flow through the second largest rain forest area in the world,[1] second only to the Amazon Rainforest in South America. The river also has the second-largest flow in the world, behind the Amazon, and the second-largest watershed of any river, again trailing the Amazon; its watershed is slightly larger than that of the Mississippi River. Because large sections of the river basin lie above and below the equator, its flow is stable, as there is always at least one river experiencing a rainy season.[2] The Congo gets its name from the ancient Kingdom of Kongo which inhabited the lands at the mouth of the river. The Democratic Republic of the Congo and the Republic of the Congo, both countries lying along the river's banks, are named after it. Between 1971 and 1997 the government of then-Zaire called it the Zaire River.

The sources of the Congo are in the highlands and mountains of the East African Rift, as well as Lake Tanganyika and Lake Mweru, which feed the Lualaba River, which then becomes the Congo below Boyoma Falls. The Chambeshi River in Zambia is generally taken as the source of the Congo in line with the accepted practice worldwide of using the longest tributary, as with the Nile River.

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 (formerly Léopoldville) and Brazzaville are on opposite sides of the river at the Pool, where 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.

History of exploration

The mouth of the Congo was visited in 1482 by the Portuguese Diogo Cão, and in 1816 by a British expedition under James Kingston Tuckey 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.

Economic importance

Although the Livingstone Falls prevent access from the sea, nearly the entire Congo is readily navigable in sections, especially between Kinshasa and Kisangani. Railways now bypass the three major falls, and much of the trade of central Africa passes along the river, including copper, palm oil (as kernels), sugar, coffee, and cotton. The river is also potentially valuable for hydroelectric power, and the Inga Dams below Pool Malebo are first to exploit the river.

In February 2005, South Africa's state-owned power company, Eskom, announced a proposal to increase the capacity of the Inga dramatically through improvements and the construction of a new hydroelectric dam. The project would bring the maximum output of the facility to 40 GW, twice that of China's Three Gorges Dam. [3]

Geological history

In the Mesozoic before continental drift opened the South Atlantic Ocean, the Congo was the upper part of a river roughly 12,000 km (7,500 miles) long which flowed west across the parts of Gondwanaland which are now Africa and South America: see Longest rivers#Amazon-Congo.

Tributaries

Course and Watershed of the Congo River with countries marked
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Course and Watershed of the Congo River with countries marked
Course and Watershed of the Congo River with topography shading.
Enlarge
Course and Watershed of the Congo River with topography shading.

Sorted in order from the mouth heading upstream.

See also

References

  1. ^ The Rainforest Foundation (2006-06-21). A fresh step towards the first indigenous rights law in Republic of Congo.
  2. ^ http://rainforests.mongabay.com/congo/congo_river.html
  3. ^ http://www.guardian.co.uk/congo/story/0,12292,1425023,00.html

Further reading

  • Tim Butcher: Blood River - A Journey To Africa's Broken Heart, 2007. ISBN 0-701-17981-3
  • H. Winternitz, East Along the Equator: A Journey up the Congo and into Zaire (1987)

External links

Coordinates: 6°04′45″S, 12°27′00″E


 
 

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Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2007. Published by Houghton Mifflin Company. All rights reserved.  Read more
Britannica Concise Encyclopedia. Britannica Concise Encyclopedia. © 2006 Encyclopædia Britannica, Inc. All rights reserved.  Read more
Columbia Encyclopedia. The Columbia Electronic Encyclopedia, Sixth Edition Copyright © 2003, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/  Read more
Geography. The New Dictionary of Cultural Literacy, Third Edition Edited by E.D. Hirsch, Jr., Joseph F. Kett, and James Trefil. Copyright © 2002 by Houghton Mifflin Company. Published by Houghton Mifflin. All rights reserved.  Read more
Wikipedia. This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Congo River" Read more

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