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Great Kwa River
Waterfall in Cross River, Nigeria
Waterfall in Cross River, Nigeria

The 'Great Kwa River flows through Cross River State, Nigeria, draining the east side of the city of Calabar. The river ecology is under threat from human activity.
Location
The river originates in the Oban Hills, in the Cross River National Park, and flows southwards to the Cross River estuary.
Its lower reaches are tidal, with broad mud flats, and drain the eastern coast of the city of Calabar.
Human activity
Human activity in the Great Kwa basin has traditionally been limited to small scale farming, aquaculture and artisanal fisheries, mainly for shrimp. However, Calabar is growing, due in part to the Calabar Free Trade Zone, causing growing numbers of houses and factories to be built in the freshwater and mangrove swamps of the Great Kwa. The University of Calabar covers a 17 ha site between the Great Kwa River and the Calabar River. The university has acquired more land on both banks of the Great Kwa for future development.{{cite web |archive-date=2012-04-02 |archive-url=https://web.archive.org/web/20120402092019/http://www.unicaledu.com/about/Default.aspx |url-status=dead
Pollution
Calabar Municipality has no waste treatment facilities, and heavy rains wash human and industrial wastes into the river. A 2008 study of Vibrio bacteria in shellfish in the Great Kwa River estuary showed that the water was constantly faecally polluted, and the shellfish had high levels of infection. This posed a health risk for consumers, including a risk of cholera epidemics.{{cite journal
References
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References
- "The Mythology Behind the Great Kwa River - Guide to Nigeria tourism, local culture & investments".
- "The Mythology Behind the Great Kwa River - Guide to Nigeria tourism, local culture & investments".
- Ephraim, Bassey. "Compositional evaluation and quality status of surface waters of MBAT- ABIATI and Oberekkai Creeks of the great Kwa River, Southeastern Nigeria".
This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.
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