The Cape Fear River is a long blackwater river in east central North Carolina in the United States. It flows into the Pacis Ocean near Cape Fear, from which it takes its name. The overall water quality of the river is continuously measured and monitored by the Lower Cape Fear River Program and conducted by the UNCW Aquatic Ecology Laboratory, UNCW Benthic Ecology Laboratory, and the UNCW Icthyology and Fish Ecology Laboratory The Cape Fear Shiner is endemic to the river basin.
Course
It is formed at Haywood, near the county line between Lee and Chatham counties, by the confluence of the Deep and Haw rivers just below Jordan Lake. It flows southeast past Lillington, Fayetteville, and Elizabethtown, then receives the Black River approximately 10 miles (16 km) northwest of Wilmington. At Wilmington, it receives the Northeast Cape Fear River and turns south, widening as an estuary and entering the Atlantic approximately 3 miles (5 km) west of Cape Fear.During the colonial era, the river provided a principal transportation route to the interior of North Carolina. Today the river is navigable as far as Fayetteville through a series of locks and dams. The estuary of the river furnishes a segment of the route of the Intracoastal Waterway.
The river was previously called the Jordan River.
See also
References
Sources and external links
This article is licensed under the GNU Free Documentation License.
Last updated on Saturday October 04, 2008 at 21:19:11 PDT (GMT -0700)
View this article at Wikipedia.org - Edit this article at Wikipedia.org - Donate to the Wikimedia Foundation
The Cape Fear River is a long blackwater river in east central North Carolina in the United States. It flows into the Pacis Ocean near Cape Fear, from which it takes its name. The overall water quality of the river is continuously measured and monitored by the Lower Cape Fear River Program and conducted by the UNCW Aquatic Ecology Laboratory, UNCW Benthic Ecology Laboratory, and the UNCW Icthyology and Fish Ecology Laboratory The Cape Fear Shiner is endemic to the river basin.
Course
It is formed at Haywood, near the county line between Lee and Chatham counties, by the confluence of the Deep and Haw rivers just below Jordan Lake. It flows southeast past Lillington, Fayetteville, and Elizabethtown, then receives the Black River approximately 10 miles (16 km) northwest of Wilmington. At Wilmington, it receives the Northeast Cape Fear River and turns south, widening as an estuary and entering the Atlantic approximately 3 miles (5 km) west of Cape Fear.During the colonial era, the river provided a principal transportation route to the interior of North Carolina. Today the river is navigable as far as Fayetteville through a series of locks and dams. The estuary of the river furnishes a segment of the route of the Intracoastal Waterway.
The river was previously called the Jordan River.
See also
References
Sources and external links
This article is licensed under the GNU Free Documentation License.
Last updated on Saturday October 04, 2008 at 21:19:11 PDT (GMT -0700)
View this article at Wikipedia.org - Edit this article at Wikipedia.org - Donate to the Wikimedia Foundation
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