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Neuse River

Neuse River
A map of the Pamlico Sound watershed, including the Pamlico, Tar and Neuse rivers.
Map
Location
CountryUnited States
StateNorth Carolina
RegionSouth
CitiesRaleigh, North Carolina, Smithfield, North Carolina, Goldsboro, North Carolina, Kinston, North Carolina, New Bern, North Carolina
Physical characteristics
SourceConfluence of the Eno and Flat rivers
 • locationDurham, North Carolina, United States
 • coordinates36°05′42″N 78°48′49″W / 36.09500°N 78.81361°W / 36.09500; -78.81361
 • elevation246 ft (75 m)
MouthPamlico Sound
 • location
Hobucken, North Carolina, United States
 • coordinates
35°07′53″N 76°30′14″W / 35.13139°N 76.50389°W / 35.13139; -76.50389
 • elevation
−11 ft (−3.4 m)
Length443 km (275 mi)
Basin size
14,600 km2 (5,600 sq mi)

The Neuse River (/nuːs/ NOOSE, Tuscarora: Neyuherú·kęʔ Kì·nęʔ)[1] is a river rising in the Piedmont of North Carolina and emptying into Pamlico Sound below New Bern. Its total length is approximately 275 miles (443 km),[2] making it the longest river entirely contained in North Carolina. The Trent River joins the Neuse at New Bern. Its drainage basin, measuring 5,630 square miles (14,600 km2) in area, also lies entirely inside North Carolina. It is formed by the confluence of the Flat and Eno rivers prior to entering the Falls Lake reservoir in northern Wake County. Its fall line shoals, known as the Falls of the Neuse, lie submerged under the waters of Falls Lake. The Neuse River Trail is a 34.5 miles (55.5 km) long greenway that stretches from Falls Lake Dam, Raleigh, North Carolina, to Legend Park, Clayton, North Carolina.[3]

Geography

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Along much of its length, the Neuse River is characterized by loose, sandy banks; muddy water year-round, and a dense tree canopy overhead.

The Neuse begins at the confluence of the Flat and Eno rivers near Durham, North Carolina.[4][5][6] The river enters Pamlico Sound just east of Maw Point Shoal near Hobucken, North Carolina while en route to the Atlantic Ocean.[4][7]

Typical of rivers in the Coastal Plain of North Carolina, the Neuse enters a basin of chocolate intermittent bottomland swamp on its journey towards its outlet. One interesting exception is the "Cliffs of the Neuse" area near Goldsboro, where the river cuts a narrow 30 m (90 ft) gorge through limestone and sandstone bluffs. The Neuse is prone to extremes in its flow carriage, often escaping its banks during wet periods, then reducing to a trickle that can be forded on foot during prolonged drought conditions.

The Neuse flows through parts of seven counties. Major cities and towns in proximity to the Neuse are Durham; Neuse Township; Raleigh, the capital of North Carolina; Smithfield; Goldsboro; Kinston and New Bern.

Neuse River in Raleigh

History

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For thousands of years before the Europeans arrived, different civilizations of indigenous peoples lived along the river. Many artifacts found along its banks have been traced to ancient prehistoric Native American settlements. Archaeological studies have shown waves of habitation.

Mouth of the "Nuss" in "A New Description of Carolina", engraved by Francis Lamb (London, Tho. Basset and Richard Chiswell, 1676). Right side of map faces north.

The river has one of the three oldest surviving English-applied placenames in the U.S.[8] Explorers named the Neuse River after the American Indian tribe known as Neusiok, with whom the early Raleigh expeditions made contact. They also identified the region as the "Neusiok". Two English captains, Arthur Barlowe and Phillip Amadas, were commissioned by Sir Walter Raleigh in 1584 to explore the New World. They landed on North Carolina's coast July 2, 1584, to begin their research. In their 1585 report to Raleigh, they wrote favorably of the Indian population in "… the country Neusiok, situated upon a goodly river called Neuse …", as it was called by the local population.

In 1865 during the American Civil War, the Confederates burned one of the last ironclad warships which they had built, the Ram Neuse, to prevent its capture by Union troops. The level of the river had fallen so that it prevented the ship from passing downriver. Nearly a century later, during another period of historically low water, the remains of the ship were discovered. It was raised in 1963. Later, the ship was installed beside the river at the Governor Caswell Memorial in Kinston.

William Larry Stewart II, a.k.a. Billy Stewart (March 24, 1937 – January 17, 1970), an American rhythm and blues singer and pianist, died in a broad-daylight car accident in January 1970, just two months prior to his 33rd birthday. The accident happened when the Ford Thunderbird that Stewart was driving approached a bridge across the Neuse River near Smithfield, North Carolina. His car left the highway, ran along the median strip at a slight angle to the highway, struck the bridge abutment, and then plunged into the river, killing Stewart and his three passengers instantly.[9]

The low-head Quaker Neck Dam was built in 1952 at Neuse River kilometer 225 to impound cooling water for a steam electric plant. A fish ladder was included. The dam was removed in May 1998, opening up access for anadromous fish to 127 kilometres (79 mi) of the mainstem Neuse River.[10]

Water quality

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The Neuse River has experienced water-quality problems associated with wastewater discharge, stormwater runoff, and nutrient pollution. Excess nitrogen and phosphorus can contribute to eutrophication in the Neuse River Estuary, affecting algal growth and dissolved oxygen conditions. Research using long-term data from the estuary has found that river nitrogen concentrations are an important factor controlling algal levels.[11]

Nutrient removal also occurs naturally within the Neuse River Estuary. Denitrification is a process in which microorganisms convert reactive forms of nitrogen into nitrogen gas, removing nitrogen from the aquatic system. A 2023 study of flooded habitats in the upper Neuse River Estuary found net denitrification in marshes, forested wetlands, undeveloped areas, stormwater ponds, and shallow sub-tidal sediments. Nitrogen removal varied among habitats and under different nitrate and storm conditions.[12]

The effects of nutrient pollution and nitrogen removal can vary throughout the river and estuary. Historical research has documented long-term changes in nutrient inputs and river-borne nutrient exports, while more recent research has focused on how nutrient concentrations and environmental conditions influence algal growth and nitrogen processing.[11][12][13]

Tributaries

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See also

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References

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  1. ↑ Rudes, Blair (1999). Tuscarora-English/English-Tuscarora Dictionary. ISBN 9780802043368.
  2. ↑ "Neuse River" Archived 2009-06-09 at the Wayback Machine, The Columbia Gazetteer of North America
  3. ↑ "Neuse River Trail info". RaleighNC.gov. Retrieved February 14, 2022. Neuse River info & more
  4. 1 2 U.S. Geological Survey Geographic Names Information System: Neuse River
  5. ↑ U.S. Geological Survey Geographic Names Information System: Flat River
  6. ↑ Northeast Durham, North Carolina, 7.5 Minute Topographic Quadrangle, USGS, 1973 (1992 rev.)
  7. ↑ Jones Bay, North Carolina, 7.5 Minute Topographic Quadrangle, USGS, 1950 (1993 rev.)
  8. ↑ Stewart, George R. (1945) [1945]. Names on the Land: A Historical Account of Place-Naming in the United States (1st ed.). Random House. pp. 21, 22.
  9. ↑ Billy Stewart
  10. ↑ Bowman, Stephan W. (15 March 2001), American Shad and Striped Bass Spawning Migration and Habitat Selection in the Neuse River, North Carolina (PDF), NCSU, p. 2, retrieved 2018-06-23
  11. 1 2 Katin, Alexey; Giudice, Dario Del; Hall, Nathan S.; Paerl, Hans W.; Obenour, Daniel R. (2021-05-01). "Simulating algal dynamics within a Bayesian framework to evaluate controls on estuary productivity". Ecological Modelling. 447: 109497. doi:10.1016/j.ecolmodel.2021.109497. ISSN 0304-3800.{{cite journal}}: CS1 maint: article number as page number (link)
  12. 1 2 Smiley, Anne Margaret H.; Thompson, Suzanne P.; Hall, Nathan S.; Piehler, Michael F. (2023-11-28). "Storm characteristics influence nitrogen removal in an urban estuarine environment". Natural Hazards and Earth System Sciences. 23 (11). Copernicus GmbH: 3635–3649. doi:10.5194/nhess-23-3635-2023. ISSN 1561-8633.{{cite journal}}: CS1 maint: unflagged free DOI (link)
  13. ↑ Stow, Craig A; Borsuk, Mark E; Stanley, Donald W (2001-04-01). "Long-term changes in watershed nutrient inputs and riverine exports in the Neuse River, North Carolina". Water Research. 35 (6): 1489–1499. doi:10.1016/S0043-1354(00)00402-4. ISSN 0043-1354.
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