Catawba River

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Catawba River
A view of the Catawba River in McDowell County, North Carolina
Map of the Santee River watershed showing the Catawba River
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Catawba River is located in South Carolina
Catawba River
Location of the mouth of the Catawba River in South Carolina
EtymologyNamed after the Catawba Indians[2]
Native name[Eswa-Taroa[1]] Error: {{Native name}}: missing language tag (help)  (language?)
Location
CountryUnited States
StatesNorth Carolina, South Carolina
CountiesMcDowell NC, Caldwell NC, Burke NC, Alexander NC, Catawba NC, Iredell NC, Lincoln NC, Gaston NC, Mecklenburg NC, York SC, Lancaster SC, Fairfield SC
Physical characteristics
<templatestyles src="Module:Infobox/styles.css"></templatestyles>
SourceEvans Knob[3]
 • locationRidgecrest, North Carolina
 • coordinates<templatestyles src="Module:Coordinates/styles.css"></templatestyles>35°36′04″N 82°17′06″W / 35.60111°N 82.28500°W / 35.60111; -82.28500[1]
 • elevation3,044 ft (928 m)
MouthWateree River
 • location
Liberty Hill, South Carolina
 • coordinates
<templatestyles src="Module:Coordinates/styles.css"></templatestyles>34°28′01″N 80°53′20″W / 34.46694°N 80.88889°W / 34.46694; -80.88889Coordinates: <templatestyles src="Module:Coordinates/styles.css"></templatestyles>34°28′01″N 80°53′20″W / 34.46694°N 80.88889°W / 34.46694; -80.88889[1]
 • elevation
223 ft (68 m)[1]
Basin features
ProgressionCatawba → Wateree → Santee → Atlantic Ocean
River systemCatawba River
WaterbodiesLake James, Rhodhiss Lake, Lake Hickory, Lookout Shoals Lake, Lake Norman, Mountain Island Lake, Lake Wylie, Fishing Creek Reservoir,Great Falls Reservoir, Cedar Creek Reservoir, Lake Wateree
WaterfallsCatawba Falls

The Catawba River originates in Western North Carolina and flows into South Carolina, where it is known as the Wateree River. The river is approximately 220 miles (350 km) long. It rises in the Appalachian Mountains and drains into the Piedmont, where it has been impounded through a series of reservoirs for flood control and generation of hydroelectricity. The river is named after the Catawba tribe of Native Americans, which lives on its banks. In their language, they call themselves "yeh is-WAH h’reh", meaning "people of the river."[4]

The river rises in the Blue Ridge Mountains in western present-day McDowell County, North Carolina, approximately 20 miles (30 km) east of Asheville. It flows ENE, falling over two waterfalls, Upper Catawba Falls and Catawba Falls, before being dammed by Lake James, and joining the Linville River. It passes north of Morganton, then southeast through Lake Rhodhiss and Lake Hickory just north of Hickory, and into the Lake Norman reservoir. From Lake Norman it flows south, passing west of Charlotte, then flowing through the Mountain Island Lake and Lake Wylie reservoirs, where it exits the reservoirs approximately 10 miles (15 km) south of the border between North Carolina and South Carolina. The confluence of the South Fork Catawba River and Catawba River is submerged by Lake Wylie near the NC/SC state line.

The river flows into northern South Carolina, passing Rock Hill, through Fishing Creek Reservoir near Great Falls, and into the Lake Wateree reservoir, approximately 30 miles (50 km) northeast of Columbia. At the now-submerged confluence with Wateree Creek, it becomes known as the Wateree River.

Dams

Map of the Catawba River in South Carolina

The Catawba has been controlled by several dams, including the following:

North Carolina

South Carolina

Controversy

In 2006 the river became the center of a water use controversy between the residents of the Catawba watershed and Cabarrus County, North Carolina. The cities of Concord and Kannapolis are expecting a daily shortfall of 22 million US gallons (83,000 m3) of water a day by 2035 [5] and want to pump up to 36 million US gallons (140,000 m3) of water daily from the Catawba River.[6] The Concord/Kannapolis Interbasin Transfer (IBT) proposal calls for water to be permanently transferred from one river basin to another river basin. Such a transfer is unlike the more common water usage, in which municipalities within the Catawba basin pump water from the river and treat it for residential use. Much of that treated water eventually returns to the Catawba River.

Though neither Concord nor Kannapolis is located in the Catawba River basin (both are located in the Pee Dee River basin), the cities said the Catawba River is a regional resource. Opponents of the IBT argued that towns and cities along the Catawba River basin are growing as well, and that the cities' request is too large.

On January 10, 2007, the North Carolina state environmental panel authorized Concord and Kannapolis to pump up to 10 million US gallons (38,000 m3) a day from the Catawba River. This decision represented a compromise recommended by hearing officers for the Environmental Management Commission. The mayors of Morganton and Valdese said that they were adamantly against the transfer and that the panel's ruling was skewed and biased.[7] Concord's city manager said the approval of the water transfer was "bittersweet", since the panel authorized an amount much lower than was originally requested and the action is likely to be delayed by lawsuits.

“Well, (officials from) Hickory are going to file an appeal,” said Concord Mayor Scott Padgett, who spoke briefly with Hickory Mayor Rudy Wright after the EMC meeting. “His major concern is changing the (interbasin transfer) process. My appeal to him is that there should be a truce. To file an appeal is just going to prolong something we deserve, is less than what we asked for and is going to further hard feelings this has already created.” [8]

The controversy ended in early 2010 when all the parties reached a settlement. It further limits the amount of water available to Concord and Kannapolis under drought conditions.

A river at risk

Starting in the early autumn months of 2007, residents and businesses of the Catawba basin, along with large swaths of the Southern United States, began to feel the effects of an extreme drought. On October 15, 2007, the Morganton News Herald reported that North Carolina Governor Mike Easley described the drought as "the worst in recorded history".[9]

On January 29, 2008, Duke Energy, the utility responsible for managing the Catawba River, extended its estimated time frame for Stage 4 water restrictions to August. The extension was possible because of conservation measures and the 6 inches of rain the basin received in December. However, area leaders converged on Valdese to hear presentations from representatives of the N.C. Rural Center, N.C. Department of Commerce, N.C. Department of Environment and Natural Resources, and the Appalachian Regional Commission about grants and loans available to help pay for solutions to the drought.[10]

In April 2008 the environmental group American Rivers named the Catawba-Wateree River "the most endangered river in America."[11] Reasons cited for the river's condition are the drought, the presence of 11 hydroelectric dams, global warming, and unchecked development along its banks, with the latter reported as the most serious threat.[12]

On June 11, 2008, South Carolina Governor Mark Sanford signed legislation denoting the Catawba as a state scenic river. The designation carries no land-use restrictions, but it allows the state to convene an advisory group to address river-related concerns.

On June 29, 2009, the EPA announced that four of the top 44 "High Hazard Ash Ponds" in the United States are on the Catawba River. Two ash ponds are adjacent to and discharge into Mountain Island Lake. The EPA High Hazard list also includes ash ponds on Lake Wylie and Lake Norman.[13]

On December 11, 2014, Duke Energy received approval from North Carolina to dump coal ash (containing arsenic, lead, thallium and mercury, among other heavy metals) from the Marshall Steam Station into Lake Norman in order to repair a rusted, leaking pipe at their facility.[14] Groundwater at the Marshall Steam Station flows toward Lake Norman, and the contaminated field abuts the lake for about 30 feet of shoreline near its largest coal ash basin, threatening water quality in the lake.[15]

On October 3, 2015, Duke Energy reported that a sinkhole had formed at the base of the Marshall Steam Station dam north of Charlotte on Lake Norman. The Department of Environmental Quality (DEQ) says Duke Energy placed a liner in the hole and filled it with crushed stone.[16]

The Catawba River basin is one of only four areas left in the southeast with significant populations of Hymenocallis coronaria, the Shoals spider lily. It has one large population left at Landsford Canal State Park.[17]

Crossings

On the Catawba River

The Catawba River is crossed by many highways over its course. (Note: this list may be incomplete)

North Carolina

South Carolina

See also

References

  1. ↑ 1.0 1.1 1.2 1.3 <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Catawba River". Geographic Names Information System. United States Geological Survey. June 17, 1980. Retrieved December 28, 2020.
  2. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"North Carolina Gazetteer". Retrieved December 28, 2020.
  3. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Evans Knob". Geographic Names Information System. United States Geological Survey. June 17, 1980. Retrieved December 28, 2020.
  4. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"About The Nation". www.catawbaindian.net. Retrieved Dec 2, 2020.
  5. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Whose Water Is It?". The News Herald. Archived from the original on 2007-05-29. Retrieved 2008-02-22.
  6. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Political hot potato for region's water users". Mooresville Tribune. Archived from the original on 2007-07-15. Retrieved 2008-02-22.
  7. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Panel Opens Up Catawba River" (PDF). News Harald. Retrieved 2008-02-22.{{cite web}}: CS1 maint: url-status (link)[permanent dead link]
  8. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Water transfer approved" (PDF). The Independent Tribune. Retrieved 2008-02-22.{{cite web}}: CS1 maint: url-status (link)[permanent dead link]
  9. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Gov: Drought worse in recorded history". Morganton News Herald. Retrieved 2008-02-22.{{cite web}}: CS1 maint: url-status (link)[permanent dead link]
  10. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Small reprieve comes in drought, towns still preparing". The Morganton News Herald. Retrieved 2008-02-22.{{cite web}}: CS1 maint: url-status (link)[permanent dead link]
  11. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"America's 10 Most Endangered Rivers 2008". Environment News Service. Retrieved 2008-04-20.
  12. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"Defending the Catawba: Biggest threat is lack of sensible land-use planning". Charlotte Observer/Charlotte.com. Retrieved 2008-04-20.[permanent dead link]
  13. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>"EPA Coal Ash Fact Sheet". EPA/EPA.gov. Retrieved 2009-11-19.
  14. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>Press, MICHAEL BIESECKER Associated. "Duke to repair leaky pipe at coal ash dump in Catawba County". hickoryrecord.com. Retrieved 21 April 2018.
  15. ↑ [1]
  16. ↑ [2]
  17. ↑ <templatestyles src="Module:Citation/CS1/styles.css"></templatestyles>Markwith, Scott H.; Scanlon, Michael J. (May 11, 2006). "Multiscale analysis of Hymenocallis coronaria (Amaryllidaceae) genetic diversity, genetic structure, and gene movement under the influence of unidirectional stream flow". American Journal of Botany. Botanical Society of America. 94 (2): 151–60. doi:10.3732/ajb.94.2.151. PMID 21642217. Retrieved October 1, 2012.

External links

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