| Nolichucky River | |
|---|---|
 The Nolichucky River atEmbreeville, Tennessee | |
 Nolichucky watershed | |
| Location | |
| Country | United States |
| State | North Carolina,Tennessee |
| Physical characteristics | |
| Source | North Toe River |
| • location | Avery County,North Carolina |
| • coordinates | 35°15′57″N81°53′13″W / 35.26583°N 81.88694°W /35.26583; -81.88694[1] |
| • elevation | 4,350 ft (1,330 m) |
| 2nd source | Cane River |
| • location | Yancey County,North Carolina |
| • coordinates | 35°45′55″N82°18′33″W / 35.76528°N 82.30917°W /35.76528; -82.30917[2] |
| • elevation | 3,553 ft (1,083 m) |
| Source confluence | |
| • location | Yancey County,North Carolina |
| • coordinates | 36°01′44″N82°19′37″W / 36.02889°N 82.32694°W /36.02889; -82.32694[3] |
| • elevation | 2,021 ft (616 m) |
| Mouth | French Broad River |
• location | Cocke County/Hamblen County line,Tennessee |
• coordinates | 36°04′55″N83°13′45″W / 36.08194°N 83.22917°W /36.08194; -83.22917[3] |
• elevation | 1,001 ft (305 m)[3] |
| Length | 115 mi (185 km) |
| Basin size | 1,744 sq mi (4,520 km2)[4] |
| Discharge | |
| • location | Embreeville, Tennessee(mean for water years 1920–2005)[5] |
| • average | 1,378 cu ft/s (39.0 m3/s)(mean for water years 1920–2005)[5] |
| • minimum | 88 cu ft/s (2.5 m3/s)September 1925[5] |
| • maximum | 120,000 cu ft/s (3,400 m3/s)May 1901[5] |
| Basin features | |
| Progression | Nolichucky →French Broad →Tennessee →Ohio →Mississippi →Gulf of Mexico |
TheNolichucky River is a 115-mile (185 km) river that flows throughwestern North Carolina andEast Tennessee in the southeastern United States.[6] Traversing thePisgah National Forest and theCherokee National Forest in theBlue Ridge Mountains, the river's watershed includes some of the highest mountains in theAppalachians, includingMount Mitchell in North Carolina, the highest point in theeastern United States. The river is a tributary of theFrench Broad River and is impounded byNolichucky Dam nearGreeneville, Tennessee.
The Nolichucky River rises as theconfluence of theNorth Toe River and theCane River near the community ofHuntdale, North Carolina. The stream succeeds the North Toe as the boundary betweenYancey County andMitchell County, North Carolina. Trending roughly westward, it flows along the northern base of Flattop Mountain. The gorge is especially steep on its north side. Geologically, the area is predominantly underlain bymetamorphic rock ofPrecambrian age.
The river then entersUnicoi County, Tennessee, as it drops through a whitewater gorge, flowing between the ranges of theBald Mountains (to the south) and theUnaka Mountains (to the north). Turning northwest, the stream is bridged by theAppalachian Trail and byU.S. Highway 19W southwest ofErwin, Tennessee. Near Erwin, twotributary streams, South Indian Creek and North Indian Creek, join the Nolichucky River. Turning more to the north, the stream is paralleled for several miles byState Route 81, (which is also concurrent withTennessee State Route 107 for several miles) crossing intoWashington County. The river cuts between several mountains at this point, including Rich Mountain to the south and Buffalo Mountain to the north.
Shortly after entering Washington County, the river makes a horseshoe bend nearEmbreeville, where it is bridged by SR 81 and SR 107 for the first time. At the northeastern end of Embreeville Mountain, the stream emerges from a largegap and turning west-southwest is bridged by SR 81 again. Here it exits theBlue Ridge Mountains and enters theRidge and Valley province, which is underlain primarily bysedimentary rock of the LowerPaleozoic Era. The river then continues west-southwest for several miles, paralleled by SR 107. The river leaves the roadside nearMt. Carmel. From there it flows northwest over a winding course toDavid Crockett Birthplace State Park near the Washington County–Greene County line. Many tributary creeks join the river in Washington and Greene counties. At the county line, one of the larger tributaries, Big Limestone Creek, joins the river.State Route 351 crosses the river west of Crockett's birthplace.
The river then flows southwestward, following the trends of the Ridge and Valley province's underlying geology. Bridged by SR 107 again just east ofTusculum, the stream continues southwestward, later bridged byState Route 350 just above an impoundment caused byNolichucky Dam.
This dam was constructed as ahydroelectric project by the former Tennessee Electric Power Company in 1912. The dam was sold to theTennessee Valley Authority (TVA) in 1939, when the agency was established by theFranklin D. Roosevelt administration during theGreat Depression. The TVA continued to operate the dam for electrical power purposes until the 1970s. The degree ofsiltation of thereservoir, calledDavy Crockett Lake, had made continued efforts to operate the facility for hydroelectric purposes impracticable. The agency retired the dam as a power source but continues to maintain it and to use it for flood control and recreational purposes. Just west of the dam, the river crossesState Route 70 and SR 107 for a third and final time.
Continuing almost due west, the river is bridged byU.S. Highway 321. Just before reaching the Greene County–Cocke County line, the river is bridged byState Route 340. Just past this point, the river becomes the border between the counties. A few miles below this point it is bridged by Knob Creek Road. South ofInterstate 81, Greene, Cocke, andHamblen counties come to a point at a bend in river, where Lick Creek joins the river. From this point on, the meandering stream forms the Hamblen County–Cocke County line.
The confluence of the Nolichucky with theFrench Broad River occurs in the upstream portion of theDouglas Lake impoundment, caused byDouglas Dam, aWorld War II-era TVA project located downstream along the French Broad. The mouth of the Nolichucky lies near the point where Hamblen, Cocke, andJefferson counties meet. Near the mouth is the Rankin Wildlife Management Area, a reserve operated by theTennessee Wildlife Resources Agency.
While the origins of the name-place have long been debated and remain unclear, it is believed to be derived from the name of theCherokee villageNa’na-tlu gun’yi, or "Spruce-Tree Place," that once stood near modernJonesborough, Tennessee.[7][8] Some claim that according to local lore, it means "Rushing Water(s)",[9] "Dangerous Water(s)", or "Black Swirling Water".
During the 1770s, European frontiersmen established the "Nolichucky settlements" along the river in modern Greene County, in what was then part of Cherokee territory. These settlements were aligned with theWatauga settlements in what is nowElizabethton. As hostilities intensified in the mid-1770s between the settlers and a faction of the Cherokee, known as the "Chickamaugas," who were opposed to the settlements,John Sevier, at the time a young militia officer, began overseeing the construction of Fort Lee. After an invasion was launched by Chickamauga leaderDragging Canoe in July 1776, Sevier abandoned the unfinished fort and fled to the Watauga settlements. Sevier would later acquire the nickname "Nolichucky Jack" or "Chucky Jack" for his exploits along the river and in its vicinity.[10]
Famed frontiersmanDavy Crockett was born along the river nearLimestone, Tennessee, in 1786. The site is now the focus of David Crockett Birthplace State Park.[10]
The turn of the century brought trains hauling passengers (until 1955) and mostly coal on theClinchfield Railroad (now operated byCSX), which still runs alongside the river through the gorge with bridged crossings at Unaka Springs (Erwin) andPoplar, North Carolina. At least one sunken railcar sits at the bottom of the river near the entrance to theLost Cove Settlement, a civil-war era ghost town just upriver (and uphill) from the once-disputed Tennessee-North Carolina border.
Between Poplar, North Carolina, and Unaka Springs, Tennessee, the Nolichucky River Gorge provides one of the more scenic and technical whitewater trips in theSouthern United States, due in large part to its constant (and often rapid) fluctuations.[11] The naturally flowing Nolichucky River is a popularwhitewaterrafting andcanoeing destination having stretches of both whitewater areas and calm water. Rainfall upstream around Mount Mitchell makes the upper section rapids ever more impressive with significant rain causing extremely big water and un-runnable routes in otherwise ordinary areas.
"Frank Gentry describes such a trip through the gorge with Bob Lawson on a rubber raft. Frank says, 'I just went along for the ride and a look at the scenery. Man-a-live, I didn't have time to look at anything! When that raft hit those rapids at "Rooster Tail" we were going round and round, dived into "Souse Hole", slammed into rocks here and more rocks there. Seemed like the harder you paddled the more rocks you'd hit. You'd just whirl and twirl and wham into more big boulders you hadn't even seen. Sometimes that white-faced water would stand straight up and slam you smack-kadab all over the raft, or out of it. Man, that was a wild trip!"[12]
Inversely, a lack of adequate rainfall throughout the summer considerably increases the difficulty of navigating the pre-existing aspects of the rapids, which already tend towards being both technically difficult and challenging for rafters. These dry conditions and concomitant low water levels reveal a vast diversity of features. These hazards are ordinarily submerged during summers with normal seasonal rainfall patterns. Seasonal droughts can make rafting trips inadvisable or impassable, prompting local rafting companies in Unicoi County to sometimes divert whitewater river trips to theWatauga River running throughElizabethton, Tennessee inCarter County. The TVA regulates flow of the Watauga River and guarantees a minimum release schedule accommodating whitewater rafting companies during the summer season with the regular release of deep, impounded reservoir waters from behind both theWatauga Dam and theWilbur Dam.[13]
