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Watauga River
The Watauga River () is a large stream of western North Carolina and East Tennessee. It is long with its headwaters in Linville Gap to the South Fork Holston River at Boone Lake. Course The Watauga River rises from a spring located south to the base of Peak Mountain at Linville Gap in Avery County, North Carolina. The spring emanates from the western side of the Tennessee Valley Divide, which is, at this location, congruent with the Eastern Continental Divide. On the other side of the divide at Linville Gap are the headwaters of the Linville River in the Upper Catawba watershed. Waters of the Linville River eventually reach the Atlantic Ocean, whereas waters of the Watauga River reach the Gulf of Mexico; hence the Eastern Continental Divide. The river then flows across Watauga County, North Carolina, crossing the Tennessee state line (River Mile (RM) 55.1) at Johnson County, then into Carter County, Tennessee and ends at its confluence with the Holston River's South Fork ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valle Crucis, North Carolina
Valle Crucis in an unincorporated community and census-designated place located in Watauga County, North Carolina, United States. The name of the town is Latin for "Vale of the Cross," a reference to a valley in the area where three streams converge to form a shape similar to an archbishop's cross. The community is located along NC 194, between the towns of Banner Elk and Boone. Demographics History Before the 1840s, there has been scattered settlements in the area but not permanently until the Valle Crucis Episcopal Mission was established. Founded by Levi Silliman Ives, an Episcopal missionary, "Easter Chapel" served as the first Episcopal church in the area. Its successor, the Holy Cross Episcopal Church, was built in 1926 and modeled on a now-defunct medieval monastery in Wales and is noteworthy for its architecture. Geography and climate Valle Crucis is located at the banks of Dutch Creek and Watauga River, at an elevation of above sea level. To its north and ea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long, large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known, amongst others, as brook, creek, rivulet, rill, run, tributary, feeder, freshet, narrow river, and streamlet. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roan Creek
Roan Creek is a tributary of the Watauga River that rises near the border between the U.S. states of Tennessee and North Carolina. Its source is located along the slopes of Snake Mountain near Trade in Johnson County, Tennessee. From its source, Roan Creek flows north, then turns west around the northern end of Stone Mountain. Then it flows south and west through Cherokee National Forest in the valley between Stone Mountain and Doe Mountain, until entering the Watauga River and Watauga Lake, the reservoir behind Watauga Dam. Its waters eventually flow through the Watauga River, the Holston River, the Tennessee River, the Ohio River, and the Mississippi River to the Gulf of Mexico. In 2005 Roan Creek was cited as one of the top ten most endangered rivers by American Rivers, a national non-profit A nonprofit organization (NPO), also known as a nonbusiness entity, nonprofit institution, not-for-profit organization, or simply a nonprofit, is a non-governmental (private) leg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elk River (North Carolina–Tennessee)
The Elk River is a large stream in the North Carolina High Country and East Tennessee. The headwaters begin from the Northwestern slopes of Peak Mountain in Avery County, North Carolina and end at the Watauga River in Carter County, Tennessee. Hydrography With the headwaters beginning from the Northwestern slopes of Peak Mountain, it flows west to Banner Elk then towards Elk Park. For most of the river's course, it runs in a deep gorge. Just before the Elk River crosses into Tennessee it flows over "Big Falls" (also called "Elk Falls"), a locally-known attraction which is approximately a 60-foot (18 m) drop. It then flows down a narrow, relatively steep valley to the tiny community of Elk Mills, which is named for a former water-powered mill built on this river at this point by early white settlers. Between the state line and Elk Mills, it flows over Twisting Falls, a drop of approximately 30 feet (nine m). At this point, it is bridged by U.S. Highway 321. Shortly be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watauga Lake
Watauga Lake, located east of Elizabethton, Tennessee, is the local name of the Watauga Reservoir created by the Tennessee Valley Authority (TVA) with the 1948 completion of the TVA Watauga Dam. According to lake expert Holly C Ward, Watauga Lake is the third cleanest in the country. The Cherokee National Forest surrounds both the Tennessee Valley Authority Watauga Reservoir and Wilbur Reservoir in an area of northeast Tennessee that TVA describes as being located "in some of the most beautiful country in the Tennessee River watershed". History Construction of Watauga Dam began in early 1942 but was curtailed later that year in favor of other World War II building efforts. Work on TVA Watauga Dam resumed in 1946, and finished at the end of 1948, impounding both the Watauga River and Elk River for the purposes of flood, hydropower generation and downstream navigation on the Tennessee River and Reservoir system. The original town of Butler, Tennessee, now sits at the bo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watauga Dam
Watauga Dam is a hydroelectric and flood control dam on the Watauga River in Carter County, in the U.S. state of Tennessee. It is owned and operated by the Tennessee Valley Authority, which built the dam in the 1940s as part of efforts to control flooding in the Tennessee River watershed. At , Watauga is the second-highest dam in the TVA river and reservoir system (behind only Fontana), and at the time of its completion was one of the highest earth-and-rock dams in the United States. The dam impounds the TVA Watauga Reservoir of , and its tailwaters feed into Wilbur Lake.Tennessee Valley Authority, ''The Upper Holston Projects: Watauga, South Holston, Boone, and Fort Patrick Henry; a Comprehensive Report on the Planning, Design, Construction, Initial Operations, and Costs of Four Hydro Projects in the Holston Basin at the Eastern Tip of Tennessee'', Technical Report No. 14 (Washington, D.C.: U.S. Government Printing Office, 1958), pp. 1-6, 13-14, 23, 31, 42-43. Its namesake, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tennessee Valley Authority
The Tennessee Valley Authority (TVA) is a federally owned electric utility corporation in the United States. TVA's service area covers all of Tennessee, portions of Alabama, Mississippi, and Kentucky, and small areas of Georgia, North Carolina, and Virginia. While owned by the federal government, TVA receives no taxpayer funding and operates similarly to a private for-profit company. It is headquartered in Knoxville, Tennessee, and is the sixth-largest power supplier and largest public utility in the country. The TVA was created by Congress in 1933 as part of President Franklin D. Roosevelt's New Deal. Its initial purpose was to provide navigation, flood control, electricity generation, fertilizer manufacturing, regional planning, and economic development to the Tennessee Valley, a region that had suffered from lack of infrastructure and even more extensive poverty during the Great Depression than other regions of the nation. TVA was envisioned both as a power supplier and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Linville River
The Linville River is a river in western North Carolina, United States. The river begins in the slopes of Peak Mountain, Sugar Mountain and Flattop Mountain, in the Linville Gap area (also known as Tynecastle). As it goes south through Avery County, it passes through the communities of Grandfather, Linville, Pineola, Crossnore and finally at Linville Falls. After entering Burke County at the community of Linville Falls, the river becomes the centerpiece of the Linville Falls and the Linville Gorge, an area referred to as "the Grand Canyon of North Carolina." After approximately 30 miles (48 km), the river ends at Lake James and the Catawba River The Catawba River is a major river located in the Southeastern United States. It originates in Western North Carolina and flows into South Carolina, where it later becomes known as the Wateree River. The river is approximately 220 miles (350&nbs ...; the original confluence with the Catawba River has been flooded by th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Continental Divide
The Eastern Continental Divide, Eastern Divide or Appalachian Divide is a drainage divide, hydrological divide in eastern North America that separates the easterly Atlantic Seaboard drainage basin, watershed from the westerly Gulf of Mexico watershed. It is one of six continental hydrological divides of North America which define several drainage basins, each of which drains to a particular body of water. The divide nearly spans the United States from south of Lake Ontario through the Florida peninsula, and consists of raised terrain including the Appalachian Mountains to the north, the southern Piedmont Plateau and lowland ridges in the Atlantic Coastal Plain to the south. Course Northern portion The divide's northern portion winds through the middle of the Appalachian Mountains, either through the interior of the Allegheny Plateau or along the Allegheny Mountains. In this portion, the western drainage of the divide flows into the watersheds of the Allegheny River, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tennessee Valley Divide
The Tennessee Valley Divide is the boundary of the drainage basin of the Tennessee River and its tributaries. The Tennessee River drainage basin begins with its tributaries in southwestern Virginia and flows generally west to the confluence of the Tennessee with the Ohio River at Paducah, Kentucky. The Tennessee Valley Divide forms a loop surrounding the drainage basin, beginning and ending at the river's mouth in Paducah. The divide passes through or touches the states of West Virginia, Virginia, North Carolina, South Carolina, Georgia, Alabama, Mississippi, Tennessee and Kentucky. Course Northern portion The northern portion of the divide mostly separates the Tennessee River watershed from that of Cumberland River, except for a portion in the northeast that bounds the Big Sandy River and New River watersheds. All four rivers empty into the Ohio River. Following the Divide in a clockwise direction, it leads east and southeast through western Kentucky through th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peak Mountain (North Carolina)
Peak Mountain is a mountain in the North Carolina High Country, near the town of Seven Devils. It is known by several other names such as Tynecastle Peak, Invershiel Peak and Dunvegan Peak. It is wholly in the Pisgah National Forest. Its elevation reaches . The headwaters of the Elk River begins from the Northwestern slopes of the mountain; along the Southwestern slopes, it shares with Sugar Mountain and Flattop Mountain as the headwaters of the Linville River; along the Southeastern slopes, it shares with Grandfather Mountain as the headwaters of the Watauga River The Watauga River () is a large stream of western North Carolina and East Tennessee. It is long with its headwaters in Linville Gap to the South Fork Holston River at Boone Lake. Course The Watauga River rises from a spring located south to .... Attractions ''Hawksnest Snow Tubing and Zipline'', located along northern ridge of the mountain in the town of Seven Devils, offers zip lining year round and s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrology)
A spring is a natural exit point at which groundwater emerges from an aquifer and flows across the ground surface as surface water. It is a component of the hydrosphere, as well as a part of the water cycle. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. A spring produced by the emergence of geothermally heated groundwater is known as a hot spring. The yield of spring water varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the water table reaches above the surface level, or if the terrain depresses sharply. Springs may also be formed as a result of karst topography, aquifers or volcanic activity. Springs have also been ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
