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Blue Ridge Lake is a reservoir in Fannin County, in the northern portion of the U.S. state of Georgia. The reservoir encompasses 3,300-acre (1,300 ha) of water, and a "full summer pool" of approximately 1,686 feet (514 m) above mean sea level .
The Blue Ridge Mountains are a physiographic province of the larger Appalachian Highlands range. The mountain range is located in the Eastern United States and extends 550 miles southwest from southern Pennsylvania through Maryland, West Virginia, Virginia, North Carolina, South Carolina, Tennessee, and Georgia. [1]
Carters Lake is a man-made reservoir located on the Coosawattee River in the Blue Ridge Mountains in Gilmer and Murray counties in the U.S. state of Georgia. It is the state's deepest lake. It is the state's deepest lake.
Blue Ridge Dam is a hydroelectric dam on the Toccoa River in Fannin County, in the U.S. state of Georgia. It is the uppermost of four dams on the Toccoa/Ocoee River owned and operated by the Tennessee Valley Authority. The dam impounds the 3,300-acre (1,300 ha) Blue Ridge Lake on the southwestern fringe of the Blue Ridge Mountains. [1]
Blue Ridge Dam, a hydroelectric dam in Fannin Co., Georgia Lake Blue Ridge, a lake created by the completion of Blue Ridge Dam; Blue Ridge Mountain (New York), an elevation in Hamilton County; Blue Ridge Mountains, a major range of the Appalachian Mountains Blue Ridge Mountain, in Virginia and West Virginia
The National Park Service preserves the peaks and lake as part of the Blue Ridge Parkway. Thomas Jefferson once wrote that "the mountains of the Blue Ridge, and of these the Peaks of Otter, are thought to be of a greater height, measured from their base, than any others in our country, and perhaps in North America."
Table Rock State Park is a 3,083-acre (12.48 km 2) park at the edge of the Blue Ridge Mountains in northern Pickens County, South Carolina. The park includes Pinnacle Mountain, the tallest mountain totally within the state. [4]
The park is located along the western part of the Blue Ridge anticlinorium, a regional-scale Paleozoic structure at the eastern margin of the Appalachian fold and thrust belt. Rocks within the park were folded, faulted, distorted, and metamorphosed during the late Paleozoic Alleghanian orogeny (325 to 260 million years ago). [8]