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The Blue Ridge is mostly composed of Precambrian basement rocks (igneous & metamorphics). The mountains of the Blue Ridge are generally rounded and not very tall. This is unlike the tall, mostly sharp-peaked mountains of western America's Cordillera, the Andes of South America, the Alps of Europe, and the Himalayas of Asia.
Blue Ridge Mountains - Front Royal, Virginia Although the term "Blue Ridge" is sometimes applied exclusively to the eastern edge or front range of the Appalachian Mountains, the geological definition of the Blue Ridge province extends westward to the Ridge and Valley area, encompassing the Great Smoky Mountains, the Great Balsams, the Roans, the Blacks, and other mountain ranges.
The southernmost peak in the Blue Ridge Mountains, [2] the mountain has an elevation of 3,288 feet (1,002 m), making it the highest point in Pickens County, and the Atlanta Metropolitan Area. Mount Oglethorpe served as the southern terminus of the Appalachian Trail from when the trail was completed in 1937 until 1958.
The Blue Ridge Mountains as seen from the Blue Ridge Parkway near Mount Mitchell. The following is a list of mountains constituting the Blue Ridge, a mountain range stretching about 450 miles from Pennsylvania to Georgia in the USA. The Blue Ridge is part of the larger Appalachian Mountain Range.
Mount Pisgah is a mountain in the Appalachian mountain range and part of the Blue Ridge Mountains of North Carolina, United States.The mountain's height is 5,721 feet (1,744 m) above sea level, and it sits approximately 15 miles (24 kilometers) southwest of Asheville, near the crossing of the boundaries of Buncombe, Haywood, Henderson and Transylvania counties.
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."