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Many of the features found in the Blue Ridge and documented by Tollo and others have confirmed that the rocks exhibit many similar features in other North American Grenville, mountain Top Hotel, king between Washington and St. Hemlock and mixed, frequently Asked Questions”.
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The Blue Ridge Mountains are a physiographic province of the larger Appalachian Mountains range. This province consists of northern and southern physiographic regions, which divide near the Roanoke River gap. The Blue Ridge Mountains are noted for having a bluish color when seen from a distance.
Trees put the “blue” in Blue Ridge, from the isoprene released into the atmosphere, thereby contributing to the characteristic haze on the mountains and their distinctive color. The Blue Ridge Mountains as seen from Blowing Rock, North Carolina. The Blue Ridge extends as far north into Pennsylvania as South Mountain. The Blue Ridge contains the highest mountains in eastern North America south of Baffin Island.
Southern Appalachians and links two national parks: Shenandoah and Great Smoky Mountains. Most of the rocks that form the Blue Ridge Mountains are ancient granitic charnockites, metamorphosed volcanic formations, and sedimentary limestone. Many of the features found in the Blue Ridge and documented by Tollo and others have confirmed that the rocks exhibit many similar features in other North American Grenville-age terranes. The Blue Ridge Mountains began forming during the Silurian Period over 400 million years ago. Approximately 320 Mya, North America and Europe collided, pushing up the Blue Ridge.