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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.
Blue Ridge Mountain consists mostly of anticlinal Catoctin Greenstone and is not underlain by Old Rag Granite, as is the Blue Ridge south of Manassas Gap. This is why the mountain is more ridgelike and less rugged than sections to the south. The greenstone was deposited during the Catoctin Formation and uplifted during the Alleghenian Orogeny.
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.
The mountains are made of highly deformed metamorphic rocks, largely developed during the Precambrian age over 541 million years ago. The mountains include schists, gneisses, slates, and quartzites, and are extensively intruded by igneous bodies. The Blue Ridge Mountains contain the highest mountains in eastern North America south of Baffin Island.
The Appalachian–Blue Ridge forests are an ecoregion in the Temperate broadleaf and mixed forests Biome, in the Eastern United States. The ecoregion is located in the central and southern Appalachian Mountains , including the Ridge-and-Valley Appalachians and the Blue Ridge Mountains .
The Unaka Mountains. The Unaka Range is a mountain range on the border of Tennessee and North Carolina, in the southeastern United States.It is a subrange of the Appalachian Mountains and is part of the Blue Ridge Mountains physiographic province.
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