Difference between revisions 166199784 and 166199785 on dewiki{{for|the lunar range|Smoky Mountains (Moon)}} {{Infobox mountain range | name = Great Smoky Mountains | photo = Clifftops4-7-07.jpg | photo_size = 300 | photo_caption = The Smoky Mountains, viewed from atop [[Mount Le Conte (Tennessee)|Mount Le Conte]]. | country = United States | state = Tennessee (contracted; show full) ==Geology== [[Image:Alum-cave-bluffs-tn1.jpg|thumb|300px|The [[Alum Cave Trail|Alum Cave Bluffs]].]] Most of the rocks in the Great Smoky Mountains consist of Late [[Precambrian]] rocks that are part of a formation known as the '''Ocoee Supergroup'''. The Ocoee Supergroup consists primarily of slightly metamorphosed sandstones, phyllites, schists, and slate, and trace amounts of calcium carbonate<Geology. National Park Service. Retrieved from https://www.nps.gov/grsm/learn/nature/geology.htm#10/35.6238/-83.5757> . Early Precambrian rocks, which include the oldest rocks in the Smokies, comprise the dominant rock type in the Raven Fork Valley (near [[Oconaluftee (Great Smoky Mountains)|Oconaluftee]]) and upper Tuckasegee River between [[Cherokee, North Carolina|Cherokee]] and [[Bryson City, North Carolina|Bryson City]]. They consist primarily of metamorphic [[gneiss]], [[granite]], and [[schist]]. Cambrian sedimentary rocks are found among the outer reaches of the Foothills to the northwest and in limestone coves (contracted; show full)[[Category:Landforms of Sevier County, Tennessee]] [[Category:Landforms of Cocke County, Tennessee]] [[Category:Landforms of Swain County, North Carolina]] [[Category:Landforms of Haywood County, North Carolina]] [[Category:Natural history of the Great Smoky Mountains| 01]] [[Category:Appalachian culture]] [[Category:Old growth forests]] [[Category:Southern Sixers]] All content in the above text box is licensed under the Creative Commons Attribution-ShareAlike license Version 4 and was originally sourced from https://de.wikipedia.org/w/index.php?diff=prev&oldid=166199785.
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