File:Thunderhead Sandstone (Neoproterozoic; Chimney Tops overlook roadcut, Great Smoky Mountains, Tennessee, USA) 5 (36885030092).jpg

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Sandstone in the Precambrian of Tennessee, USA.

This is an outcrop of Thunderhead Sandstone in the Great Smoky Mountains. It's one of many stratigraphic units in the ~50,000 feet thick Ocoee Supergroup. The Ocoee has considerable deposits of sandstone and shale originally deposited as sands and muds in an ancient ocean trench. Trenches form along subduction zones, where a tectonic plate composed of thin, heavy oceanic lithosphere dives down into the mantle below another tectonic plate of either oceanic lithosphere or thick, lightweight continental lithosphere.

The Thunderhead Sandstone in the park consists of coarse-grained sandstone with granules. It has quartz and potassium feldspar - it's an arkosic sandstone. Subangular grains appear to dominate. Some phyllite interbeds are present - these were originally shales, but have been metamorphosed.

Stratigraphy: Thunderhead Sandstone, Great Smoky Group, Ocoee Supergroup, Neoproterozoic

Locality: roadcut along Newfound Gap Road (Rt. 441) at mile marker 5.4 of Moore (1988) (A Roadside Guide to the Geology of the Great Smoky Mountains National Park, page 90) (= park service milepost 7), near Chimney Tops overlook, Great Smoky Mountains National Park, southern Sevier County, eastern Tennessee, USA
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Source Thunderhead Sandstone (Neoproterozoic; Chimney Tops overlook roadcut, Great Smoky Mountains, Tennessee, USA) 5
Author James St. John

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/36885030092. It was reviewed on 6 December 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

6 December 2019

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Date/TimeThumbnailDimensionsUserComment
current02:17, 6 December 2019Thumbnail for version as of 02:17, 6 December 20191,989 × 2,798 (5.65 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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