File:Sentinel Butte Formation (Paleocene; Painted Canyon, Little Missouri Badlands, North Dakota, USA) 10.jpg

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English: These are Paleocene-aged, nonmarine, mostly siliciclastic sedimentary rocks, weathered and eroded into badlands topography. The reddish-brown areas are clinker beds, which are naturally burned-out lignite coal horizons.

Stratigraphy: Sentinel Butte Formation, Upper Paleocene

Locality: Painted Canyon rim overlook, Little Missouri Badlands, Roosevelt National Park, western North Dakota, USA
Date
Source https://www.flickr.com/photos/47445767@N05/51842604752/
Author James St. John

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This file is licensed under the Creative Commons Attribution 2.0 Generic license.
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/51842604752. It was reviewed on 17 February 2022 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

17 February 2022

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current17:33, 17 February 2022Thumbnail for version as of 17:33, 17 February 20223,008 × 2,000 (5.38 MB)Ser Amantio di Nicolao (talk | contribs)Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/51842604752/ with UploadWizard

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