File:Mudchips in sandstone (Vinton Member, Logan Formation, Lower Mississippian; Mohawk Dam emergency spillway, western Coshocton County, Ohio, USA) 3 (26620254223).jpg

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Mudchips in sandstone from the Mississippian of Ohio, USA. (geology hammer for scale)

The mostly-gray structures shown above are thin, discoidal pieces of mudshale. The surrounding light-colored host rock is sandstone. Abundant mudshale chips in a host rock are referred to as mudchip breccias. Mudchip breccias and mudchips in sandstone form when erosion removes thin layers of previously-deposited muds, followed by transportation and deposition in coarser-grained sediments. Mudchips usually become aligned with the horizontal stratification. After burial, diagenesis, uplift, and erosion, mudchip-rich horizons tend to be readily exposed on split surfaces because they are planes of weakness.

Stratigraphy: Vinton Member, upper Logan Formation, Osagean Stage, upper Lower Mississippian

Locality: Mohawk Dam emergency spillway, northwest of the town of Nellie, western Coshocton County, eastern Ohio, USA (vicinity of 40º 21' 26.42" North latitude, 82º 04' 57.97" West longitude)
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Source Mudchips in sandstone (Vinton Member, Logan Formation, Lower Mississippian; Mohawk Dam emergency spillway, western Coshocton County, Ohio, USA) 3
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@N05/26620254223 (archive). It was reviewed on 10 October 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

10 October 2019

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current02:13, 10 October 2019Thumbnail for version as of 02:13, 10 October 20193,845 × 2,635 (4.22 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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