File:Raccoon Shale (Lower Mississippian; South Fork of the Licking River, Heath, Ohio, USA) (44443928574).jpg
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Summary
| Description |
(photo by James Cheshire) The Cuyahoga Formation is a marine, mixed-siliciclastics succession in the Lower Mississippian of eastern Ohio. Many members and submembers have been named, based on whether the dominant lithology is shale or sandstone. At the river cut shown here, gray shale is interbedded with siltstones and finer-grained sandstones. This is the Raccoon Shale Member, named after Raccoon Creek, which runs from Alexandria to Granville to Newark, Ohio. Stratigraphy: Raccoon Shale Member, Cuyahoga Formation, Kinderhookian Stage, lower Lower Mississippian Locality: outcrop along the South Fork of the Licking River, Licking County, east-central Ohio, USA |
| Date | |
| Source | Raccoon Shale (Lower Mississippian; South Fork of the Licking River, Heath, Ohio, USA) |
| 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@N05/44443928574 (archive). It was reviewed on 7 December 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 18:21, 7 December 2019 | | 5,472 × 3,648 (9.88 MB) | Ser Amantio di Nicolao | Transferred from Flickr via #flickr2commons |
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