File:Fossiliferous limestone (Delaware Limestone, Middle Devonian; Olentangy River at Lazarus Run confluence, Delaware County, Ohio, USA) 9 (29390905993).jpg

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Limestone in the Devonian of Ohio, USA.

The Delaware Limestone is a significant carbonate unit in the Middle Devonian of central and northern Ohio. It's actually part of a much more widespread sheet of Devonian carbonates that extends from New York State to the Midwest. The Delaware Limestone represents deposition in a subtropical, shallow-water, carbonate platform environment. The rocks are principally micritic limestones, fossiliferous wackestones, and fossiliferous packstones. Fossils are typical Paleozoic shallow marine invertebrates.

The thin-bedded Delaware Limestone is underlain by the thick-bedded Columbus Limestone (also Middle Devonian). The contact is a prominent disconformity (a type II sequence boundary). Biostratigraphic studies have shown that one conodont biozone is missing at the Columbus-Delaware contact in central Ohio, probably representing ~1 to 3 million years. The Delaware Limestone is overlain by soft gray clayshales of the Olentangy Shale (lower Upper Devonian).

Stratigraphy: Delaware Limestone, Eifelian Stage, lower Middle Devonian

Locality: creek cut along Lazarus Run, eastern side of Chapman Road, south of the town of Delaware, central Delaware County, central Ohio, USA (~40º 13’ 58.97” North latitude, ~83º 03’ 37.55” West longitude)
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Source Fossiliferous limestone (Delaware Limestone, Middle Devonian; Olentangy River at Lazarus Run confluence, Delaware County, Ohio, USA) 9
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@N05/29390905993 (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.

7 December 2019

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Date/TimeThumbnailDimensionsUserComment
current18:58, 7 December 2019Thumbnail for version as of 18:58, 7 December 20193,000 × 3,497 (5.36 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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