File:Geode (Fort Payne Formation, Lower Mississippian; Burkesville West Rt. 90 roadcut, Kentucky, USA) 15 (27409930197).jpg

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Geodes are small to large, subspherical to irregularly-shaped, crystal-lined cavities in rocks. They form when water enters a void in a host rock and precipitates crystals. The most common geode-lining mineral is quartz.

The cracked geode shown here is from the Fort Payne Formation, a fossiliferous shale-and-limestone unit in the Lower Mississippian of Kentucky and Tennessee. Geodes are relatively common in this unit. Geode-lining minerals observed at this site were quartz, calcite, and dolomite.

Stratigraphy: Fort Payne Formation, Osagean Stage, upper Lower Mississippian

Locality: roadcut on the southern side of Route 90, just west of Burkesville, Kentucky, USA (36° 47’ 58.30” North latitude, 85° 22’ 58.20” West longitude)
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Source Geode (Fort Payne Formation, Lower Mississippian; Burkesville West Rt. 90 roadcut, Kentucky, USA) 15
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@N05/27409930197 (archive). It was reviewed on 12 October 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

12 October 2019

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Date/TimeThumbnailDimensionsUserComment
current04:03, 12 October 2019Thumbnail for version as of 04:03, 12 October 20193,658 × 2,646 (4.1 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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