File:Geode (lower Warsaw Formation, Lower Mississippian; Warsaw, Hancock County, Illinois, USA) (41598898692).jpg

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Quartz geode from the Mississippian of Illinois, USA. (public display, Geology Department, Wittenberg University, Springfield, Ohio, USA)

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, as in this Illinois example.

Stratigraphy: derived from dolostone or dolomitic limestone of the lower member of the Warsaw Formation, Osagean Stage, upper Lower Mississippian

Locality: unrecorded/undisclosed site at or near Warsaw, far-western Hancock County, far-western Illinois, USA
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Source Geode (lower Warsaw Formation, Lower Mississippian; Warsaw, Hancock County, Illinois, USA)
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@N05/41598898692. It was reviewed on 5 December 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

5 December 2019

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Date/TimeThumbnailDimensionsUserComment
current02:07, 5 December 2019Thumbnail for version as of 02:07, 5 December 20191,816 × 1,605 (2.14 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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