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