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Ames Limestone

Geologic formation in the United States From Wikipedia, the free encyclopedia

Ames Limestone
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The Ames Limestone is a geologic formation in Ohio, Kentucky, Pennsylvania and West Virginia. It is part of the Conemaugh Group. Formerly know at "Crinoidal Limestone" and "Green Fossiliferous Lime" it was renamed to Ames.[1]

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Fossils of Echinoderm, Brachiopod, and Gastropoda are commonly found in the Ames.[2]

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Description

The Ames is a thin Marker bed of Limestone and/or Fossiliferous limestone. It marks a transition from a predominantly marine environment to predominantly alluvial environment. The Ames serves as a marker for the boundary for the Casselman Formation and the Glenshaw Formation. [2]

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