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Fort Payne Chert
Stratigraphic range: Viséan
Chertified fossiliferous limestone (Ft. Payne Limestone, Lower Mississippian; Lake Cumberland, Kentucky, USA) 2 (30748692874).jpg
Chertified fossiliferous limestone from the Fort Payne Formation (Kentucky)
Type Formation
Underlies Tuscumbia Limestone and Ullin Formation
Overlies Maccrady Formation and Springville Formation
Location
Region Appalachia and Southeastern United States
Country United States
Extent Illinois, Kentucky, Mississippi, Missouri, Tennessee, and Virginia

The Fort Payne Formation, or Fort Payne Chert, is a geologic formation found in the southeastern region of the United States. It is a Mississippian Period cherty limestone, that overlies the Chattanooga Shale (or locally the Maury Formation), and underlies the St. Louis Limestone (lower Tuscumbia Limestone in Alabama). To the north, it grades into the siltstone Borden Formation. It preserves fossils dating back to the Carboniferous period.

Eugene Allen Smith named the Fort Payne Formation for outcrops at Fort Payne, Alabama.

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