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Utica Shale

The Utica Shale is a stratigraphical unit of Upper Ordovician age in the Appalachian Basin. It
underlies much of the northeastern United States and adjacent parts of Canada.
It takes the name from the city of Utica, New York, as it was first described as an outcrop along the Starch Factory Creek east of the city by Ebenezer Emmons in 1842.

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