Geology of the County | ||
In Lincoln County, water is obtained from consolidated sedimentary rocks ranging in age from Ordovician to Mississippian, and from unconsolidated sediments of Quaternary age. The oldest rocks exposed on the surface in Lincoln County were deposited in shallow seas 450 million years ago during the Late Ordovician Period. Above the Ordovician rocks are rocks of the Devonian Period, which includes the New Albany Shale. The New Albany Shale, also called the black shale, was formed 400 million years ago when the deep sea floor became covered with an organic black muck. The muck is now hard, black shale (an oil shale) and is one of the most distinctive of all geologic formations in Kentucky. The Mississippian sandstones and siltstones are the result of a great influx of muds, silts, and sands brought in by rivers and streams from uplands many miles away and deposited as a great delta. The Mississippian limestones found in Lincoln County were deposited 350 million years ago in the bottom of a warm, shallow sea. Over the last million years, unconsolidated Quaternary sediments have been deposited along the larger streams and rivers. Geologic Formations in the County Limestones Dolomites Interbedded clay shales, siltstones, and sandstones Fractured shales Clay shales Interbedded limestones and shales Interbedded shales and limestones For more information, see the definitions of geologic terms and rock descriptions, a geologic map of Lincoln County, a summary of the geology of Kentucky, and a discussion of fossils and prehistoric life in Kentucky. Previous--Next--Back to "Groundwater Resources in Kentucky"
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