Geology of the County | ||
In Caldwell County, water is obtained from consolidated sedimentary
rocks of Mississippian through Pennsylvanian ages and from unconsolidated
sediments of the Cretaceous and Quaternary ages. Geologists call the
oldest rocks found at the surface in Caldwell County the St. Louis Limestone.
The most common rock types in Caldwell County are Mississippian limestones,
which were deposited 350 million years age in the bottom of a warm,
shallow sea. At the end of the Mississippian, 320 million years ago,
the seas receded and sediments of the Pennsylvanian were deposited.
The warm climate of the Pennsylvanian grew extensive forests and great
coastal swamps at the edges of water bodies. Marine waters advanced
and receded many times, which produced many layers of sandstone, shale,
and coal. Vegetation of all sorts fell into the water and was buried
under blankets of sediments, which over long geologic time were compressed
into coal. The nonvegetative sediments such as sand, clay, and silt
were compressed into sandstone and shale. During the latter part of
the Cretaceous, 130 million years ago, the Gulf of Mexico inundated
much of the southern United States and covered all the Geologic Formations in the County Limestones Sandstones Coals, sandstones, and shales Interbedded limestones, sandstones, and shales For more information, see the definitions of geologic terms and rock descriptions, a geologic map of the 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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