Topography | ||
Discussion from McGrain and Currens (1978) Clinton
County is located in the Mississippian Plateaus area of south-central
Kentucky. The southern boundary of the county is the Kentucky-Tennessee
state line. The topography is diverse. Much of the terrain is a gently
rolling, limestone plain, approximately 1,000 feet in elevation, with
characteristic sinkhole topography. Erosional remnants of the western
edge of the Cumberland Escarpment dot the landscape in the eastern part
of the county and rise above the sinkhole plain as isolated knobs and
mountain-like ridges. Tributary valleys of the deeply entrenched Cumberland
River, which lies just north of Clinton County, dissect the surface
of the limestone plain in the northern part of the county. The southern
part of the county is similarly dissected through stream erosion by
the Wolf River and its tributaries. The highest elevation, 1,780 feet, is a knob on an upland complex of
sandstone-capped ridges known as Poplar Mountain, located east-northeast
of Albany. Other knobs and mountains in the area also attain elevations
of 1,700 feet or greater, approximately 700 feet above the limestone
plain. These include Copperas Knob, 1,711 feet; Kennedy Mountain, 1,720
feet; and Sewell Mountain, 1,760 feet. Bald Rock, on the Clinton-Wayne
County line just north of the Kentucky-Tennessee state line, also has
an elevation of 1,760 feet. The elevation of Albany, the county seat, is 960 feet. Cumberland City has an elevation of 1,053 feet, and Ida is at 921 feet. The 7.5-minute topographic quadrangle maps that cover Clinton County
are shown by name and index code (Kentucky Natural Resources and Environmental
Protection Cabinet) on the index
map. Previous--Next--Back to "Groundwater Resources in Kentucky"
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