thumbnail

Potentiometric surface of the Mississippian aquifer in parts of Trigg, Lyon, Caldwell, and Christian Counties, Mississippian Plateau region, Kentucky

Water-Resources Investigations Report 78-25
By:

Links

Abstract

Ground-water levels in a 600 square mile area of the Cumberland River drainage basin in parts of Trigg, Lyon Caldwell, and Christian Counties, Mississippian Plateau Region, Kentucky are shown by means of contours on the potentiometric surface. Generaly, ground water moves toward and with the surface drainage to Lake Barkley and the Cumberland River. The potentiometric map indicates a minimum drilling depth to water. The bedrock is composed largely of sandstone, cavernous limestone, or jointed and fractured limestone. All of these rock types yield sufficient water for domestic and stock purposes. The cavernous limestone is extremely vulnerable to pollution. 

Study Area

Publication type Report
Publication Subtype USGS Numbered Series
Title Potentiometric surface of the Mississippian aquifer in parts of Trigg, Lyon, Caldwell, and Christian Counties, Mississippian Plateau region, Kentucky
Series title Water-Resources Investigations Report
Series number 78-25
DOI 10.3133/wri7825
Year Published 1978
Language English
Publisher U.S. Geological Survey
Description 6 Plates: 48.46 x 25.72 inches or smaller
Country United States
State Kentucky
County Caldwell County, Christian County, Lyon County, Trigg County
Other Geospatial Mississippian aquifer
Google Analytic Metrics Metrics page
Additional publication details