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Geology and water availability of Cullman County, Alabama

Robert J. Faust·Patrick O. Jefferson
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Abstract

The Pottsville Formation of Pennsylvanian age underlies most of Cullaman County in northern Alabama. It consists mostly of interbedded sandstones and shales that dip southward about 40 feet per mile. The Bangor Limestone of Mississippian age underlies the Pottsville and crops out in a few valleys along the northern boundary of the county. The principal source of ground water in the county is the Pottsville Formation. Sandstones of the Pottsville Formation underlying low topographic areas will yield as Much as 200 gpm (gallons per minute) to individual wells 200 feet deep or less in the southeastern part of the the county and 25-100 gpm in other parts. Those underlying high topographic areas generally yield less than 5 gpm. The average flow of streams in and adjoining Cullman County is about 1,500 mgd (million gallons per day) which includes about 780 mgd that originates in the county. Discharge from ground-water storage is small, and most streams cease to flow during extended dry periods. Sipsey Fork and Mulberry Fork are the only streams in and adjoining Cullman County that have median annual 7-day low flows that exceed 2 mgd.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 33.86015274030232° to 34.30374065672995° latitude; -87.10922241210938° to -86.47064208984375° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Robert J. Faust, Patrick O. Jefferson. 1975. Geology and water availability of Cullman County, Alabama. https://doi.org/10.3133/ofr75451

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