Groundwater Availability
 

Alluvium (Qa)
Topography
The alluvium forms terraces and floodplains along the Cumberland River and tributaries.

Hydrology
Most wells in the alluvium are inadequate for a domestic supply.

Ste. Genevieve Limestone Member of the Monteagle Limestone (Mgl)
Topography
The limestone underlies rolling and dissected karst areas, forming steep bluffs along Lake Cumberland.

Hydrology
The limestone yields more than 50 gallons per minute to wells from large solution openings in karst areas. Most wells penetrate solution openings, but in areas high above perennial streams these solution openings are dry in late summer and fall, and many wells are inadequate. Wells that do not intersect karst conduits generally are inadequate for domestic use. Springs having low flows ranging from less than 10 gallons per minute to more than 200 gallons per minute occur at or near stream level or near contact with the underlying St. Louis Limestone.

St. Louis Limestone (Mgl)
Topography
The St. Louis forms steep bluffs along Lake Cumberland. It underlies rolling karst areas, but commonly has less relief than karst in areas underlain by the Ste. Genevieve Limestone. Close to Lake Cumberland and tributaries the St. Louis is dissected. Resistant siltstone alternating with nonresistant shale layers forms discontinuous minor benches on hillsides.

Hydrology
The St. Louis yields more than 50 gallons per minute to wells from large openings in karst areas. Most wells penetrate some solution openings, but where openings are small or high above perennial streams, yields are often inadequate for domestic supply. Yields of wells close to major streams are large where solution openings are penetrated, but otherwise are inadequate. A major spring horizon occurs near the top of the formation in the karst areas. Many seepage springs occur throughout the formation; low flows range from less than 10 gallons per minute to more than 1,000 gallons per minute. The lower part of the formation is composed of siltstone and argillaceous limestone. Yields from these sedimentary rocks are low and generally are not adequate for a domestic supply.

Salem and Warsaw Formations (Msh)
Topography
These formations underlie gentle to dissected rolling uplands, forming steep bluffs where the limestone overlies rocks of Osagean age and along Lake Cumberland. In some areas numerous small sinkholes occur in the formation.

Hydrology
These formations yield enough water for a domestic supply where they are dominantly limestone and close to perennial stream level. Yields are low where siltstone or argillaceous limestone is penetrated. A minor spring horizon occurs at the contact of the limestone with the underlying siltstone or argillaceous limestone. Another spring horizon occurs near the contact of the Warsaw and Fort Payne. Springs low flows generally are less than 5 gallons per minute.

Fort Payne Formation (Mbf), limestone bodies within Fort Payne (ls), Knifley Sandstone Member (Mfk)
Topography
These formations underlie dissected rolling uplands, forming steep valley sides in maturely dissected topography. Small valleys are steep and V-shaped. Siltstone and chert form discontinuous ledges on hillsides.

Hydrology
Wells in lowland areas close to streams produce enough water for a domestic supply and may produce more than 5 gallons per minute from solution openings. Most wells obtain water from perched or semiperched water bodies supported by discontinuous shale layers, and many are dry during late summer and fall. Minor spring horizons occur throughout the formation. Flows are as much as 30 gallons per minute, but most springs go dry in late summer or fall. Where shale layers are conspicuous, most wells are inadequate for domestic use. Where chert layers are thick and extensive in area, yields of more than 5 gallons per minute may be obtained.

Borden Formation (MDbb)
Topography
The Borden forms the main part of Mississippian escarpment, ridges, and knobs. Shale forms dissected slopes, massive siltstone forms cliffs, and limestone forms ledges on shale slopes.

Hydrology
The Borden yields 100 to 500 gallons per day to wells in valley bottoms. It may yield more than 500 gallons per day to drilled wells in broad valley bottoms from fractured sandy rocks near streams. It yields almost no water to wells on hills. Water from wells drilled below stream level may contain salt, sulfate, or iron less than 100 feet below the level of the principal valley bottoms. Water from dug wells and small springs is soft and has a low dissolved solids content Water from shale is soft; from the siltstone, hard; and from the limestone, very hard. Because much of this formation is soft and silty, it has been well suited to the construction of dug wells in the past; such wells generally produce less than 500 gallons per day and often go dry in late summer and fall.

Chattanooga Shale (MDnb)
Topography
Chattanooga Shale forms steep slopes near the base of the Cumberland Escarpment and "knobs." It underlies small round hills (knobs) near the base of the escarpment. Resistant layers in the Chattanooga form small discontinuous ledges and minor waterfalls in streams.

Hydrology
The shale yields little or no water to wells. Seepage springs are present at numerous horizons, but most go dry during late summer and fall.

Laurel and Brassfield Dolomites, Osgood Formation (Slb)
Topography
Dolomite beds form resistant ledges on valley sides.

Hydrology
These rocks yield small quantities of water to wells near the Cumberland River.

Cumberland Formation, Leipers Limestone, Catheys Formation (Ocl)
Topography
These formations create moderate to steep slopes and bluffs near the Cumberland River. Limestone layers, interbedded with shales, form discontinuous ledges along hillsides in some areas.

Hydrology
In lowland areas bordering large streams these formations yield enough water for a domestic supply (more than 500 gallons per day). Elsewhere, they yield little water to wells, and small quantities of water to springs. Deep wells generally yield sulfurous water or brines.

The U.S. Geological Survey's Hydrologic Atlas Series, published cooperatively with the Kentucky Geological Survey, provides hydrologic information for the entire state.

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