Groundwater Availability
 

Alluvium (Qa)
Topography
The alluvium forms narrow floodplains and underlies terraces. At least one well-developed terrace is present along the principal streams of the region.

Hydrology
The alluvium yields more than 100 gallons per day to most dug wells. Where sandy material is present and saturated thickness great enough, the alluvium may yield more than 500 gallons per day to screened drilled wells.

Breathitt Group (Pbl, Pbm) (Four Corners Formation, Hyden Formation, Pikeville Formation)
Topography
The Breathitt Group underlies the valleys and forms the hills. Tops of hills and ridges commonly are capped by sandstone. Shales form wide valleys and moderate or gentle slopes on hills.

Hydrology
The Breathitt yields more than 500 gallons per day to almost half of the wells drilled in valley bottoms and more than 100 gallons per day to about half the wells drilled on hillsides and on ridges. Sandstones yield water to most wells. Shales also yield water to many wells, and coal yields water to a few. Near-vertical joints and openings along bedding planes yield most of the water to wells. Waters are highly variable in chemical character.

Grundy, Alvy Creek Formations (contains Lee-type quartzose sandstones of the former Lee Formation) (Plc, Plr)
Topography
Thick, resistant sandstones of the Grundy underlie an extensive upland in McCreary County.

Hydrology
Generally, the Grundy yields more than 500 gallons per day to about three-quarters of the wells drilled in valley bottoms and lowland areas bordering streams and on hillsides. About half the wells on hilltops yield more than 500 gallons per day. Deep wells that penetrate fractures produce enough for a domestic supply and sometimes yield as much as 5 gallons per minute. Deep wells penetrating the entire thickness of thick sandstone units in excess of 500 feet may yield enough water for small municipal or industrial supplies. Sandstone is the principal aquifer, but shale yields water to some wells and coal to a few. Joints and openings along bedding planes, best developed in sandstones, supply most of the water to wells. Waters are generally soft or moderately hard and contain noticeable amounts of iron.

Paragon Formation (Mpk)
Topography
The Paragon forms moderate slopes beneath outcrops of massive sandstone units of the Grundy Formation.

Hydrology
The Paragon yields little or no water to wells.

Bangor Limestone, Hartselle Formation, Kidder Limestone (Chesterian Limestones) (Mpk)
Topography
The limestones form steep hillsides or underlie broad rolling karst areas and dissected uplands.

Hydrology
The limestones yield more than 500 gallons per day from solution openings. Some wells produce more than 5 gallons per minute from large solution openings. Near outcrop areas, particularly near major escarpments, yields generally are inadequate during dry periods.

Ste. Genevieve Limestone (Mgl)
Topography
The Ste. Genevieve underlies valleys.

Hydrology
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 the contact with the underlying St. Louis Limestone.

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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