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Edgerton, Wisconsin

Well Drillers Near Edgerton, Wisconsin

The typical geological profile in the Edgerton region consists of a thick sequence of sand and gravel extending from the surface, generally underlain by clay or silty gravel layers, and in deeper areas, glacial deposits transition into limestone and then sandstone bedrock. Most private residential wells are screened in the sand and gravel (surficial aquifer) or the upper sandstone, with a typical residential well depth around 80-100 feet and high capacity wells extending into the sandstone and limestone below 120 feet.

Showing contractors within 60 miles of Edgerton. 94 results found.

Typical depth
85 ft
Water table
18 ft
Contractors
94

94 Contractors

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View Local Geology Report

A geological estimate for the Edgerton area.

Typical Well Depth
85 ft
Static Water Level
18 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Geological data from a representative sample of Edgerton and surrounding area wells indicates the most common layer sequence starts with sand and gravel from the surface (extending typically 40-80+ ft), occasionally interrupted or underlain by clay or clayey gravel. In high-capacity or older wells, the sequence continues to limestone (avg. 130-160 ft) and sandstone (below ~130 ft, anchoring wells to about 180-210 ft in the deepest cases). The median static water level ranges from 10-30 ft below grade. Most domestic wells target the sand/gravel aquifer or the top of the sandstone for sustainable high yields (15-35 GPM commonly reported). Standard casing extends to the bottom of the unconsolidated drift or just into the bedrock, with grout (cement or bentonite) typically placed to at least casing depth.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 60 ftSand & GravelCoarse to medium sand and gravel, occasional stones, tan/brown color, may be interbedded with minor clay or silt lenses.Color: Tan/Brown
Hardness: Loose to medium
60 – 75 ftClay/Clayey Gravel/Silty GravelGray or brown clay, occasionally with gravel or silty material, acts as an aquitard in some locations.Color: Gray/Brown
Hardness: Hard to sticky
75 – 91 ftGravel/Sand & StonesClean gravel and sand, possible large stones, transition to coarser material near base of unconsolidated section.Color: Mixed/Grey
Hardness: Medium to hard
91 – 130 ftClay or Silt (locally present, may be thin or absent)Dense gray or brown clay; sometimes silty, sometimes absent; where present can vary 5-15 ft thick.Color: Gray/Brown
Hardness: Hard
130 – 160 ftLimestone/DolomiteHard, gray limestone or dolomite bedrock; upper few feet may be fractured or shaly.Color: Gray
Hardness: Hard
160 – 210 ftSandstoneSoft to firm, water-bearing sandstone; color from buff to reddish, high porosity; continues beyond 180 ft in deeper wells.Color: Buff/Reddish
Hardness: Soft to medium

Frequently Asked Questions

A typical residential well in the Edgerton area is drilled to approximately 85 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 18 feet below the surface in this region.

Geological data from a representative sample of Edgerton and surrounding area wells indicates the most common layer sequence starts with sand and gravel from the surface (extending typically 40-80+ ft), occasionally interrupted or underlain by clay or clayey gravel. In high-capacity or older wells, the sequence continues to limestone (avg. 130-160 ft) and sandstone (below ~130 ft, anchoring wells to about 180-210 ft in the deepest cases). The median static water level ranges from 10-30 ft below grade. Most domestic wells target the sand/gravel aquifer or the top of the sandstone for sustainable high yields (15-35 GPM commonly reported). Standard casing extends to the bottom of the unconsolidated drift or just into the bedrock, with grout (cement or bentonite) typically placed to at least casing depth.