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Kansasville, Wisconsin

Well Drillers Near Kansasville, Wisconsin

The representative geological profile for the Kansasville region consists of surface soil/clay, a thick interbedded clay/hardpan sequence, overlying sand and/or sand & gravel, with limestone or dolomite bedrock present at greater depths in certain areas. The most productive residential wells are completed in thick sand & gravel or shallow fractured rock, typically at 120-180 ft depth.

Showing contractors within 60 miles of Kansasville. 102 results found.

Typical depth
150 ft
Water table
55 ft
Contractors
102

102 Contractors

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E.G. Aschauer & Sons Inc

Kansasville, WI 53139
(262) 534-2788
Well DrillingPump ServicesWell Maintenance

Egofske Porter Drilling Inc

5.0 (1)
Mukwonago, WI 53149
(262) 363-7395
Well Drilling

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View Local Geology Report

A geological estimate for the Kansasville area.

Typical Well Depth
150 ft
Static Water Level
55 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on synthesis of multiple well logs across the Kansasville and surrounding Racine/Kenosha areas, the most typical stratigraphy consists of (1) a thin topsoil or organic layer, (2) a thick clay unit (often subdivided by color and consistency; blue, gray, yellow, sometimes with hardpan), (3) variable but regionally persistent sand and gravel aquifer, and in some wells, (4) fractured limestone or dolomite at depth. Productive residential wells (capable of 5-15+ GPM) are consistently finished in either the thicker sand & gravel zone or, for deeper completions, the upper portion of limestone. Static water levels are most commonly recorded between 30-80 ft below surface. Typical total well depths are 120-180 ft for sand/gravel, but may reach 200-345 ft if completed in bedrock.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 2 ftTopsoil/OrganicThin surface soil or organic material. Occasionally reported as dark or organic-rich.Color: Dark/Brown
Hardness: Soft
2 – 25 ftClay (Yellow/Brown/Tan)Generally yellow, brown, or tan clay. Commonly soft to firm, locally contains silt or a minor hardpan.Color: Yellow/Brown/Tan
Hardness: Firm
25 – 120 ftClay (Blue/Gray, often with Hardpan/Stoney)Thick, blue or gray clay, often described as stoney or interbedded with hardpan at zones (often near 40-60 ft and/or 120-140 ft). Major confining unit, locally with some silty sand/silt.Color: Blue/Gray
Hardness: Firm/Hard
120 – 135 ftHardpan/Clayey HardpanClayey hardpan, often gray or consolidated; occasionally alternating with thin clay lenses.Color: Gray/Tan
Hardness: Hard
135 – 180 ftSand & GravelCoarse sand, gravel, and locally some pea gravel or minor cobbles. Principle aquifer; highly productive, often with rapid water inflow.Color: Varies (Tan/Gray/Yellow)
Hardness: Loose/Unconsolidated
180 – 200 ftClay with Gravel Lenses / InterbedsIn some wells, thin clay or intermixed clay and gravel lenses. May not be continuous regionally.Color: Gray/Brown
Hardness: Firm/Loose
200 – 300 ftLimestone/DolomiteFractured and hard limestone or dolomite, often called Niagara or Silurian dolomite regionally. May include thin zones of broken rock/gravel at top contact.Color: Light Gray/Tan
Hardness: Very Hard

Frequently Asked Questions

A typical residential well in the Kansasville area is drilled to approximately 150 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 55 feet below the surface in this region.

Based on synthesis of multiple well logs across the Kansasville and surrounding Racine/Kenosha areas, the most typical stratigraphy consists of (1) a thin topsoil or organic layer, (2) a thick clay unit (often subdivided by color and consistency; blue, gray, yellow, sometimes with hardpan), (3) variable but regionally persistent sand and gravel aquifer, and in some wells, (4) fractured limestone or dolomite at depth. Productive residential wells (capable of 5-15+ GPM) are consistently finished in either the thicker sand & gravel zone or, for deeper completions, the upper portion of limestone. Static water levels are most commonly recorded between 30-80 ft below surface. Typical total well depths are 120-180 ft for sand/gravel, but may reach 200-345 ft if completed in bedrock.