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Whitelaw, Wisconsin

Well Drillers Near Whitelaw, Wisconsin

Typical Whitelaw/Manitowoc area geology consists of a sequence of topsoil or hardpan over sand, overlain by thick clay, and underlain by limestone bedrock. Limestone is the common aquifer for residential wells.

Showing contractors within 60 miles of Whitelaw. 65 results found.

Typical depth
130 ft
Water table
30 ft
Contractors
65

65 Contractors

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View Local Geology Report

A geological estimate for the Whitelaw area.

Typical Well Depth
130 ft
Static Water Level
30 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Across representative well construction logs in the Whitelaw and broader Manitowoc region, the prevailing geological profile from ground surface to typical well depth is: a thin surficial layer (topsoil, hardpan, or gravelly sand); a substantial sand layer (sometimes gravelly); a thick clay (often red, blue, or sandy); and then a transition to limestone bedrock, which forms the main water-producing zone. Some variability in clay color/composition and presence of gravel/sand is present, but the most persistent sequence is sand over clay over limestone. Residential wells commonly terminate in or just below the limestone, with high yield (5–15+ GPM) at depths between 100–150 feet. High capacity wells may extend deeper depending on bedrock characteristics.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 3 ftTopsoil/Hardpan/Sand & GravelThin surficial material—topsoil, hardpan or gravel/sand, sometimes with boulders.Color: Brown/Gray/Yellow
Hardness: Soft to Firm
3 – 20 ftSand (or Sand & Gravel)Coarse sand, sometimes with gravel or boulders; occasional water-bearing.Color: Yellow to Brown
Hardness: Loose to Medium
20 – 90 ftClay (Red, Blue, or Sandy)Thick, predominantly red, blue, or sandy clay sequence, occasionally with sand seams or gravel inclusions.Color: Red, Blue, or Gray
Hardness: Firm to Stiff
90 – 130 ftTransition: Sandy Clay/Hardpan/GravelLocalized layer, often a denser clay, hardpan, or gravel, transitional into bedrock. Sometimes contains sand seams or voids.Color: Gray to Brown
Hardness: Hard
130 – 200 ftLimestone BedrockMassive limestone bedrock, sometimes fractured or containing sand-filled caves; main aquifer for domestic use.Color: Gray
Hardness: Very Hard

Frequently Asked Questions

A typical residential well in the Whitelaw area is drilled to approximately 130 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 30 feet below the surface in this region.

Across representative well construction logs in the Whitelaw and broader Manitowoc region, the prevailing geological profile from ground surface to typical well depth is: a thin surficial layer (topsoil, hardpan, or gravelly sand); a substantial sand layer (sometimes gravelly); a thick clay (often red, blue, or sandy); and then a transition to limestone bedrock, which forms the main water-producing zone. Some variability in clay color/composition and presence of gravel/sand is present, but the most persistent sequence is sand over clay over limestone. Residential wells commonly terminate in or just below the limestone, with high yield (5–15+ GPM) at depths between 100–150 feet. High capacity wells may extend deeper depending on bedrock characteristics.