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Well Drillers Near Brussels, Wisconsin

Typical Brussels-area wells penetrate a surface layer of clay (often with some gravel or sand), underlain by a thick limestone/dolomite bedrock sequence, with occasional thin gravel or hardpan zones. Bedrock aquifers are the primary groundwater source.

Showing contractors within 60 miles of Brussels. 25 results found.

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A geological estimate for the Brussels area.

200 ft

Typical Well Depth

40 ft

Static Water Level

Rotary - Mud Circulation

Recommended Method

Detailed Summary

Based on well logs from the Brussels region and immediate surrounds, the most representative geologic sequence is a surface layer of clay (commonly 10–80 ft thick, sometimes with sand or gravel), possibly with discrete gravel/hardpan intervals. This is consistently underlain by massive limestone or dolomite that extends through the bottom of typical residential and public wells, at least down to ~310 ft where logs terminate. Static water levels average between 15 and 80 ft below grade, with most wells drawing from 150–310 ft depths. A typical residential well (5–15+ GPM) is screened or open in the limestone at ~180–250 ft, with higher capacity wells reaching ~300+ ft. Shale or other minor beds are rarely encountered and do not warrant representation in the averaged model.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
010 ftTopsoil/Clay/GravelRed to brown clay, locally with sand, gravel, or stones; non-caving in most areas.Color: Brown/Red
Hardness: Soft to Firm
1080 ftClay/Gravel/Hardpan (Variable)Firm clay, zones of gravel or occasional hardpan; color mottled brown/gray; minor local sand.Color: Brown/Gray
Hardness: Firm to Hard
80120 ftTransition Clay/Hardpan (occasional)Clay with occasional hardpan or boulders; not always present, but common in deeper overburden.Color: Gray/Brown
Hardness: Firm
80310 ftLimestone/Dolomite BedrockWhite to light gray, hard, crystalline limestone or dolomite. Primary aquifer for water supply.Color: White/Gray
Hardness: Hard