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Brooklyn, Wisconsin

Well Drillers Near Brooklyn, Wisconsin

Brooklyn area wells typically penetrate a sequence of surficial clay or fill, followed by alternating sand/gravel and clay layers, then transition into limestone/dolomite and/or sandstone bedrock. Bedrock is generally encountered between 80-130 ft, and wells commonly terminate in sandstone or limestone/dolomite at depths of 120-250+ ft.

Showing contractors within 60 miles of Brooklyn. 75 results found.

Typical depth
140 ft
Water table
45 ft
Contractors
75

75 Contractors

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View Local Geology Report

A geological estimate for the Brooklyn area.

Typical Well Depth
140 ft
Static Water Level
45 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on surveyed well logs, the generalized subsurface profile for the Brooklyn region (Dane/Rock counties, WI) consists of a surficial clay or fill layer (often 4-12 ft thick), underlain by sand and gravel (variable thickness commonly 10-60+ ft), sometimes interbedded with clay lenses. Below these unconsolidated sediments, wells typically encounter limestone/dolomite between ~40-130 ft (often with a shaly or sandy component), frequently grading into sandstone bedrock (sometimes alternating with dolomite/limestone) to final well depths of 125-258 ft. Static water levels are most often between 15-60 ft below surface, with residential wells to 120-150 ft and high-capacity/hicap wells ranging deeper but generally under 250 ft. Rotary mud circulation is the standard drilling method, with casing/grouting extending at least to bedrock or 110-180 ft.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 4 ftClay/FillSurface fill, silty or clayey, sometimes with topsoil or weathered textureColor: Brown/tan/gray
Hardness: Soft
4 – 14 ftClay/Silt/GravelCombination of clay, silt, and local gravel inclusionsColor: Brown/gray
Hardness: Soft-medium
14 – 65 ftSand and Gravel (Unconsolidated Aquifer)Sand and gravel, sometimes in two or more layers, variably sorted, may locally include additional clay lensesColor: Variegated, tan, brown, white
Hardness: Loose-Soft
65 – 110 ftClay/Gravel and/or Additional SandMixed clay and gravel and/or thick coarse sand aquifer, may contain lenses or transitions of clayColor: Gray/tan
Hardness: Variable
110 – 132 ftLimestone/DolomiteLimestone or dolomite, sometimes shaly, may be partly sandy; marks start of consolidated bedrockColor: Tan/brown/gray/white
Hardness: Hard/Firm
132 – 208 ftSandstone (with interbedded limestone/dolomite possible)Sandstone, often hard/firm, locally with interbeds of limestone/dolomite or shaly zonesColor: Tan/white
Hardness: Hard
208 – 244 ftSandstone, Sandy Dolomite/LimestoneFine to medium sandstone, may be sandy dolomite or limestone at base, bedrock aquiferColor: White/tan/brown
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Brooklyn area is drilled to approximately 140 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 45 feet below the surface in this region.

Based on surveyed well logs, the generalized subsurface profile for the Brooklyn region (Dane/Rock counties, WI) consists of a surficial clay or fill layer (often 4-12 ft thick), underlain by sand and gravel (variable thickness commonly 10-60+ ft), sometimes interbedded with clay lenses. Below these unconsolidated sediments, wells typically encounter limestone/dolomite between ~40-130 ft (often with a shaly or sandy component), frequently grading into sandstone bedrock (sometimes alternating with dolomite/limestone) to final well depths of 125-258 ft. Static water levels are most often between 15-60 ft below surface, with residential wells to 120-150 ft and high-capacity/hicap wells ranging deeper but generally under 250 ft. Rotary mud circulation is the standard drilling method, with casing/grouting extending at least to bedrock or 110-180 ft.