Well Drillers Near Brooklyn, Wisconsin

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.