Well Drillers Near Brussels, Wisconsin

A typical residential well in the Brussels area is drilled to approximately 200 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 40 feet below the surface in this region.

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.