Well Drillers Near Akron, Michigan

A typical residential well in the Akron area is drilled to approximately 180 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 35 feet below the surface in this region.

The representative subsurface geology for the Akron, MI region consists of an uppermost sequence of glacial clays (sometimes with sand or gravel lenses), generally extending to 70–145 ft below grade. This is followed by thick bedrock sequences dominated by shale, which are commonly interlayered with thinner sandstone and occasional limestone beds. Productive residential wells usually draw from bedrock sandstone aquifers below 140 ft, with strong yields (10–35+ GPM typical). Static water levels commonly range from 11–60 ft below ground. Deeper, high-capacity wells for non-residential use may extend down to 260–335 ft or more, primarily into more transmissive sandstones. Outliers (e.g., very shallow bored wells) are less representative and not included in this model.