Well Drillers Near Shell Lake, Wisconsin

A geological estimate for the Shell Lake area.

Detailed Summary

Based on multiple well logs within the Shell Lake region, the representative geological profile consists predominantly of stratified glacial drift materials. From the surface, wells most often penetrate a thick sequence of sand, sand/gravel, and minor clay layers, occasionally interbedded with silty or stony zones. The most productive water-bearing zones are within coarse sand and gravel lenses, often between approximately 50 to 160 feet below ground surface. Wells are usually cased through the sediment column to isolate these aquifers, which provide typical residential yields (5–15+ GPM), and sometimes higher for large-diameter or deeper installations. Static water levels fluctuate from approximately 12 to 103 feet below ground depending on local hydrogeology and recent precipitation, but are most commonly in the 20–65 foot range.

Expected Geological Layers