Well Drillers Near Ray Twp, Michigan

A geological estimate for the Ray Twp area.

Detailed Summary

Synthesizing multiple well logs from Ray Township and adjacent areas in Macomb County, the region exhibits a predictable glacially derived sequence. The most common layers begin with a thin topsoil, then brown or gray clay, often interbedded with sand, gravel, or stones. Thick continuous clay (sometimes called 'hardpan' or 'gray clay') is typical, with intervals of sand, sand/gravel, or gritty layers indicating aquifer materials. Water is most consistently produced near the base of the clay sequence in sand or sand/gravel intervals, commonly found between 40 and 80 ft. Well construction usually involves PVC or steel casing set through clay and into the upper sand/gravel aquifer. Static water levels are typically within 3–30 ft. of ground surface. Deeper, higher-yield or high-capacity wells may penetrate up to ~180–220 ft. to reach thicker, deeper sand/gravel units where present.

Expected Geological Layers