Well Drillers Near Highland, Michigan

A geological estimate for the Highland area.

Detailed Summary

The most representative geological profile for the Highland area consists of a surficial brown/yellow sand or sand with gravel, underlain by alternating layers of clay (gray, blue, or sometimes with stones/silt), and again by water-bearing sand or sand/gravel at depth. Clay layers commonly separate upper and lower sand/gravel zones. Most wells encounter the main water-bearing, high-yield (often 10–20 GPM+) sand or sand/gravel formation beneath 60–100 ft. Residential wells typically target these deeper aquifers, avoiding locally thin surficial sands. A typical residential well depth ranges from 70 to 120 ft, with high-capacity (municipal/irrigation) wells potentially going to 120—180 ft+ if needed by local hydrogeology. The static water level is variable but often between 20 and 65 ft below grade, occasionally artesian.

Expected Geological Layers