Well Drillers Near Caro, Michigan

A geological estimate for the Caro area.

Detailed Summary

Based on a synthesis of regional well logs, the Caro area typically exhibits a sequence of Quaternary glacial drift (clay, sand, and gravel layers) from surface to depths of ~100-140 ft, underlain by alternating layers of shale and sandstone. Shallower wells often terminate in coarse sand/gravel or shallow sandstone, but most high-yield or high-capacity wells penetrate deeper into fractured or porous sandstone aquifers (often at 150-220+ ft). Shale intervals are common between and above these aquifers. The most consistent sequence is surface clay transitioning through sand/gravel, then into alternating shale and sandstone. Static water levels are moderate (15-45 ft below grade). Bedrock sandstone is the principal source for large capacity yields (>10 GPM), with typical residential wells set from 100-220 ft depending on desired yield and geology at the site.

Expected Geological Layers