Well Drillers Near Saranac, Michigan

A geological estimate for the Saranac area.

Detailed Summary

A representative geological profile for the Saranac, MI region consists of an upper sequence of variable surficial loams, sands, and gravels (0–35 ft), followed by thick clay sections (often red, gray, or blue, sometimes interbedded with gravels and sands) extending to about 80–120 ft. Between 30–130 ft, significant intervals of water-bearing sand, sand/gravel, or fine sand are common and serve as the primary aquifer for residential and higher-capacity wells, producing 10–50+ GPM. In most cases, deeper layers return again to dense clay or hardpan, and in a minority of deeper wells, shallow bedrock (shale/sandstone) is found around 300–340 ft. Most residential wells are cased through the upper silts and clays and terminate within the main sand/gravel aquifer zone. Static water levels typically range from 13–89 ft below grade, depth depending on site and aquifer. Grouting is usually bentonite or cement from surface to at least 30 ft, using rotary or cable tool methods.

Expected Geological Layers