Well Drillers Near Comstock Park, Michigan

A geological estimate for the Comstock Park area.

Detailed Summary

Based on a synthesis of the sampled well logs from the Comstock Park and immediate region, the representative geological profile is characterized by initial surficial sand or sandy-clayey material (0-5 ft), underlain by thick sections of clay with subordinate inclusions of stones or gravel (5-60 ft). These are typically followed by a series of sand, sand with gravel, or sandy/gravelly clay units (60-145 ft), with the principal water-bearing zone (moderate to high-yield) encountered from about 90 to 145 ft below grade. Occasional deeper clay and sand/gravel/clay units may occur, but most residential wells are completed within the upper 100-150 ft. Wells yielding 5-20+ GPM are frequently reported when completed in these sand or sand/gravel zones.

Expected Geological Layers