Chat with us, powered by LiveChat
NewSee the ground in 3DLook
Comstock Park, Michigan

Well Drillers Near Comstock Park, Michigan

Comstock Park area wells typically encounter alternating layers of clay and sand/sand & gravel, with minor gravelly or stony intervals, to average depths between 100 and 150 feet, with water-bearing sands commonly found from 60 to 145 feet.

Showing contractors within 60 miles of Comstock Park. 81 results found.

Typical depth
120 ft
Water table
35 ft
Contractors
81

81 Contractors

Sort by:

Browse all of Michigan

See every licensed contractor across Michigan.

← All Michigan contractors

Well records near Comstock Park

Check depths and logs of existing wells in the area before you drill.

Open well map →

Michigan well owner guide

Costs, permits, maintenance tips for private wells in Michigan.

Open guide →

Nearby Michigan city directories

Not in Comstock Park? Search well drilling near me in the national directory, or find well service and repair near me and well pump service near me for work on an existing well.

View Local Geology Report

A geological estimate for the Comstock Park area.

Typical Well Depth
120 ft
Static Water Level
35 ft
Recommended Method
Rotary - Mud Circulation

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

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 5 ftSand/Sand & ClayFine surficial sand or sandy-clayey loam, occasional stonesColor: Light brown to gray
Hardness: Loosely consolidated
5 – 60 ftClay (with stones/gravel layers)Hard to firm gray or brown clay, may contain stones/gravel layers or lenses, occasional silty intervalsColor: Gray to reddish-brown
Hardness: Hard to compact
60 – 90 ftSand/Silty Sand/Sand & GravelMedium to coarse sand, locally silty with gravel inclusions, water bearingColor: Tan to gray
Hardness: Loose to medium compact
90 – 145 ftSand & Gravel / Coarse SandCoarse sand and gravel, principal aquifer zone, high permeability, frequent well screens hereColor: Variegated gray/yellow
Hardness: Loose to moderate
145 – 160 ftClay/Sandy Clay (local)Clay, sandy clay, or clay with gravel, less frequent and may locally be absentColor: Gray to brown
Hardness: Compact

Frequently Asked Questions

A typical residential well in the Comstock Park area is drilled to approximately 120 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 35 feet below the surface in this region.

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.