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Free Soil, Michigan

Well Drillers Near Free Soil, Michigan

The representative geological profile for the Free Soil, MI region typically consists of an upper clay or clayey sand unit transitioning to thick sequences of sand, interbedded occasionally with gravel or thin lenses of clay. Most residential wells are completed within coarse to medium sand units at depths of 60-100 ft.

Showing contractors within 60 miles of Free Soil. 251 results found.

Typical depth
90 ft
Water table
22 ft
Contractors
251

251 Contractors

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Brighton Drilling Co

Active Driller5.0 (12)
Brighton, MI 48114
Residential Well DrillingCommercial Well DrillingPump Services+5 more

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View Local Geology Report

A geological estimate for the Free Soil area.

Typical Well Depth
90 ft
Static Water Level
22 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Well logs across the Free Soil area consistently reveal surficial deposits of clay, red clay, or clayey hardpan, usually 10-52 ft thick. Beneath the clay, the predominant sequence is coarse or medium sand—often in multiple horizons—sometimes interbedded with gravel, gray clay, or sandy/gravelly mixtures. Water-bearing sand zones are well-developed and generally begin below 40-60 ft, continuing to terminal depths of 75–110 ft. Static water levels tend to be shallow (10-35 ft) with residential wells producing 5–22+ GPM at completion depths of 60–100 ft. Typical well completions include PVC or steel casing to 50–90 ft, screens set in the basal sand units, and bentonite slurry grout.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 20 ftClay (occasional clayey sand or hardpan in places)Red to gray clay, sometimes with minor sand; locally includes hardpan or minor gravel.Color: Red/Gray
Hardness: Firm-Plastic
20 – 60 ftSand (Coarse/Medium, sometimes with minor gravel or clay intermixed)Predominantly medium to coarse sand with occasional gravel or thin clay layers; zones are generally water bearing.Color: Tan/Gray
Hardness: Loose-Friable
60 – 100 ftSand & Gravel (variable, main aquifer zone)Coarse sand with gravel layers; main water-bearing formation; some interbeds of silty or clayey sand possible.Color: Tan/Gray
Hardness: Loose
100 – 110 ftClay/Clay with Sand/Gravel (local basal confining unit)Gray clay, clay & sand, or clay & gravel acting as low permeability boundary in some logs.Color: Gray
Hardness: Stiff

Frequently Asked Questions

A typical residential well in the Free Soil area is drilled to approximately 90 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 22 feet below the surface in this region.

Well logs across the Free Soil area consistently reveal surficial deposits of clay, red clay, or clayey hardpan, usually 10-52 ft thick. Beneath the clay, the predominant sequence is coarse or medium sand—often in multiple horizons—sometimes interbedded with gravel, gray clay, or sandy/gravelly mixtures. Water-bearing sand zones are well-developed and generally begin below 40-60 ft, continuing to terminal depths of 75–110 ft. Static water levels tend to be shallow (10-35 ft) with residential wells producing 5–22+ GPM at completion depths of 60–100 ft. Typical well completions include PVC or steel casing to 50–90 ft, screens set in the basal sand units, and bentonite slurry grout.