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Chase, Michigan

Well Drillers Near Chase, Michigan

A typical well in the Chase area is completed to a depth of 70-80 ft for residential supply and penetrates unconsolidated glacial deposits dominated by sequences of sand, interbedded clays, and minor gravel, with static water levels averaging 25-40 ft below ground.

Showing contractors within 60 miles of Chase. 252 results found.

Typical depth
75 ft
Water table
30 ft
Contractors
252

252 Contractors

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View Local Geology Report

A geological estimate for the Chase area.

Typical Well Depth
75 ft
Static Water Level
30 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Synthesizing data from representative well logs in the Chase region, the typical geological sequence encountered comprises an upper sand layer (20-35 ft), followed by significant clay or mixed clay-sand (20-50+ ft), and capped by water-bearing sand or sand/gravel layers at depth. Occasional variations exist (notably thicker clay in some local wells or coarser basal material), but this sequence is regionally consistent. The majority of residential wells (5–15+ GPM) are constructed to 70–80 ft depths, which reliably intercept the water-bearing sand at the base of these profiles. High-capacity wells may be drilled deeper (120–150 ft) to target thicker and sometimes multiple sand units. Static water level is most often about 25–40 ft below surface, with rotary methods and PVC casing the prevailing construction approach; cement or bentonite grout is standard to the base of casing (~60–70 ft).

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 30 ftSand (occasionally minor silt)Fine to medium brown sand, clean, unconsolidated, locally minor silt.Color: Brown/tan
Hardness: Loose
30 – 60 ftClay (locally mixed with sand)Gray or blue clay, sometimes mixed with layers of fine sand, plastic, low permeability.Color: Gray/blue
Hardness: Firm–plastic
60 – 75 ftSand (water-bearing, may include minor gravel)Medium to coarse sand, locally with fine gravel, saturated, primary aquifer zone.Color: Tan/yellow
Hardness: Loose
75 – 135 ftInterbedded Sand and ClayAlternating layers of sand (water-bearing) and clay, typical below main residential aquifer, more variable, only present in deeper/high-capacity wells.Color: Mixed tan (sand)/gray (clay)
Hardness: Varies

Frequently Asked Questions

A typical residential well in the Chase area is drilled to approximately 75 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 30 feet below the surface in this region.

Synthesizing data from representative well logs in the Chase region, the typical geological sequence encountered comprises an upper sand layer (20-35 ft), followed by significant clay or mixed clay-sand (20-50+ ft), and capped by water-bearing sand or sand/gravel layers at depth. Occasional variations exist (notably thicker clay in some local wells or coarser basal material), but this sequence is regionally consistent. The majority of residential wells (5–15+ GPM) are constructed to 70–80 ft depths, which reliably intercept the water-bearing sand at the base of these profiles. High-capacity wells may be drilled deeper (120–150 ft) to target thicker and sometimes multiple sand units. Static water level is most often about 25–40 ft below surface, with rotary methods and PVC casing the prevailing construction approach; cement or bentonite grout is standard to the base of casing (~60–70 ft).