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Coopersville, Michigan

Well Drillers Near Coopersville, Michigan

Typical Coopersville area well geology: surficial sand/gravel over thick glacial clay, underlain by sand/gravel, with water-bearing bedrock (sandstone/Marshall formation) below ~190–200 feet.

Showing contractors within 60 miles of Coopersville. 74 results found.

Typical depth
150 ft
Water table
55 ft
Contractors
74

74 Contractors

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Raymer Water Wells logo

Raymer Water Wells

Active Driller4.8 (35)
Marne, MI 49435
Residential Well DrillingMunicipal Well DrillingIndustrial Well Drilling+14 more
Sytsma Well Drilling logo

Sytsma Well Drilling

Active Driller5.0 (11)
Allendale, MI 49401
Well DrillingResidential Well DrillingCommercial Well Drilling+4 more
Central Wells & Pumps LLC logo

Central Wells & Pumps LLC

Active Driller4.6 (46)
Muskegon, MI 49444
Residential Well DrillingCommercial Well DrillingIndustrial Well Drilling+5 more
M & J Water Wells logo

M & J Water Wells

Active Driller4.7 (18)
Casnovia, MI 49318
Well DrillingResidential Well DrillingCommercial Well Drilling+3 more
Wahlfield Drilling Co logo

Wahlfield Drilling Co

Active Driller4.4 (55)
Comstock Park, MI 49321
Residential Well DrillingLivestock Well DrillingCable Tool+8 more
Wolcott's Water Well Drilling logo

Wolcott's Water Well Drilling

Active Driller4.5 (17)
Sparta, MI 49345
Well DrillingResidential Well DrillingCommercial Well Drilling+10 more

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View Local Geology Report

A geological estimate for the Coopersville area.

Typical Well Depth
150 ft
Static Water Level
55 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on synthesis of multiple well logs from the greater Coopersville region, the typical vertical profile includes: a shallow surficial layer (sand, sand/gravel, or topsoil) between 0–15 ft, followed by a substantial glacial clay sequence (mostly gray, blue, or red clay—often laminated or with occasional gravel), extending to roughly 120–160 ft below grade. Interbedded sand and gravel intervals commonly occur within and just below the clay, frequently forming a significant sand/gravel aquifer between 110–130 ft. Bedrock (mainly sandstone, sometimes with shale) is consistently encountered below ~190–200 ft and is often noted as a productive aquifer. Most household wells achieving 10–15+ GPM water yields reach total depths of 120–200 ft, either terminating in deep sand/gravel or at the top of water-bearing sandstone.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
03 ftTopsoil/SandLoose surficial soil, sand or topsoil.Color: Brown/Yellow
Hardness: Soft
315 ftSand/GravelFine to medium sand and/or gravel, sometimes mixed with clay. Highly variable water-yield potential.Color: Brown/Yellow
Hardness: Loose
15120 ftClay (Glacial Till, mostly Gray/Blue/Red)Dense glacial clay, variably gray, blue, or red; some interlayers of gravel or silty sand. May include ~10–25% thin sand/gravel seams.Color: Gray/Blue/Red
Hardness: Stiff/Hard
120145 ftSand/GravelMedium to coarse sand and/or well-sorted gravel, locally water-bearing. Major aquifer for municipal and high-yield residential wells.Color: Gray/Tan
Hardness: Medium
145190 ftClay, Silty or with gravelDense clay with inclusions of silt or gravel; low permeability.Color: Gray/Blue
Hardness: Hard
190240 ftSandstone (Marshall Sandstone or Equivalent)Fine to medium fractured sandstone; major water-producing bedrock aquifer in the region. Sometimes interbedded with silt or minor shale.Color: Gray/Tan
Hardness: Hard
240288 ftSandstone/Shale (Bedrock)Alternating sandstone and shale layers, sometimes described as Marshall Sandstone. Yields decrease with depth.Color: Gray
Hardness: Very hard

Frequently Asked Questions

A typical residential well in the Coopersville area is drilled to approximately 150 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 55 feet below the surface in this region.

Based on synthesis of multiple well logs from the greater Coopersville region, the typical vertical profile includes: a shallow surficial layer (sand, sand/gravel, or topsoil) between 0–15 ft, followed by a substantial glacial clay sequence (mostly gray, blue, or red clay—often laminated or with occasional gravel), extending to roughly 120–160 ft below grade. Interbedded sand and gravel intervals commonly occur within and just below the clay, frequently forming a significant sand/gravel aquifer between 110–130 ft. Bedrock (mainly sandstone, sometimes with shale) is consistently encountered below ~190–200 ft and is often noted as a productive aquifer. Most household wells achieving 10–15+ GPM water yields reach total depths of 120–200 ft, either terminating in deep sand/gravel or at the top of water-bearing sandstone.