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Byron Center, Michigan

Well Drillers Near Byron Center, Michigan

Byron Center area wells typically encounter a sequence of surface clay, sand & gravel, deeper clay or clayey gravel, and then consolidated bedrock formations (often limestone/shale/sandstone) with the most productive residential aquifers found within coarse sand & gravel zones at 60–110 ft, and deeper bedrock or sandstone aquifers below 150 ft for high capacity or municipal yields.

Showing contractors within 60 miles of Byron Center. 96 results found.

Typical depth
90 ft
Water table
35 ft
Contractors
96

96 Contractors

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Jr Water Well Drilling

Grand Rapids, MI 49509
Well DrillingPump InstallationWell Maintenance
Kelley Dewatering and Construction Co logo

Kelley Dewatering and Construction Co

Active Driller
Wyoming, MI 49548-5655
Dewatering Wells
Midwest Geothermal LLC logo

Midwest Geothermal LLC

Active Driller
Grand Rapids, MI 49548-7522
Closed Loop SystemsVertical Loop InstallationHorizontal Loop Installation+3 more

Plumb Drilling Co

Byron Center, MI 49315
Well DrillingPump InstallationWell Maintenance
Straight Line Directional Drilling and GeoThermal logo

Straight Line Directional Drilling and GeoThermal

Grandville, MI 49426
Water Line InstallationService Line InstallationClosed Loop Systems+7 more
Well and Septic Guys logo

Well and Septic Guys

3.4 (5)
Grand Rapids, MI 49508
Well InspectionWater TestingWater Sampling
Bayes Water Treatment logo

Bayes Water Treatment

5.0 (5)
Sparta, MI 49345
Well DisinfectionWater TestingFiltration+2 more

Bob Wahlfield Drilling

Sparta, MI 49345
Residential Well DrillingCommercial Well DrillingPump Installation+3 more
Buer Well Drilling logo

Buer Well Drilling

Active Driller
Caledonia, MI 49316
Well DrillingWell Maintenance
De Wind Wells & De Watering logo

De Wind Wells & De Watering

2.4 (5)
Zeeland, MI 49464
Well DrillingEmergency Water ServicesAgricultural Irrigation Wells+3 more
Dewind Water Well Service logo

Dewind Water Well Service

Zeeland, MI 49464
Well DrillingResidential Well DrillingCommercial Well Drilling+16 more
EDAC Drilling Co logo

EDAC Drilling Co

Holland, MI 49424
Air RotaryMud RotaryHollow Stem Auger+4 more

Great Lakes Drilling Co

Active Driller
Allegan, MI 49010
Well Drilling
Koops Well Drilling Inc. logo

Koops Well Drilling Inc.

Active Driller
Holland, MI 49423
Well DrillingWell Maintenance
Kraai Well Drilling & Water Softening logo

Kraai Well Drilling & Water Softening

Active Driller
Shelbyville, MI 49344
Well DrillingPump ServicesPump Repair+2 more
Mateco Drilling Co logo

Mateco Drilling Co

5.0 (2)
Grand Rapids, MI 49505
Sonic DrillingMonitoring WellsGeotechnical
Mateco Drilling Company logo

Mateco Drilling Company

Rockford, MI 49341-7828
Hollow Stem AugerDirect Push / GeoprobeSonic Drilling+3 more
Raymer Water Wells logo

Raymer Water Wells

Active Driller
Marne, MI 49435
Residential Well DrillingMunicipal Well DrillingIndustrial Well Drilling+14 more
Rosendall Well Drilling logo

Rosendall Well Drilling

Active Driller
Grand Rapids, MI 49525
Well DrillingWell MaintenanceWell Inspection+3 more

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View Local Geology Report

A geological estimate for the Byron Center area.

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

Detailed Summary

A representative geological cross-section for the Byron Center region, based on synthesis of well logs, indicates a surface layer of clay or sandy clay (3–24 ft), followed by alternating sand, gravel, and clay layers. Statistically, a significant sand & gravel aquifer is encountered between 20–70 ft, sometimes bounded above and below by blue or red clay (impervious layers identified by some drillers). Deeper zones typically transition to consolidated strata such as limestone with shale (often blue), then Marshall Sandstone or similar bedrock formations below approximately 170–215 ft. Most residential wells target the upper sand & gravel aquifers at 60–110 ft for reliable yields (5–15+ GPM), while high-capacity or long-term supplies locally extend casings through clay into consolidated or sandstone beds below 180 ft. Static water levels generally fall between 11–54 ft below grade. Rotary (mud) is the most common drilling method, and bentonite or cement grouts are frequently used for sealing.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
03 ftTopsoil/Red or Sandy ClaySurface topsoil and sandy or red clay; sometimes weathered or mixed.Color: Brown, Red, or Gray
Hardness: Soft
318 ftClay (occasionally blue or mixed sandy clay)Plastic or firm clay layer; commonly blue, gray, or mottled; local minor sand lenses.Color: Blue/Gray
Hardness: Firm
1830 ftSand and GravelMixed sand and gravel aquifer; major water-bearing unit.Color: Tan to Gray
Hardness: Loose
3046 ftClay (potentially blue/gray with some gravel inclusions)Thicker clay; strong aquitard; sometimes interbedded with thin sands or gravels.Color: Blue/Gray
Hardness: Firm
4667 ftSand/Sand & Gravel (coarse/gritty/cobbley zones possible)Highly productive sand, coarse gravel, and stone mix; primary aquifer for residential wells.Color: Tan to Light Gray
Hardness: Loose/Medium
67116 ftClay & Gravel (often blue/gray); minor consolidated materialMixed impervious clay layers with interbedded gravel or occasional stone/consolidated sections.Color: Blue, Gray, Brown
Hardness: Firm/Medium
116180 ftLimestone/Shale (blue) with minor sand; base of surficial aquiferTransition to consolidated limestone and shale, sometimes with thin sand seams. Water may be found in fracture zones.Color: Blue/Gray
Hardness: Hard
180215 ftSandstone (Marshall Sandstone or similar)Thick massive or bedded sandstone. Major regional aquifer for deep or high capacity wells.Color: Tan/Gray
Hardness: Hard
215300 ftDeeper Shale/Sandstone (with possible limestone/gypsum breaks)Lower consolidated bedrock sequence; yields significant flows for high capacity or industrial wells if penetrated.Color: Gray/Dark Gray
Hardness: Very Hard

Frequently Asked Questions

A typical residential well in the Byron Center 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 35 feet below the surface in this region.

A representative geological cross-section for the Byron Center region, based on synthesis of well logs, indicates a surface layer of clay or sandy clay (3–24 ft), followed by alternating sand, gravel, and clay layers. Statistically, a significant sand & gravel aquifer is encountered between 20–70 ft, sometimes bounded above and below by blue or red clay (impervious layers identified by some drillers). Deeper zones typically transition to consolidated strata such as limestone with shale (often blue), then Marshall Sandstone or similar bedrock formations below approximately 170–215 ft. Most residential wells target the upper sand & gravel aquifers at 60–110 ft for reliable yields (5–15+ GPM), while high-capacity or long-term supplies locally extend casings through clay into consolidated or sandstone beds below 180 ft. Static water levels generally fall between 11–54 ft below grade. Rotary (mud) is the most common drilling method, and bentonite or cement grouts are frequently used for sealing.