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Ray Twp, Michigan

Well Drillers Near Ray Twp, Michigan

The representative geological profile for Ray Township, Macomb County, MI, consists of surficial clay (often with some sand or gravel), underlain by thick sequences of gray or mixed clay, grading to glacially derived sands and gravels near the base. Residential wells typically target water-bearing sands or sand-and-gravel layers between ~40–80 ft., but some deeper wells may be constructed depending on local variation or desired supply.

Showing contractors within 60 miles of Ray Twp. 24 results found.

Typical depth
70 ft
Water table
18 ft
Contractors
24

24 Contractors

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Ries Well Drilling Inc. logo

Ries Well Drilling Inc.

Active Driller
Romeo, MI 48065
Well DrillingConstant Pressure SystemsWell Maintenance+2 more
Suburban Installers, Inc. logo

Suburban Installers, Inc.

Active Driller
Ray Twp, MI 48096
Well DrillingWell Maintenance
Utica Pump Company logo

Utica Pump Company

4.4 (5)
Utica, MI 48317
Pump ServicesPump InstallationPump Repair

A&A Edwards Well Drilling

Emmett, MI 48022
Well DrillingPump InstallationPump Repair+2 more
A&B Well Drilling logo

A&B Well Drilling

Active Driller
Kimball, MI 48074
Well DrillingPump ServicesWell Maintenance+2 more
B & J Well Drilling logo

B & J Well Drilling

Active Driller
Yale, MI 48097
Well DrillingPump RepairWell Maintenance+3 more
B&B Well Drilling logo

B&B Well Drilling

Active Driller
Leonard, MI 48367
Well DrillingCable ToolPump Repair+2 more
Clearwater Well Services Columbus MI logo

Clearwater Well Services Columbus MI

Active Driller
Columbus, MI 48063
Well DrillingPump InstallationPump Replacement+4 more
Corsaut Co Inc logo

Corsaut Co Inc

5.0 (3)
Oak Park, MI 48237
Pump InstallationFiltrationWater Line Installation+1 more
John Cameron & Son Inc logo

John Cameron & Son Inc

Active Driller
Oxford, MI 48371
Well DrillingWell MaintenanceFiltration
Larry A John Well Drilling & Repair, Inc logo

Larry A John Well Drilling & Repair, Inc

Richmond, MI 48062
Pump ServicesFiltrationAgricultural Irrigation Wells
Maglothin Well and Water Treatment LLC logo

Maglothin Well and Water Treatment LLC

Waterford Twp, MI 48329
Well DrillingPump ServicesWell Maintenance+4 more
MERSINO DEWATERING LLC logo

MERSINO DEWATERING LLC

AUBURN HILLS, MI 48326
DewateringDewatering WellsWellpoint Systems+1 more

Pieprzak Well Drilling

China Township, MI 48054
Well DrillingWell MaintenanceWater Line Installation

Valley Well & Pump LLC

Casco, MI 48064
Well DrillingPump ServicesPump Repair+2 more
Welser Well Drilling LLC logo

Welser Well Drilling LLC

St Clair, MI 48079
Well DrillingWell MaintenanceGeothermal Services
Adam's Well Drilling & Water Treatment logo

Adam's Well Drilling & Water Treatment

Howell, MI 48843
Well DrillingCommercial Well DrillingIndustrial Well Drilling+16 more
Adams Well Drilling logo

Adams Well Drilling

Active Driller5.0 (1)
Milford, MI 48843
Well DrillingResidential Well DrillingCommercial Well Drilling+11 more

Alderman's Well Drilling

Active Driller
Davison, MI 48423
Well DrillingPump InstallationWell Maintenance+1 more
Ayers Water Systems logo

Ayers Water Systems

5.0 (5)
White Lake, MI 48386
Pump RepairWell InspectionFiltration+1 more

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View Local Geology Report

A geological estimate for the Ray Twp area.

Typical Well Depth
70 ft
Static Water Level
18 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Synthesizing multiple well logs from Ray Township and adjacent areas in Macomb County, the region exhibits a predictable glacially derived sequence. The most common layers begin with a thin topsoil, then brown or gray clay, often interbedded with sand, gravel, or stones. Thick continuous clay (sometimes called 'hardpan' or 'gray clay') is typical, with intervals of sand, sand/gravel, or gritty layers indicating aquifer materials. Water is most consistently produced near the base of the clay sequence in sand or sand/gravel intervals, commonly found between 40 and 80 ft. Well construction usually involves PVC or steel casing set through clay and into the upper sand/gravel aquifer. Static water levels are typically within 3–30 ft. of ground surface. Deeper, higher-yield or high-capacity wells may penetrate up to ~180–220 ft. to reach thicker, deeper sand/gravel units where present.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
02 ftTopsoil / Brown ClayThin surficial soil layer, often brown clay or topsoil.Color: Brown
Hardness: Soft
220 ftClay, occasionally sandy or stonyDense glacial clay, sometimes interbedded with sand or stones. Occasional isolated sand streaks.Color: Gray/Brown
Hardness: Medium
2060 ftGray Clay (massive), intermittent sand, occasional stonesThick deposit of gray or mixed clay, variable presence of sand/gravel streaks or stones, may include hardpan.Color: Gray
Hardness: Hard
6080 ftSand / Sand & Gravel (main aquifer zone)Water-bearing sand or sand/gravel, often medium to coarse texture, typically producing best residential yields.Color: Gray/Yellow
Hardness: Unconsolidated
80200 ftClay with deeper sand/gravel lenses (where present)Additional thick gray clay with lenses of sand or gravel, especially in deeper wells toward 180–220 ft.; deeper sands represent high-capacity zones.Color: Gray
Hardness: Medium to Hard
200220 ftSand & Gravel (deep aquifer, not always present)Deep, coarse sand and gravel, principal water-bearing unit for large/industrial supply in deepest wells.Color: Yellow/Gray
Hardness: Unconsolidated

Frequently Asked Questions

A typical residential well in the Ray Twp area is drilled to approximately 70 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 18 feet below the surface in this region.

Synthesizing multiple well logs from Ray Township and adjacent areas in Macomb County, the region exhibits a predictable glacially derived sequence. The most common layers begin with a thin topsoil, then brown or gray clay, often interbedded with sand, gravel, or stones. Thick continuous clay (sometimes called 'hardpan' or 'gray clay') is typical, with intervals of sand, sand/gravel, or gritty layers indicating aquifer materials. Water is most consistently produced near the base of the clay sequence in sand or sand/gravel intervals, commonly found between 40 and 80 ft. Well construction usually involves PVC or steel casing set through clay and into the upper sand/gravel aquifer. Static water levels are typically within 3–30 ft. of ground surface. Deeper, higher-yield or high-capacity wells may penetrate up to ~180–220 ft. to reach thicker, deeper sand/gravel units where present.