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Coloma, Michigan

Well Drillers Near Coloma, Michigan

Typical Coloma area well geology: alternating sand/clay with significant sand/gravel aquifers below ~80-120 ft, static water level ~30-80 ft, most residential wells 110-140 ft deep.

Showing contractors within 60 miles of Coloma. 68 results found.

Typical depth
130 ft
Water table
50 ft
Contractors
68

68 Contractors

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Collins Well Drilling

Active Driller3.3 (25)
Benton Harbor, MI 49022
Well DrillingWell Maintenance

Mike's Well Drilling

Active Driller4.2 (25)
Coloma, MI 49038
Well DrillingResidential Well DrillingPump Installation+3 more

Richcreek Water Pump Sales

5.0 (1)
Hartford, MI 49057
Well DrillingPump ServicesPump Installation+1 more

Brinks Brothers & Son

4.0 (5)
South Haven, MI 49090
Well DrillingPump Installation
Dohm Well Drilling logo

Dohm Well Drilling

Active Driller4.3 (44)
Dowagiac, MI 49047
Well DrillingResidential Well DrillingCommercial Well Drilling+8 more

Duke's Wells Service

Bloomingdale, MI 49026
Pump InstallationWell Maintenance
Earl Sanders & Son Well Drilling Inc logo

Earl Sanders & Son Well Drilling Inc

Active Driller4.8 (36)
Lawton, MI 49065
Well DrillingResidential Well DrillingCommercial Well Drilling+11 more
Foune Well Drilling Inc logo

Foune Well Drilling Inc

Active Driller4.4 (88)
Paw Paw, MI 49079-0146
Well DrillingResidential Well DrillingMunicipal Well Drilling+10 more
J.E. Marks Well Drilling LLC logo

J.E. Marks Well Drilling LLC

4.3 (7)
Berrien Center, MI 49102
Well DrillingResidential Well DrillingCommercial Well Drilling+7 more
James Lewis Mosier Well Drilling logo

James Lewis Mosier Well Drilling

Active Driller5.0 (56)
Dowagiac, MI 49047-9770
Well DrillingPump Repair
Martin J. Mosier Water Well Services logo

Martin J. Mosier Water Well Services

Active Driller4.9 (88)
Dowagiac, MI 49047
Residential Well DrillingPump InstallationPump Repair+4 more
McCarty Well Drilling ,Inc. logo

McCarty Well Drilling ,Inc.

Active Driller4.9 (158)
Buchanan, MI 49107
Well DrillingMud RotaryWater Testing+4 more

The Well Guy LLC

5.0 (24)
South Haven, MI 49090
Well DrillingWell Maintenance

Yordy & Sons

Decatur, MI 49045
Well DrillingWell MaintenanceWater System Maintenance
A+ Well Service logo

A+ Well Service

Active Driller5.0 (221)
Richland, MI 49083
Well DrillingPump RepairWell Maintenance+3 more

All J's Water Well Service

Active Driller4.9 (60)
Delton, MI 49046
Well DrillingPressure Tank Installation
Bohs Well Drilling Inc logo

Bohs Well Drilling Inc

4.5 (47)
Elkhart, IN 46514
Well DrillingPump ServicesPump Installation+9 more
C & B Pump Services & Well Drill logo

C & B Pump Services & Well Drill

Active Driller4.9 (36)
Three Rivers, MI 49093
Well DrillingPump ServicesPump Repair+6 more
Clearwater Well & Pump logo

Clearwater Well & Pump

4.7 (55)
Rolling Prairie, IN 46371
Well DrillingComplete Water System InstallationWater System Maintenance

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View Local Geology Report

A geological estimate for the Coloma area.

Typical Well Depth
130 ft
Static Water Level
50 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

The most representative geology beneath Coloma consists of an upper sand or sand & gravel layer (often with fine sand), followed by thick clay and/or clay with silt, transitioning into successively alternating layers of sand (fine to medium, occasionally coarse) and clay. Below roughly 80-120 ft, a thick, transmissive sand and/or sand & gravel unit is common, providing the main aquifer tapped for residential and high-capacity wells. Typical static water levels occur between 30-85 ft below grade, with residential well completions most frequently between 110-140 ft, and high capacity (public supply) wells extending as deep as 180-195 ft. Outlier or single-well inclusions (such as very thin or anomalously thick layers) are omitted in this generalized model.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
08 ftSand (fine to medium), locally with gravelTopsoil and unconsolidated fine to medium sand, occasional gravelColor: Brown/Light Brown
Hardness: Unconsolidated
840 ftClay (with variable silt and sand)Mostly brown to gray clay, some silt and minor sand lensesColor: Brown to Gray
Hardness: Soft to Firm
4050 ftSand & Silt or GravelSand & silt or isolated sand/gravel stringers, variable occurrenceColor: Brown to Gray
Hardness: Unconsolidated
5090 ftClay (some with silt/sand interbeds)Thick clay (gray or brown), with possible thin moist sand/clay stringersColor: Brown to Gray
Hardness: Firm to Hard
90115 ftSand & Gravel, Sand (medium-fine)Thick sand and/or sand & gravel, primary aquifer unit, water bearingColor: Brown/Gray/Tan
Hardness: Unconsolidated
115145 ftClay (locally silty or sandy, some hard clay)Another thick clay interval, potential for hard or moist characterColor: Gray/Dark Gray
Hardness: Firm to Hard
145175 ftSand (medium to coarse), locally with silt or clayLower sand and/or sand with silt or clay, marks base of typical water supply formation in deeper wellsColor: Brown/Gray
Hardness: Unconsolidated
175195 ftSand & Clay (coarse/fine alternations)Alternating coarse sand with clay, basal interval seen in deeper high-capacity wells; merge with above for typical residential wellsColor: Gray/Brown
Hardness: Unconsolidated

Frequently Asked Questions

A typical residential well in the Coloma area is drilled to approximately 130 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 50 feet below the surface in this region.

The most representative geology beneath Coloma consists of an upper sand or sand & gravel layer (often with fine sand), followed by thick clay and/or clay with silt, transitioning into successively alternating layers of sand (fine to medium, occasionally coarse) and clay. Below roughly 80-120 ft, a thick, transmissive sand and/or sand & gravel unit is common, providing the main aquifer tapped for residential and high-capacity wells. Typical static water levels occur between 30-85 ft below grade, with residential well completions most frequently between 110-140 ft, and high capacity (public supply) wells extending as deep as 180-195 ft. Outlier or single-well inclusions (such as very thin or anomalously thick layers) are omitted in this generalized model.