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Ortonville, Michigan

Well Drillers Near Ortonville, Michigan

A typical Ortonville-area well penetrates a sequence of unconsolidated gravel, clay, and sand layers overlying bedrock (often sandstone or limestone), with residential wells drawing from gravel or sand aquifers at moderate depths.

Showing contractors within 60 miles of Ortonville. 97 results found.

Typical depth
95 ft
Water table
40 ft
Contractors
97

97 Contractors

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BCB Well Pump And Tank Service logo

BCB Well Pump And Tank Service

Lapeer, MI 48446
Residential Well DrillingAgricultural Irrigation Wells
C.E. Layman & Son Water Well Drilling & Well Service logo

C.E. Layman & Son Water Well Drilling & Well Service

Active Driller4.2 (5)
Ortonville, MI 48462
Well DrillingWell Maintenance
Fleming Well Drilling logo

Fleming Well Drilling

Active Driller5.0 (5)
Ortonville, MI 48462
Well DrillingResidential Well DrillingWell Maintenance
John Cameron & Son Inc logo

John Cameron & Son Inc

Active Driller
Oxford, MI 48371
Well DrillingWell MaintenanceFiltration
Mike LaLone Well Service logo

Mike LaLone Well Service

Active Driller
Ortonville, MI 48462
Well DrillingPump ServicesPump Installation+5 more
Mike LaLone Well Service logo

Mike LaLone Well Service

Active Driller2.5 (11)
Davisburg, MI 48350
Well DrillingResidential Well DrillingCommercial Well Drilling+14 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
B. W. Layman & Sons Inc. logo

B. W. Layman & Sons Inc.

Active Driller
White Lake, MI 48383
Well DrillingTest Well DrillingPump Services+11 more
B&B Well Drilling logo

B&B Well Drilling

Active Driller
Leonard, MI 48367
Well DrillingCable ToolPump Repair+2 more
Brown Drilling & Water Treatment logo

Brown Drilling & Water Treatment

Howell, MI 48843
Well DrillingCommercial Well DrillingIndustrial Well Drilling+10 more
Cascade Flint logo

Cascade Flint

Flint, MI 48507
Well DrillingMonitoring WellsRemediation+1 more
Coon Well Drilling logo

Coon Well Drilling

Grand Blanc, MI 48439
Well DrillingWell MaintenanceWell Inspection

Ernest Morris Well Drilling

Active Driller
Highland, MI 48357
Well DrillingWell MaintenanceWater Line Installation
Gil Sunde Well Drilling & Service logo

Gil Sunde Well Drilling & Service

Active Driller
Flint, MI 48532
Well DrillingPump ReplacementWell Maintenance+1 more

Hazard Well Drilling Inc

Flint, MI 48506
Well DrillingResidential Well DrillingWell Maintenance
Joe Curry Well Drilling logo

Joe Curry Well Drilling

Holly, MI 48442-9199
Well DrillingWell Maintenance

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Well records near Ortonville

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View Local Geology Report

A geological estimate for the Ortonville area.

Typical Well Depth
95 ft
Static Water Level
40 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on synthesis of multiple well logs from the Ortonville and surrounding region (Oakland/Genesee/Lapeer counties), the most representative geological profile is as follows: The shallowest layers are typically surficial gravels (sometimes sandy or red), often up to 40-45 ft thick, underlain by varying thicknesses of clay (often brown or gray, sometimes hard, 20-60 ft), with additional water-bearing sand or sand/gravel intervals typically encountered below these clays (15-30 ft thick, often used as domestic aquifers). At greater depths (>100 ft), wells may encounter additional thick gravel/sand or transition into fractured bedrock (sandstone, limestone, granite), which serve as high-capacity aquifers. The static water level is usually between 17 and 65 ft below grade, and residential wells are most commonly completed at 70 to 120 ft for reliable yields (10-20 GPM). High-capacity/bedrock wells can extend to 180-260 ft or deeper.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
040 ftGravel (occas. sandy/red), locally mixed with clayCoarse to medium gravel, sometimes sandy or reddish, forming the basal surficial layer; water may be present in basal portions.Color: Brown-Red
Hardness: Loose to medium consolidated
4070 ftClay (occas. sandy/hard/gray/red/brown)Firm to hard clay, often brown, gray, or reddish; acts as a confining layer between aquifers.Color: Brown-Gray-Red
Hardness: Hard to very firm
7095 ftSand & Gravel (Water Bearing)Sand and gravel (often medium to coarse), principal domestic aquifer for residential wells, generally saturated.Color: Gray-Brown
Hardness: Unconsolidated to semi-consolidated
95140 ftClay or Sandy Clay (subordinate gravel/sand layers possible)Mostly clay; may include sandy or gravel lenses; less permeable, locally acts as aquitard.Color: Brown-Gray
Hardness: Hard
140200 ftSandstone or Sand & Gravel TransitionCoarse sand, sandstone, or mixed gravels; high-yield zones for deeper or higher capacity wells; can include transition to fractured bedrock (limestone/sandstone).Color: Light brown, gray, tan
Hardness: Consolidated (bedrock); loose before bedrock

Frequently Asked Questions

A typical residential well in the Ortonville area is drilled to approximately 95 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 40 feet below the surface in this region.

Based on synthesis of multiple well logs from the Ortonville and surrounding region (Oakland/Genesee/Lapeer counties), the most representative geological profile is as follows: The shallowest layers are typically surficial gravels (sometimes sandy or red), often up to 40-45 ft thick, underlain by varying thicknesses of clay (often brown or gray, sometimes hard, 20-60 ft), with additional water-bearing sand or sand/gravel intervals typically encountered below these clays (15-30 ft thick, often used as domestic aquifers). At greater depths (>100 ft), wells may encounter additional thick gravel/sand or transition into fractured bedrock (sandstone, limestone, granite), which serve as high-capacity aquifers. The static water level is usually between 17 and 65 ft below grade, and residential wells are most commonly completed at 70 to 120 ft for reliable yields (10-20 GPM). High-capacity/bedrock wells can extend to 180-260 ft or deeper.