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Grand Rapids, Michigan

Well Drillers Near Grand Rapids, Michigan

The typical Grand Rapids-area geological profile consists of an upper clay layer overlying significant sand/gravel aquifers, sometimes interbedded with silty or gravelly strata, and occasionally (in deeper sections) underlain by consolidated limestone or sandstone bedrock.

Showing contractors within 60 miles of Grand Rapids. 81 results found.

Typical depth
85 ft
Water table
33 ft
Contractors
81

81 Contractors

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View Local Geology Report

A geological estimate for the Grand Rapids area.

Typical Well Depth
85 ft
Static Water Level
33 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Synthesis of representative well logs indicates the prevalent Grand Rapids region sequence is 15–25 ft of clay at the surface, followed by alternating sand/gravel (often 20–50 ft thick) and additional clay or sandy clay. Below 40–60 ft, wells often encounter coarser sand and gravel layers, typically used for water supply. In the deepest (100–150+ ft) wells, a few logs encounter limestone or sandstone bedrock. The most common water-bearing zones are major sand or sand/gravel strata between 25 and 90 ft. Static water levels are typically found at 15–50 ft below grade. A standard residential well for 5–15+ GPM is usually completed between 60–100 ft, with high-capacity wells extending to deeper sand/gravel or into the top of bedrock, around 120–160 ft total depth. Thin gravels or varying silt are noted but are less consistent and omitted in this generalization.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 20 ftClayDense, brown to gray clay, commonly found at surface; may include minor silt or sandy inclusions.Color: Brown/Gray
Hardness: Hard
20 – 45 ftSand and Gravel (with minor silt/clay layers)Medium to coarse sand and gravel, possible interbedded silt or clay lenses, moderate sorting; major aquifer zone.Color: Light brown/yellow/tan
Hardness: Medium
45 – 60 ftClay or Sandy ClayFirm to hard clay or sandy clay, sometimes with gravel inclusions.Color: Brown/gray
Hardness: Hard
60 – 90 ftSand and Gravel (Main Aquifer)Coarse sand and gravel, primary water-bearing formation for most wells; occasionally with thin clay/silt partings.Color: Light brown/yellow
Hardness: Medium
90 – 150 ftConsolidated Bedrock (Limestone/Sandstone)Gray limestone or buff to yellowish sandstone (where present in deeper wells); not present in all locations.Color: Gray/Buff
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Grand Rapids area is drilled to approximately 85 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 33 feet below the surface in this region.

Synthesis of representative well logs indicates the prevalent Grand Rapids region sequence is 15–25 ft of clay at the surface, followed by alternating sand/gravel (often 20–50 ft thick) and additional clay or sandy clay. Below 40–60 ft, wells often encounter coarser sand and gravel layers, typically used for water supply. In the deepest (100–150+ ft) wells, a few logs encounter limestone or sandstone bedrock. The most common water-bearing zones are major sand or sand/gravel strata between 25 and 90 ft. Static water levels are typically found at 15–50 ft below grade. A standard residential well for 5–15+ GPM is usually completed between 60–100 ft, with high-capacity wells extending to deeper sand/gravel or into the top of bedrock, around 120–160 ft total depth. Thin gravels or varying silt are noted but are less consistent and omitted in this generalization.