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Muskegon, Michigan

Well Drillers Near Muskegon, Michigan

A typical Muskegon-area water well profile consists of surficial sand, interbedded clay or silt, and multiple water-bearing glaciofluvial sand/gravel layers, with static water typically found 10–20 ft below grade. Residential wells commonly reach 40–70 ft for reliable water supply.

Showing contractors within 60 miles of Muskegon. 61 results found.

Typical depth
55 ft
Water table
15 ft
Contractors
61

61 Contractors

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View Local Geology Report

A geological estimate for the Muskegon area.

Typical Well Depth
55 ft
Static Water Level
15 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Analysis of representative well logs from Muskegon County shows a dominant sequence of surficial dry sand (10–20+ ft), then a mix of finer water-bearing sands or occasional clay/silt layers (10–20 ft thick), and most often a significant, lower water-bearing sand or sand/gravel formation extending to final depths from 40 to 90 ft. Thin clay/silt lenses (3–10 ft) are frequent but discontinuous. The most productive aquifers are consistently sands and sand/gravel either above or below minor confining clay/silt layers. Static water levels in wells average 10–20 ft below grade. A typical residential well for adequate and sustainable yield (5–15+ GPM) is generally completed at 45–70 ft, with high-capacity wells extending to 70–90 ft.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 13 ftSandSurficial dry sand, loose to medium; occasional topsoil coverColor: Light brown / brown
Hardness: Loose
13 – 26 ftSand (wet/moist or medium/fine, often water bearing)Transitional sand, fine to medium; becomes water bearing downwardColor: Brown or grayish
Hardness: Medium
26 – 36 ftClay/Silt (interbedded, sometimes absent)Clay or silt, sometimes with thin wet/fine sand lenses; confining layer in placesColor: Gray
Hardness: Firm/plastic
36 – 45 ftFine/Very Fine Sand (water bearing)Water-bearing fine to very fine sand, productive aquiferColor: Light gray/tan
Hardness: Medium
45 – 70 ftSand/Sand & Gravel (coarse, water bearing)Major aquifer: coarse sand and sand & gravel, abundant water, best yieldsColor: Brown/tan with gravel
Hardness: Medium to loose
70 – 90 ftSand (water bearing, locally with gravel)Deeper extension of water-bearing sand and gravel; highly productive at some sitesColor: Tan, possible mix with gravel
Hardness: Loose

Frequently Asked Questions

A typical residential well in the Muskegon area is drilled to approximately 55 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 15 feet below the surface in this region.

Analysis of representative well logs from Muskegon County shows a dominant sequence of surficial dry sand (10–20+ ft), then a mix of finer water-bearing sands or occasional clay/silt layers (10–20 ft thick), and most often a significant, lower water-bearing sand or sand/gravel formation extending to final depths from 40 to 90 ft. Thin clay/silt lenses (3–10 ft) are frequent but discontinuous. The most productive aquifers are consistently sands and sand/gravel either above or below minor confining clay/silt layers. Static water levels in wells average 10–20 ft below grade. A typical residential well for adequate and sustainable yield (5–15+ GPM) is generally completed at 45–70 ft, with high-capacity wells extending to 70–90 ft.