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Harrison, Michigan

Well Drillers Near Harrison, Michigan

The typical Harrison, MI area well profile features a surficial sand or sand & clay mix overlying thick sequences of silty/clayey material, with the main water-bearing zone as a coarse sand and/or sand and gravel layer, typically reached between 40 and 100 feet. Wells for household use average 70-100 ft with a static water level of 15-25 ft below grade, yielding 10-15 GPM or more.

Showing contractors within 60 miles of Harrison. 89 results found.

Typical depth
85 ft
Water table
18 ft
Contractors
89

89 Contractors

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View Local Geology Report

A geological estimate for the Harrison area.

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

Detailed Summary

Based on a synthesis of multiple wells across Harrison, MI, the most representative geological sequence begins with a surficial sand, sand & clay, or thin topsoil layer (often 1-5 ft), underlain by extensive zones of brown/red/yellow/gray clay or sand & clay mixtures (15–60 ft thick globally), sometimes with thin lenses of gravel or sand. The persistent, most productive water-bearing aquifer occurs as a coarse sand or sand and gravel unit found between 40 and 100 ft bgs, thickness typically 10–30+ ft, often preceded and followed by clay layers. Static water levels cluster between 12 and 25 ft, and the best producing wells use rotary or hollow rod methods and PVC or steel casing, typically 4–5 inches in diameter, set nearly the entire depth. Grouting is generally bentonite slurry or dry granular bentonite, and most wells use a screened interval positioned through the basal sand/gravel. A typical residential well needs to reach the bottommost sand/gravel, which is where reliable 10+ GPM supply is consistently found.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 1 ftTopsoil/SandOccasional black topsoil or surficial sandColor: Black/Brown/Yellow
Hardness: Soft
1 – 15 ftSand and/or Sand & ClayBrown/Yellow Sand, sometimes mixed with clay; discontinuousColor: Brown/Yellow
Hardness: Medium
15 – 50 ftClay / Sand & ClayBrown, red, blue or gray silty clay or sand & clay mixture; low permeability, may contain lenses of sand.Color: Gray/Brown/Red/Blue
Hardness: Firm/Soft
50 – 70 ftSand & Gravel (Minor Clay)Increasingly sandy with some gravel; transition to aquifer zone.Color: Brown/Gray
Hardness: Medium/Loose
70 – 100 ftSand & Gravel (Major Aquifer)Coarse/fine to medium sand and gravel, main water-bearing unit; generally clean and well sorted.Color: Brown/Gray/White
Hardness: Loose
100 – 150 ftClay (deeper wells only)Gray or brown clay, occasionally interrupted with sand/gravel seamsColor: Gray/Brown
Hardness: Firm
150 – 167 ftSand/GravelDeep sand and gravel aquifer (only in deep/high-capacity wells), high yield.Color: Brown
Hardness: Loose

Frequently Asked Questions

A typical residential well in the Harrison 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 18 feet below the surface in this region.

Based on a synthesis of multiple wells across Harrison, MI, the most representative geological sequence begins with a surficial sand, sand & clay, or thin topsoil layer (often 1-5 ft), underlain by extensive zones of brown/red/yellow/gray clay or sand & clay mixtures (15–60 ft thick globally), sometimes with thin lenses of gravel or sand. The persistent, most productive water-bearing aquifer occurs as a coarse sand or sand and gravel unit found between 40 and 100 ft bgs, thickness typically 10–30+ ft, often preceded and followed by clay layers. Static water levels cluster between 12 and 25 ft, and the best producing wells use rotary or hollow rod methods and PVC or steel casing, typically 4–5 inches in diameter, set nearly the entire depth. Grouting is generally bentonite slurry or dry granular bentonite, and most wells use a screened interval positioned through the basal sand/gravel. A typical residential well needs to reach the bottommost sand/gravel, which is where reliable 10+ GPM supply is consistently found.