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Benton Harbor, Michigan

Well Drillers Near Benton Harbor, Michigan

Typical Benton Harbor wells encounter alternating sand and clay layers, with common medium to fine sand aquifers beneath clay confining units.

Showing contractors within 60 miles of Benton Harbor. 58 results found.

Typical depth
85 ft
Water table
40 ft
Contractors
58

58 Contractors

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View Local Geology Report

A geological estimate for the Benton Harbor area.

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

Detailed Summary

Based on a synthesis of random well logs from the Benton Harbor area and adjacent townships, the most representative geological sequence begins with surficial fine sand or sand/topsoil, commonly underlain by significant clay (or silty/clayey) layers, with further alternations of sand/gravel aquifers and clay, transitioning to deeper, more extensive sand or gravelly sand units. Well yields are typically high, with water-bearing sand/gravel layers encountered usually below confining clay. For residential wells, depths of 70–130 ft commonly achieve 5–20+ GPM, with static water levels from 12–65 ft b.g.s. Rotary-mud circulation is the standard drilling method. Casing and grouting practices are consistent with industry standards for unconsolidated glacial deposits.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 2 ftTopsoil/SandBrown or tan fine sand, may include organic-rich topsoil.Color: Brown/Tan
Hardness: Soft
2 – 20 ftSand (fine-medium)Fine to medium sand, some local gravel lenses possible.Color: Tan/Brown
Hardness: Soft
20 – 45 ftClay/SiltBrown, gray, or tan clay, locally silty or sandy.Color: Brown/Gray
Hardness: Firm
45 – 85 ftSand (Water-Bearing)Brown or tan, medium to coarse sand, permeable, commonly main residential aquifer.Color: Brown/Tan
Hardness: Loose
85 – 130 ftClay with lenses of Sand/SiltGray or brown clay, often with embedded sand and silt streaks.Color: Gray/Brown
Hardness: Firm
130 – 170 ftSand and Gravel (Aquifer)Gray to brown coarse sand and gravel, high yielding, deeper aquifer for high-capacity wells.Color: Gray/Brown
Hardness: Loose
170 – 185 ftSand (Water-Bearing)Fine to medium sand, water bearing, found in deeper portions of some wells.Color: Gray
Hardness: Loose

Frequently Asked Questions

A typical residential well in the Benton Harbor 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 40 feet below the surface in this region.

Based on a synthesis of random well logs from the Benton Harbor area and adjacent townships, the most representative geological sequence begins with surficial fine sand or sand/topsoil, commonly underlain by significant clay (or silty/clayey) layers, with further alternations of sand/gravel aquifers and clay, transitioning to deeper, more extensive sand or gravelly sand units. Well yields are typically high, with water-bearing sand/gravel layers encountered usually below confining clay. For residential wells, depths of 70–130 ft commonly achieve 5–20+ GPM, with static water levels from 12–65 ft b.g.s. Rotary-mud circulation is the standard drilling method. Casing and grouting practices are consistent with industry standards for unconsolidated glacial deposits.