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Battle Creek, Michigan

Well Drillers Near Battle Creek, Michigan

Glacial till (sand/gravel/clay) overlying Marshall Sandstone, minor shale near base.

Showing contractors within 60 miles of Battle Creek. 81 results found.

Typical depth
100 ft
Water table
25 ft
Contractors
81

81 Contractors

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Well records near Battle Creek

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View Local Geology Report

A geological estimate for the Battle Creek area.

Typical Well Depth
100 ft
Static Water Level
25 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

The representative geologic profile for the Battle Creek region shows a surficial sequence of unconsolidated glacial deposits composed of varying sand, gravel, and clay, typically extending down to 60-70 ft depth. Below this, wells consistently encounter competent Marshall Sandstone, often water-bearing, extending for several tens of feet, sometimes interbedded with or underlain by thin shale or consolidated formations. Most private residential wells are completed at 80-120 ft to obtain 10-20 GPM. Municipal and irrigation wells may be much deeper, exceeding 140 ft. Static water levels are commonly 18-32 ft below grade.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 35 ftUnconsolidated Glacial DepositsTan/Brown Sand, Gravel, and Clay—moderately compacted, mixed texture.Color: Brown/Tan/Gray
Hardness: Soft to Medium
35 – 70 ftClay & Gravel / Fine SandBrown/gray clay, occasional gravel beds, locally zones of fine sand.Color: Brown/Gray
Hardness: Medium
70 – 110 ftMarshall Sandstone (sometimes with thin shale or broken zones)Gray to light gray massive sandstone, locally indurated, water-bearing, minor shale or consolidated seams possible.Color: Gray/Light Gray
Hardness: Hard
110 – 150 ftMarshall Sandstone (deeper section)Light gray or blue-gray sandstone, transitional to zones with shale; may be increasingly indurated with depth.Color: Light Gray/Blue-Gray
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Battle Creek area is drilled to approximately 100 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 25 feet below the surface in this region.

The representative geologic profile for the Battle Creek region shows a surficial sequence of unconsolidated glacial deposits composed of varying sand, gravel, and clay, typically extending down to 60-70 ft depth. Below this, wells consistently encounter competent Marshall Sandstone, often water-bearing, extending for several tens of feet, sometimes interbedded with or underlain by thin shale or consolidated formations. Most private residential wells are completed at 80-120 ft to obtain 10-20 GPM. Municipal and irrigation wells may be much deeper, exceeding 140 ft. Static water levels are commonly 18-32 ft below grade.