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Richmond, Michigan

Well Drillers Near Richmond, Michigan

Typical Richmond-area wells encounter alternating clay and sand/gravel layers to depths of 100–125 ft, with water-bearing sands generally located below 30–45 ft and/or at greater depths. Residential wells for 5–15+ GPM are typically 80–125 ft deep.

Showing contractors within 60 miles of Richmond. 62 results found.

Typical depth
100 ft
Water table
20 ft
Contractors
62

62 Contractors

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View Local Geology Report

A geological estimate for the Richmond area.

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

Detailed Summary

The representative geology for the Richmond region consists of an upper sequence of 10–24 ft of clay or clay with some gravel, followed by interbedded sandy or gravelly intervals and additional clay layers. The most consistent pattern is: initial clay (10–24 ft), then sand or sandy gravel (few to ~8 ft), followed by more clay (sometimes extending to ~78–118 ft). Deeper water-bearing zones, usually coarse sand or sand/gravel, are typically found below 80–100 ft and can run to total well depths of 100–125 ft. Static water levels range from 5 to 45 ft below grade. Most wells use rotary mud circulation and are cased with 4–5 in. PVC to near total depth, with screens set at the bottom in coarser, water-bearing material. Typical residential well depths for 5–15+ GPM yield are 80–110 ft, with higher-capacity wells possible down to 125 ft.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 15 ftClayYellow to gray, sometimes stoney or with minor gravel.Color: Yellow/Gray
Hardness: Hard
15 – 22 ftSand/GravelInterbedded fine to coarse sand, sometimes gravelly, occasional water-bearing zones.Color: Gray/Yellow
Hardness: Medium
22 – 78 ftClayThick clay, may be interlaminated with occasional sand; some portions may be dense/stoney.Color: Gray
Hardness: Hard
78 – 98 ftSand/GravelGravelly sand, occasional cemented gravel. Common site of residential well screens.Color: Gray
Hardness: Loose to medium
98 – 124 ftSand (Water-bearing)/GravelCoarse sand and sand & gravel aquifer, sometimes cemented zones. Principal water-bearing unit.Color: Gray
Hardness: Loose

Frequently Asked Questions

A typical residential well in the Richmond 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 20 feet below the surface in this region.

The representative geology for the Richmond region consists of an upper sequence of 10–24 ft of clay or clay with some gravel, followed by interbedded sandy or gravelly intervals and additional clay layers. The most consistent pattern is: initial clay (10–24 ft), then sand or sandy gravel (few to ~8 ft), followed by more clay (sometimes extending to ~78–118 ft). Deeper water-bearing zones, usually coarse sand or sand/gravel, are typically found below 80–100 ft and can run to total well depths of 100–125 ft. Static water levels range from 5 to 45 ft below grade. Most wells use rotary mud circulation and are cased with 4–5 in. PVC to near total depth, with screens set at the bottom in coarser, water-bearing material. Typical residential well depths for 5–15+ GPM yield are 80–110 ft, with higher-capacity wells possible down to 125 ft.