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Kalamazoo, Michigan

Well Drillers Near Kalamazoo, Michigan

Typical Kalamazoo-area well geology shows a thick sequence of clay, sand, and gravel layers overlying variable water-bearing sand/gravel intervals within the upper 100–185 feet.

Showing contractors within 60 miles of Kalamazoo. 92 results found.

Typical depth
100 ft
Water table
67 ft
Contractors
92

92 Contractors

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View Local Geology Report

A geological estimate for the Kalamazoo area.

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

Detailed Summary

Based on synthesis of well logs from across the Kalamazoo region, the most representative well begins with topsoil or fill, followed by alternating clay (often blue/gray or brown) and sandy or gravelly layers. Coarse sand and sand & gravel units commonly form the main aquifers, typically occurring below significant thicknesses of fine sand or clay. The static water level is usually found well above the primary producing zone. Typical residential wells are cased to near the aquifer and screened in coarse, water-bearing sand or sand/gravel. High-capacity wells would extend to the lower sand & gravel aquifers.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 5 ftTopsoil or FillTopsoil, possibly with gravel or sand fill in disturbed areasColor: Brown/variable
Hardness: Soft
5 – 25 ftSand & Gravel / ClayInterbedded sand, fine gravel, and brown/gray or blue clayColor: Brown to gray or blue
Hardness: Soft to firm
25 – 70 ftClay (often blue/gray), some fine sandThick sequence of blue/gray/brown clay, with localized beds of sand or fine gravelColor: Blue, gray, brown
Hardness: Medium to hard
70 – 100 ftSand & Gravel (water bearing)Coarse sand with gravel, primary household-aquifer; may alternate with thin clay streaksColor: Yellow, gray, tan
Hardness: Medium
100 – 145 ftClay, Clay with Sand & GravelDense clay, may contain some sand and gravel layersColor: Gray, blue, brown
Hardness: Hard
145 – 170 ftSand & Gravel (coarser, water bearing)Thicker, coarser sand and gravel, serves as a major aquifer for deeper residential and high-capacity wellsColor: Yellow, tan, mixed
Hardness: Medium
170 – 185 ftSand and Gravel (saturated, possible lower aquifer)Very coarse, clean sand and gravel, thick saturated zone in deepest wellsColor: Gray, tan
Hardness: Medium

Frequently Asked Questions

A typical residential well in the Kalamazoo 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 67 feet below the surface in this region.

Based on synthesis of well logs from across the Kalamazoo region, the most representative well begins with topsoil or fill, followed by alternating clay (often blue/gray or brown) and sandy or gravelly layers. Coarse sand and sand & gravel units commonly form the main aquifers, typically occurring below significant thicknesses of fine sand or clay. The static water level is usually found well above the primary producing zone. Typical residential wells are cased to near the aquifer and screened in coarse, water-bearing sand or sand/gravel. High-capacity wells would extend to the lower sand & gravel aquifers.