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Highland, Michigan

Well Drillers Near Highland, Michigan

Typical Highland area well: alternating sand/gravel and clay, water-bearing sandy/gravel zones below 60-100 ft, residential wells usually completed from 60 to 120 ft.

Showing contractors within 60 miles of Highland. 93 results found.

Typical depth
90 ft
Water table
35 ft
Contractors
93

93 Contractors

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View Local Geology Report

A geological estimate for the Highland area.

Typical Well Depth
90 ft
Static Water Level
35 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

The most representative geological profile for the Highland area consists of a surficial brown/yellow sand or sand with gravel, underlain by alternating layers of clay (gray, blue, or sometimes with stones/silt), and again by water-bearing sand or sand/gravel at depth. Clay layers commonly separate upper and lower sand/gravel zones. Most wells encounter the main water-bearing, high-yield (often 10–20 GPM+) sand or sand/gravel formation beneath 60–100 ft. Residential wells typically target these deeper aquifers, avoiding locally thin surficial sands. A typical residential well depth ranges from 70 to 120 ft, with high-capacity (municipal/irrigation) wells potentially going to 120—180 ft+ if needed by local hydrogeology. The static water level is variable but often between 20 and 65 ft below grade, occasionally artesian.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 6 ftSand (Brown/Yellow, locally with gravel)Loose fine sand or sand/gravel mix near the surfaceColor: Brown/Yellow
Hardness: Loose
6 – 15 ftClay (Brown/Yellow/Blue)Plastic to firm clay, locally sandy, may contain some siltColor: Brown/Yellow/Blue
Hardness: Firm to plastic
15 – 40 ftSand (Brown/Gray, fine to medium)Sand, typically increasing in moisture with depthColor: Brown/Gray
Hardness: Loose to medium
40 – 70 ftClay (Gray/Blue/Gray with stones/silt)Stiff blue/gray clay, can be interbedded with silty or sandy streaks. Occasional stones.Color: Gray/Blue
Hardness: Stiff
70 – 100 ftSand/Gravel (Gray, water-bearing)Main aquifer zone: clean sand, sometimes with gravel, high permeabilityColor: Gray
Hardness: Loose
100 – 120 ftSand/Gravel (Gray, water-bearing or transitions to clay)Deeper permeable sand/gravel, often targeted for high-capacity wells, may grade into clay at depthColor: Gray
Hardness: Loose
120 – 140 ftClay/Silt (Gray/Blue; typically less consistent, localized)Deeper clay/silt (not always present in residential wells, but occurs in deeper holes)Color: Gray/Blue
Hardness: Stiff
140 – 180 ftSand (Fine to coarse, rarely with gravel)Deep, clean sand, yields variable depending on local settingColor: Yellow/Gray
Hardness: Loose

Frequently Asked Questions

A typical residential well in the Highland area is drilled to approximately 90 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 35 feet below the surface in this region.

The most representative geological profile for the Highland area consists of a surficial brown/yellow sand or sand with gravel, underlain by alternating layers of clay (gray, blue, or sometimes with stones/silt), and again by water-bearing sand or sand/gravel at depth. Clay layers commonly separate upper and lower sand/gravel zones. Most wells encounter the main water-bearing, high-yield (often 10–20 GPM+) sand or sand/gravel formation beneath 60–100 ft. Residential wells typically target these deeper aquifers, avoiding locally thin surficial sands. A typical residential well depth ranges from 70 to 120 ft, with high-capacity (municipal/irrigation) wells potentially going to 120—180 ft+ if needed by local hydrogeology. The static water level is variable but often between 20 and 65 ft below grade, occasionally artesian.