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Sterling, Michigan

Well Drillers Near Sterling, Michigan

Sterling area wells typically encounter surficial sand, extensive clay, with deeper layers of sand, shale, gravel, and sandstone or consolidated rock, with residential wells usually completed between 60 and 180 ft.

Showing contractors within 60 miles of Sterling. 77 results found.

Typical depth
120 ft
Water table
20 ft
Contractors
77

77 Contractors

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Fred Glass & Son Well Drlg

5.0 (2)
Comstock Park, MI 49321
(616) 784-2240
Well DrillingPump ServicesWell Maintenance

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View Local Geology Report

A geological estimate for the Sterling area.

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

Detailed Summary

The representative Sterling well profile begins with a surficial sand or sand & gravel layer (3–12 ft), underlain by thick sequences of clay (often in multiple beds) generally extending to 80–140 ft. Interbedded sand or sand/gravel layers are commonly found at various depths within these clays. Most wells reach into consolidated bedrock formations—typically shale, sandstone, or a sequence of both—beginning about 90–165 ft deep and extending as deep as 200+ ft in some cases. The most prolific water-bearing zones are often sand/gravel seams or the upper portions of sandstone or fractured consolidated rock. Shale is present and may be hard or soft; sandstone intervals can also be significant. Expected static water levels are commonly 10–40 ft below grade, with 5–15+ gpm possible at 80–180 ft depths for residential use. High-capacity wells may require deeper construction, often to the top of sandstone, typically 160–200+ ft.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 8 ftSandSurficial sand layer, occasional mixed sand & gravelHardness: Loose
8 – 38 ftClayThick clay, sometimes blue or red; commonly subdivided into stiffer and softer bedsColor: Red/Blue/Grey
Hardness: Soft to firm
38 – 78 ftClay with occasional Sand LensesMixed beds of clay with occasional lenses of sand or sandy clay; possible thin gravel seamsHardness: Variable
78 – 130 ftClay and ShaleClay gradually transitions to soft then hard shale; some sites report blue or black shaleColor: Dark grey/black/blue
Hardness: Soft to hard
130 – 165 ftShale, Sandstone, and/or GravelAlternating layers of hard shale, sandstone, with occasional gravel seam at base; quality and thickness vary locallyHardness: Hard
165 – 200 ftSandstone and ShaleMassive sandstone with interbedded shale; may include limestone at base in some isolated locationsHardness: Consolidated rock
200 – 235 ftHard Bedrock (Shale/Sandstone/Limestone)Base of typical well profile; some wells penetrate additional thin limestone or persistent shaleHardness: Very hard

Frequently Asked Questions

A typical residential well in the Sterling area is drilled to approximately 120 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 Sterling well profile begins with a surficial sand or sand & gravel layer (3–12 ft), underlain by thick sequences of clay (often in multiple beds) generally extending to 80–140 ft. Interbedded sand or sand/gravel layers are commonly found at various depths within these clays. Most wells reach into consolidated bedrock formations—typically shale, sandstone, or a sequence of both—beginning about 90–165 ft deep and extending as deep as 200+ ft in some cases. The most prolific water-bearing zones are often sand/gravel seams or the upper portions of sandstone or fractured consolidated rock. Shale is present and may be hard or soft; sandstone intervals can also be significant. Expected static water levels are commonly 10–40 ft below grade, with 5–15+ gpm possible at 80–180 ft depths for residential use. High-capacity wells may require deeper construction, often to the top of sandstone, typically 160–200+ ft.