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Harbor Springs, Michigan

Well Drillers Near Harbor Springs, Michigan

Typical Harbor Springs well geology: surficial sand/gravel, interbedded clay/silt, underlain by thick sand or sand & gravel, commonly transitioning to limestone and shale at greater depths. Most residential wells terminate in sand/gravel before hard rock.

Showing contractors within 60 miles of Harbor Springs. 34 results found.

Typical depth
180 ft
Water table
90 ft
Contractors
34

34 Contractors

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View Local Geology Report

A geological estimate for the Harbor Springs area.

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

Detailed Summary

The representative geological profile for the Harbor Springs region starts with a thin layer of sand or topsoil, followed by interbedded sand and gravel units often containing one or more clay layers. At depths of approximately 100 to 200 feet, layers of water-bearing sand and gravel are typical, frequently serving as the primary aquifer for household supply. In some areas and deeper wells, limestone, shale, and additional clay layers are present below 150-200 ft, with the deepest wells often ending in fractured limestone or mixed limestone/shale with occasional water-bearing zones. Most residential wells (yielding 5–15+ GPM) are completed between 120 and 220 ft, usually in the more permeable sand/gravel aquifer above bedrock.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 3 ftTopsoil or SandBrown sand, topsoil, or surficial sedimentsColor: Brown
Hardness: Loose
3 – 20 ftSand & Gravel/Clay InterbedsBrown sand and gravel with occasional thin clay lensesColor: Brown/Light Brown
Hardness: Loose to Semi-compact
20 – 60 ftClay/Silt with Sand and GravelClay, sometimes sandy, with medium to coarse sand/gravel intervalsColor: Light Brown/Gray/Pink
Hardness: Medium
60 – 155 ftSand/Sand & Gravel (Water-Bearing)Thick sequences of light to medium brown sand and gravel; dominant aquifer zoneColor: Light Brown
Hardness: Loose to Moderately compact
155 – 220 ftSand & Gravel with some Clay and SiltCoarser sand and gravel alternating with minor clay streaks; strong water yieldColor: Light to Medium Brown
Hardness: Loose
220 – 260 ftClay/Sandy ClayGray or pink clay and clayey sand; transitional zone above bedrockColor: Gray/Pink/Tan
Hardness: Firm
260 – 325 ftLimestone with Some ShaleHard limestone, locally with shale partings or clay seams; sometimes water-bearing in fracturesColor: Gray/Light Gray
Hardness: Hard rock

Frequently Asked Questions

A typical residential well in the Harbor Springs area is drilled to approximately 180 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 90 feet below the surface in this region.

The representative geological profile for the Harbor Springs region starts with a thin layer of sand or topsoil, followed by interbedded sand and gravel units often containing one or more clay layers. At depths of approximately 100 to 200 feet, layers of water-bearing sand and gravel are typical, frequently serving as the primary aquifer for household supply. In some areas and deeper wells, limestone, shale, and additional clay layers are present below 150-200 ft, with the deepest wells often ending in fractured limestone or mixed limestone/shale with occasional water-bearing zones. Most residential wells (yielding 5–15+ GPM) are completed between 120 and 220 ft, usually in the more permeable sand/gravel aquifer above bedrock.