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Mecosta, Michigan

Well Drillers Near Mecosta, Michigan

Typical Mecosta residential wells penetrate alternating layers of sand, clay, and gravel, with the most common water-bearing zones found in medium-coarse sand or sand/gravel layers below one or more clay confining units.

Showing contractors within 60 miles of Mecosta. 122 results found.

Typical depth
45 ft
Water table
22 ft
Contractors
122

122 Contractors

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View Local Geology Report

A geological estimate for the Mecosta area.

Typical Well Depth
45 ft
Static Water Level
22 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

A representative geological profile for Mecosta wells consists, from ground surface downward, of a shallow upper sand (often mixed with some gravel or silt), underlain by one or more confining clay layers. At moderate depths (generally 20–50 ft), a medium-to-coarse sand or sand/gravel layer commonly serves as the principal aquifer and yields the best residential water supplies (5-15+ GPM). In some locations, deeper clay or alternating clay/gravel units are present, and select deeper wells may penetrate second or lower sand-rich aquifers, sometimes mixed with consolidated or ‘unknown water-bearing’ zones. The static water table typically lies between 6–34 ft below land surface. Average residential casing extends to near the base of the first major clay or confining layer, with screened intervals set through the most consistent sand or sand/gravel aquifer. Grouting of casing with bentonite slurry (typically from surface to base casing) is standard for protection against surface contamination.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 6 ftSand/topsoil (occasionally sandstone)Brown to tan, fine to medium sand or sandy topsoil, locally some sandstone or silt.Color: Brown/tan
Hardness: Soft
6 – 20 ftClay (occasionally includes gravel or silt)Mostly brown or gray clay, locally silty or with fine gravel. Acts as a confining unit.Color: Brown/gray
Hardness: Firm-stiff
20 – 40 ftSand and/or Sand & Gravel (Water-Bearing)Medium to coarse sand, often with varying amounts of gravel. Primary aquifer in most wells; typically water-bearing.Color: Tan/yellow/gray
Hardness: Medium (unconsolidated)
40 – 55 ftClay (occasionally with gravel or silt)Gray or brown clay, sometimes with interbedded gravel. Acts as a lower confining or semi-confining unit.Color: Gray/brown
Hardness: Stiff
55 – 90 ftSand & Gravel to Clay/Gravel Alternations (Deeper Aquifer)Alternating thick sand/gravel strata and clay; not present in all wells but present in deep wells (deeper than ~70 ft). Sometimes, 'unknown water-bearing' or consolidated intervals are logged here.Color: Tan/yellow/gray
Hardness: Medium to firm

Frequently Asked Questions

A typical residential well in the Mecosta area is drilled to approximately 45 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 22 feet below the surface in this region.

A representative geological profile for Mecosta wells consists, from ground surface downward, of a shallow upper sand (often mixed with some gravel or silt), underlain by one or more confining clay layers. At moderate depths (generally 20–50 ft), a medium-to-coarse sand or sand/gravel layer commonly serves as the principal aquifer and yields the best residential water supplies (5-15+ GPM). In some locations, deeper clay or alternating clay/gravel units are present, and select deeper wells may penetrate second or lower sand-rich aquifers, sometimes mixed with consolidated or ‘unknown water-bearing’ zones. The static water table typically lies between 6–34 ft below land surface. Average residential casing extends to near the base of the first major clay or confining layer, with screened intervals set through the most consistent sand or sand/gravel aquifer. Grouting of casing with bentonite slurry (typically from surface to base casing) is standard for protection against surface contamination.