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Lachine, Michigan

Well Drillers Near Lachine, Michigan

Typical Lachine area wells penetrate unconsolidated glacial materials (clays, gravels, sands) overlying bedrock, with increasing prevalence of limestone and shale at depth. Shallow to moderate wells (60–120 ft) are productive; deeper bedrock wells are sometimes needed.

Showing contractors within 60 miles of Lachine. 26 results found.

Typical depth
75 ft
Water table
15 ft
Contractors
26

26 Contractors

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View Local Geology Report

A geological estimate for the Lachine area.

Typical Well Depth
75 ft
Static Water Level
15 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

A representative geological profile for the Lachine area of Alpena County, MI, based on synthesis from multiple well logs, consists of a surficial sequence of unconsolidated glacial deposits (clay, gravel, sand) of variable thickness from surface to 40–60 feet, typically grading into more gravelly or sandy zones. Beneath this zone, wells commonly encounter set intervals of consolidated bedrock, most often alternating between limestone and shale of various colors and hardness, from approximately 44–60 feet down to depths exceeding 200 feet in deeper wells. The most productive residential wells typically terminate in coarse sand/gravel or upper limestone, with high-yield wells achieved at moderate depths. Static water levels are generally shallow (3–40 ft below ground). The most common drilling method is rotary with mud circulation, and casing is typically installed through the unconsolidated zones and at least partially into bedrock for deeper wells.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 7 ftClay & GravelGray/brown glacial till: clay matrix with gravel inclusions, possibly some sand.Color: Gray/Brown
Hardness: Soft–Firm
7 – 25 ftSand & GravelCoarse sand and gravel, often water-bearing, includes some clay layers.Color: Brown–Tan
Hardness: Loose–Medium
25 – 44 ftGravel/Sand & ClayeyMixture of sand, gravel, occasional clay seams. Main shallow aquifer zone.Color: Variegated
Hardness: Soft–Medium
44 – 60 ftClay (occasional Stones/Gravelly)Dense clay or clay with stones, locally can be confining.Color: Gray/Tan
Hardness: Firm–Hard
60 – 85 ftLimestone with Shale (soft/interbedded)Transition to bedrock; alternating soft shale & limestone seams. May include brown, gray, tan or black limestone.Color: Brown/Gray/Black
Hardness: Medium–Hard
85 – 210 ftLimestone (various)Massive limestone, occasionally interbedded with thin shale; zones of brown, gray, tan, black, or white limestone.Color: Gray/Brown/Black/White
Hardness: Hard
210 – 250 ftLimestone with interbedded ShaleAlternating hard limestone and softer shale layers, some clayey.Color: Gray/Black/Tan
Hardness: Medium–Hard
250 – 300 ftLimestone (Tan/Gray, Hard)Thick section of hard limestone, locally fossiliferous.Color: Tan/Gray
Hardness: Hard
300 – 320 ftShaleSoft, dark shale, marks transition to deeper bedrock.Color: Dark gray/Black
Hardness: Soft

Frequently Asked Questions

A typical residential well in the Lachine area is drilled to approximately 75 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 15 feet below the surface in this region.

A representative geological profile for the Lachine area of Alpena County, MI, based on synthesis from multiple well logs, consists of a surficial sequence of unconsolidated glacial deposits (clay, gravel, sand) of variable thickness from surface to 40–60 feet, typically grading into more gravelly or sandy zones. Beneath this zone, wells commonly encounter set intervals of consolidated bedrock, most often alternating between limestone and shale of various colors and hardness, from approximately 44–60 feet down to depths exceeding 200 feet in deeper wells. The most productive residential wells typically terminate in coarse sand/gravel or upper limestone, with high-yield wells achieved at moderate depths. Static water levels are generally shallow (3–40 ft below ground). The most common drilling method is rotary with mud circulation, and casing is typically installed through the unconsolidated zones and at least partially into bedrock for deeper wells.