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Manistique, Michigan

Well Drillers Near Manistique, Michigan

Typical Manistique area residential well: surficial sand, gravel, and clay, overlying thick sequence of limestone (often with interbedded shale, clay, and dolomite), water from fractured or sandy limestone.

Showing contractors within 60 miles of Manistique. 4 results found.

Typical depth
120 ft
Water table
30 ft
Contractors
4

4 Contractors

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Kopecky Well Drilling-Pump Services logo

Kopecky Well Drilling-Pump Services

Active Driller
Manistique, MI 49854
Well DrillingPump InstallationPump Repair+6 more

Saunders & Son Well Drilling

McMillan, MI 49853
Well DrillingWell Maintenance

Howard's Water Pumps & Services

Escanaba, MI 49829
Pump InstallationPump Repair

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View Local Geology Report

A geological estimate for the Manistique area.

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

Detailed Summary

Wells in the Manistique area most commonly encounter an upper layer of sand and/or gravel, sometimes interbedded with clay or loam, to depths of approximately 10–30 ft. Below this, a substantial clay or clay-gravel unit is often present, ranging from 10–50 ft in thickness. The remainder of the well interval almost universally consists of limestone bedrock—commonly with interlayers of tan, brown, white, and gray limestone, frequent minor inclusions of shale, dolomite, gravel, and clay, and occasional water-bearing fractures or sandy seams. The water table is encountered near the top of the bedrock or within the limestone, typically at variable depths depending on local elevation. Most residential wells achieve yields of 10–15+ GPM in the depth range of 100–140 ft, with deeper wells increasing the likelihood of encountering larger water-bearing fractures for higher capacity needs.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
03 ftSand / Loam / GravelBrown to sandy loam or sand, locally with gravel or topsoil. Occasional surface clay.Color: Brown/gray
Hardness: Loose to firm
328 ftClay / Sandy Clay / Gravelly ClayMostly red or gray clay, sometimes sandy or gravely; locally includes some stratified sand or gravel seams.Color: Red/gray
Hardness: Soft to stiff
2850 ftTransition Zone (Gravel/Sand/Clay/Weathered Limestone)Interbedded gravel, sand, and weathered limestone; may locally include broken limestone or cherty horizons.Color: Varied—gray, brown, tan
Hardness: Loose to moderately hard
50100 ftLimestone and Interbedded FormationsGray, tan, brown, or white limestone, commonly cherty in sections; may include dolomite, shale, clay seams, or minor sand—water-bearing features often encountered in this interval.Color: Gray/tan/brown/white
Hardness: Hard
100140 ftMassive LimestonePredominantly limestone, with sparse interbeds of shale or clay; fractures and sandy seams present, principal aquifer zone for higher-yield wells.Color: Gray/tan/white
Hardness: Very hard
140160 ftLower Limestone (Locally with Dolomite)Gray to tan limestone, potentially with dolomite, minor clay, and dark streaks; only encountered in deepest sampled wells.Color: Gray/tan
Hardness: Very hard

Frequently Asked Questions

A typical residential well in the Manistique 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 30 feet below the surface in this region.

Wells in the Manistique area most commonly encounter an upper layer of sand and/or gravel, sometimes interbedded with clay or loam, to depths of approximately 10–30 ft. Below this, a substantial clay or clay-gravel unit is often present, ranging from 10–50 ft in thickness. The remainder of the well interval almost universally consists of limestone bedrock—commonly with interlayers of tan, brown, white, and gray limestone, frequent minor inclusions of shale, dolomite, gravel, and clay, and occasional water-bearing fractures or sandy seams. The water table is encountered near the top of the bedrock or within the limestone, typically at variable depths depending on local elevation. Most residential wells achieve yields of 10–15+ GPM in the depth range of 100–140 ft, with deeper wells increasing the likelihood of encountering larger water-bearing fractures for higher capacity needs.