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Howard City, Michigan

Well Drillers Near Howard City, Michigan

Typical Howard City area wells encounter a sequence of clay and sand, often alternating, with water-bearing sand or sand/gravel typically found between 35 and 110 feet deep.

Showing contractors within 60 miles of Howard City. 77 results found.

Typical depth
50 ft
Water table
18 ft
Contractors
77

77 Contractors

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View Local Geology Report

A geological estimate for the Howard City area.

Typical Well Depth
50 ft
Static Water Level
18 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

The most representative geological profile in the Howard City area, as seen from multiple well logs, starts at the surface with a layer of clay (frequently brown, red, or gray), followed by alternating layers of sand and clay. Water-bearing sand or sand mixed with gravel is a consistent aquifer unit, usually found below the primary confining clay layer, commonly between 35 and 110 feet. Clay layers tend to show color variations, and the usable aquifer is most frequently a medium to coarse sand or sand and gravel. The average static water level is around 16 to 22 feet below grade. Most residential wells producing 10–15+ GPM are completed between 45 and 80 feet, while higher capacity wells may target thicker sand/gravel units extending to 100–110 feet.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 3 ftTopsoil/ClayBrown, red, or gray clay or soil at surface, sometimes with topsoil.Color: Brown/Red/Gray
Hardness: Soft
3 – 15 ftClay (with some sand inclusions in places)Primarily clay; often transitions from brown to gray; may include thin sand seams.Color: Brown to Gray
Hardness: Soft to Medium
15 – 35 ftSand (occasionally thin clay layers)Fine to medium sand, minor clay partings in some wells.Color: Brown
Hardness: Loose
35 – 45 ftClay or Clay with GravelGray or mixed clay with some gravel; moderate confining material.Color: Gray
Hardness: Medium
45 – 75 ftSand or Sand & Gravel (water-bearing)Main aquifer zone – coarse to medium sand, often with significant gravel content.Color: Brown
Hardness: Loose
75 – 99 ftSand with Clay partingsDeeper sand, with some layers of brown or gray clay; locally more gravelly.Color: Brown/Gray
Hardness: Moderate
99 – 110 ftSand & Gravel (deep aquifer extension)Thick, coarse sand/gravel, excellent water producer where present.Color: Brown
Hardness: Loose

Frequently Asked Questions

A typical residential well in the Howard City area is drilled to approximately 50 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 18 feet below the surface in this region.

The most representative geological profile in the Howard City area, as seen from multiple well logs, starts at the surface with a layer of clay (frequently brown, red, or gray), followed by alternating layers of sand and clay. Water-bearing sand or sand mixed with gravel is a consistent aquifer unit, usually found below the primary confining clay layer, commonly between 35 and 110 feet. Clay layers tend to show color variations, and the usable aquifer is most frequently a medium to coarse sand or sand and gravel. The average static water level is around 16 to 22 feet below grade. Most residential wells producing 10–15+ GPM are completed between 45 and 80 feet, while higher capacity wells may target thicker sand/gravel units extending to 100–110 feet.