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Danbury, Wisconsin

Well Drillers Near Danbury, Wisconsin

Typical Danbury wells encounter a sequence of sand and gravel, sometimes with clay, extending to moderate depths, with abundant water-bearing units suited for residential use.

Showing contractors within 60 miles of Danbury. 48 results found.

Typical depth
90 ft
Water table
25 ft
Contractors
48

48 Contractors

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Well records near Danbury

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View Local Geology Report

A geological estimate for the Danbury area.

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

Detailed Summary

The representative geological profile for the Danbury, WI area, synthesized from a sample of well logs, shows a consistent pattern dominated by unconsolidated sand and gravel layers, often interbedded with clay or occasional cobbles/boulders. Wells are generally completed entirely within these glacial/fluvial deposits. Static water levels are shallow to moderate, typically 16–45 ft below grade. The most common sequence is: a surface soil and/or upper sand & gravel unit; local clay/gravel/silt or hardpan interbeds, especially at intermediate depths; then a basal sand (sometimes with gravel) which is commonly the primary aquifer. Wells for reliable residential yield (5–15+ GPM) are typically completed at 80–110 ft. Higher capacity wells or those supplying larger demands may be screened slightly deeper or within thicker sand/gravel units extending to 150–200+ ft where present.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 2 ftTopsoilThin organic or loamy soil horizon; may include silt and cobbles.Color: Brown
Hardness: Loose
2 – 50 ftSand and GravelClean to dirty sand and gravel, local zones with cobbles, moderate caving; excellent water bearing.Color: Varies: yellow-brown/dark brown
Hardness: Loose to medium
50 – 80 ftClay with Gravel/Silty SandInterbedded sandy clay, sandy red clay, or clayey gravel; some localized hardpan or compacted layers. May act as minor aquitard.Color: Red/brown/gray
Hardness: Firm to hard
80 – 110 ftCoarse Sand and GravelCoarse water-bearing sand & gravel, commonly caving, sometimes with occasional cobbles. Major aquifer unit.Color: Light brown/yellow/gray
Hardness: Loose
110 – 180 ftSandy Clay/Clay with Sand (deeper wells only)Layer not always present; found in deeper or outlying wells. Dense sandy to firm clay, intermixed with sand.Color: Brown/gray
Hardness: Firm to hard
180 – 206 ftSand (Deep Basal Unit)Clean to slightly gravelly sand, major water-producing zone in deepest wells.Color: Gray/yellow
Hardness: Loose

Frequently Asked Questions

A typical residential well in the Danbury area is drilled to approximately 90 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 25 feet below the surface in this region.

The representative geological profile for the Danbury, WI area, synthesized from a sample of well logs, shows a consistent pattern dominated by unconsolidated sand and gravel layers, often interbedded with clay or occasional cobbles/boulders. Wells are generally completed entirely within these glacial/fluvial deposits. Static water levels are shallow to moderate, typically 16–45 ft below grade. The most common sequence is: a surface soil and/or upper sand & gravel unit; local clay/gravel/silt or hardpan interbeds, especially at intermediate depths; then a basal sand (sometimes with gravel) which is commonly the primary aquifer. Wells for reliable residential yield (5–15+ GPM) are typically completed at 80–110 ft. Higher capacity wells or those supplying larger demands may be screened slightly deeper or within thicker sand/gravel units extending to 150–200+ ft where present.