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Sheboygan Falls, Wisconsin

Well Drillers Near Sheboygan Falls, Wisconsin

Typical Sheboygan Falls wells penetrate thick glacial sediments (mostly clay and some sand/gravel), becoming bedrock wells in dolomitic limestone below ~60–90 ft. Total depths for residential supply are often 150–300+ ft. The estimated static water level is ~35 ft. Most use rotary mud drilling, with casing set into the upper bedrock.

Showing contractors within 60 miles of Sheboygan Falls. 71 results found.

Typical depth
175 ft
Water table
35 ft
Contractors
71

71 Contractors

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View Local Geology Report

A geological estimate for the Sheboygan Falls area.

Typical Well Depth
175 ft
Static Water Level
35 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

The representative geological cross-section for Sheboygan Falls area wells (based on multiple sampled logs) shows a sequence starting at the surface with clay (often mottled with red/gray colors), locally mixed with lenses of sand or gravel. The upper glacial sediments typically reach depths of 50–90 ft, and may include thin sandy/gravelly zones or isolated stoney layers. Casing is generally set to the top of competent limestone or dolomite bedrock (60–90 ft). The underlying bedrock aquifer—dominantly dolomite or limestone—extends well below the bottom of the cased interval, often comprising the majority of the final well depth (to 150–350+ ft). Most residential wells are completed by drilling into this bedrock; yields are commonly in the 10–30 GPM range with static water levels around 10–55 ft below ground surface. Drilling is by rotary with mud circulation, with cement/bentonite sealing to casing depth. Anomalous thick clay or sand zones above bedrock may reflect local variations but do not affect the general model.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 50 ftClay (variable color)Mixed glacial clay, sometimes red/gray or with minor sand & gravel stringers; plastic to stiffColor: Red/Gray variable; may be mottled
Hardness: Soft to firm
50 – 65 ftSand & Gravel / Stoney layersInterbedded sand, gravel, and possible stoney clay/gravel layers; lenses, sometimes coarseColor: Gray/Tan
Hardness: Loose to firm
65 – 90 ftClay, stoney or siltyDense clay, sometimes with stones/gray coloration; at or near top of bedrockColor: Gray (may include stones, some sand)
Hardness: Stiff
90 – 300 ftDolomite/Limestone BedrockHard, gray, fractured dolomitic limestone (Silurian dolomite typical); water-bearing, main aquifer zoneColor: Gray/Tan
Hardness: Very hard (bedrock)

Frequently Asked Questions

A typical residential well in the Sheboygan Falls area is drilled to approximately 175 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 35 feet below the surface in this region.

The representative geological cross-section for Sheboygan Falls area wells (based on multiple sampled logs) shows a sequence starting at the surface with clay (often mottled with red/gray colors), locally mixed with lenses of sand or gravel. The upper glacial sediments typically reach depths of 50–90 ft, and may include thin sandy/gravelly zones or isolated stoney layers. Casing is generally set to the top of competent limestone or dolomite bedrock (60–90 ft). The underlying bedrock aquifer—dominantly dolomite or limestone—extends well below the bottom of the cased interval, often comprising the majority of the final well depth (to 150–350+ ft). Most residential wells are completed by drilling into this bedrock; yields are commonly in the 10–30 GPM range with static water levels around 10–55 ft below ground surface. Drilling is by rotary with mud circulation, with cement/bentonite sealing to casing depth. Anomalous thick clay or sand zones above bedrock may reflect local variations but do not affect the general model.