
Well Drillers Near Mayville, Wisconsin
A typical Mayville area well penetrates unconsolidated clay (sometimes gravelly), soft sediments, and a sequence of dolomitic limestone and shale, reaching bedrock within 80–140 ft; deeper wells encounter alternating limestone, shale, and, in a minority, sandstone (up to ~600 ft).
Showing contractors within 60 miles of Mayville. 108 results found.
- Typical depth
- 120 ft
- Water table
- 50 ft
- Contractors
- 108
108 Contractors


Antonioni Well & Pump Service Inc.
Rick's Well & Pump Service
4-D Water Well & Pump Service LLC
Anhalt Well Drilling & Pumps

Central Well And Pump Service, Inc
Daniel J Steffes

DJ's Water Service LLC
Douglas J Morin
Groth Drilling Co Inc

Hahn's Water Well Pump Service, Inc.
Jake J Schaitel

Jennemans Hardware Hank Inc

K-K Well Drilling

Ken Schaefer Well Pump and Water Treatment Consulting LLC
Klemme Brothers Water Well

Laabs Well & Pump LLC.
Well records near Mayville
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View Local Geology Report
A geological estimate for the Mayville area.
- Typical Well Depth
- 120 ft
- Static Water Level
- 50 ft
- Recommended Method
- Rotary - Mud Circulation
Detailed Summary
In the Mayville region, the most typical subsurface profile begins with a significant thickness of unconsolidated clay (sometimes including gravel, stones, or soft sand), generally from ground surface to 30–90 feet—averaging ~55 ft. Below this, hard or silty clay sometimes grades into a weathered or broken dolomitic limestone (Limerock) layer, which transitions to more competent limestone/dolostone. From about 80 ft downward, most wells encounter alternating layers of limestone and shale. High-capacity or deeper wells may reach a deeper sequence of massive limestone, thick shale, then optionally down to sandstone below 600 ft. For residential wells (yielding 5–15+ GPM), total depths of 80–180 ft are typical, with water most commonly sourced from shallow limestone or shale fractures. Static water levels average between 40–60 feet below the surface.
Expected Geological Layers
| Depth (Feet) | Formation Type | Description | Characteristics |
|---|---|---|---|
| 0 – 16 ft | Clay | Brown, silty to sandy clay, uppermost soil zone, occasionally some gravel/stones near base | Color: Brown/Gray Hardness: Soft |
| 16 – 55 ft | Clay with Gravel/Stones | Dense clay with scattered stones and/or gravel—may include soft/silty/clayey intervals or minor sand | Color: Brown-Gray Hardness: Medium |
| 55 – 90 ft | Limestone (weathered) | Broken or weathered dolomite/limestone, partially clay-filled; transitional bedrock interface | Color: Gray Hardness: Soft to Medium |
| 90 – 130 ft | Limestone/Dolomite | Massive dolomite/limestone, relatively competent; main aquifer zone for residential supply | Color: Gray Hardness: Hard |
| 130 – 185 ft | Shale | Gray, soft to hard shale, acts as confining layer; water strikes possible in fractured shale | Color: Gray/Greenish Hardness: Soft to Hard |
| 185 – 240 ft | Limestone | Limestone or dolostone intervals, possible water-bearing fractures, deeper wells only | Color: Light Gray Hardness: Medium-Hard |
| 240 – 390 ft | Shale | Thick shale (gray/green), less likely to be major aquifer, deeper wells only | Color: Gray-Green Hardness: Soft |
| 390 – 615 ft | Limestone | Massive limestone/dolomite, interbedded, deeper municipal or high-capacity supply | Color: Gray/Tan Hardness: Hard |
| 615 – 640 ft | Sandstone | Clean, fine sandstone; only present in deepest municipal/hicap wells | Color: Light Brown/Tan Hardness: Medium |
