Well Drillers Near Kewaunee, Wisconsin
A typical Kewaunee County residential well penetrates a sequence of clay-rich glacial sediments, underlain by a sand/gravel or stony zone, grading into limestone bedrock—the principal aquifer.
Showing contractors within 60 miles of Kewaunee. 24 results found.
- Typical depth
- 125 ft
- Water table
- 45 ft
- Contractors
- 24
24 Contractors
Chuck Massart Well & Pump Repair LLC
Dan's Pump Services
Directional drilling services inc
Euclide Well Drilling

Kimmes Well & Pump, Inc.
Peterson's Pump and Well Repair LLC

Retzlaff & Gregorich Well Drilling
Abitz Water Services
Chicken Young Well Drilling

Ground Source

Ground Source Well Drilling
Kozikowski Well & Pump, Inc.

Leo Van De Yacht Well Drilling Inc

Luisier Drilling Inc
Schmidt's Well Drilling & Pump
Twenty-Four-Seven Well & Pump

Vande Yacht Pump Installing Inc

Weber Well Drilling Inc
Well records near Kewaunee
Check depths and logs of existing wells in the area before you drill.
Open well map →Wisconsin well owner guide
Costs, permits, maintenance tips for private wells in Wisconsin.
Open guide →View Local Geology Report
A geological estimate for the Kewaunee area.
- Typical Well Depth
- 125 ft
- Static Water Level
- 45 ft
- Recommended Method
- Rotary - Mud Circulation
Detailed Summary
Synthesizing well logs across Kewaunee County, the most representative geologic profile begins with a substantial interval of clay (sometimes with stones or gravel), extending from the surface to approximately 30-140 feet, depending on local conditions. This is frequently underlain by a discontinuous sand and/or gravel or stony interval of moderate thickness (ranging from 10 to 40 feet), acting as a transition to the underlying limestone/dolomite bedrock aquifer. The bedrock limestone is universally encountered and constitutes the primary water-bearing formation. Casing generally anchors into the top of bedrock, with wells completed open-hole in limestone. Static water levels are highly variable but most commonly range from 15 to 100 feet below ground surface. Wells producing 5–40+ GPM for a residential setting typically reach 100–165 feet, with high-capacity systems extending to 200+ feet as needed. All wells are constructed by rotary mud circulation with a cement or clay slurry grout seal.
Expected Geological Layers
| Depth (Feet) | Formation Type | Description | Characteristics |
|---|---|---|---|
| 0 – 5 ft | Clay | Brown or gray clay, locally may have stones | Color: Brown/Gray Hardness: Soft |
| 5 – 40 ft | Sand/Gravel or Stony Clay | Sand with gravel or clay with stones, may be interbedded; significant as transition zone | Color: Mixed Hardness: Medium |
| 40 – 120 ft | Clay | Hard compact silty or sandy clay, sometimes with gravel; non-caving | Color: Brown/Grey Hardness: Hard |
| 120 – 140 ft | Gravel/Stone | Coarse gravel or stone, occasional thin sand layers | Color: Brown/Gray Hardness: Hard |
| 140 – 220 ft | Limestone/Dolomite | Fractured, gray limestone or dolomite bedrock; primary aquifer, water bearing | Color: Gray Hardness: Hard |
