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. 45 results found.
- Typical depth
- 125 ft
- Water table
- 45 ft
- Contractors
- 45
45 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

Ground Source

Ground Source Well Drilling
Kozikowski Well & Pump, Inc.

Leo Van De Yacht Well Drilling Inc

Luisier Drilling Inc

Packerland Well Service
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 →Nearby Wisconsin city directories
Not in Kewaunee? Search well drilling near me in the national directory, or find well service and repair near me and well pump service near me for work on an existing well.
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 |