
Well Drillers Near Waukesha, Wisconsin
The typical geological profile for the Waukesha region features a sequence of clay, sand/gravel, hardpan or clay cobbles/silty clay, and limestone/dolomite bedrock, with residential wells commonly drawing from the upper limestone layers.
Showing contractors within 60 miles of Waukesha. 99 results found.
- Typical depth
- 180 ft
- Water table
- 80 ft
- Contractors
- 99
99 Contractors


CTW Corporation

Guthrie & Frey Water Conditioning LLC

Roschi Brothers Well Drilling & Pump Service, Inc.

Roschi Brothers Well Drilling & Pump Service, Inc.

Water Doctors
4-D Water and Pump Service LLC
4-D Water Well & Pump Service LLC
Anhalt Well Drilling & Pumps

Aqua Well & Pump Systems, Inc

Biersack Well Service

Bracker Pump & Well Service-Wellpumps.com

Clean Water Center

Cost Less Well Service

D&D Well & Pumps LLC

Groth Water Wells Inc.
Well records near Waukesha
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 →Not in Waukesha? Search well drilling near me in the national directory, or find well repair near me and well pump service near me for work on an existing well.
View Local Geology Report
A geological estimate for the Waukesha area.
- Typical Well Depth
- 180 ft
- Static Water Level
- 80 ft
- Recommended Method
- Rotary - Mud Circulation
Detailed Summary
Based on the synthesis of multiple well logs from the Waukesha area, the most representative subsurface profile consists of: (1) a surficial clay layer; (2) an interval of sand and gravel; (3) a thicker zone of hardpan, sandy clay, or clay with cobbles; (4) underlain by competent limestone or dolomite bedrock. Minor local variations occur, but these four units are routinely present across the area. The limestone bedrock typically serves as the main aquifer zone for residential and municipal wells, and is encountered at median depths of 90–120 ft below ground, with wells commonly finished between 140 and 200 ft, but municipal wells may extend deeper. Static water levels are usually between 65 and 100 ft below ground. Rotary mud drilling is the standard method. Casing is generally set through the entire unconsolidated sequence (typically to the top of limestone), with grout or sealing to comparable depths.
Expected Geological Layers
| Depth (Feet) | Formation Type | Description | Characteristics |
|---|---|---|---|
| 0 – 10 ft | Clay | Brown to gray clay, silty or sandy in places | Color: Brown/Gray Hardness: Soft |
| 10 – 45 ft | Sand and Gravel | Clean to silty sand and gravel, occasional cobbles, good permeability | Color: Tan/Gray Hardness: Loose |
| 45 – 90 ft | Hardpan / Clay / Sandy Clay / Clay with Cobbles | Dense hard clay, sandy or with gravel/cobbles, sometimes called hardpan or containing silt | Color: Brown/Gray/Blue Hardness: Stiff to hard |
| 90 – 200 ft | Limestone / Dolomite (Bedrock) | Competent limestone or dolomite, fractured in some intervals, primary water-bearing zone for most wells (uppermost 20–60 ft often most productive). Niagara Dolomite common. | Color: Light gray to tan Hardness: Hard |

