
Well Drillers Near Weyauwega, Wisconsin
The typical geology for the Weyauwega area is a sequence of clay-rich glacial till or clay, often interbedded with minor gravel, underlain by thick sands and gravels, with minor zones of silty sand or coarse sand at depth.
Showing contractors within 60 miles of Weyauwega. 90 results found.
- Typical depth
- 145 ft
- Water table
- 25 ft
- Contractors
- 90
90 Contractors


Allied Well, Septic & Pump
Valley Well Drilling
WELLS BY WELCH
Wells By Welch
Canopy Water Works Inc

CLEAN WATER TESTING

Dj's Water Services

Hintzke Well Drilling Inc.

Thoma Water Works

Town And Country Well Drilling, L.L.C.

Town And Country Well Drilling, L.L.C.

Abitz Water Services

Badger Well Drilling, Inc.

BADGERLAND CONNECTIONS LLC
Bertram-Junemann Well Drilling

Central Well And Pump Service, Inc
Daniel J Steffes
Well records near Weyauwega
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View Local Geology Report
A geological estimate for the Weyauwega area.
- Typical Well Depth
- 145 ft
- Static Water Level
- 25 ft
- Recommended Method
- Rotary - Mud Circulation
Detailed Summary
Based on a synthesis of representative well logs from around Weyauwega and surrounding Waupaca County, the most common subsurface sequence consists of a surface layer of clay (occasionally red or mixed with gravel) to around 70-110 feet, commonly interbedded with thinner lenses of gravel or stones in the upper profile. This is followed by a significant sequence (typically extending to 140-180 feet or deeper) of sand, gravel, or sand and gravel mixtures—often with variable coarseness (fine to coarse sand). Occasional silty sand and some transitions from sand to gravel are common near the bottom of the main aquifer zone. The total depths for residential wells that provide sustained 5-20 GPM typically range between 80 and 180 feet, with high-capacity and monitoring wells reaching depths of over 150-330+ feet in some cases. The static water level is typically encountered between 10 and 40 feet below ground surface. Casing is generally set through the clay and part or all of the sand/gravel layer to prevent caving, and completed wells use rotary mud circulation as the drilling method. Cement or bentonite grout is used to seal the annulus above the screen.
Expected Geological Layers
| Depth (Feet) | Formation Type | Description | Characteristics |
|---|---|---|---|
| 0 – 72 ft | Clay (glacial till, may include some gravel, can be red or brown) | Over-consolidated clay, locally interbedded with thin gravel, can be red or tan-brown. Common caving risk. Stiff to hard. | Color: Red/Brown/Tan Hardness: Stiff to Hard |
| 72 – 75 ft | Gravel/Stones | Gravel and stones, possibly transitional lag at base of glacial till. | Color: Mixed Hardness: Hard |
| 75 – 142 ft | Clay (glacial, may include silt or minor gravel) | Continued clay, often red, can be slightly silty or sandy, locally interbedded. | Color: Red/Brown Hardness: Stiff |
| 142 – 155 ft | Coarse Sand | Tan/brown coarse sand, high permeability, base of glacial sequence, beginning of main water-bearing aquifer units. | Color: Tan/Brown Hardness: Loose to Medium |
| 155 – 183 ft | Sand & Gravel | Mixed sand and gravel, variable sorting, water-bearing. Main aquifer zone for residential supply. | Color: Tan/Gray Hardness: Loose |
| 183 – 330 ft | Sand/Gravel with Interbeds | Coarse to fine sand and gravel, with pottery silt or clay-rich layers. Increasing proportions of gravel at greater depth, may include cobbles or transition to consolidated zones. | Color: Tan/Gray Hardness: Loose to Medium |
