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Weyauwega, Wisconsin

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

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FEATURED
Sam's Well Drilling logo

Sam's Well Drilling

Active Driller
Randolph, WI 53956
Well DrillingResidential Well DrillingCommercial Well Drilling+7 more
Allied Well, Septic & Pump logo

Allied Well, Septic & Pump

4.2 (5)
Waupaca, WI 54981
Well DrillingPump RepairWell Abandonment+1 more
Valley Well Drilling logo

Valley Well Drilling

Weyauwega, WI 54983
Well DrillingPump InstallationWell Maintenance+1 more

WELLS BY WELCH

Active Driller
FREMONT, WI 54940-9602
Well DrillingResidential Well DrillingCable Tool+5 more

Wells By Welch

Active Driller
Fremont, WI 54940
Residential Well DrillingPump RepairWell Rehabilitation+2 more

Canopy Water Works Inc

Hortonville, WI 54944
Pump RepairWell AbandonmentFiltration+1 more
CLEAN WATER TESTING logo

CLEAN WATER TESTING

APPLETON, WI 54914-
Well InspectionBacteria/Coliform TestingWater Sampling
Dj's Water Services logo

Dj's Water Services

Active Driller5.0 (20)
AMHERST, WI 54406-
Well DrillingPump ServicesPressure Tank Installation
Hintzke Well Drilling Inc. logo

Hintzke Well Drilling Inc.

Active Driller4.3 (30)
NEW LONDON, WI 54961-9802
Well DrillingPump ServicesPump Repair+3 more
Thoma Water Works logo

Thoma Water Works

5.0 (5)
Berlin, WI 54923
Pump InstallationWell InspectionPotability Testing+3 more
Town And Country Well Drilling, L.L.C. logo

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

Berlin, WI 54923
Well DrillingPump RepairWell Abandonment
Town And Country Well Drilling, L.L.C. logo

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

BERLIN, WI 54923-
Well DrillingPump Installation
Abitz Water Services logo

Abitz Water Services

Freedom, WI 54130
Pump ServicesPump InstallationPump Repair+9 more
Badger Well Drilling, Inc. logo

Badger Well Drilling, Inc.

MT CALVARY, WI 53057-
Well DrillingPump InstallationPump Repair+5 more
BADGERLAND CONNECTIONS LLC logo

BADGERLAND CONNECTIONS LLC

MALONE, WI 53049
Horizontal Directional DrillingExcavationTrenching

Bertram-Junemann Well Drilling

Active Driller
Rudolph, WI 54475
Well DrillingPump InstallationWater Line Installation
Central Well And Pump Service, Inc logo

Central Well And Pump Service, Inc

BRANDON, WI 53919-0405
Pump InstallationWell DisinfectionWell Abandonment+2 more

Daniel J Steffes

Active Driller
Mt. Calvary, WI 53057
Well DrillingPump InstallationPump Replacement+3 more

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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 TypeDescriptionCharacteristics
072 ftClay (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
7275 ftGravel/StonesGravel and stones, possibly transitional lag at base of glacial till.Color: Mixed
Hardness: Hard
75142 ftClay (glacial, may include silt or minor gravel)Continued clay, often red, can be slightly silty or sandy, locally interbedded.Color: Red/Brown
Hardness: Stiff
142155 ftCoarse SandTan/brown coarse sand, high permeability, base of glacial sequence, beginning of main water-bearing aquifer units.Color: Tan/Brown
Hardness: Loose to Medium
155183 ftSand & GravelMixed sand and gravel, variable sorting, water-bearing. Main aquifer zone for residential supply.Color: Tan/Gray
Hardness: Loose
183330 ftSand/Gravel with InterbedsCoarse 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

Frequently Asked Questions

A typical residential well in the Weyauwega area is drilled to approximately 145 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 25 feet below the surface in this region.

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.