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Richland Center, Wisconsin

Well Drillers Near Richland Center, Wisconsin

Typical Richland Center area wells encounter a sequence from surface clays and/or sandy silts, into alternating shale and sandstone formations, with deeper wells encountering firmer/harder shale and thick, regionally extensive sandstone aquifers.

Showing contractors within 60 miles of Richland Center. 43 results found.

Typical depth
140 ft
Water table
55 ft
Contractors
43

43 Contractors

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Advanced Pump and Well Solutions Inc logo

Advanced Pump and Well Solutions Inc

Richland Center, WI 53581
Pump ServicesPump RepairConstant Pressure Systems+7 more
D&T Well Services LLC logo

D&T Well Services LLC

Soldiers Grove, WI 54655
Well DrillingPump ReplacementWell Maintenance+3 more
Kouba Group logo

Kouba Group

Active Driller
Reedsburg, WI 53959
Well DrillingExcavation
Affordable Pump & Well Repair Inc logo

Affordable Pump & Well Repair Inc

La Crosse, WI 54601
Pump RepairPump ReplacementWater Testing
Culligan Total Water of Baraboo logo

Culligan Total Water of Baraboo

2.6 (5)
Baraboo, WI 53913
Water TestingFiltrationReverse Osmosis+1 more
Faherty & Son Well Drilling LLC logo

Faherty & Son Well Drilling LLC

Active Driller
Platteville, WI 53818
Residential Well DrillingCommercial Well DrillingGeothermal Services+1 more
KOUBA DRILLING LLC logo

KOUBA DRILLING LLC

Active Driller
REEDSBURG, WI 53959-
Well DrillingResidential Well DrillingCommercial Well Drilling+2 more
Marshall Well Drilling Corp. logo

Marshall Well Drilling Corp.

Active Driller
Wisconsin Dells, WI 53965
Well DrillingWater TestingFiltration
Mid-Wisconsin Pump & Well Service LLC logo

Mid-Wisconsin Pump & Well Service LLC

Sparta, WI 54656
Pump ServicesPump InstallationConstant Pressure Systems+3 more

Nelson Well Service, LLC

Active Driller
Genoa, WI 54632
Pump InstallationJet PumpsWell Maintenance+1 more

Walker Well Drilling

Active Driller
Wisconsin Dells, WI 53965
Well DrillingPump ServicesPump Installation+1 more
Watermaker Well Drilling logo

Watermaker Well Drilling

Arena, WI 53503
Driven Well ConstructionPump InstallationWater Line Installation
Wepking Pump Service Inc. logo

Wepking Pump Service Inc.

Lancaster, WI 53813
Pump InstallationPump RepairConstant Pressure Systems+5 more
Wisconsin Well & Water Systems logo

Wisconsin Well & Water Systems

GRAND MARSH, WI 53936-
Well DrillingPump InstallationPump Repair+3 more

MCAFEE WELL DRLG & PUMP SERV INC

La Valle, WI 53941
Well DrillingPump ServicesPump Installation+1 more

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View Local Geology Report

A geological estimate for the Richland Center area.

Typical Well Depth
140 ft
Static Water Level
55 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on well records from across Richland County in the vicinity of Richland Center, the most representative geological profile starts with a surface layer of clay, sandy silt, or sandy dirt (with or without gravel), becoming interbedded with silty or organic clay. This is typically followed by a thick sequence of shaley materials (often tan/brown, soft or hard), sometimes with thin limestone layers in the upper part of the sequence. Progressing deeper, alternating but dominated by hard shale and medium to hard brown or white sandstone units are observed. Sandstone becomes especially significant below 90–100 ft in most wells, comprising the principal drinking water aquifer. Shallower, high-yield unconsolidated sand/gravel aquifers occur in some areas but are not regionally extensive. Typical residential wells (5–15+ GPM) are completed in the upper to middle portions of the main sandstone unit, generally between 100 and 250 ft. High-capacity wells or deeper residential wells may extend 250 to 400 ft, accessing thicker, regional sandstones below more extensive shale units.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
018 ftClay/Silt, Sandy Dirt/SoilSurface clay or silty sandy soil—may be organic, soft, often moist, sometimes with gravelColor: Brown/gray/tan
Hardness: Soft
1840 ftClay with Shale & occasional LimestoneSilty or pure clay with interbedded shale or occasional limestone; increasing shale and firmness downwardColor: Tan to brown
Hardness: Soft to medium
4090 ftShaleShaley clay, shaley silt, or massive shale (locally with some limestone layers/pockets)Color: Tan to brown, occasionally gray
Hardness: Medium to hard
90140 ftSandstone (minor shale interbeds)White, tan, or brown sandstone, often fine to medium grained, main water-bearing zone for residential wellsColor: White, tan, brown
Hardness: Medium to hard
140180 ftShale (firm to hard)Thicker, firmer shale, brown to blue, often described as hard; minor soft pockets possibleColor: Brown, gray-blue
Hardness: Hard
180250 ftSandstone (principal regional aquifer)Thicker, regionally extensive sandstone—white, tan, or brown, main aquifer for higher capacity wells and some residential wellsColor: Tan, brown, white
Hardness: Medium to hard
250400 ftSandstone and occasional ShaleVery thick sandstone sequence with less frequent interbedded hard shale layers; becomes dominant below 250 ft in deep wellsColor: White, tan, brown
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Richland Center area is drilled to approximately 140 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 55 feet below the surface in this region.

Based on well records from across Richland County in the vicinity of Richland Center, the most representative geological profile starts with a surface layer of clay, sandy silt, or sandy dirt (with or without gravel), becoming interbedded with silty or organic clay. This is typically followed by a thick sequence of shaley materials (often tan/brown, soft or hard), sometimes with thin limestone layers in the upper part of the sequence. Progressing deeper, alternating but dominated by hard shale and medium to hard brown or white sandstone units are observed. Sandstone becomes especially significant below 90–100 ft in most wells, comprising the principal drinking water aquifer. Shallower, high-yield unconsolidated sand/gravel aquifers occur in some areas but are not regionally extensive. Typical residential wells (5–15+ GPM) are completed in the upper to middle portions of the main sandstone unit, generally between 100 and 250 ft. High-capacity wells or deeper residential wells may extend 250 to 400 ft, accessing thicker, regional sandstones below more extensive shale units.