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Oxford, Wisconsin

Well Drillers Near Oxford, Wisconsin

The typical Oxford-area well penetrates a sequence of sand and clay-dominated unconsolidated materials, underlain by sandstone, with occasional gravel or hard rock layers. Most residential wells (5-30 gpm) are completed between 80 and 140 feet, with irrigation/high-capacity wells extending deeper as needed for yield.

Showing contractors within 60 miles of Oxford. 24 results found.

Typical depth
100 ft
Water table
25 ft
Contractors
24

24 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+9 more

Roos Well Drilling Inc

Oxford, WI 53952
Water well drillingWell pump installationWell repair+3 more

Walker Well Drilling

Active Driller
Wisconsin Dells, WI 53965
Well drillingWell repairPump service+1 more
Wisconsin Well & Water Systems logo

Wisconsin Well & Water Systems

GRAND MARSH, WI 53936-
Water well drilling (PVC and steel)Geothermal drillingPump installation (submersible and jet)+3 more
Culligan Total Water of Baraboo logo

Culligan Total Water of Baraboo

2.6 (5)
Baraboo, WI 53913
Free basic water testCulligan water system rentalBottled water
Marshall Well Drilling Corp. logo

Marshall Well Drilling Corp.

Active Driller
Wisconsin Dells, WI 53965
New well drillingExisting well servicingWater testing+3 more

Quinnell's Septic & Well Services

Friendship, WI 53934
Septic system inspections (for realty sales)Well inspections (for realty sales)Water sampling+1 more
Smith Well Drilling logo

Smith Well Drilling

Baraboo, WI 53913
Water well drillingPump installation and repairPump parts and supplies+1 more
Allied Well, Septic & Pump logo

Allied Well, Septic & Pump

4.2 (5)
Waupaca, WI 54981
Well DrillingSeptic SystemsWell Pump Repair+6 more
Central Well And Pump Service, Inc logo

Central Well And Pump Service, Inc

BRANDON, WI 53919-0405
Pump installations and servicePressure tank installationWell abandonments+2 more
Dj's Water Services logo

Dj's Water Services

Active Driller
AMHERST, WI 54406-
WellsWater PumpsPressure Systems

DRILLWORX LLC

RANDOLPH, WI 53956
Well DrillingHorizontal Directional DrillingPump Installation

DRILLWORX, LLC

RANDOLPH, WI 53956
Drilling MethodsWater WellHorizontal Directional Drilling
Farago Drilled Wells logo

Farago Drilled Wells

Active Driller
Plainfield, WI 54966
Well repairs and new installationsSeptic repairs and new installationsPlumbing repairs and new installations+2 more
JOHNSON WELL DRILLING logo

JOHNSON WELL DRILLING

WAUPACA, WI 54981-
Well DrillingCommercial Well DrillingResidential Well Drilling+8 more
Kouba Group logo

Kouba Group

Active Driller
Reedsburg, WI 53959
Water well drillingExcavation servicesSeptic services+3 more

Lovelace Well Drilling

Randolph, WI 53956
Well drillingWater well creationPump installation and service+3 more
Municipal Well & Pump logo

Municipal Well & Pump

WAUPUN, WI 53963-
Well ServicesTelevising & LoggingMaintenance Programs

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Well records near Oxford

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View Local Geology Report

A geological estimate for the Oxford area.

Typical Well Depth
100 ft
Static Water Level
25 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on representative well logs from the Oxford region, the subsurface profile typically consists of: (1) surficial sandy/sandy loam soils, (2) interbedded sand and occasional sandy clay or silt layers, often with some coarse or gravelly intervals, and zones of clay at variable depths, (3) a thick, generally medium to coarse sand or sand-and-gravel aquifer (primary water-producing zone for most residential wells), and (4) underlying sandstone, with some records noting soft/fine sandstone followed by harder or more consolidated bedrock at greater depths. The unconsolidated aquifer (sand/gravel) is usually cased through, with the screen or open bottom set just above or into sandstone. Typical static water levels are shallow; most residential wells achieving 10–30 gpm are completed at ~80–120 feet, while irrigation/high-capacity wells may be 275–320+ feet depending on local demand and geology. Clay intervals may extend locally to 100+ feet but are usually interbedded with water-bearing sand.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
02 ftSandy Loam/TopsoilSand or sandy loam, brown, loose; organic topsoil at surface.Color: Brown
Hardness: Soft
225 ftSand/Sandy Clay (occasional silt, loam, or boulders)Fine to medium sand, occasional sandy clay, rare boulders, some streaks of silt.Color: Tan/Yellow/Brown
Hardness: Loose to Firm
2575 ftSand (fine to medium, local coarse or with gravel)Dominantly medium to coarse sand, sometimes with fine gravel or silt layers.Color: Tan/Yellow
Hardness: Medium
75100 ftSand (medium/coarse), local coarse, gravelly or clayey sandAquifer zone; major water-producing sand, often with some gravel or clayey intervals.Color: Light Tan
Hardness: Medium to Coarse
100150 ftClay and/or Silty Sand (occasionally present as lenses)Clay or silty/clayey sand, present in some but not all wells, may be discontinuous.Color: Gray/Olive/Buff
Hardness: Soft to Firm
150272 ftSand (medium to coarse, with gravel)Aquifer continues deeper for high capacity wells, generally medium/coarse sand and occasional gravel beds.Color: Yellow/Brown
Hardness: Medium
272320 ftSandstoneSoft to hard sandstone, serves as a deeper aquifer or well bottom; harder and less productive near base.Color: Tan/Light Brown
Hardness: Soft to Firm to Hard
320340 ftShale/Rock (if present)Hard shale or consolidated rock, not always encountered; represents base of typical wells.Color: Gray
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Oxford area is drilled to approximately 100 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 representative well logs from the Oxford region, the subsurface profile typically consists of: (1) surficial sandy/sandy loam soils, (2) interbedded sand and occasional sandy clay or silt layers, often with some coarse or gravelly intervals, and zones of clay at variable depths, (3) a thick, generally medium to coarse sand or sand-and-gravel aquifer (primary water-producing zone for most residential wells), and (4) underlying sandstone, with some records noting soft/fine sandstone followed by harder or more consolidated bedrock at greater depths. The unconsolidated aquifer (sand/gravel) is usually cased through, with the screen or open bottom set just above or into sandstone. Typical static water levels are shallow; most residential wells achieving 10–30 gpm are completed at ~80–120 feet, while irrigation/high-capacity wells may be 275–320+ feet depending on local demand and geology. Clay intervals may extend locally to 100+ feet but are usually interbedded with water-bearing sand.