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Hortonville, Wisconsin

Well Drillers Near Hortonville, Wisconsin

The typical Hortonville-area well penetrates a sequence of clay/sandy material, underlain by alternating limestone/dolomite and sandstone layers, reaching residential yields of 10–30 GPM at depths ~90–160 ft, with bedrock wells often exceeding 200 ft.

Showing contractors within 60 miles of Hortonville. 64 results found.

Typical depth
130 ft
Water table
80 ft
Contractors
64

64 Contractors

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View Local Geology Report

A geological estimate for the Hortonville area.

Typical Well Depth
130 ft
Static Water Level
80 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Wells in the Hortonville region characteristically pass through a thin surficial clay (or clay with gravel or sand admixture), grading into limestone/dolomite and prominent sandstone aquifers. These carbonate and sandstone bedrock units alternate with typical first significant limestone/dolomite bedrock appearing between 10 to 45 ft, underlain by alternating sequences that may transition more than once with depths. Overall, groundwater is typically sourced from limestone/dolomite or sandstone at depths between 90 and over 200 ft for high capacity. Wells consistently use rotary-mud circulation, with surface casing extending to the base of unconsolidated material (~40–100 ft), and are sealed with neat cement or mud grout. Static water levels mostly fall in the 35–90 ft range. Given pump test yields, a reliable residential well (5–15+ GPM) is generally achieved by 130 ft, while high-capacity installations target depths of 180–230+ ft.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 20 ftClay/Clay w Gravel or SandSurficial clay with variable sand or gravel, sometimes described as sandy clay or organic soil.Color: Gray, Red, Black
Hardness: Soft
20 – 45 ftSand & Clay or HardpanCompact sandy clay, hardpan, or sand/clay interbeds.Color: Tan, Brown, Red
Hardness: Firm
45 – 70 ftLimestone/DolomiteSolid limestone or dolomite bedrock, occasionally with minor shale.Color: Tan, Brown, Gray
Hardness: Hard
70 – 120 ftSandstoneClean or slightly shaley sandstone, sometimes interbedded with limestone/dolomite.Color: White, Red, Tan, Gray
Hardness: Firm to Hard
120 – 160 ftLimestone/Dolomite (with Sandstone Interbeds Possible)Thick limestone/dolomite with potential thin sandstone or shale partings.Color: Tan, Gray, Brown
Hardness: Hard
160 – 210 ftSandstone (possible shaley part)Massive sandstone aquifer, base may be shaley.Color: Gray, Tan, Red
Hardness: Firm to Hard
210 – 230 ftSandstone/Limestone (variable)Bedrock, typically sandstone but variable thickness and lithology, may include dolomite or limestone.Color: Gray, Tan, Brown
Hardness: Firm

Frequently Asked Questions

A typical residential well in the Hortonville area is drilled to approximately 130 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 80 feet below the surface in this region.

Wells in the Hortonville region characteristically pass through a thin surficial clay (or clay with gravel or sand admixture), grading into limestone/dolomite and prominent sandstone aquifers. These carbonate and sandstone bedrock units alternate with typical first significant limestone/dolomite bedrock appearing between 10 to 45 ft, underlain by alternating sequences that may transition more than once with depths. Overall, groundwater is typically sourced from limestone/dolomite or sandstone at depths between 90 and over 200 ft for high capacity. Wells consistently use rotary-mud circulation, with surface casing extending to the base of unconsolidated material (~40–100 ft), and are sealed with neat cement or mud grout. Static water levels mostly fall in the 35–90 ft range. Given pump test yields, a reliable residential well (5–15+ GPM) is generally achieved by 130 ft, while high-capacity installations target depths of 180–230+ ft.