Chat with us, powered by LiveChat
Canton, South Dakota

Well Drillers Near Canton, South Dakota

Canton area wells commonly penetrate Quaternary sands and gravels over glacial silts and varied tills, with underlying Cretaceous shales and local quartzites at depth. The most productive aquifers are found in the coarse sand and gravel sequences between ~20 and ~60 feet, with deeper blue/gray clays and shale below.

Showing contractors within 60 miles of Canton. 20 results found.

Typical depth
75 ft
Water table
25 ft
Contractors
20

20 Contractors

Sort by:
Neighborhood Repair Pump Services logo

Neighborhood Repair Pump Services

Canton, SD 57013
Pump InstallationPump RepairWell Maintenance+1 more
Putzke Well Drilling & Pump Service logo

Putzke Well Drilling & Pump Service

Sioux Falls, SD 57106
Well DrillingPump InstallationPump Repair+2 more
605 Well Drilling and Excavating logo

605 Well Drilling and Excavating

Hartford, SD 57033
Well DrillingPump InstallationWater Line Installation+1 more
Alton Well logo

Alton Well

Ireton, IA 51027
Well DrillingWell MaintenanceAgricultural+1 more

Chase Well Drilling inc

Sioux Falls, SD 57107
Well DrillingResidential Well DrillingWell Maintenance
Heine Electric & Irrigation, Vermillion. logo

Heine Electric & Irrigation, Vermillion.

4.8 (4)
Vermillion, SD 57069
Well DrillingPump InstallationLivestock Watering Wells

Koranda Well & Pump LLC

4.8 (5)
Freeman, SD 57029
Well DrillingLivestock Well DrillingPump Installation+7 more
Thein Well Company Vermillion SD logo

Thein Well Company Vermillion SD

Vermillion, SD 57069
Well DrillingWell MaintenanceComplete Systems+3 more
Christensen Well & Irrigation, Inc. logo

Christensen Well & Irrigation, Inc.

Active Driller
Hartington, NE 68739
Residential Well DrillingMunicipal Well DrillingLivestock Well Drilling+15 more
Quality Well Service, LLC logo

Quality Well Service, LLC

St Helena, NE 68774
Well DrillingResidential Well DrillingMunicipal Well Drilling+6 more
Spartz & Sons Well Co logo

Spartz & Sons Well Co

Iona, MN 56141
Well DrillingPump ServicesTrenching
Gus Pech Manufacturing Co Inc. logo

Gus Pech Manufacturing Co Inc.

Le Mars, IA 51031
Brownfield Assessment
Paul Davis logo

Paul Davis

2.6 (5)
South Sioux City, NE 68776
Emergency Water ServicesRemediation

LEUTHOLD PLUMBING, HEATING & ELECTRIC

Lester, SD 51242-0070
Well DrillingGeothermal ServicesDirectional Boring

Browse the full directory

Thousands more licensed contractors across all 50 states.

Explore by state

Browse all of South Dakota

See every licensed contractor across South Dakota.

← All South Dakota contractors

Well records near Canton

Check depths and logs of existing wells in the area before you drill.

Open well map →

South Dakota well owner guide

Costs, permits, maintenance tips for private wells in South Dakota.

Open guide →
View Local Geology Report

A geological estimate for the Canton area.

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

Detailed Summary

The typical Canton, SD region geologic profile (based on synthesis of logs from public supply, irrigation, and monitoring wells) begins with a thin topsoil or silt layer, followed by variable brown or light brown fine sand, silty sand, or clay (0–7 ft). Most wells then penetrate a thicker sequence of sand and gravel (usually with clean or brown/gray hues) from about 7 to 54 ft, which forms the main water-bearing aquifer for both residential and high-capacity supply. Below the main aquifer, blue-gray to greenish clay, clayey sand, and intermittent gravel layers extend typically to 250–300 ft. Deeper test or municipal wells show continued interbedded clays and sands to 350+ ft, below which Cretaceous bedrock (shale, quartzite) is reached around 390–400 ft or deeper. Slight local variations (occasional cemented sand, cherty gravel, or silt zones) exist but are not persistent enough to characterize the area. A typical residential water well penetrates 40–90 ft for reliable 5–15+ GPM yields, while high-capacity wells may go 180–250+ ft for greater draw.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
02 ftTopsoil/SiltBrown or black silt, locally overlying sand or silty clay; loose to firm.Color: Brown/Tan/Black
Hardness: Soft
27 ftFine Sand/Fine to Medium SandFine to medium brown sand, minor silt or clay, occasionally with organic material.Color: Brown/Light Brown
Hardness: Loose
724 ftSand and GravelWater-bearing sand and gravel, often well-cleaned with coarse to fine fractions, occasional clay stringers.Color: Brown/Gray/Clean
Hardness: Unconsolidated
2454 ftSand/Clay W/ Gravel LayersSand and clay with interbedded gravel; locally stratified, some greenish or blue-gray clay seams.Color: Light gray/brown/greenish
Hardness: Loose to firm
5477 ftFine to Medium Sand, Sandy ClayTransition to tighter, finer sand with increasing clay content; sandy clay layers possible.Color: Gray/Greenish/Tan
Hardness: Firm
77250 ftBlue/Gray Clay with Interbedded Clayey Sand & GravelThick blue-gray or greenish clay (glacial till) with local sand or gravel seams, increasingly consolidated with depth.Color: Blue-gray/green/tan
Hardness: Firm to stiff
250375 ftDense Clay, Clayey Sand, Some GravelHard blue clay, scattered sand and gravel lenses, minor chalk or calcareous seams.Color: Blue/gray/white
Hardness: Very firm/stiff
375398 ftHard/Quartzite/BedrockVery hard sand, occasionally with quartzite or siltstone; base of most water supply drilling.Color: Blue, gray, white
Hardness: Very hard

Frequently Asked Questions

A typical residential well in the Canton area is drilled to approximately 75 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.

The typical Canton, SD region geologic profile (based on synthesis of logs from public supply, irrigation, and monitoring wells) begins with a thin topsoil or silt layer, followed by variable brown or light brown fine sand, silty sand, or clay (0–7 ft). Most wells then penetrate a thicker sequence of sand and gravel (usually with clean or brown/gray hues) from about 7 to 54 ft, which forms the main water-bearing aquifer for both residential and high-capacity supply. Below the main aquifer, blue-gray to greenish clay, clayey sand, and intermittent gravel layers extend typically to 250–300 ft. Deeper test or municipal wells show continued interbedded clays and sands to 350+ ft, below which Cretaceous bedrock (shale, quartzite) is reached around 390–400 ft or deeper. Slight local variations (occasional cemented sand, cherty gravel, or silt zones) exist but are not persistent enough to characterize the area. A typical residential water well penetrates 40–90 ft for reliable 5–15+ GPM yields, while high-capacity wells may go 180–250+ ft for greater draw.