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Jefferson, South Dakota

Well Drillers Near Jefferson, South Dakota

Typical Jefferson residential wells encounter topsoil, thick clay, sand/gravel aquifer, and sandstone to bedrock within 280–350 ft.

Showing contractors within 60 miles of Jefferson. 18 results found.

Typical depth
160 ft
Water table
21 ft
Contractors
18

18 Contractors

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Alton Well logo

Alton Well

Ireton, IA 51027
Well DrillingWell MaintenanceAgricultural+1 more
Christensen Well & Irrigation, Inc. logo

Christensen Well & Irrigation, Inc.

Active Driller
Hartington, NE 68739
Residential Well DrillingMunicipal Well DrillingLivestock Well Drilling+15 more
Christensen Well & Irrigation, Inc. (Formerly Salmon Well Company) logo

Christensen Well & Irrigation, Inc. (Formerly Salmon Well Company)

Wakefield, NE 68784
Residential Well DrillingPump ServicesAgricultural+2 more
Heine Electric & Irrigation, Vermillion. logo

Heine Electric & Irrigation, Vermillion.

4.8 (4)
Vermillion, SD 57069
Well DrillingPump InstallationLivestock Watering Wells
Neighborhood Repair Pump Services logo

Neighborhood Repair Pump Services

Canton, SD 57013
Pump InstallationPump RepairWell Maintenance+1 more
Quality Well Service, LLC logo

Quality Well Service, LLC

St Helena, NE 68774
Well DrillingResidential Well DrillingMunicipal Well Drilling+6 more
Thein Well Company Vermillion SD logo

Thein Well Company Vermillion SD

Vermillion, SD 57069
Well DrillingWell MaintenanceComplete Systems+3 more

Wisner Well Services

Wisner, NE 68791
Well DrillingFiltrationWell Servicing
Buchanan Well Company logo

Buchanan Well Company

Active Driller
Osmond, NE 68765
Residential Well DrillingCommercial Well DrillingMunicipal Well Drilling+9 more
Dietz Well & Pump Co. logo

Dietz Well & Pump Co.

Active Driller
Norfolk, NE 68701
Pump ServicesPump InstallationWell Maintenance
Pump Shop logo

Pump Shop

Tekamah, NE 68061
Pump ServicesPump InstallationPump Repair+4 more
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

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Well records near Jefferson

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View Local Geology Report

A geological estimate for the Jefferson area.

Typical Well Depth
160 ft
Static Water Level
21 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Analysis of well logs for the Jefferson region reveals a common stratigraphic sequence: a thin layer of topsoil, underlain by thick glacial clay, followed by a significant sand and/or gravel aquifer beginning around 60–120 ft, and then sandstone or bedrock often reached between 280 and 350 ft. The most productive residential wells for reliable yields (5–15+ GPM) are generally completed in the sand/gravel or basal sandstone intervals at 130–300 ft, with static water levels typically 15–25 ft below ground.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
02 ftTopsoilsurface organicsColor: Dark brown
Hardness: Soft
222 ftClayglacial till, compact, occasionally siltyColor: Brown-grey
Hardness: Stiff
2261 ftFine Sandfine sand, trace silt or gravel in placesColor: Tan-yellow
Hardness: Medium
61119 ftSand & Gravelwater-bearing coarse sand and pea-to-medium gravelColor: Light tan
Hardness: Loose
119287 ftWater-Bearing Sand/Gravel with Siltaquifer zone; mostly sand with intermixed gravel, some silt; main water sourceColor: Light grey-tan
Hardness: Loose
287289 ftSandstonebedrock transition, fine-grained, occasional shale streaksColor: Light brown
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Jefferson area is drilled to approximately 160 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 21 feet below the surface in this region.

Analysis of well logs for the Jefferson region reveals a common stratigraphic sequence: a thin layer of topsoil, underlain by thick glacial clay, followed by a significant sand and/or gravel aquifer beginning around 60–120 ft, and then sandstone or bedrock often reached between 280 and 350 ft. The most productive residential wells for reliable yields (5–15+ GPM) are generally completed in the sand/gravel or basal sandstone intervals at 130–300 ft, with static water levels typically 15–25 ft below ground.