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Hot Springs, South Dakota

Well Drillers Near Hot Springs, South Dakota

A typical Hot Springs-area well penetrates thin unconsolidated material, then successive carbonate and sandstone aquifers, reaching productive Minnelusa sandstone below 300 ft.

Showing contractors within 60 miles of Hot Springs. 17 results found.

Typical depth
375 ft
Water table
150 ft
Contractors
17

17 Contractors

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Dependable Well Service logo

Dependable Well Service

Hot Springs, SD 57747
Well DrillingWell MaintenanceFiltration

Scion Drilling LLC

Active Driller
Custer, SD 57730
Residential Well DrillingCommercial Well DrillingTest Well Drilling+6 more
Alexander Drilling Company logo

Alexander Drilling Company

Active Driller
Hill City, SD 57745
Residential Well DrillingCommercial Well DrillingTest Well Drilling+7 more

Don's Pump Services

Rapid City, SD 57703
Pump ServicesPump RepairCisterns+2 more
Farmers Supply LLC logo

Farmers Supply LLC

Rapid City, SD 57701
Well DrillingPump ServicesPump Repair
Geo Enterprises, Inc. logo

Geo Enterprises, Inc.

Rapid City, SD 57703-8531
Residential Well DrillingWell MaintenanceWell Abandonment+2 more
Grimm's Pump & Industrial Supply logo

Grimm's Pump & Industrial Supply

2.2 (5)
Rapid City, SD 57701
Pump ServicesPressure Tank Installation
Johnathan Johnson Well Service logo

Johnathan Johnson Well Service

Newcastle, WY 82701
Pump RepairPump ReplacementSubmersible Pumps+7 more

Pump & Well Work

Rapid City, SD 57703
Well DrillingPump InstallationPump Repair
Taylor Drilling Company logo

Taylor Drilling Company

Rapid City, SD 57702-8062
Well DrillingMonitoring WellsGeotechnical

Wagoner Well Services

Newcastle, WY 82701
Well DrillingFiltrationExploration+1 more
WaterTree | Drinking Water • Water Softeners • Water Treatment logo

WaterTree | Drinking Water • Water Softeners • Water Treatment

5.0 (5)
Rapid City, SD 57702
FiltrationSediment FiltrationWhole House Filtration+2 more

Jim's Well Service Inc.

Crawford, NE 69339
Well DrillingPump InstallationWell Maintenance

Infinity Properties LLC

Piedmont, SD 57769
Well DrillingMunicipal Well Drilling

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View Local Geology Report

A geological estimate for the Hot Springs area.

Typical Well Depth
375 ft
Static Water Level
150 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on multiple well completion and plugging reports sampled from Hot Springs and adjacent regions, the most common geologic sequence is a thin surficial cover (sand, silt, clay, or topsoil) followed by several distinctive consolidated sedimentary formations, starting with Spearfish, then Minnekahta limestone, Opeche shale, and reaching primary Minnelusa sandstones. The Minnekahta and Minnelusa units serve as main water-bearing zones. Average static water levels are reported between 100–300 ft, and wells for typical household supply (5–15 GPM) are usually drilled to depths of 360–380 ft, with higher yields possible below 380 ft.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
05 ftUnconsolidated/topsoilTopsoil, sand and silt, possibly some brown clay.Color: Light brown
Hardness: Soft
530 ftRed shale / Gypsum / Clay / SandVariable: Alternating clay, red shale, some gypsum; locally includes sand and gravel lenses.Color: Red-brown to gray
Hardness: Soft to medium
3040 ftSpearfish FormationRed beds, mostly shale and siltstone, minor gypsum layers.Color: Red to gray
Hardness: Soft-medium
4075 ftMinnekahta LimestoneMassive limestone; solid carbonate aquitard or minor aquifer.Color: Light gray
Hardness: Hard
75120 ftOpeche ShaleThick shale unit, may include thin siltstone or sandstone beds.Color: Red-gray
Hardness: Soft-medium
120355 ftMinnelusa FormationSandstone (dominant), thin interbeds of shale, siltstone; includes multiple water-bearing sand layers. Major aquifer zone.Color: Pink, tan, gray
Hardness: Medium
355390 ftMinnelusa Sandstone (main water zone)Coarser sandstone/very permeable aquifer; primary production zone for most wells.Color: Pink-tan
Hardness: Medium

Frequently Asked Questions

A typical residential well in the Hot Springs area is drilled to approximately 375 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 150 feet below the surface in this region.

Based on multiple well completion and plugging reports sampled from Hot Springs and adjacent regions, the most common geologic sequence is a thin surficial cover (sand, silt, clay, or topsoil) followed by several distinctive consolidated sedimentary formations, starting with Spearfish, then Minnekahta limestone, Opeche shale, and reaching primary Minnelusa sandstones. The Minnekahta and Minnelusa units serve as main water-bearing zones. Average static water levels are reported between 100–300 ft, and wells for typical household supply (5–15 GPM) are usually drilled to depths of 360–380 ft, with higher yields possible below 380 ft.