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Marion, South Dakota

Well Drillers Near Marion, South Dakota

The typical Marion area well passes through topsoil, yellow and blue/brown clays, with main aquifers in sand and gravel below 170-300 ft; final depths often reach 300-350 ft, with static water 50-80 ft below surface.

Showing contractors within 60 miles of Marion. 16 results found.

Typical depth
180 ft
Water table
60 ft
Contractors
16

16 Contractors

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View Local Geology Report

A geological estimate for the Marion area.

Typical Well Depth
180 ft
Static Water Level
60 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on synthesis of multiple well logs in the Marion region of Turner County, SD, the typical geological sequence begins with a thin layer of topsoil, underlain by a considerable section of yellow and blue/brown clay (commonly 15-120 ft thick). This is followed by sand and local gravel/sandstone units, often intermittently layered with more clay. Deeper wells commonly penetrate additional clay and occasional till or hardpan before encountering thicker sand/gravel aquifers generally between 170 and 300 ft. Substantial yields (5–15+ GPM for residential use) are most often from sand/gravel layers in this interval. Bedrock or hard conglomerate (occasionally granite or cemented material) may be found below 300-350 ft. Static water levels are typically 50–80 ft below land surface. Typical residential wells are cased to the base of the aquifer layer.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 2 ftTopsoil/Fine Silty SandSoft, organic-rich, may include fill or fine sandColor: Black/Brown
Hardness: Soft
2 – 30 ftClay (Silty/Lean, sometimes yellow)Plasticky, sometimes mottled, may include a little gravelColor: Yellow/Brown
Hardness: Plastic/Soft
30 – 80 ftClay (Blue or Brown)Dense, low permeability, forms a confining unitColor: Blue/Brown/Gray
Hardness: Firm/Plastic
80 – 120 ftSand (Minor gravel, some blue/sandy clay)Fine to medium sand with localized clay or gravel, variably moistColor: Tan/Blue/Brown
Hardness: Loose/Medium
120 – 170 ftClay/Sandy ClayMostly clay with some sandy or gravelly lenses, forming aquitardColor: Blue/Brown/Gray
Hardness: Firm
170 – 300 ftSand & Gravel (Main aquifer zone)Medium to coarse sand with significant gravel, major water-bearing strata; some zones interlayered with thin clay or siltColor: Tan/Gray
Hardness: Loose/Medium
300 – 336 ftGravel/Clayey GravelSimilar to above, increasing gravel content, possibly with clay layersColor: Gray
Hardness: Medium
336 – 350 ftClay/Till/HardpanDense clay, occasional pebbly till or hardpan, forms lower aquitard; may act as base for casingColor: Gray/Brown
Hardness: Hard/Very Firm
350 – 490 ftHard Rock/Granite/Cemented Layer (locally variable, seldom used for water supply)Hard, cemented or granitic rock, not typically water-bearing in domestic wells in this regionColor: Red/Gray
Hardness: Very Hard

Frequently Asked Questions

A typical residential well in the Marion area is drilled to approximately 180 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 60 feet below the surface in this region.

Based on synthesis of multiple well logs in the Marion region of Turner County, SD, the typical geological sequence begins with a thin layer of topsoil, underlain by a considerable section of yellow and blue/brown clay (commonly 15-120 ft thick). This is followed by sand and local gravel/sandstone units, often intermittently layered with more clay. Deeper wells commonly penetrate additional clay and occasional till or hardpan before encountering thicker sand/gravel aquifers generally between 170 and 300 ft. Substantial yields (5–15+ GPM for residential use) are most often from sand/gravel layers in this interval. Bedrock or hard conglomerate (occasionally granite or cemented material) may be found below 300-350 ft. Static water levels are typically 50–80 ft below land surface. Typical residential wells are cased to the base of the aquifer layer.