Sundheim Well Repair
Jefferson, SD57038
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. 11 results found.
A geological estimate for the Jefferson area.
Typical Well Depth
Static Water Level
Recommended Method
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.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 2 ft | Topsoil | surface organics | Color: Dark brown Hardness: Soft |
2 – 22 ft | Clay | glacial till, compact, occasionally silty | Color: Brown-grey Hardness: Stiff |
22 – 61 ft | Fine Sand | fine sand, trace silt or gravel in places | Color: Tan-yellow Hardness: Medium |
61 – 119 ft | Sand & Gravel | water-bearing coarse sand and pea-to-medium gravel | Color: Light tan Hardness: Loose |
119 – 287 ft | Water-Bearing Sand/Gravel with Silt | aquifer zone; mostly sand with intermixed gravel, some silt; main water source | Color: Light grey-tan Hardness: Loose |
287 – 289 ft | Sandstone | bedrock transition, fine-grained, occasional shale streaks | Color: Light brown Hardness: Hard |