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Rhinelander, Wisconsin

Well Drillers Near Rhinelander, Wisconsin

Rhinelander wells typically encounter caving sand, sand and gravel, and occasional fine or coarse sands with limited clay, overlying crystalline bedrock. Most residential wells are completed at 38–60 feet, with water-bearing zones primarily in unconsolidated sand and gravel.

Showing contractors within 60 miles of Rhinelander. 32 results found.

Typical depth
40 ft
Water table
15 ft
Contractors
32

32 Contractors

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View Local Geology Report

A geological estimate for the Rhinelander area.

Typical Well Depth
40 ft
Static Water Level
15 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on a synthesis of well logs from the Rhinelander area, the most representative geologic profile consists of an upper layer of caving sand (sometimes intermixed with gravel), transitioning to sand and gravel units (including both fine and coarse fractions), rarely with thin clay or silt interbeds, overlying granite or crystalline bedrock (sometimes as shallow as ~65 feet but only occasionally reached in residential wells). The static water level typically falls between 10 and 32 feet. Wells for typical residential use (to yield 5–15+ GPM) are generally completed at depths of 35–60 feet, cased almost to total depth and screened in coarse or mixed sand/gravel zones. High-capacity wells (rare in the sample set) may go deeper into coarse sand/gravel or potentially to bedrock if required.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 17 ftCaving Sand & GravelLoose, caving, often water-bearing sand and gravel; locally interbedded with some silt.Color: Brown to yellowish
Hardness: Unconsolidated
17 – 41 ftFine to Medium Sand (with Silt/Fine Sand interbeds possible)Predominantly medium to fine sand, with variable silt or silty sand beds; locally grades into more gravelly zones.Color: Light brown to tan
Hardness: Unconsolidated
41 – 59 ftCoarse Sand / Sand & GravelCoarse brown sand and/or well-washed sand & gravel, main aquifer zone; high-yielding for local wells.Color: Brown
Hardness: Unconsolidated
59 – 65 ftClayey sand & fine clay (rare, may be absent or very limited)Intermittent thin clay, sandy clay, or silty clay, often immediately above rock or thick gravel sequences.Color: Gray to light brown
Hardness: Semi-consolidated
65 – 66 ftCrystalline Bedrock (Granite)Weathered or fresh granite, typically encountered as refusal; seldom completed into for residential wells.Color: Pink to gray
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Rhinelander area is drilled to approximately 40 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 15 feet below the surface in this region.

Based on a synthesis of well logs from the Rhinelander area, the most representative geologic profile consists of an upper layer of caving sand (sometimes intermixed with gravel), transitioning to sand and gravel units (including both fine and coarse fractions), rarely with thin clay or silt interbeds, overlying granite or crystalline bedrock (sometimes as shallow as ~65 feet but only occasionally reached in residential wells). The static water level typically falls between 10 and 32 feet. Wells for typical residential use (to yield 5–15+ GPM) are generally completed at depths of 35–60 feet, cased almost to total depth and screened in coarse or mixed sand/gravel zones. High-capacity wells (rare in the sample set) may go deeper into coarse sand/gravel or potentially to bedrock if required.