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Auburndale, Wisconsin

Well Drillers Near Auburndale, Wisconsin

Auburndale region wells typically penetrate thick clay and till, with minor sand, overlying a transition zone (sand/sandstone or decomposed rock) that gives way to competent granite or, less commonly, sandstone at depth.

Showing contractors within 60 miles of Auburndale. 44 results found.

Typical depth
130 ft
Water table
15 ft
Contractors
44

44 Contractors

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View Local Geology Report

A geological estimate for the Auburndale area.

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

Detailed Summary

Based on a synthesis of multiple well logs from the Auburndale area, the representative geological profile begins with a substantial upper clay (sometimes clay-with-stones or till) unit, often extending from the surface down to approximately 30–60 ft. Below this, there is typically a transition layer that may include sand, sand and clay, sandstone, or highly weathered granite (when present). The dominant bedrock is granite, encountered at depths ranging from about 50–65 ft and extending to the full depth of most wells (commonly 100–240 ft), with occasional wells reporting sandstone instead of granite. The most productive residential wells for 5–15+ GPM generally penetrate into the granite bedrock and are typically completed between 100 and 160 ft. High capacity municipal or irrigation wells may use the full granite thickness to 200–240 ft as observed in several logs.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 40 ftClay/Till (occasional stones)Dense, often brown or tan clay, sometimes includes stones or gravel. May locally include small amounts of silt or sand.Color: Brown/Tan
Hardness: Soft to firm
40 – 60 ftTransition (Sand, Sand+Clay, Decomposed Granite, or Sandstone)Sand, mixed sand and clay, or decomposed/weathered bedrock. In some areas, this horizon may be absent or represented as layered sandstone within clay.Color: Tan, Brown, Yellow, or Mixed
Hardness: Loose to medium
60 – 220 ftGranite Bedrock (occasionally Sandstone lower; see local variability)Competent crystalline granite, occasionally overlain or interbedded with sandstone in some locations. This is the primary water-producing formation in the area.Color: Pink, Black, Gray
Hardness: Very hard

Frequently Asked Questions

A typical residential well in the Auburndale area is drilled to approximately 130 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 multiple well logs from the Auburndale area, the representative geological profile begins with a substantial upper clay (sometimes clay-with-stones or till) unit, often extending from the surface down to approximately 30–60 ft. Below this, there is typically a transition layer that may include sand, sand and clay, sandstone, or highly weathered granite (when present). The dominant bedrock is granite, encountered at depths ranging from about 50–65 ft and extending to the full depth of most wells (commonly 100–240 ft), with occasional wells reporting sandstone instead of granite. The most productive residential wells for 5–15+ GPM generally penetrate into the granite bedrock and are typically completed between 100 and 160 ft. High capacity municipal or irrigation wells may use the full granite thickness to 200–240 ft as observed in several logs.