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Weyerhaeuser, Wisconsin

Well Drillers Near Weyerhaeuser, Wisconsin

The typical Weyerhaeuser well penetrates a sequence of surficial sand/gravel, clay or clay/gravel, deeper sand/gravel, and in deeper wells, transitions into sandstone or shale. Most residential wells are completed in sand and gravel aquifers between 30-70 feet.

Showing contractors within 60 miles of Weyerhaeuser. 48 results found.

Typical depth
48 ft
Water table
22 ft
Contractors
48

48 Contractors

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View Local Geology Report

A geological estimate for the Weyerhaeuser area.

Typical Well Depth
48 ft
Static Water Level
22 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Analysis of well logs in the Weyerhaeuser region reveals a consistent geological sequence. Most wells begin with a thin organic/soil layer, followed by extensive sand and gravel, interbedded with clay or clay/gravel layers. Where wells are drilled deeper (typically over 70-90 feet), a transition to bedrock (sandstone, sometimes with shale) occurs. The most productive sand/gravel zones for standard residential wells occur from approx. 20-70 feet. Deeper high-capacity wells (>90 feet) typically finish in sandstone. Static water levels are commonly between 12-39 feet. The 'Rotary - Mud Circulation' method is standard, and cement grout with steel casing to the productive horizon is typical.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 1 ftSOIL/ORGANICTopsoil or organic layer, sometimes listed separately from glacial sediments.Color: Brown
Hardness: Soft
1 – 20 ftSAND & GRAVELCaving sand and gravel, generally brown, primary water-bearing unit near surface.Color: Brown
Hardness: Soft/Medium
20 – 35 ftCLAY, CLAY & GRAVEL, or SILTY CLAYInterbedded silty clay, clay, or clay with gravel; usually brown, mostly non-caving or mixed.Color: Brown
Hardness: Soft
35 – 70 ftSAND & GRAVELCoarse sand and gravel, often the primary aquifer for residential wells.Color: Brown
Hardness: Medium/Hard
70 – 100 ftSANDSTONE (occasional SHALE interbeds)Bedrock sandstone, good aquifer for higher-capacity wells; some shale possible.Color: Light brown to reddish
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Weyerhaeuser area is drilled to approximately 48 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 22 feet below the surface in this region.

Analysis of well logs in the Weyerhaeuser region reveals a consistent geological sequence. Most wells begin with a thin organic/soil layer, followed by extensive sand and gravel, interbedded with clay or clay/gravel layers. Where wells are drilled deeper (typically over 70-90 feet), a transition to bedrock (sandstone, sometimes with shale) occurs. The most productive sand/gravel zones for standard residential wells occur from approx. 20-70 feet. Deeper high-capacity wells (>90 feet) typically finish in sandstone. Static water levels are commonly between 12-39 feet. The 'Rotary - Mud Circulation' method is standard, and cement grout with steel casing to the productive horizon is typical.