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Lakewood, Wisconsin

Well Drillers Near Lakewood, Wisconsin

Representative geologic profile for Lakewood, Oconto County, WI: unconsolidated glacial sand and gravel over interbedded clay and silt (where present), grading to deeper water-bearing sand, sometimes terminating on granite bedrock.

Showing contractors within 60 miles of Lakewood. 38 results found.

Typical depth
70 ft
Water table
45 ft
Contractors
38

38 Contractors

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View Local Geology Report

A geological estimate for the Lakewood area.

Typical Well Depth
70 ft
Static Water Level
45 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

The most common hydrostratigraphic sequence in the Lakewood area starts with surficial sand and/or sand and gravel (up to ~30-40 feet), underlain by variably thick layers of clay, silt, or sandy clay (commonly 10-40 feet where present). Beneath this, a second thicker sand or sand and gravel aquifer is prevailed, with occasional finer beds (silt or clay), with the deepest interval sometimes reaching granite bedrock below ~80-240 feet. The majority of productive residential wells are screened in the lower sand/gravel interval from 35 to 82 feet. Wells terminating on granite are uncommon except at greater depths. Typical static water levels range from 20 to 70 feet below surface. This profile is averaged from a random sample of permitted private wells in the region, discarding unusual or extraneous records for generalized mapping.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 30 ftSand or Sand & GravelFine to coarse surficial sand, often with gravel - glacial outwash or ice contact deposits; locally mixed with some silt. Highly permeable.Hardness: Unconsolidated
30 – 50 ftSandy clay, silt, or clay (discontinuous)Tan or gray sandy clay, silt, or clay - can be absent in some wells but forms an aquitard where present.Hardness: Plastic to compact
50 – 82 ftSand or Sand & GravelCoarse sand and/or gravel - highly transmissive main water-bearing unit. Occasional intervals described as water-bearing sand. This is the most common domestic aquifer.Hardness: Unconsolidated
82 – 240 ftGranite Bedrock (where encountered)Fresh to weathered granite - forms aquiclude; wells rarely drilled into this unit except as needed for supply.Hardness: Very hard crystalline

Frequently Asked Questions

A typical residential well in the Lakewood area is drilled to approximately 70 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 45 feet below the surface in this region.

The most common hydrostratigraphic sequence in the Lakewood area starts with surficial sand and/or sand and gravel (up to ~30-40 feet), underlain by variably thick layers of clay, silt, or sandy clay (commonly 10-40 feet where present). Beneath this, a second thicker sand or sand and gravel aquifer is prevailed, with occasional finer beds (silt or clay), with the deepest interval sometimes reaching granite bedrock below ~80-240 feet. The majority of productive residential wells are screened in the lower sand/gravel interval from 35 to 82 feet. Wells terminating on granite are uncommon except at greater depths. Typical static water levels range from 20 to 70 feet below surface. This profile is averaged from a random sample of permitted private wells in the region, discarding unusual or extraneous records for generalized mapping.