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Ringle, Wisconsin

Well Drillers Near Ringle, Wisconsin

Ringle area wells typically encounter a surficial mixed sand/gravel/clay layer, underlain by decomposed/weathered granite, then transition to solid granite bedrock.

Showing contractors within 60 miles of Ringle. 46 results found.

Typical depth
125 ft
Water table
18 ft
Contractors
46

46 Contractors

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View Local Geology Report

A geological estimate for the Ringle area.

Typical Well Depth
125 ft
Static Water Level
18 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Analysis of representative well logs in the Ringle region reveals a typical stratigraphic sequence: a shallow sand, gravel, and occasional clay cover (often caving, brown or mixed in color), typically extending from the surface to approximately 10–20 feet, is followed by a zone of decomposed, weathered, or broken granite which may include some clay or iron oxide staining (roughly 10–40 feet). Beyond this, solid granite of varying hardness and occasional color changes (gray, red, or green tints) dominates, commonly extending much deeper than domestic well requirements. Most residential wells that provide 5–15+ GPM are completed between 100–140 feet, occasionally deeper if higher yields are needed or if initial granite yields are low.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 15 ftSand/Gravel/ClayMixed surficial material; coarse sand, gravel, occasional clay, brown to yellowish, caving in some locations.Color: Brown/Yellowish
Hardness: Soft to medium
15 – 40 ftDecomposed/Weathered Granite (with possible clay or iron staining)Decomposed or weathered granite, sometimes with interbedded clay or iron-rich zones, variable texture, transitional to bedrock.Color: Red, gray, greenish, or mottled
Hardness: Soft to firm
40 – 200 ftGranite BedrockDense granite bedrock, occasional color variation (gray, greenish, reddish), often the productive aquifer zone.Color: Gray, red, greenish
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Ringle area is drilled to approximately 125 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 18 feet below the surface in this region.

Analysis of representative well logs in the Ringle region reveals a typical stratigraphic sequence: a shallow sand, gravel, and occasional clay cover (often caving, brown or mixed in color), typically extending from the surface to approximately 10–20 feet, is followed by a zone of decomposed, weathered, or broken granite which may include some clay or iron oxide staining (roughly 10–40 feet). Beyond this, solid granite of varying hardness and occasional color changes (gray, red, or green tints) dominates, commonly extending much deeper than domestic well requirements. Most residential wells that provide 5–15+ GPM are completed between 100–140 feet, occasionally deeper if higher yields are needed or if initial granite yields are low.