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Lake Hallie, Wisconsin

Well Drillers Near Lake Hallie, Wisconsin

Lake Hallie area wells typically penetrate glacial sand/gravel and sandy/clayey overburden, then thick sequences of tan/gray sandstone with occasional interbedded clay and occasional quartzite at depth.

Showing contractors within 60 miles of Lake Hallie. 46 results found.

Typical depth
115 ft
Water table
60 ft
Contractors
46

46 Contractors

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Kline Well & Pump Inc

Loyal, WI 54446
Well DrillingPump ServicesWell Maintenance

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Well records near Lake Hallie

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View Local Geology Report

A geological estimate for the Lake Hallie area.

Typical Well Depth
115 ft
Static Water Level
60 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on synthesis of well logs from the Lake Hallie region, the representative geological profile starts with topsoil (very thin), brown sand and/or gravel, followed by a significant interval of tan/brown sand or sand with some clay. Most wells transition into thick zones of medium to hard, tan or gray sandstone, sometimes with beds described as soft or shaley, before possibly reaching quartzite or similar hard rock at greater depths. Residential wells (5–15+ GPM) commonly finish within 95–130 feet, corresponding to the hard sandstone. Static water levels usually occur between 30–70 feet below ground. High capacity well intakes may extend slightly deeper into the hard sandstone, often not exceeding 140 feet.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 2 ftTopsoilThin organic-rich surface layer.Color: Dark
Hardness: Soft
2 – 8 ftSand/GravelBrown/tan sand and gravel, sometimes with minor clay.Color: Brown/Tan
Hardness: Loose/Soft
8 – 40 ftSand, Sand with ClayTan/brown sand and occasional clay layers or sandy clay.Color: Tan/Brown
Hardness: Loose/Soft/Medium
40 – 80 ftSandstoneMedium to hard tan or gray sandstone, sometimes shaley or with clay seams.Color: Tan/Gray
Hardness: Medium to Hard
80 – 130 ftSandstoneThick, hard/firm tan or gray sandstone; principal aquifer for most wells.Color: Tan/Gray
Hardness: Hard/Firm
130 – 198 ftSandstone/Quartzite (where reached)In some cases, transitions to coarse or firm sandstone or possible quartzite; otherwise sandstone persists.Color: Tan/Gray
Hardness: Hard/Very Hard

Frequently Asked Questions

A typical residential well in the Lake Hallie area is drilled to approximately 115 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 60 feet below the surface in this region.

Based on synthesis of well logs from the Lake Hallie region, the representative geological profile starts with topsoil (very thin), brown sand and/or gravel, followed by a significant interval of tan/brown sand or sand with some clay. Most wells transition into thick zones of medium to hard, tan or gray sandstone, sometimes with beds described as soft or shaley, before possibly reaching quartzite or similar hard rock at greater depths. Residential wells (5–15+ GPM) commonly finish within 95–130 feet, corresponding to the hard sandstone. Static water levels usually occur between 30–70 feet below ground. High capacity well intakes may extend slightly deeper into the hard sandstone, often not exceeding 140 feet.