Precision Drilling & Installation of Wisconsin, Inc.
E2625 Co Rd G, Kewaunee, WI 54216
Phone: +1 920-737-9008
A typical Kewaunee County residential well penetrates a sequence of clay-rich glacial sediments, underlain by a sand/gravel or stony zone, grading into limestone bedrock—the principal aquifer.
Showing contractors within 60 miles of Kewaunee. 25 results found.
E2625 Co Rd G, Kewaunee, WI 54216
Phone: +1 920-737-9008
2121 N Ronsman Rd, New Franken, WI 54229
Phone: +1 920-866-2344
5861 Marys Rd, New Franken, WI 54229
Phone: (920) 866-9464
2094 Double Q Rd, Green Bay, WI 54311
Phone: +1 920-489-2938
1122 Roosevelt Ct, Brussels, WI 54204
Phone: +1 920-825-7620
3188 Manitowoc Rd, Green Bay, WI 54311
Phone: +1 920-863-2355
8103 WI, Two Rivers, WI 54241
Phone: (920) 860-0717
Quote Available
2496 Stone Rd, Sturgeon Bay, WI 54235
Phone: +1 920-825-7575
3671 Monroe Rd, De Pere, WI 54115
Phone: (920) 336-3659
7170 County W PP, Greenleaf, WI 54126
Phone: +1 920-864-2173
146 Lincoln St, Whitelaw, WI 54247
Phone: (920) 732-1600
Quote Available
1267 Lakeview Dr, Green Bay, WI 54313
Phone: (866) 434-2969
1710 Flowing Wells Ct, Suamico, WI 54173
Phone: (920) 434-1903
W3494 Dundas Rd, Kaukauna, WI 54130
Phone: (920) 766-4192
W2015 Industrial Dr, Kaukauna, WI 54130
Phone: (920) 733-7209
537 Caldwell Ave, Oconto Falls, WI 54154
Phone: +1 920-848-2407
220 Marks Dr, Oconto Falls, WI 54154
Phone: (920) 848-5239
5515 Elmwood Rd, Menominee, MI 49858
Phone: (906) 863-9573
N5406 12 Corners Rd, Black Creek, WI 54106
Phone: +1 920-739-8100
9584 Rose Rd, Gillett, WI 54124
Phone: +1 920-855-2060
A geological estimate for the Kewaunee area.
Typical Well Depth
Static Water Level
Recommended Method
Synthesizing well logs across Kewaunee County, the most representative geologic profile begins with a substantial interval of clay (sometimes with stones or gravel), extending from the surface to approximately 30-140 feet, depending on local conditions. This is frequently underlain by a discontinuous sand and/or gravel or stony interval of moderate thickness (ranging from 10 to 40 feet), acting as a transition to the underlying limestone/dolomite bedrock aquifer. The bedrock limestone is universally encountered and constitutes the primary water-bearing formation. Casing generally anchors into the top of bedrock, with wells completed open-hole in limestone. Static water levels are highly variable but most commonly range from 15 to 100 feet below ground surface. Wells producing 5–40+ GPM for a residential setting typically reach 100–165 feet, with high-capacity systems extending to 200+ feet as needed. All wells are constructed by rotary mud circulation with a cement or clay slurry grout seal.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 5 ft | Clay | Brown or gray clay, locally may have stones | Color: Brown/Gray Hardness: Soft |
5 – 40 ft | Sand/Gravel or Stony Clay | Sand with gravel or clay with stones, may be interbedded; significant as transition zone | Color: Mixed Hardness: Medium |
40 – 120 ft | Clay | Hard compact silty or sandy clay, sometimes with gravel; non-caving | Color: Brown/Grey Hardness: Hard |
120 – 140 ft | Gravel/Stone | Coarse gravel or stone, occasional thin sand layers | Color: Brown/Gray Hardness: Hard |
140 – 220 ft | Limestone/Dolomite | Fractured, gray limestone or dolomite bedrock; primary aquifer, water bearing | Color: Gray Hardness: Hard |