Chuck Massart Well & Pump Repair LLC
1122 Roosevelt Ct, Brussels, WI 54204
Phone: +1 920-825-7620
Typical Brussels-area wells penetrate a surface layer of clay (often with some gravel or sand), underlain by a thick limestone/dolomite bedrock sequence, with occasional thin gravel or hardpan zones. Bedrock aquifers are the primary groundwater source.
Showing contractors within 60 miles of Brussels. 25 results found.
1122 Roosevelt Ct, Brussels, WI 54204
Phone: +1 920-825-7620
2496 Stone Rd, Sturgeon Bay, WI 54235
Phone: +1 920-825-7575
5861 Marys Rd, New Franken, WI 54229
Phone: (920) 866-9464
2121 N Ronsman Rd, New Franken, WI 54229
Phone: +1 920-866-2344
1710 Flowing Wells Ct, Suamico, WI 54173
Phone: (920) 434-1903
2094 Double Q Rd, Green Bay, WI 54311
Phone: +1 920-489-2938
1267 Lakeview Dr, Green Bay, WI 54313
Phone: (866) 434-2969
3188 Manitowoc Rd, Green Bay, WI 54311
Phone: +1 920-863-2355
E2625 Co Rd G, Kewaunee, WI 54216
Phone: +1 920-737-9008
5515 Elmwood Rd, Menominee, MI 49858
Phone: (906) 863-9573
537 Caldwell Ave, Oconto Falls, WI 54154
Phone: +1 920-848-2407
220 Marks Dr, Oconto Falls, WI 54154
Phone: (920) 848-5239
3671 Monroe Rd, De Pere, WI 54115
Phone: (920) 336-3659
9584 Rose Rd, Gillett, WI 54124
Phone: +1 920-855-2060
7170 County W PP, Greenleaf, WI 54126
Phone: +1 920-864-2173
W8301 Co Rd, Crivitz, WI 54114
Phone: (920) 373-0847
8103 WI, Two Rivers, WI 54241
Phone: (920) 860-0717
Quote Available
W2015 Industrial Dr, Kaukauna, WI 54130
Phone: (920) 733-7209
146 Lincoln St, Whitelaw, WI 54247
Phone: (920) 732-1600
Quote Available
N5406 12 Corners Rd, Black Creek, WI 54106
Phone: +1 920-739-8100
A geological estimate for the Brussels area.
Typical Well Depth
Static Water Level
Recommended Method
Based on well logs from the Brussels region and immediate surrounds, the most representative geologic sequence is a surface layer of clay (commonly 10–80 ft thick, sometimes with sand or gravel), possibly with discrete gravel/hardpan intervals. This is consistently underlain by massive limestone or dolomite that extends through the bottom of typical residential and public wells, at least down to ~310 ft where logs terminate. Static water levels average between 15 and 80 ft below grade, with most wells drawing from 150–310 ft depths. A typical residential well (5–15+ GPM) is screened or open in the limestone at ~180–250 ft, with higher capacity wells reaching ~300+ ft. Shale or other minor beds are rarely encountered and do not warrant representation in the averaged model.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 10 ft | Topsoil/Clay/Gravel | Red to brown clay, locally with sand, gravel, or stones; non-caving in most areas. | Color: Brown/Red Hardness: Soft to Firm |
10 – 80 ft | Clay/Gravel/Hardpan (Variable) | Firm clay, zones of gravel or occasional hardpan; color mottled brown/gray; minor local sand. | Color: Brown/Gray Hardness: Firm to Hard |
80 – 120 ft | Transition Clay/Hardpan (occasional) | Clay with occasional hardpan or boulders; not always present, but common in deeper overburden. | Color: Gray/Brown Hardness: Firm |
80 – 310 ft | Limestone/Dolomite Bedrock | White to light gray, hard, crystalline limestone or dolomite. Primary aquifer for water supply. | Color: White/Gray Hardness: Hard |