
Municipal Well & Pump
1212 Storbeck Dr, Waupun, WI 53963-9691
Phone: (920) 324-3400
Quote Available
Typical Waupun area geology is glacial clay/gravel over bedrock, with extensive limestone/dolomite, occasional shale, and deep sandstone.
Showing contractors within 60 miles of Waupun. 49 results found.
1212 Storbeck Dr, Waupun, WI 53963-9691
Phone: (920) 324-3400
Quote Available
400 S Woodward St, Brandon, WI 53919
Phone: +1 920-346-5114
Quote Available
N9935 Pleasant Rd, Randolph, WI 53956
Phone: (800) 321-5193
Quote Available
W2831 Zion Church Rd, Mayville, WI 53050
Phone: (920) 387-2624
Quote Available
W706 Friesland Rd, Randolph, WI 53956
Phone: +1 920-326-3220
W2721 WI-33, Mayville, WI 53050
Phone: +1 920-387-5434
742 WI-33, Allenton, WI 53002
Phone: +1 262-628-2228
Quote Available
N7900 Locust Ln, Mt Calvary, WI 53057
Phone: (920) 753-2406
Quote Available
180 Grant St, Hartford, WI 53027
Phone: (262) 670-6800
Quote Available
1480 WI, Hartford, WI 53027
Phone: (262) 789-7334
Quote Available
N698 WI-49, Berlin, WI 54923
Phone: +1 920-410-8483
4932 Co Rd, Kewaskum, WI 53040
Phone: (262) 626-4592
N534 WI-67, Ashippun, WI 53003
Phone: +1 920-474-3757
251 Stockhausen Ln, West Bend, WI 53095
Phone: +1 262-251-0960
N87W36051 Mapleton St, Oconomowoc, WI 53066-8902
Phone: (920) 474-4777
Quote Available
315 N 7848, North Lake, WI 53064
Phone: (262) 538-4007
N 82 W 28160 Marshall Dr, Hartland, WI 53029
Phone: (262) 538-4007
N6331 County Rd F, Oconomowoc, WI 53066
Phone: +1 262-567-0803
Quote Available
W185N9681 Appleton Ave, Germantown, WI 53022
Phone: +1 262-255-7739
9403 Tri-county Rd, Fremont, WI 54940
Phone: (920) 209-3335
A geological estimate for the Waupun area.
Typical Well Depth
Static Water Level
Recommended Method
Based on compiled logs from multiple sampled wells around Waupun, the most typical subsurface profile begins with a surficial layer of glacial material (mainly clay, frequently mixed with gravel and sometimes minor sand or boulders), transitioning sharply to a thick sequence of limestone or dolomite bedrock. Some wells encounter thin shale interbeds within the carbonate interval. At deeper locations, the carbonate bedrock gives way to sandstone, which can form a significant lower aquifer. Well construction is rotary with mud circulation, using steel casing generally set to the base of unconsolidated material. Typical residential wells are completed in the upper carbonate aquifer, with deeper completions necessary for higher yields or high-capacity needs.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 5 ft | Clay (occasionally with Gravel/Silt/Loam) | Brown to gray, plastic, caving, glacial till and occasional surficial fill. | Color: Brown/Grey Hardness: Soft |
5 – 35 ft | Clay & Gravel (Glacial, may contain boulders/sand as local variant) | Mixed glacial outwash. May contain some loam, boulders, or silt. Water bearing may occur at base. | Color: Mixed Brown/Grey Hardness: Soft to Medium |
35 – 90 ft | Limestone/Dolomite | Sedimentary bedrock, locally fractured, dense, in places slightly shaly. | Color: Gray/Buff Hardness: Hard |
90 – 150 ft | Limestone/Dolomite (minor Shale beds possible) | Dense carbonate, some shale interlaminations, commonly water bearing. | Color: Light Gray Hardness: Hard |
150 – 185 ft | Limestone/Dolomite (occasional Shale) | Similar to above, transitions to increasing sand content lower down. | Color: Gray Hardness: Hard |
185 – 265 ft | Sandstone | Fine to medium grained quartzose sandstone; water bearing. | Color: Light Tan/Yellow Hardness: Medium |