Tri County Well Drilling Shop
040011990001, Sparta, WI 54656
Phone: +1 608-269-4226
Typical Sparta-area wells encounter a surficial sand or sandy loam, with thick, regionally-persistent sandstone forming the main aquifer. Minor discontinuous clay or clayey sand layers may occasionally interrupt the sand or sandstone but are not regionally dominant.
Showing contractors within 60 miles of Sparta. 30 results found.
040011990001, Sparta, WI 54656
Phone: +1 608-269-4226
17660 Icecap Rd, Sparta, WI 54656
Phone: +1 608-269-5178
W5479 Co Rd, La Crosse, WI 54601
Phone: (608) 788-6451
Quote Available
5069 County Highway M, Tomah, WI 54660
Phone: +1 608-372-0891
N 5514 County Rd, Onalaska, WI 54650
Phone: (608) 526-4900
Quote Available
N3751 Big Field Rd, Black River Falls, WI 54615
Phone: +1 715-284-5287
W6295 Co Rd D, Holmen, WI 54636
Phone: +1 608-797-0877
Bluffview Ct, Holmen, WI 54636
Phone: (608) 526-9282
Quote Available
624 Amy Dr, Holmen, WI 54636
Phone: +1 608-526-9345
N5452 Eagle Cir Ln W, Onalaska, WI 54650
Phone: (608) 526-9629
N5858 WI-54, Black River Falls, WI 54615
Phone: +1 715-579-0368
Quote Available
533 N 3rd St, La Crescent, MN 55947
Phone: +1 507-895-6181
W9273 Co Rd A, New Lisbon, WI 53950
Phone: +1 608-853-0979
Quote Available
S5166 Shingle Hollow Rd, Genoa, WI 54632
Phone: (608) 689-2941
702 E 12th St, Winona, MN 55987
Phone: (507) 452-4818
44664 WI, Gays Mills, WI 54631
Phone: (608) 606-5596
Quote Available
1894 Dakota Ave, Friendship, WI 53934
Phone: +1 608-339-6705
278 W Court St, Richland Center, WI 53581
Phone: (608) 649-4488
Quote Available
325 S Park St #2, Reedsburg, WI 53959
Phone: +1 866-799-1199
Quote Available
3774 13th Dr, Wisconsin Dells, WI 53965
Phone: (608) 253-2751
Quote Available
A geological estimate for the Sparta area.
Typical Well Depth
Static Water Level
Recommended Method
The representative Sparta-area geological profile comprises an unconsolidated surficial layer (sand, sandy loam, or clay) usually 10–21 feet thick, underlain by a moderately thick to very thick interval of saturated sand (where deep alluvium/glacial fill is present) or direct transition into sandstone bedrock. Sandstone is the persistent and dominant water-bearing formation, usually encountered from 18–21 feet and extending to well depths beyond 90–115 feet. Minor, localized clay or clayey sand or occasional gravel may appear between the unconsolidated surface and the main sandstone aquifer. Groundwater is generally encountered within the sandstone at moderate static levels. The average casing depth is 55–60 feet, and residential wells are typically completed between 73–117 feet. Rotary - Mud Circulation is the prevalent construction method, with cement or neat cement grout use for sealing.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 19 ft | Sand/Sandy Loam/Clay | Unconsolidated surficial unit, often sand or sandy loam; may include clay or mixed sand and clay in some areas. | Color: Tan/Brown/Gray/White (varies between logs) Hardness: Loose to Firm |
19 – 85 ft | Sand/Sandstone transition | Saturated sand (sometimes with minor clay, clayey sand, or gravel beds); this interval is thickest where alluvium/glacial deposits persist. | Color: Tan/Brown/White/Gray Hardness: Loose to Firm |
85 – 117 ft | Sandstone | Massive sandstone—regionally extensive, main aquifer, most wells are completed in this unit. | Color: White/Tan/Gray Hardness: Hard/Firm |