West Michigan Water Wells
5904 Zahm Rd, Belding, MI 48809
Phone: +1 616-794-3333
The typical Belding-area well penetrates a surficial clay layer underlain by alternating sand, clay, and gravel/sand units, with most residential wells ending in a basal sand/gravel aquifer between 50 and 130 ft deep.
Showing contractors within 60 miles of Belding. 80 results found.
5904 Zahm Rd, Belding, MI 48809
Phone: +1 616-794-3333
12944 Lincoln Lake Ave NE, Gowen, MI 49326
Phone: (616) 754-5032
Quote Available
10634 14 Mile Rd NE, Rockford, MI 49341
Phone: (616) 835-9355
Quote Available
PO Box 1 5820 W Riverside Dr, Saranac, MI 48881-0001
Phone: (616) 642-9415
Quote Available
8468 Macarthur Rd, Saranac, MI 48881
Phone: (616) 920-0099
271 Rockford Park Dr NE, Rockford, MI 49341-7828
Phone: (616) 863-6890
Quote Available
6085 17 Mile Rd NE, Cedar Springs, MI 49319
Phone: (616) 696-2699
Quote Available
4181 Knapp St NE, Grand Rapids, MI 49525
Phone: (616) 363-2683
Quote Available
727 Knoll Rd, Portland, MI 48875
Phone: (616) 374-0955
Quote Available
950 Crystal Rd, Crystal, MI 48818
Phone: +1 989-235-6730
1725 S Crystal, Crystal, MI 48818
Phone: +1 989-235-3485
585 Fonger St NE, Sparta, MI 49345
Phone: (616) 889-4748
387 10 Mile Rd NW, Sparta, MI 49345
Phone: +1 616-887-0822
9600 Looking Glass Rd, Portland, MI 48875
Phone: +1 517-627-5052
Quote Available
4449 Westshire Dr NW, Comstock Park, MI 49321
Phone: (616) 784-1214
13194 Long Lake Dr, Sparta, MI 49345
Phone: +1 616-262-7271
8782 E 124th St, Sand Lake, MI 49343
Phone: (616) 636-5684
2700 N Tallman Rd, Fowler, MI 48835
Phone: +1 989-666-6426
Quote Available
6974 Hammond Ave SE, Dutton, MI 49316-8351
Phone: (616) 698-7770
Quote Available
239 E Main St SE, Caledonia, MI 49316
Phone: (616) 891-8137
A geological estimate for the Belding area.
Typical Well Depth
Static Water Level
Recommended Method
Based on a synthesis of several well logs from Belding and surrounding townships, the regional geology commonly consists of a surficial clay (often brown/gray), overlying sand or mixed sand/silt, with further alternations between clay, sand, and occasionally gravel below 30–40 feet. The main aquifer utilized for household supply is typically a thick sand or mixed sand/gravel unit, often reached around 50–130 ft deep. Clay layers dominate above and between sand zones, and many wells transition into coarser or water-bearing zones near their base. Static water levels typically range from 10–60 ft below grade, and most residential wells achieve 5–20+ GPM when completed in the principal sand/gravel aquifer.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 4 ft | Topsoil | Black or brown topsoil, sometimes with silt | Color: Black/Brown Hardness: Soft |
4 – 25 ft | Clay | Brown/gray clay, may include boulders, silt or hard layers | Color: Brown to gray Hardness: Soft to hard |
25 – 35 ft | Sand/Silt | Sand or mixed sand & silt, sometimes interbedded with thin clay | Color: Brown or gray Hardness: Medium |
35 – 50 ft | Clay (with sand or gravel interbeds) | Gray or brown clay with lenses of sand or minor gravel | Color: Brown/Gray Hardness: Medium to hard |
50 – 60 ft | Sand | Clean sand, sometimes water-bearing | Color: Yellow/brown/gray Hardness: Medium |
60 – 110 ft | Clay (with silt, hard zones or boulders) | Predominantly gray hard clay, sometimes cemented with boulders | Color: Gray Hardness: Hard |
110 – 126 ft | Sand/Gravel | Coarse sand and gravel, main aquifer unit, usually water-bearing | Color: Gray/brown Hardness: Loose to medium |