
Sam's Well DrillingDrillerDB Preferred
N9935 Pleasant Rd, Randolph, WI 53956
Phone: (800) 321-5193
Quote Available
Grand Marsh area wells typically encounter surficial sand overlying variable clay, then coarser sand and gravel, occasionally with finer silts, with sandstone bedrock sometimes present at greater depths.
Showing contractors within 60 miles of Grand Marsh. 32 results found.
N9935 Pleasant Rd, Randolph, WI 53956
Phone: (800) 321-5193
Quote Available
673 Fern Ave, Grand Marsh, WI 53936
Phone: (608) 584-5000
Quote Available
3199 8th Ave, Wisconsin Dells, WI 53965
Phone: +1 608-586-5608
128 S Oxford St, Oxford, WI 53952
Phone: +1 608-586-5694
1894 Dakota Ave, Friendship, WI 53934
Phone: +1 608-339-6705
3774 13th Dr, Wisconsin Dells, WI 53965
Phone: (608) 253-2751
Quote Available
3898 5th Dr, Wisconsin Dells, WI 53965
Phone: +1 608-547-7819
3774 State Rd 13, Wisconsin Dells, WI 53965
Phone: (608) 253-2751
Quote Available
229 Short St, Plainfield, WI 54966
Phone: (715) 335-4398
Quote Available
W9273 Co Rd A, New Lisbon, WI 53950
Phone: +1 608-853-0979
Quote Available
325 S Park St #2, Reedsburg, WI 53959
Phone: +1 866-799-1199
Quote Available
E10704B WI-136, Baraboo, WI 53913
Phone: +1 608-356-3372
618 WI-73, Nekoosa, WI 54457
Phone: +1 715-886-4118
6522 Oak Dr, Amherst, WI 54406
Phone: (715) 824-2801
Quote Available
N698 WI-49, Berlin, WI 54923
Phone: +1 920-410-8483
W706 Friesland Rd, Randolph, WI 53956
Phone: +1 920-326-3220
1500 Post Rd, Plover, WI 54467
Phone: (715) 344-4747
Quote Available
2535 Collins Rd, Rudolph, WI 54475
Phone: +1 715-435-3379
5069 County Highway M, Tomah, WI 54660
Phone: +1 608-372-0891
1036 Townsend Rd, Waupaca, WI 54981
Phone: +1 715-281-2485
Quote Available
A geological estimate for the Grand Marsh area.
Typical Well Depth
Static Water Level
Recommended Method
A synthesis of well logs from Grand Marsh and immediate surrounding areas shows the following common stratigraphic sequence: a surficial blanket of fine to medium sand (sometimes interbedded with yellow or brown soil/loam), underlain by discontinuous clay layers (often grey or brown), followed by alternating units of medium and coarse sand and gravel. The coarser zones typically provide the principal aquifer for residential wells (with 10-15 GPM yields frequently noted). At greater depths, particularly in irrigation/commercial wells, a transition to sandstone bedrock is observed. Static water levels in residential wells are typically 18–28 feet below ground surface. High capacity wells are screened much deeper, corresponding with thick coarse sand and gravel or fractured sandstone aquifers. Construction is dominated by rotary or jetted mud circulation methods, with steel casing to the aquifer zone and grout/bentonite cement for sanitary sealing.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 15 ft | Sand | Fine to medium (yellow, brown, or white) sand; may include sandy loam or topsoil at surface | Color: Yellow/Brown/White Hardness: Soft |
15 – 30 ft | Clay | Discontinuous, sometimes silty, firm to hard clay layer; locally grey or brown; variable thickness | Color: Grey/Brown Hardness: Firm |
30 – 55 ft | Sand | Intermediate to medium sand, can include some finer silts or clay lenses | Color: Light brown/yellow Hardness: Medium |
55 – 70 ft | Sand and Gravel | Coarse to medium sand and gravel; principal aquifer zone for residential wells | Color: Yellow/White Hardness: Loose to medium |
70 – 120 ft | Sand and Gravel/Occasional Silt | Alternating beds of medium to coarse sand, gravel, and some silty-fine sand, increasing with depth; high-yielding zones likely here | Color: Tan/Yellow/White Hardness: Varies |
120 – 230 ft | Sand and Gravel (Thick, Coarse) | Thick, coarse sand and gravel; high-cap wells target this zone if present; occasional silty and fine sand beds | Color: Tan/Light Brown Hardness: Medium to loose |
230 – 400 ft | Sandstone (locally present, deeper wells) | Cemented yellow/tan sandstone, water bearing; only encountered in deepest wells | Color: Yellow/Tan Hardness: Hard rock |