
Tim Lysaker Well Drill & Pump
Holmen, WI54636
The typical Holmen-area well penetrates a thick unconsolidated sand (or sand and gravel) aquifer, sometimes underlain by sandstone, with static water levels generally moderate to deep.
Showing contractors within 60 miles of Holmen. 27 results found.
A geological estimate for the Holmen area.
Typical Well Depth
Static Water Level
Recommended Method
Holmen and greater La Crosse County wells predominantly encounter a thick brown sand or sand-and-gravel unit from land surface to between 60 and 130 feet. A minority of wells (especially to the south/east) may encounter sandstone or shaley sandstone beneath the unconsolidated aquifer, but most household supply wells are completed within the sand/gravel. Static water levels are variable, most commonly ranging from 10-90 feet below ground surface, with pumping levels for 10+ GPM commonly 20-110 feet. Casing typically extends to near the bottom of the sand/gravel, with screen or open intake at the base. Rotary mud circulation is the most common drilling method. The most reliable geology is: thick unconsolidated brown sand/sand-gravel, locally with clay-rich cap, over possible sandstone/shale at greater depths.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 20 ft | Clay or clayey silt (local, discontinuous cap) | Brown clay with rocks or sandy silt, locally hard, usually forming the uppermost layer in some wells, otherwise gradational to sand. | Color: Brown Hardness: Hard/stiff |
0 – 120 ft | Sand/Sand & Gravel | Thick, brown, medium-to-coarse sand with frequent gravel, common throughout all wells; occasionally some cobbles or stones; forms the main aquifer. | Color: Brown to tan Hardness: Loose/medium |
120 – 155 ft | Sandstone (occasional, deeper wells only) | Light brown sandstone and locally shaley sandstone at the base of the sand/gravel, not always encountered in typical residential wells. | Color: Tan to brown Hardness: Hard |