
Sam's Well Drilling
Randolph, WI53956
Typical Ashippun-area geology is unconsolidated clay, gravel, and sand overlying limestone or dolomite bedrock. Most residential wells access water from sand and gravel aquifers above the rock.
Showing contractors within 60 miles of Ashippun. 44 results found.
A geological estimate for the Ashippun area.
Typical Well Depth
Static Water Level
Recommended Method
Based on regional well logs, the typical Ashippun-area geological profile begins with a surficial clay (with cobbles and gravel) unit, typically 5-10 feet thick, followed by a sand and gravel aquifer extending to depths of about 40-60 feet. Some wells encounter secondary clay/gravel or clayey sand layers below, and in deeper locations, a transition to limestone/dolomite bedrock occurs, commonly starting between about 120-130 ft depth but occasionally documented deeper. Residential well screens are most often set in the sand and gravel aquifer above any bedrock, which provides sufficient yield for typical household demands. The static water table generally sits between 18 and 64 feet below grade, with drawdown typically moderate. The most common drilling method is rotary with mud circulation, and casings are set just above or into bedrock, grouted with cement or granular bentonite.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 8 ft | Clay with Gravel, Cobbles | Brown to gray, sandy, may contain cobbles/boulders | Color: Brown/Gray Hardness: Soft to medium |
8 – 45 ft | Sand & Gravel | Mostly clean to mixed sand and gravel aquifer; main water-bearing zone | Color: Light brown/yellow/gray Hardness: Medium |
45 – 130 ft | Clay or Clayey Gravel (interbedded with sand in some wells) | Gray to brown dense clay, sometimes with gravel; locally contains sand lenses | Color: Gray/Brown Hardness: Hard |
130 – 300 ft | Limestone/Dolomite Bedrock | Dense lithified carbonate; fractured in zones, occasional water bearing | Color: Gray Hardness: Hard |