
Sam's Well Drilling
Randolph, WI53956
The typical Germantown area well geology consists of a surficial sand/gravel/clay zone overlying thick limestone bedrock, with most residential wells fully penetrating the limestone aquifer.
Showing contractors within 60 miles of Germantown. 39 results found.
A geological estimate for the Germantown area.
Typical Well Depth
Static Water Level
Recommended Method
Based on representative well logs from Germantown and the surrounding area, the most common sequence is an upper unconsolidated unit of sand, gravel, and clay, generally 20-40 feet thick, followed by extensive limestone bedrock. Occasionally, deeper wells may encounter thin shale layers or additional limestone bands. Residential wells (providing 5–15+ GPM) typically reach 120–220 feet, terminating within the limestone. Static water levels for these wells range from 1 to 90 feet below ground surface, with construction via rotary mud circulation and steel casing set through the unconsolidated materials. High capacity or deeper wells (>300 ft) are rarely needed except for large users or anomalously low-yield sites.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 35 ft | Sand/Gravel/Clay | Interbedded sand, gravel, and clay; unconsolidated glacial and alluvial material forming the upper aquitard and sometimes local shallow aquifers. | Color: Tan/Brown Hardness: Soft to firm |
35 – 185 ft | Limestone | Dense, competent dolomitic limestone bedrock; primary regional aquifer with good yield for residential and small community supply. | Color: Gray to buff Hardness: Very hard |
185 – 245 ft | Limestone (w/ occasional shale) | Continued limestone, with occasional thin shale partings or layers reported at greater depths. | Color: Gray with occasional dark bands Hardness: Very hard with softer shale intervals |