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Friendship, Wisconsin

Well Drillers Near Friendship, Wisconsin

Typical geology in the Friendship, Adams County region is a sequence of unconsolidated sands, interbedded with minor sandy clay, gravel, and occasional clay, overlying sandstone at greater depths. Most domestic wells are constructed entirely within these unconsolidated sand and gravel units.

Showing contractors within 60 miles of Friendship. 65 results found.

Typical depth
70 ft
Water table
25 ft
Contractors
65

65 Contractors

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View Local Geology Report

A geological estimate for the Friendship area.

Typical Well Depth
70 ft
Static Water Level
25 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on the sample of well logs from Friendship and surrounding areas in Adams County, the most representative geological sequence begins with a surface sand layer (commonly extending 25–35 ft), underlain by sandy clay or clay (when present) for roughly 5–15 ft, then transitioning to thick zones of sand or sand/gravel mixtures typically continuing to the base of the commonly drilled interval (60 to 105 ft). In deeper, high-capacity wells or rotary wells, sandstone is frequently encountered beneath these deposits. The water table (static level) usually sits between 10 and 35 feet below ground. A standard residential well seeking 5–15+ GPM yield is most often completed at about 65–75 feet, with some higher-capacity or rotary wells going deeper, commonly to 100–105 feet, with screens set in the deeper sand or initial bedrock zones.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 30 ftSandLoose to medium sand, sometimes fine, generally clean, non-cavingColor: Tan to light brown
Hardness: Unconsolidated
30 – 40 ftSandy Clay / ClaySandy clay or clay, sometimes gray or mixed, minor gravel may occur; acts as a semi-confining layer in some locationsColor: Gray to brown
Hardness: Firm
40 – 65 ftSand & GravelMedium to coarse sand with increasing gravel content below 45 ft; excellent aquifer zone, common screen locationColor: Tan to gray
Hardness: Unconsolidated
65 – 100 ftCoarse Sand / WatersandCoarse sand, sometimes with gravel or recorded as 'watersand'; most productive water-bearing interval for most wells. Deeper wells may encounter transition to sandy or fractured sandstone.Color: Light brown to yellowish
Hardness: Unconsolidated to soft rock
100 – 105 ftSandstone (where applicable)Soft sandstone; not present in all wells, encountered mainly in deepest rotary-drilled wellsColor: Light brown
Hardness: Soft rock

Frequently Asked Questions

A typical residential well in the Friendship area is drilled to approximately 70 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 25 feet below the surface in this region.

Based on the sample of well logs from Friendship and surrounding areas in Adams County, the most representative geological sequence begins with a surface sand layer (commonly extending 25–35 ft), underlain by sandy clay or clay (when present) for roughly 5–15 ft, then transitioning to thick zones of sand or sand/gravel mixtures typically continuing to the base of the commonly drilled interval (60 to 105 ft). In deeper, high-capacity wells or rotary wells, sandstone is frequently encountered beneath these deposits. The water table (static level) usually sits between 10 and 35 feet below ground. A standard residential well seeking 5–15+ GPM yield is most often completed at about 65–75 feet, with some higher-capacity or rotary wells going deeper, commonly to 100–105 feet, with screens set in the deeper sand or initial bedrock zones.