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Cornell, Wisconsin

Well Drillers Near Cornell, Wisconsin

Typical Cornell area geology: surficial sand/sand & gravel, interbedded clay/silt, grading at depth to sand/gravel or local bedrock. Residential wells: ~40-70 ft, often finished in sand/gravel.

Showing contractors within 60 miles of Cornell. 38 results found.

Typical depth
55 ft
Water table
19 ft
Contractors
38

38 Contractors

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Kline Well & Pump Inc

Loyal, WI 54446
Well DrillingPump ServicesWell Maintenance

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View Local Geology Report

A geological estimate for the Cornell area.

Typical Well Depth
55 ft
Static Water Level
19 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

A representative geologic profile for the Cornell region, based on multiple well construction logs, generally shows an upper zone of sand or silty sand, with significant intervals of sand & gravel. Interbedded and sometimes thick clay or silty clay layers are common but discontinuous. Deeper units typically remain unconsolidated sand/gravel, but in some outlying areas, granite or bedrock is encountered beyond ~40-70 ft, often deeper. The aquifer for most residential wells is in sand & gravel at moderate depth, with static water level commonly between 9 and 33 feet below ground surface, and tested yields commonly above 5 GPM, frequently 10-15 GPM or more.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 15 ftSand (occasional Sandy Gravel)Brown, caving, soft; may include surface silt or minor fine gravel.Color: Brown
Hardness: Soft to moderate
15 – 23 ftSand & Gravel (occasional Hardpan, Gravel, or Silty Sand)Coarse, brown, caving, some local hardpan/gravel; potential for high permeability.Color: Brown
Hardness: Moderate to hard
23 – 41 ftClay or Clay/Silt (occasionally sandy or silty)Brown to grey, non-caving or weakly caving, soft to hard; not always present or continuous.Color: Brown/Grey
Hardness: Soft to hard
41 – 62 ftSand & Gravel (frequently silty)Brown or grey, caving, soft to moderate; primary water-bearing unit for residential use.Color: Brown/Grey
Hardness: Soft to moderate
62 – 71 ftSilty Sand/Gravel, possible transition to coarser gravel or sandCaving, brown/grey, soft to moderate; may include scattered hard layers or increase in coarseness at depth.Color: Brown/Grey
Hardness: Soft to hard
71 – 75 ftOccasional Bedrock (e.g., Granite - rare)Hard, non-caving localized occurrence; mostly outside common residential well range.Color: Grey/Pink
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Cornell area is drilled to approximately 55 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 19 feet below the surface in this region.

A representative geologic profile for the Cornell region, based on multiple well construction logs, generally shows an upper zone of sand or silty sand, with significant intervals of sand & gravel. Interbedded and sometimes thick clay or silty clay layers are common but discontinuous. Deeper units typically remain unconsolidated sand/gravel, but in some outlying areas, granite or bedrock is encountered beyond ~40-70 ft, often deeper. The aquifer for most residential wells is in sand & gravel at moderate depth, with static water level commonly between 9 and 33 feet below ground surface, and tested yields commonly above 5 GPM, frequently 10-15 GPM or more.