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Irons, Michigan

Well Drillers Near Irons, Michigan

Typical Irons, MI area wells encounter alternating sand, gravel, and clay layers, with sand/gravel being the dominant aquifer zone. Residential wells usually reach 70–80 ft for 10–15 GPM yield.

Showing contractors within 60 miles of Irons. 257 results found.

Typical depth
75 ft
Water table
29 ft
Contractors
257

257 Contractors

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View Local Geology Report

A geological estimate for the Irons area.

Typical Well Depth
75 ft
Static Water Level
29 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Synthesis of well log data from the Irons, MI region indicates a largely unconsolidated glacial geology dominated by interbedded sand, gravel, and occasional clay layers. The most consistent sequence is upper sand or sand/gravel, possibly with minor silt/clay, transitioning to deeper, more persistent sand and gravel aquifers. Clay, when present, is a thin confining or interbedded layer, not a regional aquitard. Most wells target the deeper sand/gravel zone for reliable residential yields (typically 10+ GPM), with final well depths and screens set 70–85 ft below grade. Static water levels are generally between 18–45 ft below grade. Rotary or cable tool methods are common, with 4–5 in. casing and bentonite/cement grout to depths of 36–72 ft.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 4 ftSand (often fine/medium)Surface sand, sometimes with minor silt or organic debrisColor: Yellow to Brown
Hardness: Loose
4 – 15 ftSand & GravelInterbedded sand and gravel, becoming coarser with depthColor: Brown to Gray
Hardness: Loose to Moderately compact
15 – 42 ftSand & Gravel (main aquifer)Primary upper aquifer unit, high permeabilityColor: Mixed
Hardness: Loose/Unconsolidated
42 – 50 ftClay (local, discontinuous)Silty clay or clay lens, not always present or continuous; occasional confining roleColor: Gray or Tan
Hardness: Plastic
50 – 85 ftSand & Gravel (deep aquifer, water bearing)Thickest, most reliably productive aquifer zone, typically targeted for screens and residential supplyColor: Yellow/Brown/Gray
Hardness: Loose to Moderately compact

Frequently Asked Questions

A typical residential well in the Irons area is drilled to approximately 75 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 29 feet below the surface in this region.

Synthesis of well log data from the Irons, MI region indicates a largely unconsolidated glacial geology dominated by interbedded sand, gravel, and occasional clay layers. The most consistent sequence is upper sand or sand/gravel, possibly with minor silt/clay, transitioning to deeper, more persistent sand and gravel aquifers. Clay, when present, is a thin confining or interbedded layer, not a regional aquitard. Most wells target the deeper sand/gravel zone for reliable residential yields (typically 10+ GPM), with final well depths and screens set 70–85 ft below grade. Static water levels are generally between 18–45 ft below grade. Rotary or cable tool methods are common, with 4–5 in. casing and bentonite/cement grout to depths of 36–72 ft.