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Grayling, Michigan

Well Drillers Near Grayling, Michigan

The typical Grayling area well penetrates a sequence of sand (often coarse to medium) with interbedded clay and gravel layers, transitioning to clean sand and/or gravel aquifers below. Residential wells are usually completed at 50-70 ft to secure 5-15+ GPM yield.

Showing contractors within 60 miles of Grayling. 263 results found.

Typical depth
60 ft
Water table
16 ft
Contractors
263

263 Contractors

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View Local Geology Report

A geological estimate for the Grayling area.

Typical Well Depth
60 ft
Static Water Level
16 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Representative well logs indicate an upper section dominated by sand (yellow to brown, medium to coarse), with local layers containing clay or small gravel. In many wells, a significant clay or sand-with-clay layer is encountered at intermediate depths (20-40 ft), followed by thick, permeable water-bearing sand or sand/gravel aquifers extending to the base of most wells. Occasional color changes (e.g., blue clay) and thin capillary zones are present but often short-lived. Static water levels are typically 12-20 ft below grade except in rare flowing conditions. Typical residential wells are finished at 50-70 ft; high-capacity wells often finish between 70 and 85 ft, both targeting the base sand/gravel aquifers.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 7 ftSandYellow to brown, medium to coarse sand, loose to medium denseColor: Yellow-brown
Hardness: Loose
7 – 22 ftSand with Clay/SiltSand with variable clay, some zones may contain stones or fine gravel, locally forming a more cohesive unitColor: Brown, sometimes mixed grey/blue
Hardness: Medium
22 – 42 ftClay or Silty SandInterbedded clay or blue clay and sandy layers, may include minor gravel; represents a local aquitard in some wellsColor: Blue-gray to brown
Hardness: Firm
42 – 60 ftSand, Water-BearingMedium to coarse sand, well sorted, occasionally interspersed with fine gravel; strong, consistent aquifer zoneColor: Buff to red/yellow
Hardness: Loose to medium
60 – 80 ftSand and Gravel AquiferSand with significant gravel content, often forming main aquifer; highly permeableColor: Brown, tan, red
Hardness: Loose

Frequently Asked Questions

A typical residential well in the Grayling area is drilled to approximately 60 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 16 feet below the surface in this region.

Representative well logs indicate an upper section dominated by sand (yellow to brown, medium to coarse), with local layers containing clay or small gravel. In many wells, a significant clay or sand-with-clay layer is encountered at intermediate depths (20-40 ft), followed by thick, permeable water-bearing sand or sand/gravel aquifers extending to the base of most wells. Occasional color changes (e.g., blue clay) and thin capillary zones are present but often short-lived. Static water levels are typically 12-20 ft below grade except in rare flowing conditions. Typical residential wells are finished at 50-70 ft; high-capacity wells often finish between 70 and 85 ft, both targeting the base sand/gravel aquifers.