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Perry, Michigan

Well Drillers Near Perry, Michigan

A typical Perry-area well encounters a thick sequence of glacial till, sand/gravel, and multiple interbedded clay layers overlying deep shale and sandstone bedrock. Residential wells most commonly finish in the shallowest water-bearing sand/gravel or in bedrock sandstone.

Showing contractors within 60 miles of Perry. 96 results found.

Typical depth
140 ft
Water table
30 ft
Contractors
96

96 Contractors

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View Local Geology Report

A geological estimate for the Perry area.

Typical Well Depth
140 ft
Static Water Level
30 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on synthesized data from several nearby wells, the most representative profile for Perry and its region begins with brown/yellow clay and occasional gravel to ~15-25 ft, followed by interbedded fine to coarse sand and gravel with mixed clays extending to approximately 85-110 ft. Beneath is a variable sequence of clay with stones, silty or gravely clays (often reaching around 150-180 ft). The most consistent bedrock contact appears as black and gray shale starting near 100-175 ft, often quickly interbedded with gray/white sandstone that may become fully dominant at greater depths. The consolidated sandstone and shale beds continue to the bottom of most logs, with water yields generally best in the lower sandy/sandstone units. Static water levels are typically 20-45 ft below grade, depending on surficial geology and proximity to recharge. Residential wells with 5–15+ GPM capacity commonly finish at 100-160 ft, generally at or just below the first persistent coarse sand/gravel or shallow bedrock sandstone.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
015 ftClay (Brown/Yellow)Soft, occasionally contains gravel; typical of glacial till.Color: Brown-Yellow
Hardness: Soft-Plastic
1555 ftSand & Gravel (Fine-Coarse, with Some Clay)Interbeds of fine to coarse sand, occasional gravel, mixed with lenses of clay. Main surficial aquifer where present.Color: Gray-Tan
Hardness: Medium
5595 ftClay with Stones / Gravelly ClayGray or reddish clay, often with gravel or stones. Locally silty or sandy.Color: Gray-Red
Hardness: Firm
95110 ftSand & Gravel (Water-Bearing)Mostly clean, medium-coarse sand/gravel, possible thin clay partings. Main shallow aquifer unit.Color: Light Gray
Hardness: Medium
110175 ftShale (Black & Gray, Locally with Clay)Consolidated shale; color varies from black to gray. May include thin sandstone or clay beds.Color: Gray-Black
Hardness: Hard
175220 ftSandstone & Shale (Alternating, with White Sandstone Prominent)Alternating layers; lower section increasingly dominated by fine-grained white sandstone, major aquifer for deep wells.Color: White-Gray
Hardness: Hard
220305 ftConsolidated Sandstone/Shale (Bedrock)Regionally extensive aquifer - white or gray sandstone, parting shale. Continues to maximum logged well depths.Color: White-Gray
Hardness: Very Hard

Frequently Asked Questions

A typical residential well in the Perry area is drilled to approximately 140 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 30 feet below the surface in this region.

Based on synthesized data from several nearby wells, the most representative profile for Perry and its region begins with brown/yellow clay and occasional gravel to ~15-25 ft, followed by interbedded fine to coarse sand and gravel with mixed clays extending to approximately 85-110 ft. Beneath is a variable sequence of clay with stones, silty or gravely clays (often reaching around 150-180 ft). The most consistent bedrock contact appears as black and gray shale starting near 100-175 ft, often quickly interbedded with gray/white sandstone that may become fully dominant at greater depths. The consolidated sandstone and shale beds continue to the bottom of most logs, with water yields generally best in the lower sandy/sandstone units. Static water levels are typically 20-45 ft below grade, depending on surficial geology and proximity to recharge. Residential wells with 5–15+ GPM capacity commonly finish at 100-160 ft, generally at or just below the first persistent coarse sand/gravel or shallow bedrock sandstone.