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Fowler, Michigan

Well Drillers Near Fowler, Michigan

Averaged profile shows alternating sand/gravel and clay units, with significant clay layers overlying sand/gravel aquifers, and in deeper wells, occasional shale and sandstone at depth.

Showing contractors within 60 miles of Fowler. 102 results found.

Typical depth
95 ft
Water table
20 ft
Contractors
102

102 Contractors

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View Local Geology Report

A geological estimate for the Fowler area.

Typical Well Depth
95 ft
Static Water Level
20 ft
Recommended Method
Rotary - Mud Circulation

Detailed Summary

Based on a synthesis of 7 well logs in the greater Fowler region (including adjacent Gratiot, Clinton, and Ionia counties), the most typical stratigraphic sequence includes: an upper surficial layer of topsoil/sand and gravel, followed by thick clay or clay with stones, then a major sand and gravel aquifer zone, and deeper sequences may include more clay, shale and sandstone. Nearly all wells are completed in sand and gravel or, for deeper/high-capacity wells, in sandstone layers. Lithology colors are generally brown or gray, with sand/gravel layers described as unconsolidated and clay relatively stiff to soft. Residential wells (5–15+ GPM) most commonly reach the upper sand/gravel aquifer between 70–100 ft; high capacity or bedrock wells may be deeper (150–245 ft). Static water levels range 10–30 ft for residential, ~72 ft at a single high-capacity site.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 5 ftTopsoil / Sandy Gravel / MuckBrown sand & gravel, possible organic muck or topsoil. Unconsolidated.Color: Brown/Gray
Hardness: Soft
5 – 20 ftSand & Gravel (w/stones)Unconsolidated sand and gravel, sometimes with stones. Main shallow permeable layer.Color: Brown to gray
Hardness: Loose
20 – 60 ftClay (with occasional stones, sandy or mixed)Predominantly brown or gray clay, can include stones or sand lenses. Dense, low permeability.Color: Brown/Gray
Hardness: Stiff to soft
60 – 85 ftSand & GravelMain sand and gravel aquifer; target for most residential and moderate-yield wells.Color: Gray to brown
Hardness: Loose
85 – 135 ftClay (with stones or minor gravel)Dense clay, often gray, with possible stones; low-permeability confining unit.Color: Gray
Hardness: Stiff
135 – 170 ftSand & Gravel (deep)Gravelly sand and sand aquifer; target for deeper high capacity or irrigation wells.Color: Gray to brown
Hardness: Loose
170 – 215 ftClay, Shale, or Claystone (locally)Gray-black clay, minor shale and claystone; regional confining or semi-confining unit.Color: Gray/Black
Hardness: Moderate-hard
215 – 245 ftSandstone (locally includes shale or hardpan)Fractured or weakly cemented sandstone, occasional shale partings. Bedrock aquifer for deep/municipal wells.Color: Brown/Gray/White
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Fowler area is drilled to approximately 95 feet to ensure a reliable water supply of 5-15+ gallons per minute.

The static water level, or water table, is typically found around 20 feet below the surface in this region.

Based on a synthesis of 7 well logs in the greater Fowler region (including adjacent Gratiot, Clinton, and Ionia counties), the most typical stratigraphic sequence includes: an upper surficial layer of topsoil/sand and gravel, followed by thick clay or clay with stones, then a major sand and gravel aquifer zone, and deeper sequences may include more clay, shale and sandstone. Nearly all wells are completed in sand and gravel or, for deeper/high-capacity wells, in sandstone layers. Lithology colors are generally brown or gray, with sand/gravel layers described as unconsolidated and clay relatively stiff to soft. Residential wells (5–15+ GPM) most commonly reach the upper sand/gravel aquifer between 70–100 ft; high capacity or bedrock wells may be deeper (150–245 ft). Static water levels range 10–30 ft for residential, ~72 ft at a single high-capacity site.