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Waterford Twp, Michigan

Well Drillers Near Waterford Twp, Michigan

The typical Waterford Twp. well intersects alternating sand/gravel and clay layers, with residential wells commonly targeting sand/gravel aquifers between 40 and 70 ft, and deeper high capacity wells extending >100 ft. Most layers are unconsolidated glacial materials; bedrock is not encountered in typical wells.

Showing contractors within 60 miles of Waterford Twp. 90 results found.

Typical depth
65 ft
Water table
16 ft
Contractors
90

90 Contractors

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View Local Geology Report

A geological estimate for the Waterford Twp area.

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

Detailed Summary

Synthesis of regional water well logs indicates a representative profile of glacial sediments: surface sand or sand and gravel overlain by blue/brown/gray clay and/or silty layers, with water-bearing sand and gravel zones typically found between 30-70 ft and a deeper sequence of alternating clays and gravel/sand extending to about 120 ft. While some variations exist, the most reliable aquifers for residential supply are found in medium to coarse sand/gravel between 35 and 65 ft, overlain and underlain by confining clay. Deeper wells (high capacity) tap thicker, sometimes multi-layered sand/gravel aquifers beneath further tills and clays, often from about 110-126 ft. Static water levels typically range from 5 ft to 30 ft below grade. Most drilling uses mud rotary or cable tool methods. Casing (often 5" PVC) is set to the bottom of upper clay, and bentonite or cement grout is used to a similar depth.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 8 ftSand/Silt/TopsoilFine- to medium-grained brown sand/silt, may include organic topsoil horizonColor: Brown
Hardness: Loose
8 – 32 ftSand & GravelBrown or red sand and gravel, water-bearing in places; may have minor clay/silt layersColor: Brown/Red
Hardness: Medium
32 – 60 ftClay (often Blue or Brown), Silt, with thin sandsPlastic, stiff blue or brown clay; may include silty or sandy streaks; acts as aquitardColor: Blue, Brown, Gray
Hardness: Hard/Plastic
60 – 78 ftSand & Gravel (Aquifer)Gray or brown sand and gravel, commonly water-bearing with high yields; target for screensColor: Gray/Brown
Hardness: Loose to Coarse
78 – 112 ftClay with Sand/GravelThick blue or gray clay, sometimes silty or with sand/gravel stringers; some water-bearing potentialColor: Blue/Gray
Hardness: Hard
112 – 126 ftSand & Gravel (Deep Aquifer)Black, gray, or brown sand and gravel, coarse and highly permeable; main deep aquifer for high-capacity wellsColor: Black/Gray/Brown
Hardness: Coarse

Frequently Asked Questions

A typical residential well in the Waterford Twp area is drilled to approximately 65 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.

Synthesis of regional water well logs indicates a representative profile of glacial sediments: surface sand or sand and gravel overlain by blue/brown/gray clay and/or silty layers, with water-bearing sand and gravel zones typically found between 30-70 ft and a deeper sequence of alternating clays and gravel/sand extending to about 120 ft. While some variations exist, the most reliable aquifers for residential supply are found in medium to coarse sand/gravel between 35 and 65 ft, overlain and underlain by confining clay. Deeper wells (high capacity) tap thicker, sometimes multi-layered sand/gravel aquifers beneath further tills and clays, often from about 110-126 ft. Static water levels typically range from 5 ft to 30 ft below grade. Most drilling uses mud rotary or cable tool methods. Casing (often 5" PVC) is set to the bottom of upper clay, and bentonite or cement grout is used to a similar depth.