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Ludington, Michigan

Well Drillers Near Ludington, Michigan

Ludington area wells penetrate a typical sequence of surficial sand, followed by interbedded clays and sand layers, with major water-bearing coarse sand or sand/gravel zones encountered below a thick clay section.

Showing contractors within 60 miles of Ludington. 242 results found.

Typical depth
75 ft
Water table
25 ft
Contractors
242

242 Contractors

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Brighton Drilling Co

Active Driller5.0 (12)
Brighton, MI 48114
Residential Well DrillingCommercial Well DrillingPump Services+5 more

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View Local Geology Report

A geological estimate for the Ludington area.

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

Detailed Summary

Based on synthesis of representative well logs from Ludington and adjacent townships, the typical stratigraphy consists of an upper sand or sandy loam (including topsoil), underlain by sequences of clay (often red, sometimes with sand/gravel interbeds). The thickest and most consistent confining unit is clay, generally overlain or underlain by varying sand layers. The main aquifer tapped for residential supply is most commonly a medium to coarse sand or sand/gravel unit found below a persistent clay layer, typically at depths of 50-80 feet, but sometimes as deep as 110-125 feet. The static water table is generally between 13 and 41 feet below grade, with most residential wells yielding 12-20 GPM at total depths averaging 78 feet. High-capacity (public or flowing) wells are deeper (~103-125 feet) to maximize gravel/sand aquifer thickness. The region is developed almost exclusively with rotary (mud) drilling, with PVC or steel casing and bentonite slurry grout.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 2 ftTopsoil/OrganicBlack to brown topsoil, some sandy loam possibleColor: Black/Brown
Hardness: Soft
2 – 15 ftSand (dry/fine/medium)Loose, clean sand, sometimes with silt or fine pebbles; dry or dampColor: Tan/Yellow
Hardness: Loose
15 – 40 ftClay (Red/Brown, occasional gravel lenses)Mostly dense clay, varies in color; occasional thin sand or gravel stringersColor: Red/Brown
Hardness: Hard/Plastic
40 – 60 ftInterbedded Sand and ClayAlternating beds of sand and clay, may include some silt or fine gravelColor: Mixed
Hardness: Variable
60 – 80 ftClay (Thick Confining Layer)Dense, massive clay, sometimes with minor sand or gravel seamsColor: Red/Brown/Grey
Hardness: Very Dense
80 – 110 ftSand/Coarse Sand/Gravel Aquifer (Water-Bearing)Medium to coarse sand, some gravel; primary water-yielding zoneColor: Tan/Yellow/Grey
Hardness: Loose to medium

Frequently Asked Questions

A typical residential well in the Ludington 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 25 feet below the surface in this region.

Based on synthesis of representative well logs from Ludington and adjacent townships, the typical stratigraphy consists of an upper sand or sandy loam (including topsoil), underlain by sequences of clay (often red, sometimes with sand/gravel interbeds). The thickest and most consistent confining unit is clay, generally overlain or underlain by varying sand layers. The main aquifer tapped for residential supply is most commonly a medium to coarse sand or sand/gravel unit found below a persistent clay layer, typically at depths of 50-80 feet, but sometimes as deep as 110-125 feet. The static water table is generally between 13 and 41 feet below grade, with most residential wells yielding 12-20 GPM at total depths averaging 78 feet. High-capacity (public or flowing) wells are deeper (~103-125 feet) to maximize gravel/sand aquifer thickness. The region is developed almost exclusively with rotary (mud) drilling, with PVC or steel casing and bentonite slurry grout.