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Dowagiac, Michigan

Well Drillers Near Dowagiac, Michigan

Dowagiac area typical subsurface: surficial sand/gravel, interbedded clay, major sand & gravel aquifer zones, with larger clay and occasional sand lenses at depth.

Showing contractors within 60 miles of Dowagiac. 68 results found.

Typical depth
110 ft
Water table
30 ft
Contractors
68

68 Contractors

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Dohm Well Drilling logo

Dohm Well Drilling

Active Driller4.3 (44)
Dowagiac, MI 49047
Well DrillingResidential Well DrillingCommercial Well Drilling+8 more
J.E. Marks Well Drilling LLC logo

J.E. Marks Well Drilling LLC

4.3 (7)
Berrien Center, MI 49102
Well DrillingResidential Well DrillingCommercial Well Drilling+7 more
Martin J. Mosier Water Well Services logo

Martin J. Mosier Water Well Services

Active Driller4.9 (88)
Dowagiac, MI 49047
Residential Well DrillingPump InstallationPump Repair+4 more
Thomas J. Mosier Water Well Drilling logo

Thomas J. Mosier Water Well Drilling

Active Driller4.6 (42)
Cassopolis, MI 49031
Well DrillingPump ServicesPump Installation+2 more
Earl Sanders & Son Well Drilling Inc logo

Earl Sanders & Son Well Drilling Inc

Active Driller4.8 (36)
Lawton, MI 49065
Well DrillingResidential Well DrillingCommercial Well Drilling+11 more

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View Local Geology Report

A geological estimate for the Dowagiac area.

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

Detailed Summary

A representative geological profile for Dowagiac, based on well logs from across the city and nearby, shows a surficial unit of sand and gravel (with some topsoil), commonly 20-40 feet thick, overlaying alternating intervals of clay (variously sandy, silty, or gravelly) and sand/gravel aquifer units extending to at least 200 ft. The thickest aquifer zones—either sand or sand/gravel, ranging from fine to coarse—commonly occur (~35-90 ft and ~120-200 ft depths); they are separated by gray or brown clay units, which vary from 10 to 65 ft thick. Shallower static water levels (12–50 ft) are typical in newer wells. A typical residential well tapping a 5–15+ GPM source would be completed at 80–130 ft, while high capacity wells go to 180–220+ ft. Almost all wells use rotary (mud) drilling, with PVC casing set and bentonite-slurry grout. Outliers (like deep shale or thin local lenses) were ignored in this synthesis.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
02 ftTopsoil / SandBrown topsoil or surface sand, sometimes with some gravel.Color: Brown
Hardness: Soft
230 ftSand & GravelMedium to coarse sand and gravel. Major surficial aquifer zone.Color: Brown/Tan
Hardness: Medium
3060 ftClay (interbedded, silty or sandy)Mostly gray or brown clay, sometimes sandy or with fine gravel.Color: Gray/Brown
Hardness: Medium to Hard
6094 ftSand / Sand & Gravel (major aquifer)Thick interval of sand, sand & gravel; water-bearing zone targeted by most wells.Color: Tan/Gray
Hardness: Medium
94130 ftClay (interbedded, gray to brown, some sandy lenses)Mostly gray or brown clay, with some sandy or silty intervals; acts as aquitard.Color: Gray/Brown
Hardness: Hard
130180 ftSand & Gravel (deep aquifer)Thick water-bearing sand and gravel or coarse sand, major aquifer for higher capacity wells.Color: Gray/Tan
Hardness: Medium
180220 ftClay/sand interbeddedAlternating layers of clay, sandy clay, and sand with some gravel. Local aquifer presence.Color: Gray/Brown
Hardness: Medium

Frequently Asked Questions

A typical residential well in the Dowagiac area is drilled to approximately 110 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.

A representative geological profile for Dowagiac, based on well logs from across the city and nearby, shows a surficial unit of sand and gravel (with some topsoil), commonly 20-40 feet thick, overlaying alternating intervals of clay (variously sandy, silty, or gravelly) and sand/gravel aquifer units extending to at least 200 ft. The thickest aquifer zones—either sand or sand/gravel, ranging from fine to coarse—commonly occur (~35-90 ft and ~120-200 ft depths); they are separated by gray or brown clay units, which vary from 10 to 65 ft thick. Shallower static water levels (12–50 ft) are typical in newer wells. A typical residential well tapping a 5–15+ GPM source would be completed at 80–130 ft, while high capacity wells go to 180–220+ ft. Almost all wells use rotary (mud) drilling, with PVC casing set and bentonite-slurry grout. Outliers (like deep shale or thin local lenses) were ignored in this synthesis.