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Ithaca, Michigan

Well Drillers Near Ithaca, Michigan

The typical geological profile for the Ithaca, MI region consists of an alternating sequence of sand/gravel, clay, and occasional stony or boulder-bearing layers, with a deeper regional trend toward coarser or fractured sand or sandstone aquifers. Shallow wells commonly draw from sand/gravel or coarse sand below multiple clay tills.

Showing contractors within 60 miles of Ithaca. 24 results found.

Typical depth
95 ft
Water table
16 ft
Contractors
24

24 Contractors

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R. Oberlitner Well Drilling & Repair logo

R. Oberlitner Well Drilling & Repair

Ithaca, MI 48847
Well drillingPump service and repairWater softener installation+3 more
Bigard & Huggard Drilling Inc logo

Bigard & Huggard Drilling Inc

4.6 (5)
Mt Pleasant, MI 48858
Production WellsExcavation

Bogart Well Drilling LLC

Active Driller
Crystal, MI 48818
Water well drillingWell service
Brad Malley Well Drilling Inc logo

Brad Malley Well Drilling Inc

Active Driller
Mt Pleasant, MI 48858
Well DrillingGeothermal ServicesEnv monitoring/observation (MOW)+3 more

Crystal Clear Water Well Systems LLC

Active Driller
Crystal, MI 48818
Water well drillingWell service
Gates Drilling & Services logo

Gates Drilling & Services

Active Driller
Mt Pleasant, MI 48858
Residential well drillingCommercial well drillingWell repair services+1 more
Griffin Well Drilling & Pump Repair logo

Griffin Well Drilling & Pump Repair

Active Driller
Oakley, MI 48649
Well drillingResidential well installationWell replacement+7 more
Jandernoa Water Systems, Inc. logo

Jandernoa Water Systems, Inc.

Active Driller
Fowler, MI 48835
Water well drillingWater testingPump repair+3 more
Lilly Well Drilling & Repair logo

Lilly Well Drilling & Repair

Mt Pleasant, MI 48858
Residential well drillingCommercial well drillingWell repair+2 more

Sawade Drilling Co Inc

Active Driller
Mt Pleasant, MI 48858
Water well drillingBoring servicesWell installation+1 more
Trayer Water Wells logo

Trayer Water Wells

Active Driller
Vestaburg, MI 48891
Well DrillingPump Installation
B & B Well Drilling logo

B & B Well Drilling

Active Driller4.6 (5)
Linwood, MI 48634
Well Drilling
Bendall Well Drilling logo

Bendall Well Drilling

5.0 (1)
Owosso, MI 48867
Well drillingWell repairWater softening (installation and service)+4 more
Bendall Well Drilling & Water Softening logo

Bendall Well Drilling & Water Softening

Corunna, MI 48817
Well drillingWell repairsWater softeners+5 more
Cesal Well Drilling LLC logo

Cesal Well Drilling LLC

Active Driller
Corunna, MI 48817
Residential water well drillingCommercial water well drillingAgricultural water well drilling+4 more
Chad Malley Well Drilling logo

Chad Malley Well Drilling

Active Driller
Rosebush, MI 48878
New Well DrillingWell Maintenance & RepairPump Installation & Repair+15 more
Contract Dewatering Services Inc. logo

Contract Dewatering Services Inc.

Saranac, MI 48881
Deep WellsRelief Wells

Courtright Water Wells Inc

Active Driller
Mecosta, MI 49332
Water well servicesWater treatment systemsWater softening+1 more

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View Local Geology Report

A geological estimate for the Ithaca area.

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

Detailed Summary

Analysis of well logs from the Ithaca area shows that wells typically encounter an upper zone of sand and/or clay, followed by alternating layers of fine to coarse sand, gravel, and clay at varying thicknesses. Boulder or stony layers are present but less common. At greater depths (>150 ft), sandstone formations may be encountered, functioning as high-yield aquifers. Most residential wells are completed in coarse sand, sand/gravel, or the upper part of sandstone, at depths of 60-100 ft. Shallow aquifers are found at depths where thick sand/gravel/cobble sequences underlie multiple layers of clay, with static water levels typically between 10-23 ft. The most common drilling method is rotary with mud circulation, casing to the bottom of clay and grouted with bentonite slurry.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
02 ftTopsoilTopsoil or surficial organic materialColor: Brown/Dark
Hardness: Soft
212 ftClayBrown clay, sometimes silty or sandy; acts as a confining layerColor: Brown
Hardness: Firm
1222 ftClayGray clay (occasionally with stones or pebbles); continuous confining/till layerColor: Gray
Hardness: Hard
2232 ftSand & GravelFine to coarse sand with some gravel; may include cobbles/boulders locally, moderate aquifer potentialColor: Yellow to Tan
Hardness: Moderate
3262 ftClayGray or brown dense clay, may include scattered stones; regionally extensive till, often slightly compactedColor: Gray/Brown
Hardness: Firm
6280 ftClay w/Stones or BouldersGray clay with embedded stones or boulders; locally discontinuousColor: Gray
Hardness: Hard
80100 ftSand, Coarse or Sand & StonesCoarse sand with some gravel, stones, or cobbles; main local aquifer with good water yieldColor: Yellow/Gray
Hardness: Loose
100130 ftClayThick, hard, blue-gray to brown clay or till; forms main lower confining layerColor: Blue-Gray/Brown
Hardness: Hard
130150 ftSand & StonesMixed sand and stones or gravel, locally present, can be water-bearingColor: Gray/Tan
Hardness: Moderate
150310 ftClayBrown clay, very thick regional confining layer (only present in deep/bedrock wells)Color: Brown
Hardness: Very Hard
310335 ftGypsumMassive gypsum; regional evaporite/bedrock, not always encountered (ignore if shallower aquifer tapped)Color: White/Gray
Hardness: Very Hard
335342 ftRed SandRed sand, transitional to underlying bedrock aquiferColor: Red
Hardness: Loose
342483 ftSandstone (Red to White)Interbedded red and white sandstone; regional bedrock aquifer for high-capacity or municipal wellsColor: Red/White
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Ithaca 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 16 feet below the surface in this region.

Analysis of well logs from the Ithaca area shows that wells typically encounter an upper zone of sand and/or clay, followed by alternating layers of fine to coarse sand, gravel, and clay at varying thicknesses. Boulder or stony layers are present but less common. At greater depths (>150 ft), sandstone formations may be encountered, functioning as high-yield aquifers. Most residential wells are completed in coarse sand, sand/gravel, or the upper part of sandstone, at depths of 60-100 ft. Shallow aquifers are found at depths where thick sand/gravel/cobble sequences underlie multiple layers of clay, with static water levels typically between 10-23 ft. The most common drilling method is rotary with mud circulation, casing to the bottom of clay and grouted with bentonite slurry.