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Escanaba, Michigan

Well Drillers Near Escanaba, Michigan

The typical Escanaba-area well penetrates unconsolidated sands and clays overlying limestone bedrock, with occasional shale. Most residential wells terminate in limestone or, less commonly, sandy limestone within 65-150 ft. Deeper, high-capacity wells extend 200-400+ ft into layered limestone and shale.

Showing contractors within 60 miles of Escanaba. 21 results found.

Typical depth
110 ft
Water table
22 ft
Contractors
21

21 Contractors

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View Local Geology Report

A geological estimate for the Escanaba area.

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

Detailed Summary

Unconsolidated surficial layers in Escanaba generally begin with a thin topsoil (1-2 ft), underlain by sequences of medium to fine sands (10-30 ft) and interbedded/clayey layers (40-60 ft total thickness). These are usually followed by compact 'hardpan', gravelly clay, or sand-gravel mixes. Groundwater is commonly encountered above 20-90 ft depth. The uppermost bedrock is dominantly limestone (often with interbeds of shale or sandstone deeper), beginning at 50-150 ft depending on location. Deeper wells may encounter further sequences of blue shale or consolidated limestones down to at least 225 ft, sometimes 400 ft where deeper drilling was reported. Most wells use rotary or cable-tool drilling and are cased (commonly steel or PVC) to around 50-144 ft, and are pressure-grouted with neat cement to ~100-140 ft. Static water levels average 12-55 ft below ground. Residential wells with 5-15+ GPM yields are most often ~105 ft, up to 150 ft; higher-capacity or bedrock wells may be 225-400+ ft.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 2 ftTopsoilThin black or brown soil horizonColor: Black/Brown
Hardness: Soft
2 – 25 ftSand (medium to fine)Loose to compact sand, occasionally mixed with some silt or clayColor: Tan/Yellow/Gray
Hardness: Soft/Medium
25 – 52 ftClay and/or Sandy ClaySandy clay, clay with silt or gravel, locally with hardpan layersColor: Red/Gray/Tan
Hardness: Medium/Hard
52 – 70 ftClay & Gravel, with occasional SandVaried layers, transitional and often includes gravel or transitions into hardpanColor: Red/Gray/Brown
Hardness: Medium/Hard
70 – 90 ftClay—Gravelly or HardpanDenser clay, hardpan/compact with gravel or pebbles may be presentColor: Red/Gray/Brown
Hardness: Hard
90 – 145 ftLimestone (may include fractured or impure limestone)Transition to bedrock; occasionally starts slightly shallower or deeper. Initial limestone may be fractured or impure.Color: Gray/Tan/White
Hardness: Hard
145 – 225 ftLimestone/Sandy or Tan LimestoneThick, hard limestone layers. In some wells interbedded with sand, gravel, or fine shale.Color: Gray/Tan/White
Hardness: Very Hard
225 – 260 ftBlue/Gray ShaleCompact shale beds, occasional; often underlain or overlain by more limestone.Color: Blue/Gray
Hardness: Medium
260 – 390 ftLimestone (hard, gray-tan)Massive limestone, some sandstone/limestone interbeds deeper; only present in deep municipal or high-capacity wells.Color: Gray/Tan
Hardness: Very Hard
390 – 407 ftLimestone with SandstoneBasal limestone with interbeds or contacts with sandstone at base of sample interval.Color: Gray/Tan
Hardness: Very Hard

Frequently Asked Questions

A typical residential well in the Escanaba 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 22 feet below the surface in this region.

Unconsolidated surficial layers in Escanaba generally begin with a thin topsoil (1-2 ft), underlain by sequences of medium to fine sands (10-30 ft) and interbedded/clayey layers (40-60 ft total thickness). These are usually followed by compact 'hardpan', gravelly clay, or sand-gravel mixes. Groundwater is commonly encountered above 20-90 ft depth. The uppermost bedrock is dominantly limestone (often with interbeds of shale or sandstone deeper), beginning at 50-150 ft depending on location. Deeper wells may encounter further sequences of blue shale or consolidated limestones down to at least 225 ft, sometimes 400 ft where deeper drilling was reported. Most wells use rotary or cable-tool drilling and are cased (commonly steel or PVC) to around 50-144 ft, and are pressure-grouted with neat cement to ~100-140 ft. Static water levels average 12-55 ft below ground. Residential wells with 5-15+ GPM yields are most often ~105 ft, up to 150 ft; higher-capacity or bedrock wells may be 225-400+ ft.