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Calumet, Michigan

Well Drillers Near Calumet, Michigan

Typical Calumet area wells encounter a surficial sequence of sand, gravel, and clay, transitioning to sandstone or basalt bedrock at moderate depth.

Showing contractors within 60 miles of Calumet. 4 results found.

Typical depth
110 ft
Water table
14 ft
Contractors
4

4 Contractors

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Keranen & Eskola Well Drilling logo

Keranen & Eskola Well Drilling

Active Driller
Calumet, MI 49913
Well DrillingCable ToolPump Installation+4 more
Siirtola Well and Pump logo

Siirtola Well and Pump

Dollar Bay, MI 49922
Well DrillingPump InstallationPump Repair+2 more
Larson Well Drilling and Pump Co logo

Larson Well Drilling and Pump Co

Skanee, MI 49962
Well DrillingPump InstallationPump Repair+1 more

Smith Well Drilling

Marquette, MI 49855
Well DrillingPump ReplacementWell Maintenance

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View Local Geology Report

A geological estimate for the Calumet area.

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

Detailed Summary

Across Calumet and surrounding areas, well logs typically show an upper unconsolidated sequence largely consisting of alternating sand, gravel, and clay layers, between 30 and 60 ft thick, sometimes with boulders or cobbles. Below this, wells commonly encounter a consolidated bedrock zone, most often described as sandstone (occasionally listed as 'Freda Ss', red/soft) or basalt ('broken' or hard). The transition to bedrock usually occurs near 40–60 ft, with some variation depending on local glacial deposits or proximity to Lake Superior. Drilling is often by cable tool or rotary methods, with typical casing set into bedrock. Most residential wells reach total depths of 90–130 ft for reliable supplies of 5–15+ GPM. Deeper bedrock wells (especially in basalt) may extend to 150–200+ ft, though not all high-capacity yields are assured at these depths. Static water level is usually between 8 and 25 ft below grade, occasionally artesian.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
02 ftSand/Silt/TopsoilLoose, sandy or silty topsoil, sometimes with some gravel or clay contentColor: Brown, gray
Hardness: Soft
225 ftSand, Gravel, Clay (variable layering)Interbedded sand, gravel (sometimes with cobbles or boulders), clayey and silty intervalsColor: Varied: tan, gray, reddish
Hardness: Soft to firm
2560 ftClay, Sand & Gravel MixThicker clay-rich sections with sandy or gravelly interbeds, possible stones/boulders, some red or hard clayColor: Gray, red, brown
Hardness: Firm to stiff
6085 ftTransition Zone (Sandstone or Basalt - fractured/broken, soft bedrock)Consolidated, fractured or soft bedrock, commonly sandstone or broken basalt, can be water-bearingColor: Red (sandstone), gray-black (basalt)
Hardness: Firm to hard
85175 ftBedrock (Sandstone/Freda Ss/Basalt)Firm to hard bedrock, primary hydrostratigraphic unit is either sandstone (Freda/soft/red) or basalt (hard/gray-black); yields decrease with depth in basaltColor: Red (sandstone), gray-black (basalt)
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Calumet 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 14 feet below the surface in this region.

Across Calumet and surrounding areas, well logs typically show an upper unconsolidated sequence largely consisting of alternating sand, gravel, and clay layers, between 30 and 60 ft thick, sometimes with boulders or cobbles. Below this, wells commonly encounter a consolidated bedrock zone, most often described as sandstone (occasionally listed as 'Freda Ss', red/soft) or basalt ('broken' or hard). The transition to bedrock usually occurs near 40–60 ft, with some variation depending on local glacial deposits or proximity to Lake Superior. Drilling is often by cable tool or rotary methods, with typical casing set into bedrock. Most residential wells reach total depths of 90–130 ft for reliable supplies of 5–15+ GPM. Deeper bedrock wells (especially in basalt) may extend to 150–200+ ft, though not all high-capacity yields are assured at these depths. Static water level is usually between 8 and 25 ft below grade, occasionally artesian.