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East Lansing, Michigan

Well Drillers Near East Lansing, Michigan

Typical East Lansing area wells penetrate glacial clays and gravels, underlain by bedrock composed mainly of shale and sandstone. Water is most often sourced from the upper bedrock aquifers at depths between 120 and 200 ft.

Showing contractors within 60 miles of East Lansing. 102 results found.

Typical depth
180 ft
Water table
30 ft
Contractors
102

102 Contractors

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View Local Geology Report

A geological estimate for the East Lansing area.

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

Detailed Summary

A representative geological profile of East Lansing shows an upper sequence of brown/gray clay (with gravel in places), typically 15–30 ft thick, followed by additional silty to sandy clays with intermittent gravelly or sandy zones to about 60–75 ft. Beneath these fine-grained sediments, there is a consistent transition to bedrock, which is primarily shale interlayered with sandstone. In most wells, initial shale is encountered beneath 65–75 ft, sometimes with a thin sandstone/sandrock or sandy shale interval above or within the shale. Below this, most wells show alternating bands of shale and sandstone down to total depths of 150–425 ft. Yields are best from the upper sandstone or sandy shale zone. A typical residential well for 5–15+ GPM is completed between 140 and 200 ft, with static water levels commonly between 14 and 54 ft below ground.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
0 – 20 ftClay (Brown/Gray, Glacial)Brown and/or gray clay. Locally includes gravel or sand, especially in basal part.Color: Brown to Gray
Hardness: Soft to Firm
20 – 65 ftClay/Silty Clay (with Gravel & Sandy Lenses)Gray or brown silty to sandy clay, frequent inclusions of fine gravel or sand especially towards base. Locally stoney.Color: Gray, Brown
Hardness: Firm
65 – 90 ftSand or Sandstone TransitionRed, white, or gray sandstone, or compact sand beds, often marking base of glacial sequence or start of bedrock. Sometimes interbedded with shale.Color: Red, White, or Gray
Hardness: Medium
90 – 230 ftShale Interbedded with SandstoneMostly gray or red shale, with occasional interbeds of sandstone or sandrock, sometimes with minor clay. Yields water to wells.Color: Gray, Red
Hardness: Soft to Hard (variable)
230 – 320 ftThick Shale with Subordinate SandstoneDominantly shale, often soft to firm, with thin, hard beds or streaks of sandstone. Sometimes grades into harder sandstone below.Color: Gray, Red, Black
Hardness: Soft to Hard
320 – 425 ftSandstone and Shale (Deeper Sequence)Interbedded gray or brown sandstone and shale, more common in deepest wells. Sandstone is generally water bearing.Color: Gray, Brown
Hardness: Hard

Frequently Asked Questions

A typical residential well in the East Lansing area is drilled to approximately 180 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 of East Lansing shows an upper sequence of brown/gray clay (with gravel in places), typically 15–30 ft thick, followed by additional silty to sandy clays with intermittent gravelly or sandy zones to about 60–75 ft. Beneath these fine-grained sediments, there is a consistent transition to bedrock, which is primarily shale interlayered with sandstone. In most wells, initial shale is encountered beneath 65–75 ft, sometimes with a thin sandstone/sandrock or sandy shale interval above or within the shale. Below this, most wells show alternating bands of shale and sandstone down to total depths of 150–425 ft. Yields are best from the upper sandstone or sandy shale zone. A typical residential well for 5–15+ GPM is completed between 140 and 200 ft, with static water levels commonly between 14 and 54 ft below ground.