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Marquette, Michigan

Well Drillers Near Marquette, Michigan

A typical well in the Marquette region penetrates unconsolidated sand, clay, and gravel layers before finishing in glacial sand/gravel or bedrock. Most wells use rotary or cable tool drilling, are cased with steel to near total depth, and are screened primarily in the lower unconsolidated section, with static water levels typically between 10 ft and 60 ft below grade.

Showing contractors within 60 miles of Marquette. 8 results found.

Typical depth
80 ft
Water table
30 ft
Contractors
8

8 Contractors

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Boussum Well Drilling Inc

Active Driller
690 Railroad Ave
Channing, MI 49815
Water well drillingWell pump installationWell maintenance and repair+1 more
Kleiman Pump & Well Drilling Inc logo

Kleiman Pump & Well Drilling Inc

Active Driller
PO Box 704
Iron Mountain, MI 49801-0704
Pump installationPump repairWell service+1 more
Morin & Johnson Well Drilling & Pump Inc logo

Morin & Johnson Well Drilling & Pump Inc

670 COOLIDGE AVE
NIAGRA, WI 54151-
Well drillingCable tool well drillingHydrofracturing+10 more

Howard's Water Pumps & Services

717 Stephenson Ave
Escanaba, MI 49829
Water pump salesWater pump installationWater pump repair+3 more

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Well records near Marquette

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View Local Geology Report

A geological estimate for the Marquette area.

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

Detailed Summary

Based on a synthesis of the provided well logs for the Marquette area, the most common geological sequence begins with a surficial sand (or mixed sand and clay) horizon extending to an average of about 35–40 feet. This is often underlain by a significant clay (sometimes sandy) or clay-with-gravel sequence which typically extends to depths between 55 and 110 feet. The deeper portions of many wells (ranging from about 50–120 ft in the samples) frequently encounter gravel, sand & gravel, weathered sandstone, or a hard rock such as greenstone. Most residential wells are completed within these unconsolidated aquifers, with screen intervals set in the basal sand/gravel zone. Well casing (usually steel, 4–6 in diameter) generally reaches nearly the full depth. Static water levels show substantial variability but tend to fall between 10 ft and 60 ft below grade, reflecting a combination of surficial recharge and deeper flowpaths.

Expected Geological Layers

Depth (Feet)Formation TypeDescriptionCharacteristics
015 ftSand (fine to medium, sometimes mixed with clay)Yellowish to brown surficial sand, occasionally mixed with clay; unconsolidated, loose formationColor: Yellow/Brown
Hardness: Soft
1545 ftSand/Clay and ClayInterbedded sand and clay or sandy clay; some records note occasional gravel inclusions in this intervalColor: Brown/Orange
Hardness: Soft to firm
4575 ftGravel & Clay or Clay & GravelIncreasingly gravelly matrix, often with significant clay content; transitional zoneColor: Brown/Grey
Hardness: Medium
75110 ftSand & Gravel or Clean GravelBasal aquifer zone, frequently water-bearing; usually main screened interval for residential supplyColor: Brown/Grey
Hardness: Medium
110120 ftWeathered Bedrock (Sandstone or Greenstone)If present, transition to indurated bedrock, e.g. sandstone or greenstone; locally may begin slightly shallower or deeper depending on siteColor: Varies (Red/Green)
Hardness: Hard

Frequently Asked Questions

A typical residential well in the Marquette area is drilled to approximately 80 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.

Based on a synthesis of the provided well logs for the Marquette area, the most common geological sequence begins with a surficial sand (or mixed sand and clay) horizon extending to an average of about 35–40 feet. This is often underlain by a significant clay (sometimes sandy) or clay-with-gravel sequence which typically extends to depths between 55 and 110 feet. The deeper portions of many wells (ranging from about 50–120 ft in the samples) frequently encounter gravel, sand & gravel, weathered sandstone, or a hard rock such as greenstone. Most residential wells are completed within these unconsolidated aquifers, with screen intervals set in the basal sand/gravel zone. Well casing (usually steel, 4–6 in diameter) generally reaches nearly the full depth. Static water levels show substantial variability but tend to fall between 10 ft and 60 ft below grade, reflecting a combination of surficial recharge and deeper flowpaths.