L. Denton Water Well
Grant, MI49327
The typical geological profile for Grant, Newaygo County, MI, includes surficial sand, an intermediate clay (often blue or gray), and a thick, water-bearing sand or sand and gravel aquifer. Residential wells usually reach about 80 ft, with static water levels typically around 30 ft below ground.
Showing contractors within 60 miles of Grant. 61 results found.
A geological estimate for the Grant area.
Typical Well Depth
Static Water Level
Recommended Method
Based on the synthesis of several well logs from the Grant, MI region, the representative geologic profile consists of an initial surficial sand layer (10–20 ft thick), an intermediate blue or gray clay unit (10–20 ft thick), and a main lower sand or sand and gravel aquifer, which is generally the primary water-bearing zone. This main sand aquifer frequently extends from roughly 30–35 ft below grade to the bottom of most residential wells in the 75–100 ft depth range. Thinner or additional clay lenses may also be present locally, but as a rule, this three-layered sequence dominates. Residential wells yielding 10–25 GPM are most often completed between 75–90 ft, with static water levels averaging near 30 ft below grade. High capacity wells (Type II public or irrigation) can be completed to similar or slightly deeper depths depending on demand, but rarely exceed 110 ft in this setting.
Depth (Feet) | Formation Type | Description | Characteristics |
---|---|---|---|
0 – 15 ft | Sand | Fine to medium, surficial sand often slightly silty near top. | Color: Light brown to tan Hardness: Loose |
15 – 35 ft | Clay | Blue or gray clay, occasional thin sand partings, not water-bearing. | Color: Blue/gray Hardness: Firm-plastic |
35 – 80 ft | Sand (Aquifer) | Coarse sand to sand & gravel; primary water-bearing zone, some sections may be fine sand. | Color: Tan to gray Hardness: Loose to medium |