ZIP 59027: well depth, groundwater and water rights

Well depth

How deep are wells in ZIP 59027?

Of 587 wells with a recorded total depth, the median is 185 feet. Half were drilled between 88 and 305 feet; one in ten went deeper than 480 feet and one in ten found water shallower than 53 feet. Depth is set by local geology and position on the landscape, both of which change over short distances, so the spread matters as much as the median.

Drilling activity

Recent well drilling in ZIP 59027

86 wells have been completed here since 2016, 4 of them in the last twelve months. The newest log on file was completed August 17, 2026. Records run back to 1900.

Water rights

Water rights on file in ZIP 59027

Montana DNRC lists 1,119 water rights with a point of diversion inside this area: 632 groundwater and 487 surface water, 1,011 of them active. The median priority date is 1974, and the oldest claim dates to 1869.

Area totals describe the neighbourhood, not any one parcel. Montana publishes no authoritative link between a parcel and a water right; whether a right attaches to a specific property is a property-level question that our reports answer with the DNRC abstract linked.

Aquifers and geology

What wells in ZIP 59027 draw from

Drillers record the aquifer a well is completed in. The units below account for the wells here that carry an aquifer assignment; the median depth beside each is for wells completed in that unit.

• Absaroka Volcanics (eocene)224 wells · 41% · median 300 ft
• Glacial Drift139 wells · 25% · median 125 ft
• Alluvium (holocene)85 wells · 15% · median 50 ft
• Gneiss And Schist (early Proterozoic Or Archean)36 wells · 7% · median 240 ft
• Alluvium (quaternary)34 wells · 6% · median 93 ft

Aquifer assignments are the driller's, recorded at completion, and many older logs carry none. Absence of an assignment is not evidence about the geology.

Environmental groundwater screening

Documented environmental sites in ZIP 59027

A documented release or site in the area is not evidence that any particular well is affected. Whether a release reaches a well depends on groundwater flow direction, geology, well depth and construction, the extent of the plume and the cleanup performed. The most recent release reported here dates to 2001. A property report screens the sites within a quarter, half and one mile of a specific parcel and links the agency records.