Montana runs as four working zones. Billings and the Yellowstone Valley corridor at 200-340 mg/L on Billings Water Yellowstone River-and-aquifer-supplemented supply. Missoula and the western Montana corridor at 140-220 mg/L on Mountain Water Company aquifer supply (softer than the eastern Montana profile). The Bozeman, Helena, Great Falls, and central Montana corridor at 160-260 mg/L on mixed municipal supplies. The northwest Montana lakes corridor (Kalispell, Whitefish, Polson) at 130-200 mg/L on Flathead aquifer-and-lake-source supply. The Bakken-adjacent eastern Montana corridor (Glendive, Sidney, Wolf Point, Miles City) at 240-400 mg/L on hard aquifer and well-water systems. Rural Montana well-water statewide variable 200-400 mg/L.
HOW IT BREAKS DOWNmoderate to very hard (regional gradient)
Eastern Montana Bakken-adjacent corridor is among the hardest municipal water in the country. Mountain Water Company Missoula aquifer is genuinely softer than the eastern Montana profile. Wildfire-smoke residue heavy June through October in active fire years. High-elevation UV-accelerated IGU seal degradation in Big Sky, Whitefish Mountain Resort, Bridger Bowl, Discovery, Red Lodge, and the surrounding Mountain West corridor residential. Heavy ski-corridor seasonal commercial. Substantial post-2018 boom-residential expansion through Bozeman and Kalispell-Whitefish driven by California and Pacific Northwest migration. Bakken-corridor industrial residue on eastern Montana commercial. Winter exterior work effectively shuts down December through February statewide. Heritage residential concentration through Butte, Helena, and Bozeman.
A blended system means hardness moves with the blend. Two addresses on the same utility can read differently, and the same address can read differently across a year, depending on which source is carrying the load that season.
Montana spans 3 hardness bands, which means there is no single answer for the whole state — the method changes as you move across it. Both ends are below.
This is the band where the water starts writing on the glass. Wash with tap — the surfactant holds the minerals in suspension while you work, so the wash pass is not the problem — then rinse with distilled and pull that. The rinse is the whole intervention: it replaces the mineral-bearing water sitting on the glass with water that has nothing in it to leave. This single change resolves most of the "I cleaned it and it still looks bad" complaints in this range, and it does not require buying a system.
A distilled rinse stops being an improvement and becomes the method. Tap water left to dry on glass at this concentration deposits a visible film within minutes, and the film is cumulative: each cleaning that ends in tap water adds a layer that the next cleaning has to get through first. Glass on a sprinkler line or under a runoff drip needs a maintenance interval, not just a better wash — the deposit is arriving faster than a cleaning schedule built around dust would predict.
The hardest water in North America — Phoenix, Las Vegas, West Texas, much of the limestone Midwest. At this concentration calcium carbonate precipitates out of any water that touches the glass and dries, so what you are looking at is essentially limestone, growing one molecular layer at a time. Tap water cannot be part of the final pass under any circumstance, including "just a quick rinse." Above roughly 300 mg/L, buying distilled by the gallon stops making economic sense against a DI filter or a pure-water pole system, and a residential owner cleaning their own glass twice a year is usually better served by a service that already owns one.
Hardest first — the order that matters, because the hard end is where the method has to change. Each figure is a service-area typical for the named utility. Within Montana the spread runs from Whitefish at 165 mg/L to Billings at 260 — a difference big enough that the same bottle of cleaner behaves differently in each.
This page is about Montana's water and nothing else. For how cleaning actually works in Montana across the year — climate, seasonal timing, the local contaminants, the housing stock — see the Montana cleaning guide.
For a figure at your own address rather than your city, the Hard Water Scorer takes a ZIP code. If you run a pure-water system, the TDS diagnostic reads the other end of the same problem.
USGS national hardness survey data and utility Consumer Confidence Reports, 2023 vintage. City figures are service-area typicals for the named utility, not readings from any one tap. State ranges are the lowest and highest typical municipal values across the state, so they bracket the populated area rather than describing an average resident. Where a state blends sources seasonally, the range is wider than any single address will ever see.
Private wells are outside all of it. A well is whatever the rock under it says, and the only number that describes one is a test of that tap. Have a reading that disagrees with this table? Send it to us — a number that contradicts the table is worth more than one that confirms it.