Blackfoot Water Hardness & Quality Report (2026)
Water Hardness
180+ mg/L
Very Hardestimated Β· not lab-verified
Source
groundwater
pH Level
7.9
neutral = 7.0
Lead
0.002 mg/L
β Below action level
TDS
332 mg/L
Est. Daily Cost
$0.91
energy & soap waste
Source: See methodology section below Β· Updated 2026
0β60
mg/L
Soft
61β120
mg/L
Moderately Hard
121β180
mg/L
Hard
180+
mg/L
Very Hard
Appliance Damage Report
In Blackfoot, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In Blackfoot | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 4.7 yrs | 8.5 yrs | -45% |
| Washing Machine | 6.6 yrs | 12 yrs | -45% |
| Water Heater | 8.3 yrs | 15 yrs | -45% |
Regional Water Comparison
How Blackfoot compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Blackfoot, Idaho | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Chubbuck, Idaho | 332.1 mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Pocatello, Idaho | 350 mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Idaho Falls, Idaho | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Ammon, Idaho | 238 mg/L | 0 ppt | π΄ Very Hard | groundwater |
National Benchmark
How Blackfoot compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Blackfoot | β 180+ mg/L | π΄ High |
| USA National Avg | 151 mg/L | π Moderate |
| Scarsdale Top Rated | 0.02 mg/L | π’ None |
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What Makes Blackfoot's Water Unique?
Local geology and source profile
The City of Blackfoot, Idaho, provides municipal water to residents of Bannock County in southeastern Idaho. This vital service draws entirely from groundwater sources tapped from the Snake River Plain aquifer, a significant regional water supply. Before reaching taps, the water undergoes treatment at a facility designed to meet stringent quality standards set by the Idaho Department of Environmental Quality and adhere to the federal Safe Drinking Water Act. The utility ensures that the water delivered is safe and meets all regulatory requirements for public consumption.
The aquifer beneath Blackfoot is geologically diverse, primarily composed of Quaternary basalts and sedimentary layers. Deeper strata include Tertiary volcanic rocks, specifically Miocene-age basalts and rhyolites, typical of the Snake River Plain's volcanic history. As water filters through these mineral-rich volcanic and sedimentary formations, it naturally picks up substantial amounts of calcium and magnesium. This geological process is the direct cause of the region's characteristically very hard water supply.
Homeowners will likely observe scale buildup in common kitchen appliances like kettles and coffee makers, and in dishwashers. You'll also notice that soap and detergents don't lather as effectively with this water. Appliances such as water heaters and plumbing fixtures are especially susceptible to mineral deposits, which can impair their efficiency and shorten their lifespan. To combat these issues and protect your household equipment, installing a water softener is highly recommended. This will help maintain appliance performance and improve cleaning results. Residents can find more detailed information on water quality, including specific contaminant levels and treatment methods, in the city's annual Consumer Confidence Reports.
Geology & Source: Snake River Plain aquifer; Quaternary basalts and sedimentary deposits over Tertiary volcanic rocks; Miocene basalts and rhyolites yield very hard water
Other Idaho Water Reports
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Frequently Asked Questions
Is Blackfoot's water safe to drink?
Do I need a water softener in Blackfoot?
How does Blackfoot compare to the USA average?
Data Sources & Methodology
Water quality data for Blackfoot is derived from geographic and geological modelling of the surrounding region. No federal monitoring station data was available for this location.
Water Hardness
Modelled estimate based on state-level USGS geological survey data for this region. No direct USGS Water Quality Portal measurement was matched to this city β the value reflects a statistical range calibrated to the state's dominant rock types and typical source water characteristics.
pH
Estimated from regional geology and source water characteristics. pH is correlated with water hardness and local bedrock β values may differ from utility-reported figures.
TDS β Total Dissolved Solids
Estimated using a derived ratio from water hardness and regional conductance profiles. TDS in natural water correlates strongly with total mineral content including hardness ions.
PFAS β Perfluoroalkyl and Polyfluoroalkyl Substances
EPA UCMR5 (5th Unregulated Contaminant Monitoring Rule, 2023β2025) β sum of PFAS compounds detected at the public water system serving this city. A value of 0 indicates the system was sampled with no detection above reporting limits.
Lead
Modelled estimate based on the EPA Lead and Copper Rule 90th-percentile tap-sample methodology. No publicly available per-city lead dataset with sufficient national coverage exists. Values are a conservative baseline derived from city population tier and infrastructure age β all estimates are maintained below the EPA action level of 0.015 mg/L.
Appliance Lifespan
Calculated from water hardness using a linear degradation model. Baseline lifespans represent soft-water performance (kettle: 8.5 yrs, washing machine: 12.0 yrs, water heater: 15.0 yrs). Hard water mineral scale progressively reduces operational life in direct proportion to hardness concentration.