Rexburg Water Hardness & Quality Report (2026)
Water Hardness
180+ mg/L
Very Hardestimated Β· not lab-verified
Source
groundwater
pH Level
8.1
neutral = 7.0
Lead
0.005 mg/L
β Below action level
TDS
130 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 Rexburg, your appliances are currently losing 45% efficiency due to mineral buildup.
| Appliance | In Rexburg | 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 Rexburg compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Rexburg, Idaho | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Ammon, Idaho | 238 mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Idaho Falls, Idaho | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Blackfoot, Idaho | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Jackson, Wyoming | 293 mg/L | 3.3 ppt | π΄ Very Hard | groundwater |
National Benchmark
How Rexburg compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Rexburg | β 180+ mg/L | π΄ High |
| USA National Avg | 151 mg/L | π Moderate |
| Scarsdale Top Rated | 0.02 mg/L | π’ None |
Bring Scarsdale-quality water to your Rexburg home
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What Makes Rexburg's Water Unique?
Local geology and source profile
The City of Rexburg Public Works Department operates the municipal water utility, serving approximately 29,000 residents in Rexburg, Madison County, Idaho, and surrounding areas. Water is sourced exclusively from groundwater wells tapping the Eastern Snake River Plain Aquifer, a major alluvial aquifer system spanning southern Idaho. No named surface reservoirs or rivers are used; all supply comes from multiple production wells distributed across the service area. Treatment involves basic disinfection with chlorine, with no advanced softening or filtration infrastructure reported in available data.
The Eastern Snake River Plain watershed is a vast closed basin defined by the Snake River's path through southern Idaho, with aquifer recharge occurring via infiltration from the river, irrigation return flows, and precipitation over volcanic plains. Key geology includes Miocene-Pliocene basalt flows of the Snake River Group interlayered with sediments, overlain by Quaternary gravels and lakebed clays from ancient pluvial Lake Terreton. Limestone and carbonate deposits from Paleozoic to Cenozoic eras dissolve substantial calcium and magnesium into the groundwater, producing a very hard supply.
Very hard water in Rexburg causes severe scale buildup in pipes, water heaters, dishwashers, washing machines, and faucets, leading to reduced efficiency and frequent breakdowns β estimated annual damages can exceed $1,400 per household from mineral deposits. Soap lathering is poor, leaving films on skin, hair, and dishes, and laundry becomes stiff and grayish. A whole-home water softener is strongly recommended to exchange minerals for sodium and protect appliances. Independent analyses detect contaminants including arsenic, hexavalent chromium, nitrates, radium, and uranium, with some exceeding health advocacy guidelines (though below EPA MCLs); treatment is basic chlorination with no PFAS data available.
Geology & Source: Eastern Snake River Plain Aquifer β Miocene-Pliocene basalt flows of the Snake River Group overlain by Quaternary gravels and lakebed clays; limestone and carbonate deposits dissolve calcium and magnesium, producing extreme hardness
Other Idaho Water Reports
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Frequently Asked Questions
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How does Rexburg compare to the USA average?
Data Sources & Methodology
Water quality data for Rexburg 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.