Provo Water Hardness & Quality Report (2026)
Water Hardness
10.9 grains per gallon
Source
reservoir
pH Level
7.7
neutral = 7.0
Lead
0.004 mg/L
β Below action level
TDS
330 mg/L
Est. Daily Cost
$0.50
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 Provo, your appliances are currently losing 25% efficiency due to mineral buildup.
| Appliance | In Provo | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 3.4 yrs | 8.5 yrs | -60% |
| Washing Machine | 6.7 yrs | 12 yrs | -44% |
| Water Heater | 8.1 yrs | 15 yrs | -46% |
Regional Water Comparison
How Provo compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Provo, Utah | 187.2 mg/L | 0 ppt | π΄ Very Hard | reservoir |
| Orem, Utah | β 120β179 mg/L | 0 ppt | π Hard | reservoir |
| Springville, Utah | β 180+ mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Spanish Fork, Utah | 290 mg/L | 0 ppt | π΄ Very Hard | groundwater |
| Lindon, Utah | β 180+ mg/L | 2.6 ppt | π΄ Very Hard | groundwater |
National Benchmark
How Provo compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Provo | 187.2 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 Provo's Water Unique?
Local geology and source profile
Provo City Water Department serves approximately 115,000 residents in Provo, Utah, within Utah County along the Wasatch Front. Primary sources include surface water from the Provo River, Deer Creek Reservoir, and supplemental groundwater wells in the Provo-Orem area. Water is treated at the Provo Water Treatment Plant and several well facilities, with distribution across the city's urban core, university areas, and surrounding neighborhoods. The utility manages a mixed supply from the Uinta-Wasatch-Cache National Forest watershed to meet peak summer demands from irrigation and population growth.
The Provo River watershed drains snowmelt from the Wasatch Range into Utah Lake before diversion. Water contacts limestone-dominated geology in Provo Canyon, part of the Pennsylvanian-age Oquirrh Group and Cretaceous formations, enriching it with dissolved minerals. Groundwater tapped from the ancient Lake Bonneville bench encounters Mesozoic and Cenozoic limestone and chalk formations in Utah Valley, adding further mineralization. Mountain snowmelt initially provides softer input but hardens upon contact with lower-elevation carbonate geology, resulting in a consistently hard supply.
At hard levels (187.2 mg/L), Provo's supply promotes scale buildup in pipes, reducing water heater efficiency by up to 20β30% and shortening appliance life. Dishwashers, washing machines, and faucets show white deposits most visibly, while boilers and coffee makers require frequent descaling. Annual vinegar flushes, magnetic descalers, and professional heat exchanger inspections are recommended; a whole-house water softener is advised. Provo's 2024 Consumer Confidence Report confirms EPA compliance: pH 7.5β8.2, lead below 5 ppb, no PFAS above lab limits, trace nitrates below 5 mg/L; treatment includes filtration, UV disinfection, orthophosphate corrosion control, and fluoridation at 0.7 mg/L.
Geology & Source: Provo River through Wasatch Range limestone canyons β Oquirrh Group (Pennsylvanian) and Cretaceous formations; Lake Bonneville basin valley-fill sediments; limestone and chalk dissolve calcium carbonate and magnesium, producing hard supply
Other Utah Water Reports
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Frequently Asked Questions
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Data Sources & Methodology
Water quality data for Provo 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.