Bend Water Hardness & Quality Report (2026)
Water Hardness
3.9 grains per gallon
Source
reservoir
pH Level
7.5
neutral = 7.0
Lead
0.005 mg/L
β Below action level
TDS
142.7 mg/L
Est. Daily Cost
$0.18
energy & soap waste
Source: USGS Water Quality Portal 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 Bend, your appliances are currently losing 9% efficiency due to mineral buildup.
| Appliance | In Bend | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 7.4 yrs | 8.5 yrs | -13% |
| Washing Machine | 11.2 yrs | 12 yrs | -7% |
| Water Heater | 13 yrs | 15 yrs | -13% |
Regional Water Comparison
How Bend compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Bend, Oregon | 66 mg/L | 2 ppt | π‘ Moderately Hard | reservoir |
| Redmond, Oregon | 94.5 mg/L | 2.6 ppt | π‘ Moderately Hard | reservoir |
| The Dalles, Oregon | 22.5 mg/L | 1.2 ppt | π’ Soft | reservoir |
| Lebanon, Oregon | 42.5 mg/L | 1.6 ppt | π’ Soft | reservoir |
| Springfield, Oregon | 32 mg/L | 1.4 ppt | π’ Soft | reservoir |
National Benchmark
How Bend compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Bend | 66 mg/L | π‘ Low |
| USA National Avg | 150 mg/L | π Moderate |
| Badger Top Rated | 8.5 mg/L | π’ None |
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What Makes Bend's Water Unique?
Local geology and source profile
Bend, Oregon, in Deschutes County on the eastern slope of the Cascade Range β the largest city in central Oregon β draws its municipal water supply from the Deschutes River via the City of Bend Utilities Water Division, with treated surface water from the Upper Deschutes River system. Bend sources from Tumalo Creek (a direct Cascade Range stream) and the Deschutes River system at intake points managed by the City, with storage in the Tumalo Reservoir system and Cascade Range spring-fed flow. Water hardness in Bend measures 66 mg/L β classified as moderately soft.
Bend's moderately soft supply reflects the Cascade Range volcanic geology of the Upper Deschutes watershed. The Upper Deschutes watershed drains the High Cascades β a zone of Quaternary basalt and andesite shield volcanoes (South Sister, Broken Top, Mount Bachelor) and the flanking Western Cascades volcaniclastic sequence. These young Cascade basalts and andesites are essentially calcium-poor mafic volcanic rock β while they contain plagioclase feldspar with some calcium, the rapid permeability of the porous basaltic terrain allows water to flush through quickly, acquiring minimal calcium. The Newberry Volcano and the central Oregon lava plateau further characterise the watershed's volcanic nature. Tumalo Creek spring-fed contributions from the High Cascade volcanic aquifer maintain consistently soft supply.
With hardness at 66 mg/L, Bend residents experience minimal to moderate scale challenges. Faucet aerators and showerheads develop deposits slowly β bi-monthly cleaning with citric acid solution is sufficient. Dishwashers produce clean glassware. City of Bend Utilities Water Division consistently delivers water meeting all Oregon Health Authority and EPA Safe Drinking Water Act requirements.
Geology & Source: Surface supply from the Deschutes River (Wickiup and Crane Prairie Reservoirs, Cascade Range snowmelt) via the City of Bend Utilities β the Upper Deschutes watershed drains the Cascade Range High Cascades Quaternary basalt and andesite, the Newberry Volcano and central Oregon volcanic plateau; the volcanic Cascades terrain produces moderately soft supply at 66 mg/L.