Redding Water Hardness & Quality Report (2026)
Water Hardness
10.9 grains per gallon
Source
mixed
pH Level
8.3
neutral = 7.0
Lead
0.009 mg/L
✓ Below action level
TDS
587.8 mg/L
Est. Daily Cost
$0.50
energy & soap waste
Source: USGS Water Quality Portal · Updated 2026
0–60
mg/L
Soft
61–120
mg/L
Moderately Hard
121–180
mg/L
Hard
180+
mg/L
Very Hard
Appliance Damage Report
In Redding, your appliances are currently losing 25% efficiency due to mineral buildup.
| Appliance | In Redding | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 3.5 yrs | 8.5 yrs | -59% |
| Washing Machine | 6.7 yrs | 12 yrs | -44% |
| Water Heater | 8.2 yrs | 15 yrs | -45% |
Regional Water Comparison
How Redding compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| ▶ Redding, California | 186 mg/L | 7.4 ppt | 🔴 Very Hard | mixed |
| Red Bluff, California | 180 mg/L | 7.3 ppt | 🔴 Very Hard | mixed |
| Chico, California | 80.5 mg/L | 4.3 ppt | 🟡 Moderately Hard | mixed |
| Paradise, California | 136 mg/L | 6 ppt | 🟠 Hard | mixed |
| Oroville, California | 57 mg/L | 3.6 ppt | 🟢 Soft | mixed |
National Benchmark
How Redding compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| ▶ Redding | 186 mg/L | 🔴 High |
| USA National Avg | 150 mg/L | 🟠 Moderate |
| Badger Top Rated | 8.5 mg/L | 🟢 None |
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What Makes Redding's Water Unique?
Local geology and source profile
Redding, California, the Shasta County seat at the northern end of the Sacramento Valley, draws its municipal water supply from the Sacramento River via the City of Redding Electric Utility Department water operations, with a Sacramento River intake at the Keswick–Anderson stretch north of Redding in Shasta County. The Sacramento River at Redding is impounded by Shasta Dam (Shasta Lake) — the primary storage reservoir — which drains the upper Sacramento Valley watershed including the Trinity Alps and Shasta and Trinity Counties. Water hardness measures 186 mg/L — classified as hard, notably higher than expected for a Northern California river source.
Redding's surprisingly hard supply reflects the complex upper Sacramento watershed geology and possibly significant Trinity River Diversion influence. Shasta Lake impounds the McCloud River (from the Modoc Plateau — Columbia River Basalt and Pliocene volcanic terrain), the Pit River (from the Modoc Plateau — Tertiary basalt and calcareous marine formations of the Modoc Plateau calcareous terrain — a notably more calcium-rich watershed than expected), and the Sacramento River headwaters (Mt. Shasta volcanic terrain). The Pit River drains particularly calcareous Modoc Plateau bedrock — Cretaceous and Paleocene calcareous marine formations of the intermontane basin — contributing significant dissolved calcium. The Trinity River Diversion also carries Klamath Mountains serpentinite and calcareous schist contribution.
At 186 mg/L, Redding residents face regular hard water challenges. Scale deposits form on faucet aerators, showerheads, shower glass, and tile within weeks — monthly descaling with citric acid solution is standard maintenance. Dishwashers require rinse-aid for acceptable glassware results, and water heaters benefit from annual inspection. City of Redding consistently delivers water meeting all California SWRCB and EPA Safe Drinking Water Act requirements.
Geology & Source: River supply from the Sacramento River via the City of Redding Public Works intake at the Keswick–Anderson stretch — the upper Sacramento River at Redding drains the Klamath Mountains Paleozoic metamorphic belt (Trinity Alps), Trinity Ultramafic Belt, and the Cascade Range Lassen volcanic terrain; the Klamath–Cascade crystalline and volcanic watershed produces moderately hard supply at 186 mg/L — higher than expected for volcanic terrain.