Layton Water Hardness & Quality Report (2026)
Water Hardness
10.4 grains per gallon
Source
mixed
pH Level
8
neutral = 7.0
Lead
0.002 mg/L
β Below action level
TDS
392.2 mg/L
Est. Daily Cost
$0.47
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 Layton, your appliances are currently losing 24% efficiency due to mineral buildup.
| Appliance | In Layton | Soft Water City | Efficiency Loss |
|---|---|---|---|
| Kettle | 3.7 yrs | 8.5 yrs | -56% |
| Washing Machine | 7 yrs | 12 yrs | -42% |
| Water Heater | 8.5 yrs | 15 yrs | -43% |
Regional Water Comparison
How Layton compares to its nearest neighbours
| City | Hardness | PFAS (ppt) | Risk | Source |
|---|---|---|---|---|
| βΆ Layton, Utah | 178 mg/L | 2.3 ppt | π Hard | mixed |
| Kaysville, Utah | 147.5 mg/L | 1.9 ppt | π Hard | mixed |
| Clearfield, Utah | 257.5 mg/L | 3.6 ppt | π΄ Very Hard | mixed |
| Syracuse, Utah | 187.5 mg/L | 2.5 ppt | π΄ Very Hard | mixed |
| Clinton, Utah | 260 mg/L | 3.6 ppt | π΄ Very Hard | mixed |
National Benchmark
How Layton compares to the USA average
| Benchmark | Hardness | Appliance Risk |
|---|---|---|
| βΆ Layton | 178 mg/L | π Moderate |
| USA National Avg | 150 mg/L | π Moderate |
| Badger Top Rated | 8.5 mg/L | π’ None |
Bring Badger-quality water to your Layton home
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What Makes Layton's Water Unique?
Local geology and source profile
Layton, Utah, in Davis County on the Wasatch Front between Salt Lake City and Ogden β a major military and aerospace community (Hill Air Force Base) β draws its municipal water supply through the City of Layton Water Division, sourcing from the Weber Basin Water Conservancy District β receiving treated Weber River water from Pineview Reservoir (Weber River tributary, Ogden Valley) and Willard Bay (an off-stream reservoir filled from the Weber River) via the Weber Basin regional aqueduct system. Water hardness in Layton measures 178 mg/L β classified as hard.
Layton's hard supply reflects the Weber River watershed's Wasatch Range and Great Basin geology. The Weber River originates in the Uinta Mountains (Precambrian Uinta Mountain Group quartzite β very soft) and flows through the Wasatch Range (CambrianβOrdovician limestone and dolomite) and the Weber Valley before reaching Pineview Reservoir. In its course through the Wasatch limestone and dolomite terrain, the Weber River acquires substantial dissolved calcium. The Wasatch Front alluvial fan deposits and the Great Salt Lake Basin calcareous lake-bed sediments in the Davis County area also contribute mineral content where local groundwater is blended. The result is the 178 mg/L hard supply typical of the northern Wasatch Front.
At 178 mg/L, Layton residents face regular hard water challenges. Scale deposits form on faucet aerators, showerheads, and appliances within weeks β monthly descaling with citric acid solution is standard maintenance. Weber Basin Water Conservancy District and City of Layton Water Division consistently deliver water meeting all Utah DDW and EPA Safe Drinking Water Act requirements.
Geology & Source: Mixed supply from Weber River (Willard Bay reservoir and Pineview Reservoir) and Wasatch Front snowmelt via the City of Layton Water Division and Weber Basin Water Conservancy District β the Wasatch Range Precambrian quartzite and Cambrian limestone and the Great Salt Lake Basin calcareous alluvial terrain; hard supply at 178 mg/L in Davis County.