The water in Lake County comes from fractured rocks beneath the surface. These are old shale and other hard stones that crack and split underground. Water fills the spaces between these cracks and fragments. This type of rock layer supplies wells across the county and neighboring areas.
Manganese and lead dissolve naturally from the rock itself as water sits in contact with it underground. Chloride comes from road salt spread during winter that soaks down into the ground. Sulfate also releases from minerals in the shale. The fractured nature of these rocks means contaminants can move through more easily than they would through dense clay or limestone.
The water here is extremely hard and loaded with minerals. Iron content will stain sinks and laundry orange-brown. Sodium levels are very high, and sulfate gives the water a bitter taste. You will notice white or tan scale buildup in pipes and on fixtures, and your water heater will work harder and wear out faster.
Lead and manganese both exceed EPA health standards in Lake County well water. These metals dissolve naturally from the rock layers underground in this area. Lead is especially dangerous for children and can affect brain development. Manganese at elevated levels can harm the nervous system over time.
Your water is also extremely hard with very high sodium and sulfate. You will notice white or tan scale buildup on faucets and inside pipes. Iron in the water will stain your sinks and laundry orange or brown. The high sodium means the water may taste salty, and sulfate can cause a bitter taste.
Get your well tested by a state-certified lab right away. A basic health screen for bacteria and nitrate costs fifty to one hundred dollars, but ask for a comprehensive panel including lead, manganese, and arsenic, which runs two hundred to four hundred dollars. A whole-house treatment system with filtration and a water softener can address multiple contaminants at once.
| Contaminant | Samples ⓘ | % Above MCL ⓘ | Distribution ⓘ | Confidence ⓘ | Risk ⓘ |
|---|---|---|---|---|---|
| Manganese | 4 | 100% | 25% · 0% · 75% | Low | High |
| Lead | 6 | 60% | 50% · 0% · 50% | Low | High |
| Chloride | 104 | 47% | 45% · 9% · 46% | High | High |
| Sulfate | 47 | 9% | 72% · 19% · 8% | Moderate | Moderate |
| Arsenic | 3 | 0% | 67% · 33% · 0% | Low | Moderate |
| Fluoride | 6 | 0% | 100% · 0% · 0% | Low | Low |
| Iron | 7 | 0% | 71% · 29% · 0% | Low | Low |
| Nitrate | 3 | 0% | 100% · 0% · 0% | Low | Low |
| Nitrite | 31 | 0% | 100% · 0% · 0% | Moderate | Low |
| E. coli | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Hardness | 35 | — | — | Moderate | Low |
| pH | 22 | — | — | Moderate | Low |
| Sodium | 70 | — | — | Moderate | Low |
MCL = Maximum Contaminant Level (EPA limit for public water; used as benchmark for private wells). Distribution shows % of sampled wells in each concentration band. Methodology.
Population-level CDC data. Not individual risk prediction.
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