Your water comes from mixed underground rock and soil layers beneath Macomb County. These are not thick, uniform limestone beds like in neighboring areas. Instead, you have a jumbled combination of sand, gravel, clay, and old rock fragments left behind by glaciers thousands of years ago. This mixture holds water but lets contaminants move through it more easily than solid rock does.
Manganese, iron, and chloride show up because of what's naturally in the rock and what happens on the surface. Iron and manganese are minerals locked in the old rock particles. Chloride enters from road salt spread during winter and from other human activities that seep down into the ground. The mixed soil and rock layers do not filter these out as well as solid limestone would.
Your water is very mineral-heavy with high sodium and sulfate levels. These minerals come from the dissolving rock and trapped saltwater deep underground. Day-to-day, this water stains fixtures with orange-brown iron marks, tastes salty, and builds up scale in pipes and water heaters faster than softer water would. You'll replace appliances sooner and need regular cleaning to keep sinks and toilets looking clean.
Manganese, iron, and chloride in Macomb County well water exceed EPA health standards. This is a serious situation that needs your attention right away. Your water is flagged as high urgency based on the contamination patterns in your area.
Long-term exposure to manganese can affect brain function and development in children. Iron at these levels stains sinks, toilets, and laundry badly and can give water a metallic taste. High sodium and sulfate together make water taste salty and can damage pipes and water heaters over time.
Get your well tested by a state-certified lab to confirm what is in your water—a basic health screen runs $50–100, and a full mineral panel runs $200–400. A whole-house sediment filter paired with an iron removal system can address your contamination.
| Contaminant | Samples ⓘ | % Above MCL ⓘ | Distribution ⓘ | Confidence ⓘ | Risk ⓘ |
|---|---|---|---|---|---|
| Manganese | 5 | 75% | 20% · 20% · 60% | Low | High |
| Iron | 81 | 36% | 52% · 12% · 36% | Moderate | High |
| Chloride | 64 | 25% | 58% · 17% · 25% | Moderate | High |
| Sulfate | 46 | 2% | 85% · 13% · 2% | Moderate | Low |
| Fluoride | 24 | 0% | 100% · 0% · 0% | Moderate | Low |
| Arsenic | 6 | 0% | 83% · 17% · 0% | Low | Low |
| Radon | 3 | 0% | 33% · 67% · 0% | Low | Moderate ⓘ |
| Uranium | 5 | 0% | 100% · 0% · 0% | Low | Low |
| Nitrite | 38 | 0% | 100% · 0% · 0% | Moderate | Low |
| Nitrate | 29 | — | — | Moderate | Low |
| Fecal Coliform | 1 | — | — | Low | Safe |
| pH | 8 | — | — | Low | Low |
| Nitrate | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Sodium | 47 | — | — | Moderate | Low |
| Total Coliform | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| E. coli | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Lead | 1 | 0% | 100% · 0% · 0% | Low | Safe |
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.
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