Your well water comes from old limestone and similar carbonate rock layers buried deep underground. These rocks have cracks and tiny holes that let water flow through them. The limestone sits in valleys between ridges of harder stone, creating natural pathways for groundwater to move toward your well.
Lead, radon, and iron show up in your water because of the rock itself and human activity. Radon comes from natural radioactive materials inside the limestone that break down over time. Iron dissolves from the rock as water sits in contact with it for years. Lead enters from old pipes and also occurs naturally where the rock cracks and allows water to pick it up.
Your water is extremely hard and carries very high amounts of minerals. This means white crusty scale builds up fast inside pipes and water heaters, and it clogs fixtures. The high sulfate levels give the water a salty or bitter taste, and the iron stains sinks and laundry orange.
Lead, radon, and iron in Dauphin County wells exceed EPA health standards. This is a high-urgency situation that demands your attention now. Your water carries multiple serious contaminants that pose real health risks to your family, especially children. Testing your well is not optional—it is necessary.
Long-term exposure to lead damages children's brains and kidneys, even at low levels. Radon in water releases radioactive gas into your home during showers and washing, increasing lung cancer risk. Iron at extreme levels stains sinks, toilets, and laundry orange-red. The sulfate and sodium levels are also very high, making your water extremely hard and leaving crusty buildup inside pipes.
Get a certified lab test right now from a state-certified laboratory. A basic bacteria and nitrate screen costs fifty to one hundred dollars, but you need a comprehensive metals and radon panel for two hundred to four hundred dollars to see all contaminants. A whole-house treatment system combining aeration, water softening, and point-of-use filters addresses these problems.
| Contaminant | Samples ⓘ | % Above MCL ⓘ | Distribution ⓘ | Confidence ⓘ | Risk ⓘ |
|---|---|---|---|---|---|
| Lead | 2 | 100% | 50% · 0% · 50% | Low | High |
| Radon | 41 | 54% | 44% · 2% · 54% | Moderate | High ⓘ |
| Iron | 28 | 44% | 39% · 18% · 43% | Moderate | High |
| Sulfate | 85 | 14% | 73% · 13% · 14% | Moderate | Moderate |
| Chloride | 30 | 0% | 100% · 0% · 0% | Moderate | Low |
| Fluoride | 2 | 0% | 100% · 0% · 0% | Low | Low |
| Uranium | 21 | 0% | 95% · 5% · 0% | Moderate | Low |
| Arsenic | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Nitrite | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Fecal Coliform | 1 | — | — | Low | Safe |
| pH | 17 | — | — | Moderate | Low |
| Sodium | 91 | — | — | Moderate | Low |
| Nitrate | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Manganese | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| E. coli | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Total Coliform | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Hardness | 32 | — | — | 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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