Radon is a radioactive gas that is formed naturally by the breakdown of uranium in soil, rock and water. Radon is colourless, odourless and tasteless.
As a gas, radon can move freely through the soil enabling it to escape to the atmosphere or seep into buildings. When radon escapes from the bedrock into the outdoor air, it is diluted to such low concentrations that it poses a negligible threat to health. However, if a building is built over bedrock or soil that contains uranium, radon gas will be “sucked” into the building by the Stack Effect through cracks in foundation walls and floors or gaps around pipes and cables etc.
When radon is confined to enclosed or poorly ventilated spaces, it can accumulate to high levels. Radon levels are generally highest in basements and crawl spaces because these areas are nearest to the source and are usually poorly ventilated. In the open air, the amount of radon gas is very small and does not pose a health risk.