Why is the Ohio Shale a source of radon?
A The Ohio Shale is a geologic formation consisting of a black, organic- and clay-rich rock. In central and western Ohio, it commonly contains between 10 and 40 parts per million of uranium, and this is 5 to 20 times more uranium than the average rock in the Earth’s crust contains. Radon is a by-product of the radioactive decay of uranium.