Radon is an extremely volatile, colourless, odorless natural radioactive gas that is present in the air we breathe, it is a radio-produced gas that is produced from uranium and is found in small quantities in all types of earth and rock. Produced by three parent nuclides giving rise to three different radioactive families Thorio 232, Uranium 235 and Uranium 238. It is emitted from the ground and can accumulate in enclosed spaces, such as homes or workplaces. The amount varies according to local geology, it is measured in "bequerels" (Bq). A Bq corresponds to one disintegration per second. A concentration of 100 Bq/m3 therefore means that 100 atoms disintegrate every second in 1 m3 of the material or environment in question. The Radon (Rn) has atomic number 86, atomic weight 222, density 9.73 g/dm3, melting point -71 , boiling point -61.8 , oxidation states C. Discovered in 1900 as "emanation" of the radio, it was isolated in 1908 and called by W.Ramsay "niton"; the current name was given to him in 1923. The known isotopes are 20; the most important isotope, comes from radio, is 222Rn, which has a half-life of 3.823 days and is an alpha particle emitter. At room temperature it is a colourless gas; below the freezing point it is phosphorescent and yellow in color it turns red-orange at the temperature of the liquid air.