“…Information on geological features such as lithological variations and geochemistry is of primary importance in radon mapping (Ball and Miles, 1993;Barnet, 2004;Demongeot, 1997;Gundersen, 1991;Gundersen et al, 1992;Ielsch, 2001;Ielsch et al, 1999Ielsch et al, , 2001Ielsch et al, , 2002Ielsch and Torrenti, 2004;Kemski et al, 2005;Kies et al, 1996;Popit and Vaupotic, 2002;Quindos et al, 2004Quindos et al, , 2008Shi et al, 2006;Sundal et al, 2004). Large-scale variability is presumed to be influenced by additional factors such as faults, shears and thrusts (Ciotoli et al, 1998;Gundersen, 1991;Gundersen and Schumann, 1996;King, 1993;King et al, 1996;Lombardi and Reimer, 1990;Toutain and Baubron, 1999) and/or local uranium (U) mineralisation. However, the soil constitutes an interface cover between the solid geology (basement rocks) and the atmosphere and may also influence the vertical radon migration, according to its permeability.…”