Contamination limits of trace elements derived for soils in the Czech
Republic concern only Ap horizons (and their analogies) of soils' lack
ing extreme trace elements concentrations. An attempt has been made to
differentiate the anthropogenic and geogenic loads in the North- and
West North-Bohemian regions, where their coincidence occurs. The solut
ion is based on the comparison of profile trace elements distribution,
parent materials occurrence and immissions isolines. Whereas the prob
lem is simple in case of mafic rocks, it is complicated in metallogeni
c zones of acid igneous and metamorphic rocks. The results are display
ed in three figures. Based an this experience the ratio of geogenic an
d anthropogenic loads for immission - free and severe immission - impa
cted regions has been estimated. The uptake of trace elements from geo
genic loads by plants is very limited.