This thesis inquires into the quality of the soils at 30 archaeological sites from the periods from Late Bronze Age to Early Bronze Age (1 250 - 400 BC). The aim of the thesis is the general observation of the changes, which could appear from this period until now.
These changes are represented by the erosion, researched by various methods. The conclusion of the thesis is that a potential risk of soil erosion is the lowest in only few lowland archaeological sites.