Anthropogenic activity changes the processes of erosion on slopes. The deforestation process is connected with the deposition of material at the foot of the slope. During this process, macro-charcoals from anthropogenic-induced fires are trapped in the sediments. This paper provides an analysis of charcoal counts and sediment characteristics and is supported by historical data analysis. During this study, a discrepancy between radiocarbon dating and historical data was revealed; a probable explanation is presented.