Výmoľová erózia v čase– mapové podklady verzus korelátne sedimenty (príkladová štúdia)

Year, pages: 2011, 287 - 298

The paper deals with the occurrence of gully erosion over time in a selected area in the northern part of the Nitrianska pahorkatina Hill Land. The study was based on an analysis of maps and the correlative sediments relating to the evolution of the selected permanent gully. Historical maps from 1783, 1838, 1882 and current topographic maps were evaluated for this purpose. The analysis of correlative sediments consisted of identification and dating of the relevant components within the colluvial fan sediments and the material deposited in the mouth of the gully. Radiocarbon 14C dating of an organic material and expert age estimation of archaeological artefacts were used to determine the relative age of the layers. On the basis of achieved results occurrence of accelerated gully erosion that probably took place in the 14th century and the 19th to 20th century was detected.

Papčo, P. 2011. Výmoľová erózia v čase– mapové podklady verzus korelátne sedimenty (príkladová štúdia). In Geografický časopis, vol. 63, no.3, pp. 287-298. 0016-7193.

Papčo, P. (2011). Výmoľová erózia v čase– mapové podklady verzus korelátne sedimenty (príkladová štúdia). Geografický časopis, 63(3), 287-298. 0016-7193.