Geomorfologická charakteristika Příborské pahorkatiny (Podbeskydská pahorkatina)

Rok, strany: 1976, 180 - 197

The Příborská pahorkatina is modelled on little ressistant Flysch rocks of so called ,,podslezsko-ždánický“ nappe and it had complicated development from Neogene up to Holocene Ages. The relief was geomorphologically mapped to scale 1:25 000 and on the basis of the geomorphological analysis of all groups its evolution was studied. The main agents of the evolution were the processes of semiarid character at the end of Neogene and at the beginning of Quaternary, the cryonival processes in Pleistocene and the processes of humid character in Holocene. The morphostructural, morphometrical and genetical signs were used as the basis for the geomorphological division of the whole studied area.

ISO 690:

Buzek, L. 1976. Geomorfologická charakteristika Příborské pahorkatiny (Podbeskydská pahorkatina). In Geografický časopis, vol. 28, no.3, pp. 180-197. 0016-7193.

APA:

Buzek, L. (1976). Geomorfologická charakteristika Příborské pahorkatiny (Podbeskydská pahorkatina). Geografický časopis, 28(3), 180-197. 0016-7193.

Vydavateľ: Geografický ústav SAV/Institute of Geography of the Slovak Academy of Sciences