Niektoré aspekty pleistocénneho zaladnenia Královohoľských Tatier

Rok, strany: 1986, 236 - 244

The study has its subject in the glacial relief of the Královohoľské Tatry (Králova-Hoľa Tatra Mountains) as the eastern subunit of the Nízke Tatry (Lower Tatra Mts). On the basis of glacial forms, particularly from the frontal moraines, both maximum glaciation extent and the deglaciation process during the Wűrmian are inferred. Also the share of surface water courses in forming funnel- and dish-shaped depressions on moraine accumulations after deglaciation as well as the reasons of courses deviating to the right slopes of the valleys are studied.

ISO 690:

Škvarček, A. 1986. Niektoré aspekty pleistocénneho zaladnenia Královohoľských Tatier. In Geografický časopis, vol. 38, no.2-3, pp. 236-244. 0016-7193.

APA:

Škvarček, A. (1986). Niektoré aspekty pleistocénneho zaladnenia Královohoľských Tatier. Geografický časopis, 38(2-3), 236-244. 0016-7193.

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