Informácia o dokumente



In: Geografický časopis, vol. 63, no. 3
Rudolf Ondrášik - Vojtech Gajdoš

Riečne terasy Váhu v meandri Domašín v Strečnianskej úžine

Detaily:

Rok, strany: 2011, 275 - 285
Kľúčové slová:
Malá Fatra Mts., Strečno Gorge, River Váh terraces, terrace relics, Domašín meander, fluvial deposits

O článku:

The meander of Domašín represents a noticeable landmark of the River Váh valley in the Strečno Gorge through, the Malá Fatra Mountains. A string of remnants of river terraces indicates that the meander was created by the Pleistocene river erosion in a granitic rock mass. Remnants of river terraces were indicated on the basis of geomorphology, fluvial deposits, and geophysical survey. Geophysics also determined the depth of the substratum surface and a thickness of alluvial deposits. The stratigraphic position of 11 Pleistocene river terraces was classified on the basis of their relative elevation.

Ako citovať:

ISO 690:
Ondrášik, R., Gajdoš, V. 2011. Riečne terasy Váhu v meandri Domašín v Strečnianskej úžine. In Geografický časopis, vol. 63, no.3, pp. 275-285. ISSN 0016-7193.

APA:
Ondrášik, R., Gajdoš, V. (2011). Riečne terasy Váhu v meandri Domašín v Strečnianskej úžine. Geografický časopis, 63(3), 275-285. ISSN 0016-7193.