Riečne terasy Váhu v meandri Domašín v Strečnianskej úžine

Year, pages: 2011, 275 - 285

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.

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

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