Wpływ budowy geologicznej na układ i morfologię dolin w beskidzkiej części dorzecza Soły

Abstract

The paper presents influence of different flysch series on pattern, morphology and river gradients of longitudinal profiles in the mountain part of the Soła catchment area. Taking into account mean amount of slates, resistance of godulskie, magurskie and under magurskie layers was estimated. Per cent of longitudinal, transversal and slant valleys in these series were estimated as well. On chosen examples morphometric analysis of these valleys have been done. The clear relations between resistance of rocks and density of rivers have been stated. There are no important connections between lithology and river gradients.