Geomorfolo?ki razvoj doline Krnice in njene zadnje poledenitve

摘要

The paper deals with the geomorphological development of the elongated Krnica valley in the Julian Alps near Kranjska gora, which geneticaly resembles to the Vr?i? Pass. The basic idea is the development of this Alpine valley under the strong influence of the softer dolomitic strata which is beneath the limestone. Besides, the fault lines contribute a lot to this development. Not only the frontal moraines in the valley itself but also the two of them near Kranjska gora can be the result of the same late postwürmian stadial glacier, as this was the longest in the region.