Present state and changes of landscape's structures in high-mountain’s environment requires rigorous scientific research. There the most intensive dynamic changes have started after wind throw disaster on the 19th November 2004 and intensification of new investment construction. Massive modifications of downhill courses of Solisko (above Štrbske pleso Lake) and in Tatranska Lomnica (under Skalnaté pleso Lake) have begun since 2008. The main task is anthropic influence's evaluation of downhill courses according to data's interpretation of relationship between exposed substrate and vegetation cover. Results introduced in article represent the state until the year of 2008 and consequently they will have historical value, concerning visible changes in studied areas. We comment scientific background of invested projects and possibilities of their more sensible design
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