Granitognejsowe formy skalne masywu Gap na Pogórzu Izerskim
Journal Title: Przyroda Sudetów - Year 2017, Vol 20, Issue
Abstract
Granite gneiss rock forms of the Gapy hill, Izera Upland The paper presents the results of geomorphological mapping of rock forms of the Gapy hill, supported by measurements of joint system, geomorphometric and geological analysis of the slopes. The combined data permitted conclusions on the conditions of distribution and development of 23 tors of diverse size and morphology – elongated rock steps, high pulpits and isolated towers. Most of tors are concentrated in the upper parts of the massif where they reach their greatest high (max. 13.5 m). The rock forms are located on the convex slope breaks of NW-SE direction and mainly in the places of occurrence of coarse-grained granite.
Authors and Affiliations
Aleksandra Michniewicz
Keywords
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