Budowa geologiczna wschodniego zbocza Kopy Kondrackiej

Abstract

Geology of the east side of Mt. Kopa Kondracka

All the tectonic elements previously distinguished in the high-tatric series have been traced within the Mt. Kopa Kondracka area (eastern summit of the Czerwone Wierchy massif - fig. 1). They are the Czerwone Wierchy fold consisting of the Organy and the Ździary units, the parautochtonous Stoły fold and the crystalline core of the Giewont fold.