Budowa geologiczna wschodniego zbocza Kopy Kondrackiej
Abstract
Geology of the east side of Mt. Kopa KondrackaAll 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.Downloads
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