Budowa geologiczna Zawratu Kasprowego i Kopy Magury

Abstract

Geology of the Zawrat Kasprowy and Kopa Magury (Tatra Mts.)Finding of fossil crinoids (Dadocrinus grundeyi Jaekel) allowed to determine the ·age of Triassic series in this area as Hydasp (the lowest Anisian). Several periods of erosion between Dogger horizons were observed. Structure of this district was interpreted and partly mapped.