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Ratei Cave, with its 7,224 m length, provides a good opportunity to investigate the geology and tectonics of Leaota Mountains, the eastern end of the South Carpathians. The geological observations reveal that Ratei Cave is mainly developed in Upper Jurassic limestones, but siliciclastic and metamorphic rocks are encountered in different locations along the cave passages. The stratigraphic succession on the 69 m elevation range, which represents the positive vertical extent between the entrance and the cave end, co...