Titlebook: Cave and Karst Systems of Romania; Gheorghe M. L. Ponta,Bogdan P. Onac Book 2019 Springer International Publishing AG, part of Springer Na

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Congregate

Geology of Romania,pean (Moldavian and Scythian platforms) or of West European affinity (Foreapulian, Getic, Euxinic terranes and the North Dobrogean Orogen). The pre-Alpine terranes from the basement of the Alpine terranes of West European affinity have a peri-Gondwanan provenance of Avalonian type (late-Neoproterozo

Anal-Canal

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GEM

懸崖

懸崖

ARY

,Caves of the F?g?ras Mountains,a series of marble stripes interbedded within the metamorphic rocks, several caves developed in two areas in the central part of the mountains: Piscu Negru (at?~1200?m) and Mu?eteica-Raiosu (between?~2100 and?~2400?m). Average air temperature is around 6.5?°C inside the Piscu Negru caves and 3.3?°C

seroma

國家明智

Karst of Sebes Mountains,l range (+425?m). The karst system penetrated vertically and horizontally the entire sequence of limestone deposits of the Ponorici Cioclovina-Ohaba Ponor Plateau. ?ura Mare Cave is known for its long underground stream, spectacular domes, and large well-decorated chambers. Dye studies performed in