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

Monocle

透明

,“Emil Racovită” Institute of Speleology: World’s First Research Unit Dedicated to Karst and Cave Stia, two research groups were assembled in Bucharest and Cluj, respectively. Their mission was to prospect and identify phosphate deposits, an opportunity that led to the exploration of a large number of caves, which were simultaneously surveyed and investigated for their fauna.

LANCE

,Retezat Mountains: Jiul de Vest–Cernisoara Basins, three rivers, hydrogeological connections have developed, supported by the continuity of the limestones and by structural-tectonic features. All three rivers contribute to the recharge of the most important karst spring in Romania, Cerna Spring.

甜食

锉屑

Relationenalgebraische Grundlagen,onor Plateau. Șura Mare Cave is known for its long underground stream, spectacular domes, and large well-decorated chambers. Dye studies performed in the early eighties prove the connection with Dosul Lăcșorului and Fundătura Hobenilor shafts, making this karst system one of the most important in Romania.

Resign

Epidural-Space

是贪求

Karst of Sebes Mountains,onor Plateau. Șura Mare Cave is known for its long underground stream, spectacular domes, and large well-decorated chambers. Dye studies performed in the early eighties prove the connection with Dosul Lăcșorului and Fundătura Hobenilor shafts, making this karst system one of the most important in Romania.

观察

,Sureanu Mountains: Valea Stânii–Ponorici–Cioclovina cu Apă Karst System,ave, are just a few reasons why the Valea Stânii–Ponorici–Cioclovina cu Apă karst system represents a landmark for the Romanian karst. The scientific value of this karst region is topped by the numerous Dacian artifacts found at surface.

整洁漂亮

,Southern Carpathians: Pârgavului Cave,eological conditions existing during the Quaternary, created a unique imprint on various geomorphological aspect of the cave. Speleothems are present in the sub-horizontal part of the cave. The progressive incision of the underground river led to the formation of several generations of shelfstones.