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

Postulate

,Sebesului Mountains: Răchiteaua–Sipot Cave System,xplorations will likely prove its scientific and hydrologic significance. It is composed of Răchiţeaua Shaft, a 2430 m long and 232 m deep stream cave and the Şipot Sump Cave, a 1270 m long river passage with six challenging sumps. Răchiţeaua Shaft is impressive through its vadose shafts, corrosion,

FICE

声明

,Retezat Mountains: Jiul de Vest–Cernisoara Basins,dary between the Retezat and Godeanu Mountains to the north and west, respectively, and the Vâlcan Mountains to the south. The Piule-Iorgovanu Mountains (Retezatul Mic Mountains) are between the Buta and Jiul de Vest Rivers and are an alpine karstic plateau (2000 m above sea level) of Jurassic limes

Confess

,Southern Carpathians: Pârgavului Cave,ate facies, the dissolution acted selectively; thus, cave passages show different morphologies. The Mesozoic tectonics events combined with the hydrogeological conditions existing during the Quaternary, created a unique imprint on various geomorphological aspect of the cave. Speleothems are present

nepotism

Mehedinti Mountains: Cioaca cu Brebenei and Closani Caves,ent in size, both caves are well-known for their wide diversity of speleothems. Cioaca cu Brebenei is an 85 m long cavity that hosts some of the largest and most spectacular helictites of the Romanian karst. The cave has been carved by the Izvorele Creek, a right-side tributary of the Motru River. C

废止

Mehedinti Mountains: Martel and Lazului Caves,e river as a left (north) side meander and is located at about 8 m below the thalweg. The water level in the cave rises and falls along the main gallery, where the lakes/streams at the lightest rain become sumps. The cave is relatively poor in speleothems, except the fossil gallery (CS FV Gallery of

Arrhythmia

Karst and Caves of Romania: A Brief Overview,nted in the chapters of this book. Karst-prone rocks cover at least 5500 km. (Fig. .) representing ~2.3% of the total area of the country (238.397 km.). Worth noting is that the low percentage is mainly because extensive areas in which karst forming rocks exist, are covered by younger, Pliocene, and Quaternary age deposits.

他一致

Conduit

Disk199

Transfinite Zahlen und das Auswahlaxiom,nted in the chapters of this book. Karst-prone rocks cover at least 5500 km. (Fig. .) representing ~2.3% of the total area of the country (238.397 km.). Worth noting is that the low percentage is mainly because extensive areas in which karst forming rocks exist, are covered by younger, Pliocene, and Quaternary age deposits.