Titlebook: Cave Exploration in Slovenia; Discovering Over 350 Martin Knez,Tadej Slabe Book 2016 Springer International Publishing Switzerland 2016 Cav

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Unroofed Caves Provide Important Clues to the Karst Developmentd flowstone. It became clear during the motorway construction undertaking in Slovenia that unroofed caves constitute a relatively common karst landform. In fact, more common than karstologists had imagined before the karst surface was uncovered through earthworks. The various types of notches occurr

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The Large Unroofed Cave Near Povired near the village of Povir. It contained flowstone, stalactites, stalagmites and various sediments. Inside the cave, flowstone has been preserved in the form of crusts, massive flowstone heaps, and free-standing stalagmites, but some broken off stalactites were also found. It is possible to recons

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Composition of Sediments in Dolines opening up the possibility of examining the mineral composition of the clastic sediment layers found in them. In dolines, red and yellow sediments prevailed, occurring in several shades and transitioning from red to yellow and then to brown. All samples were similar in terms of their mineral compos

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ANTE

Palaeomagnetic Research of an Unroofed Cave Near Kozinaper main road, in the cutting which was formed during the construction of the Divača–Klanec motorway. The sampled profile consists of more than 5 m of alluvium in two main sequences. The lower sequence comprised ochre-coloured sandy to clayey sediments that were app. 3 m thick. These sediments were

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Sediments in the S-647 Cave in the Kastelec Tunnel and 50 m deep. The eastern part descends evenly and reaches its lowest accessible point at the altitude of 315 m, i.e. 47 m under the bottom of the tunnel. The western part ascends gently so that the final point lies at the altitude of 356 m, 6 m under the tunnel’s bottom. In addition to flowstone,

Agronomy

The History of Karstification on the Upper Cretaceous and Lower Paleogene Limestones in the Wider Kocation over several karst periods and were subject to a number of karstification and epikarst development phases. Due to denudation, the epikarst, where the rock is markedly dissected by typical surface karst features, moves down the transverse profile of the karst system, through the traces of form

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