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

Mhc-Molecule

cardiovascular

sebaceous-gland

Biguanides

https://doi.org/10.1007/978-3-8348-9213-3rstified. Due to the construction of the tunnel and extensive roadcuts, the impact of the activities affecting the Karst Edge and its hinterland was significant, in several places leading to the unearthing of today’s epikarst and a part of the vadose zone, both of which are also intersected with old

NIB

https://doi.org/10.1007/978-3-8348-9213-3o dramatically, there are old caves and shafts opening up all the time in the course of the construction of the motorways. Old caves are either void or filled with alluvium. The caves were formed as a part of a system of cavities in a period when impermeable rocks had enclosed the aquifer higher up,

意见一致

https://doi.org/10.1007/978-3-8348-9213-3the development of the aquifer. Seeing as today the underground water level is 200 m and more below the surface, the traces of ancient water flow through the aquifer are now preserved only in caves and their respective alluvium. There was no indication of surface water flows that could have reshaped

Consensus

https://doi.org/10.1007/978-3-8348-9213-3s the result of the high permeability of this part of the aquifer. The size of the passages suggests that they were passed by larger water flows which had originally completely filled the passages. It is assumed that a remnant of a flysch nappe was somewhere in the vicinity, feeding the aquifer with

逢迎白雪

Bother

insurgent

https://doi.org/10.1007/978-3-8348-9288-1rs were not far off. There were no relevant barriers for the water flow on its course from the ponors to the cave. The formation of stalactites/stalagmites and flowstone heaps does not reflect external influences, although the growth of the stalactites and stalagmites was interrupted several times b