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- W2496317355 abstract "The bottom of the Vipava Valley is made mostly of clastic rocks and sediments of different age and origin. The motorway between Vipava and Selo initially runs across the agriculturally changed Quaternary alluvium sediments, then it crosses the slightly undulating landscape made of Lower Eocene non-carbonate and carbonate turbidites, and in its last section it cuts across Quaternary, locally cemented talus debris. Springs can emerge at the contacts with Eocene resedimented carbonate and Quaternary carbonate rubble, as well as at the contact with the low-lying impermeable flysch. Smaller permanent springs also emerge at the contacts of predominantly pure carbonate rubble and breccia with larger blocks of rock and clay. The cavities along the route can be divided into smaller shafts which formed in flysch-bedded limestone, i.e. due to the contact or due to the accumulation of water on impermeable rock, and into caves which formed in breccia that overlays the impermeable flysch. Underneath the layer of soil which contained the remnants of prehistoric ceramics, the archaeologists have stumbled upon a sterile rubble layer. The upper surface of this layer was not even, but showed shallow sags and elongated trenches. Since it was possible that these uneven surfaces were human-made, karstologists took a closer look at profiles that have been dug out and tried to determine the origin of this layer and estimate when these uneven surfaces in its upper section were created. The layer of rubble was composed of limestone rubble mixed with yellow-brown loam. The limestone that makes up the rubble contains numerous fossils from the Jurassic era. Although we were not able to pinpoint when exactly the hollows were formed, there is a strong indication that they are of natural origin. The Slovenian literature on geomorphology describes similar surface hummocks which formed due to the corrosion in moraine rubble of various thickness." @default.
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- W2496317355 date "2015-10-16" @default.
- W2496317355 modified "2023-10-15" @default.
- W2496317355 title "Karst Phenomena Between Vipava and Selo" @default.
- W2496317355 doi "https://doi.org/10.1007/978-3-319-21203-6_23" @default.
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