Paleokarst and Caves of Velebit Mt., Dinaric karst of Croatia (CROSBI ID 636880)
Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | međunarodna recenzija
Podaci o odgovornosti
Paar, Dalibor ; Buzjak, Nenad ; Gabrovšek, Franci ; Frančišković-Bilinski, Stanislav ; Bakšić, Darko ; Stroj, Andrej ; Lacković, Damir ; Kljajo, Dubravka
engleski
Paleokarst and Caves of Velebit Mt., Dinaric karst of Croatia
In the Caves of North Velebit Mt. vertical shaft and meander morphology of vadose origin is largely prevailing, which points to single continuous phase of their speleogenesis. However, origin of large chambers, which are found in some of the Caves is not clear. They are strongly modified by collapse processes, and are possibly inherited features from the former phases of karstification, later incorporated to present caves. Other possible fragments of paleo cave levels above present epiphreatic zone are very scarce and uncertain. In the contrast to North Velebit Caves, in the most southern part of Velebit Mt. some of the largest known Dinaric karst multilevel caves are present. They are of complex origin with few paleo(epi)phreatic levels, connected with the surface by the younger invasive vadose shafts. However, detailed study of speleogenesis chronology of the Velebit Mt. Caves haven`t been conducted yet, which can be stated also for the rest of Dinaric karst area in Croatia.
caves; paleokarst; Dinaric karst; Velebit Mt.; Croatia
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Podaci o prilogu
26-27.
2016.
objavljeno
Podaci o matičnoj publikaciji
24th International Karstological School “Classical Karst” Paleokarst
Postojna: Karst Research Institute - ZRC SAZU
978-961-254-914-5
Podaci o skupu
24th International Karstological School “Classical Karst” Paleokarst
poster
13.06.2016-16.06.2016
Postojna, Slovenija