Speleomorphology of Dry Passage in Provala Cave (Croatia)

Authors

  • Neven Bočić Speleological society Karlovac, Kurelčeva 3, 47000 Karlovac
  • Nenad Buzjak Speleological society Dinaridi, Maruličev trg 19/II, 10000 Zagreb

DOI:

https://doi.org/10.3986/ac.v27i2.500

Abstract

Jama Provala, 1687 m dolga in 55 m globoka, razvita v dveh nivojih, se odpira v fluviokraškem svetu Žumberačke gore (SZ Hrvaška). Skozi spodnji nivo teče stalni vodni tok. Zgornji nivo je, glede na vodne značilnosti, mogoče razdeliti na tri dele: 1. južni s stalnim vodnim tokom, 2. del z občasnim vodnim tokom in 3. suhi del. V zadnjih dveh delih, ki se imenujeta Suhi rov, so bile opravljene morfološke raziskave.


Provala cave is located in the fluviokarst area of Žumberačka gora mountain (NW Croatia). This two-level cave is 1687 m long and 55 m deep. In the lower level there is a permanent water stream. The upper level, according to its hydrological characteristics, can be divided into three parts: 1. the southern part with permanent water stream, 2. the part with periodical water stream, and 3. dry part. The last two parts called “Dry passage” were speleomorphologically observed.

Downloads

Download data is not yet available.

Downloads

Published

2015-09-04

How to Cite

Bočić, N., & Buzjak, N. (2015). Speleomorphology of Dry Passage in Provala Cave (Croatia). Acta Carsologica, 27(2). https://doi.org/10.3986/ac.v27i2.500

Issue

Section

Original papers