Geomorphologic study of tufa on the locality Bigreni stream (Donja Bela Reka)
Geomorfološko proučavanje Bigra na lokalitetu Bigreni potok (Donja Bela Reka)
Abstract
The tufa accumulations in the valley of Bigreni stream are morphogenetically complex. The great importance for the occurrence of tufa, as in majority of other accumulations in Eastern Serbia, has the vicinity of the karst spring. The presence of cascades in the gorge of Bigreni stream enabled primary formation of waterfall tufa. After partitioning the gorge, the phase of the barrier tufa accumulation began. The erosive phase is currently present and therefore, once unique accumulation has been divided into several smaller accumulations. The possibility for protection because of the vicinity of the protected capped spring and the beauty of tufa waterfalls indicate the potential for tourist exploitation of this locality.
Bigarene akumulacije u dolini Bigrenog potoka morfogenetski su složene. Veliku važnost za pojavu bigra, kao i kod većine drugih akumulacija u Istočnoj Srbiji, ima blizina kraškog vrela. Postojanje kaskada u klisuri Bigrenog potoka omogućilo je prvobitni nastanak vodopadnog bigra. Nakon pregrađivanja klisure počinje faza akumulacije barijernog bigra. Trenutno je aktuelna erozivna faza pa je, nekada jedinstvena akumulacija, podeljena u više manjih. Mogućnost zaštite, usled blizine zaštićene kaptaže, i lepota bigrenih vodopada ukazuju na potencijal za turističku eksploataciju ovog lokaliteta.
Keywords:
tufa / models of tufa accumulation / protection of tufa / Donja Bela River / Eastern Serbia / bigar / modeli akumulacije bigra / zaštita bigra / Donja Bela Reka / Istočna SrbijaSource:
Glasnik Srpskog geografskog društva, 2009, 89, 4, 61-73Publisher:
- Srpsko geografsko društvo, Beograd
Funding / projects:
Collections
Institution/Community
Geografski fakultetTY - JOUR AU - Petrović, Aleksandar S. AU - Nikolić, Dragana PY - 2009 UR - https://gery.gef.bg.ac.rs/handle/123456789/310 AB - The tufa accumulations in the valley of Bigreni stream are morphogenetically complex. The great importance for the occurrence of tufa, as in majority of other accumulations in Eastern Serbia, has the vicinity of the karst spring. The presence of cascades in the gorge of Bigreni stream enabled primary formation of waterfall tufa. After partitioning the gorge, the phase of the barrier tufa accumulation began. The erosive phase is currently present and therefore, once unique accumulation has been divided into several smaller accumulations. The possibility for protection because of the vicinity of the protected capped spring and the beauty of tufa waterfalls indicate the potential for tourist exploitation of this locality. AB - Bigarene akumulacije u dolini Bigrenog potoka morfogenetski su složene. Veliku važnost za pojavu bigra, kao i kod većine drugih akumulacija u Istočnoj Srbiji, ima blizina kraškog vrela. Postojanje kaskada u klisuri Bigrenog potoka omogućilo je prvobitni nastanak vodopadnog bigra. Nakon pregrađivanja klisure počinje faza akumulacije barijernog bigra. Trenutno je aktuelna erozivna faza pa je, nekada jedinstvena akumulacija, podeljena u više manjih. Mogućnost zaštite, usled blizine zaštićene kaptaže, i lepota bigrenih vodopada ukazuju na potencijal za turističku eksploataciju ovog lokaliteta. PB - Srpsko geografsko društvo, Beograd T2 - Glasnik Srpskog geografskog društva T1 - Geomorphologic study of tufa on the locality Bigreni stream (Donja Bela Reka) T1 - Geomorfološko proučavanje Bigra na lokalitetu Bigreni potok (Donja Bela Reka) VL - 89 IS - 4 SP - 61 EP - 73 UR - https://hdl.handle.net/21.15107/rcub_gery_310 ER -
@article{ author = "Petrović, Aleksandar S. and Nikolić, Dragana", year = "2009", abstract = "The tufa accumulations in the valley of Bigreni stream are morphogenetically complex. The great importance for the occurrence of tufa, as in majority of other accumulations in Eastern Serbia, has the vicinity of the karst spring. The presence of cascades in the gorge of Bigreni stream enabled primary formation of waterfall tufa. After partitioning the gorge, the phase of the barrier tufa accumulation began. The erosive phase is currently present and therefore, once unique accumulation has been divided into several smaller accumulations. The possibility for protection because of the vicinity of the protected capped spring and the beauty of tufa waterfalls indicate the potential for tourist exploitation of this locality., Bigarene akumulacije u dolini Bigrenog potoka morfogenetski su složene. Veliku važnost za pojavu bigra, kao i kod većine drugih akumulacija u Istočnoj Srbiji, ima blizina kraškog vrela. Postojanje kaskada u klisuri Bigrenog potoka omogućilo je prvobitni nastanak vodopadnog bigra. Nakon pregrađivanja klisure počinje faza akumulacije barijernog bigra. Trenutno je aktuelna erozivna faza pa je, nekada jedinstvena akumulacija, podeljena u više manjih. Mogućnost zaštite, usled blizine zaštićene kaptaže, i lepota bigrenih vodopada ukazuju na potencijal za turističku eksploataciju ovog lokaliteta.", publisher = "Srpsko geografsko društvo, Beograd", journal = "Glasnik Srpskog geografskog društva", title = "Geomorphologic study of tufa on the locality Bigreni stream (Donja Bela Reka), Geomorfološko proučavanje Bigra na lokalitetu Bigreni potok (Donja Bela Reka)", volume = "89", number = "4", pages = "61-73", url = "https://hdl.handle.net/21.15107/rcub_gery_310" }
Petrović, A. S.,& Nikolić, D.. (2009). Geomorphologic study of tufa on the locality Bigreni stream (Donja Bela Reka). in Glasnik Srpskog geografskog društva Srpsko geografsko društvo, Beograd., 89(4), 61-73. https://hdl.handle.net/21.15107/rcub_gery_310
Petrović AS, Nikolić D. Geomorphologic study of tufa on the locality Bigreni stream (Donja Bela Reka). in Glasnik Srpskog geografskog društva. 2009;89(4):61-73. https://hdl.handle.net/21.15107/rcub_gery_310 .
Petrović, Aleksandar S., Nikolić, Dragana, "Geomorphologic study of tufa on the locality Bigreni stream (Donja Bela Reka)" in Glasnik Srpskog geografskog društva, 89, no. 4 (2009):61-73, https://hdl.handle.net/21.15107/rcub_gery_310 .