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Geomorphologic study of tufa on the locality Bigreni stream (Donja Bela Reka)

Geomorfološko proučavanje Bigra na lokalitetu Bigreni potok (Donja Bela Reka)

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2009
308.pdf (471.9Kb)
Authors
Petrović, Aleksandar S.
Nikolić, Dragana
Article (Published version)
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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 Srbija
Source:
Glasnik Srpskog geografskog društva, 2009, 89, 4, 61-73
Publisher:
  • Srpsko geografsko društvo, Beograd
Funding / projects:
  • Geosistemske osnove prostorno-funkcionalne organizacije Republike Srbije (RS-146010)

ISSN: 0350-3593

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URI
https://gery.gef.bg.ac.rs/handle/123456789/310
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  • Radovi istraživača
Institution/Community
Geografski fakultet
TY  - 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  - conv_242
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 = "conv_242"
}
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.
conv_242
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.
conv_242 .
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,
conv_242 .

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