TY  - JOUR
AU  - Petrović, Aleksandar S.
AU  - Ćalić, Jelena
AU  - Pantić, Marko
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/912
AB  - The article deals with the morphogenesis of the through cave Pećina na Reci Zamni (meaning in Serbian: Cave on the Zamna River; in further text: the Zamna Cave). The Zamna Cave was the subject of several geomorphological studies, mostly aimed at explaining the cave genesis through the evolutionary concept from through caves to natural bridges. In order to get better insight into the morphogenesis of this cave, modern geomorphometrical methods were applied. The cave and the surface topography above it were scanned in high resolution using the instrument Leica Nova MS50, applying the method of terrestrial laser scanning (TLS). Data processing produced the model for the analysis of the relation between surface and underground forms of karst relief. The results point to the conclusion that the Zamna Cave is an example showing that in the process of natural bridges formation by cave roof collapse, it is not necessary that there is a dry valley above the cave, as previously thought.
AB  - Pećina na reci Zamni bila je do sada predmet više istraživanja. Neka od njih imala su za cilj objašnjenje geneze pećine u svetlu evolucije tunelskih pećina ka prerastima. U cilju boljeg razumevanja geneze ove pećine primenjene su savremene morfometrijske tehnike. Pećina i površina iznad nje snimljeni su u visokoj rezoluciji uređajem Leica Nova MS50, postupkom terestričkog laserskog skeniranja (TLS). Obradom prikupljenih podataka dobijen je model na kome je moguće analizirati odnos površinskih i podzemnih kraških oblika reljefa. Rezultati analize navode na zaključak da je pećina na reci Zamni primer koji ukazuje na to da prilikom formiranja prerasti urušavanjem tavanica pećina nije pravilo da se neposredno iznad pruža suva dolina.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Through cave on the Zamna River in eastern serbia: new morphogenetic interpretations
T1  - Pećina na reci Zamni u svetlu novih morfogenetskih istraživanja
VL  - 98
IS  - 2
SP  - 29
EP  - 44
DO  - 10.2298/GSGD1802029P
UR  - https://hdl.handle.net/21.15107/rcub_gery_912
ER  - 

@article{
author = "Petrović, Aleksandar S. and Ćalić, Jelena and Pantić, Marko",
year = "2018",
abstract = "The article deals with the morphogenesis of the through cave Pećina na Reci Zamni (meaning in Serbian: Cave on the Zamna River; in further text: the Zamna Cave). The Zamna Cave was the subject of several geomorphological studies, mostly aimed at explaining the cave genesis through the evolutionary concept from through caves to natural bridges. In order to get better insight into the morphogenesis of this cave, modern geomorphometrical methods were applied. The cave and the surface topography above it were scanned in high resolution using the instrument Leica Nova MS50, applying the method of terrestrial laser scanning (TLS). Data processing produced the model for the analysis of the relation between surface and underground forms of karst relief. The results point to the conclusion that the Zamna Cave is an example showing that in the process of natural bridges formation by cave roof collapse, it is not necessary that there is a dry valley above the cave, as previously thought., Pećina na reci Zamni bila je do sada predmet više istraživanja. Neka od njih imala su za cilj objašnjenje geneze pećine u svetlu evolucije tunelskih pećina ka prerastima. U cilju boljeg razumevanja geneze ove pećine primenjene su savremene morfometrijske tehnike. Pećina i površina iznad nje snimljeni su u visokoj rezoluciji uređajem Leica Nova MS50, postupkom terestričkog laserskog skeniranja (TLS). Obradom prikupljenih podataka dobijen je model na kome je moguće analizirati odnos površinskih i podzemnih kraških oblika reljefa. Rezultati analize navode na zaključak da je pećina na reci Zamni primer koji ukazuje na to da prilikom formiranja prerasti urušavanjem tavanica pećina nije pravilo da se neposredno iznad pruža suva dolina.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Through cave on the Zamna River in eastern serbia: new morphogenetic interpretations, Pećina na reci Zamni u svetlu novih morfogenetskih istraživanja",
volume = "98",
number = "2",
pages = "29-44",
doi = "10.2298/GSGD1802029P",
url = "https://hdl.handle.net/21.15107/rcub_gery_912"
}

Petrović, A. S., Ćalić, J.,& Pantić, M.. (2018). Through cave on the Zamna River in eastern serbia: new morphogenetic interpretations. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 98(2), 29-44.
https://doi.org/10.2298/GSGD1802029P
https://hdl.handle.net/21.15107/rcub_gery_912

Petrović AS, Ćalić J, Pantić M. Through cave on the Zamna River in eastern serbia: new morphogenetic interpretations. in Glasnik Srpskog geografskog društva. 2018;98(2):29-44.
doi:10.2298/GSGD1802029P
https://hdl.handle.net/21.15107/rcub_gery_912 .

Petrović, Aleksandar S., Ćalić, Jelena, Pantić, Marko, "Through cave on the Zamna River in eastern serbia: new morphogenetic interpretations" in Glasnik Srpskog geografskog društva, 98, no. 2 (2018):29-44,
https://doi.org/10.2298/GSGD1802029P .,
https://hdl.handle.net/21.15107/rcub_gery_912 .

TY  - CHAP
AU  - Petrović, Aleksandar S.
AU  - Ćalić, Jelena
AU  - Spalević, A.
AU  - Pantić, Marko
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/908
AB  - This paper details methods that contribute towards solving the problem of the spatial relations between surface and underground karst morphology - relationships that are often unclear. The karst landforms studied in this context are karst valleys, through-caves and natural bridges. Two study sites are situated in the Carpatho-Balkan Mountains of eastern Serbia: the dry valley of the Radovanska Reka River on Mt Kučaj (together with the Pećura through-cave) and the Zamna Cave in the wider area of the Danube Gorge. The caves and the closest adjoining parts of the valleys were measured in detail using the terrestrial laser scanning method. The data obtained showed that some previous measurements at these locations, performed with classical traditional instruments, are insufficiently accurate and may lead to wrong conclusions.
PB  - Geological Society of London
T2  - Geological Society Special Publication
T1  - Relations between surface and underground karst forms inferred from terrestrial laser scanning
VL  - 466
IS  - 1
SP  - 107
EP  - 120
DO  - 10.1144/SP466.23
UR  - https://hdl.handle.net/21.15107/rcub_gery_908
ER  - 

@inbook{
author = "Petrović, Aleksandar S. and Ćalić, Jelena and Spalević, A. and Pantić, Marko",
year = "2018",
abstract = "This paper details methods that contribute towards solving the problem of the spatial relations between surface and underground karst morphology - relationships that are often unclear. The karst landforms studied in this context are karst valleys, through-caves and natural bridges. Two study sites are situated in the Carpatho-Balkan Mountains of eastern Serbia: the dry valley of the Radovanska Reka River on Mt Kučaj (together with the Pećura through-cave) and the Zamna Cave in the wider area of the Danube Gorge. The caves and the closest adjoining parts of the valleys were measured in detail using the terrestrial laser scanning method. The data obtained showed that some previous measurements at these locations, performed with classical traditional instruments, are insufficiently accurate and may lead to wrong conclusions.",
publisher = "Geological Society of London",
journal = "Geological Society Special Publication",
booktitle = "Relations between surface and underground karst forms inferred from terrestrial laser scanning",
volume = "466",
number = "1",
pages = "107-120",
doi = "10.1144/SP466.23",
url = "https://hdl.handle.net/21.15107/rcub_gery_908"
}

Petrović, A. S., Ćalić, J., Spalević, A.,& Pantić, M.. (2018). Relations between surface and underground karst forms inferred from terrestrial laser scanning. in Geological Society Special Publication
Geological Society of London., 466(1), 107-120.
https://doi.org/10.1144/SP466.23
https://hdl.handle.net/21.15107/rcub_gery_908

Petrović AS, Ćalić J, Spalević A, Pantić M. Relations between surface and underground karst forms inferred from terrestrial laser scanning. in Geological Society Special Publication. 2018;466(1):107-120.
doi:10.1144/SP466.23
https://hdl.handle.net/21.15107/rcub_gery_908 .

Petrović, Aleksandar S., Ćalić, Jelena, Spalević, A., Pantić, Marko, "Relations between surface and underground karst forms inferred from terrestrial laser scanning" in Geological Society Special Publication, 466, no. 1 (2018):107-120,
https://doi.org/10.1144/SP466.23 .,
https://hdl.handle.net/21.15107/rcub_gery_908 .

TY  - JOUR
AU  - Ilić, Marina M.
AU  - Stojković, Sanja
AU  - Rundić, Ljupko
AU  - Ćalić, Jelena
AU  - Sandić, Dejan
PY  - 2016
UR  - https://gery.gef.bg.ac.rs/handle/123456789/796
AB  - Considering the fact that urbanization is one of the most serious threats to geodiversity, it is important that this issue is taken into account in spatial development plans and georesource management strategies in urban areas. This paper presents the application of a geodiversity evaluation method by using the geodiversity index, based on the quantity of abiotic elements and relief roughness within a spatial unit. Geodiversity assessment, usually used for remote, protected and sparsely populated natural areas, is now carried out in an urban environment - the city of Belgrade, capital of Serbia, with a population of about 1.7 million inhabitants and very strong urbanization in the last few decades. The area of 3227 km(2) is processed with the spatial resolution of 1 x 1 km. The acquired results from the geodiversity index are analyzed in the context of sustainable use of georesources and the threats to which geodiversity is exposed due to the territorial expansion of the city. The mapping of specific categories of geodiversity on the basis of quantitative assessment with the use of Geographic Information Systems can help decision makers and managers to take further steps that would reduce threats and protect the natural value of Belgrade.
PB  - Croatian Geological Survey, Zagreb
T2  - Geologia Croatica
T1  - Application of the geodiversity index for the assessment of geodiversity in urban areas: an example of the Belgrade city area, Serbia
VL  - 69
IS  - 3
SP  - 325
EP  - 336
DO  - 10.4154/gc.2016.27
UR  - https://hdl.handle.net/21.15107/rcub_gery_796
ER  - 

@article{
author = "Ilić, Marina M. and Stojković, Sanja and Rundić, Ljupko and Ćalić, Jelena and Sandić, Dejan",
year = "2016",
abstract = "Considering the fact that urbanization is one of the most serious threats to geodiversity, it is important that this issue is taken into account in spatial development plans and georesource management strategies in urban areas. This paper presents the application of a geodiversity evaluation method by using the geodiversity index, based on the quantity of abiotic elements and relief roughness within a spatial unit. Geodiversity assessment, usually used for remote, protected and sparsely populated natural areas, is now carried out in an urban environment - the city of Belgrade, capital of Serbia, with a population of about 1.7 million inhabitants and very strong urbanization in the last few decades. The area of 3227 km(2) is processed with the spatial resolution of 1 x 1 km. The acquired results from the geodiversity index are analyzed in the context of sustainable use of georesources and the threats to which geodiversity is exposed due to the territorial expansion of the city. The mapping of specific categories of geodiversity on the basis of quantitative assessment with the use of Geographic Information Systems can help decision makers and managers to take further steps that would reduce threats and protect the natural value of Belgrade.",
publisher = "Croatian Geological Survey, Zagreb",
journal = "Geologia Croatica",
title = "Application of the geodiversity index for the assessment of geodiversity in urban areas: an example of the Belgrade city area, Serbia",
volume = "69",
number = "3",
pages = "325-336",
doi = "10.4154/gc.2016.27",
url = "https://hdl.handle.net/21.15107/rcub_gery_796"
}

Ilić, M. M., Stojković, S., Rundić, L., Ćalić, J.,& Sandić, D.. (2016). Application of the geodiversity index for the assessment of geodiversity in urban areas: an example of the Belgrade city area, Serbia. in Geologia Croatica
Croatian Geological Survey, Zagreb., 69(3), 325-336.
https://doi.org/10.4154/gc.2016.27
https://hdl.handle.net/21.15107/rcub_gery_796

Ilić MM, Stojković S, Rundić L, Ćalić J, Sandić D. Application of the geodiversity index for the assessment of geodiversity in urban areas: an example of the Belgrade city area, Serbia. in Geologia Croatica. 2016;69(3):325-336.
doi:10.4154/gc.2016.27
https://hdl.handle.net/21.15107/rcub_gery_796 .

Ilić, Marina M., Stojković, Sanja, Rundić, Ljupko, Ćalić, Jelena, Sandić, Dejan, "Application of the geodiversity index for the assessment of geodiversity in urban areas: an example of the Belgrade city area, Serbia" in Geologia Croatica, 69, no. 3 (2016):325-336,
https://doi.org/10.4154/gc.2016.27 .,
https://hdl.handle.net/21.15107/rcub_gery_796 .

TY  - CHAP
AU  - Pavlović, Radmila
AU  - Ćalić, Jelena
AU  - Đurović, Predrag
AU  - Trivić, Branislav
AU  - Jemcov, Igor
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/458
AB  - Serbia can be divided into two major geographical units: the Vojvodina Plain and the southern hills and mountains. In the plain fluvial and aeolian processes and landforms on loess are typical, while south of the Sava and Danube rivers, sheet and gully erosion, mass movements, fluvial, karstic, and fluvio-karstic landform evolution are most influential in shaping the present topography. Among the now inactive geomorphic processes tectonic movements, volcanic activity, coastal, glacial, and aeolian evolution have left behind traces still detectable in modern topography. Some examples of rapid topographic change resulting in the most spectacular landforms (landslides, rockfalls, natural bridges, and rock pinnacles) are presented and described in detail from various regions of Serbia.
PB  - Springer Netherlands
T2  - Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region
T1  - Recent landform evolution in Serbia
SP  - 345
EP  - 375
DO  - 10.1007/978-94-007-2448-8_13
UR  - https://hdl.handle.net/21.15107/rcub_gery_458
ER  - 

@inbook{
author = "Pavlović, Radmila and Ćalić, Jelena and Đurović, Predrag and Trivić, Branislav and Jemcov, Igor",
year = "2012",
abstract = "Serbia can be divided into two major geographical units: the Vojvodina Plain and the southern hills and mountains. In the plain fluvial and aeolian processes and landforms on loess are typical, while south of the Sava and Danube rivers, sheet and gully erosion, mass movements, fluvial, karstic, and fluvio-karstic landform evolution are most influential in shaping the present topography. Among the now inactive geomorphic processes tectonic movements, volcanic activity, coastal, glacial, and aeolian evolution have left behind traces still detectable in modern topography. Some examples of rapid topographic change resulting in the most spectacular landforms (landslides, rockfalls, natural bridges, and rock pinnacles) are presented and described in detail from various regions of Serbia.",
publisher = "Springer Netherlands",
journal = "Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region",
booktitle = "Recent landform evolution in Serbia",
pages = "345-375",
doi = "10.1007/978-94-007-2448-8_13",
url = "https://hdl.handle.net/21.15107/rcub_gery_458"
}

Pavlović, R., Ćalić, J., Đurović, P., Trivić, B.,& Jemcov, I.. (2012). Recent landform evolution in Serbia. in Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region
Springer Netherlands., 345-375.
https://doi.org/10.1007/978-94-007-2448-8_13
https://hdl.handle.net/21.15107/rcub_gery_458

Pavlović R, Ćalić J, Đurović P, Trivić B, Jemcov I. Recent landform evolution in Serbia. in Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region. 2012;:345-375.
doi:10.1007/978-94-007-2448-8_13
https://hdl.handle.net/21.15107/rcub_gery_458 .

Pavlović, Radmila, Ćalić, Jelena, Đurović, Predrag, Trivić, Branislav, Jemcov, Igor, "Recent landform evolution in Serbia" in Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region (2012):345-375,
https://doi.org/10.1007/978-94-007-2448-8_13 .,
https://hdl.handle.net/21.15107/rcub_gery_458 .