TY  - CHAP
AU  - Đurović, Predrag
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1156
AB  - The main morphological feature in the relief of Serbia is its gradual rise from the Pannonian Plain in the north to the highest parts of the Šar-Prokletije Mountains in the south and southeast. The central part of the territory encompasses the valleys of the Morava and Southern Morava Rivers, which flow from south to north. West of them lies a mountainous region with the Dinaric Mountains as the most exceptional range. The Carpathian-Balkan mountain range in the east undergoes a gradual decrease of elevation, transiting into marginal parts of the Vlaško-Pontian Plain. The relief base is made up of rocks of different age and different origin (sedimentary rocks with Quaternary alluvial and aeolian products as the most widespread and very abundant carbonate rocks), igneous rocks and diverse metamorphic rocks. The relief was formed over a long period of time with significant climate changes that led to alternation of geomorphological processes (aeolian, periglacial and glacial). In the relief of Serbia, depending on the role of geomorphological processes, it is possible to distinguish different genetic morphostructural types of relief that arose under the influence of endogenic forces (tectonic and volcanic) and exogenic processes (recent fluvial-denudation, karstic colluvial and periglacial). Preserved palaeorelief forms that arose during earlier stages of relief formation have been overprinted by recent geomorphological processes (palaeoabrasional, palaeokarstic, palaeoglacial and palaeoaeolian). Anthropogenic influence on relief (active for several centuries) was occasionally high enough to result in complete conversion of natural relief features and appearance of a new category – anthropogenic relief. Diverse lithology, a different tectonic fabric, neotectonic activity and former and recent climate changes are the major factors that have led to the formation of genetically diverse relief types, from different morphostructural relief elements to genetically various exogenic landscapes.
PB  - Springer, Cham
T2  - The Geography of Serbia: Nature, People, Economy
T1  - Geomorphological Characteristics of Serbia
SP  - 85
EP  - 98
DO  - 10.1007/978-3-030-74701-5_7
ER  - 

@inbook{
author = "Đurović, Predrag",
year = "2022",
abstract = "The main morphological feature in the relief of Serbia is its gradual rise from the Pannonian Plain in the north to the highest parts of the Šar-Prokletije Mountains in the south and southeast. The central part of the territory encompasses the valleys of the Morava and Southern Morava Rivers, which flow from south to north. West of them lies a mountainous region with the Dinaric Mountains as the most exceptional range. The Carpathian-Balkan mountain range in the east undergoes a gradual decrease of elevation, transiting into marginal parts of the Vlaško-Pontian Plain. The relief base is made up of rocks of different age and different origin (sedimentary rocks with Quaternary alluvial and aeolian products as the most widespread and very abundant carbonate rocks), igneous rocks and diverse metamorphic rocks. The relief was formed over a long period of time with significant climate changes that led to alternation of geomorphological processes (aeolian, periglacial and glacial). In the relief of Serbia, depending on the role of geomorphological processes, it is possible to distinguish different genetic morphostructural types of relief that arose under the influence of endogenic forces (tectonic and volcanic) and exogenic processes (recent fluvial-denudation, karstic colluvial and periglacial). Preserved palaeorelief forms that arose during earlier stages of relief formation have been overprinted by recent geomorphological processes (palaeoabrasional, palaeokarstic, palaeoglacial and palaeoaeolian). Anthropogenic influence on relief (active for several centuries) was occasionally high enough to result in complete conversion of natural relief features and appearance of a new category – anthropogenic relief. Diverse lithology, a different tectonic fabric, neotectonic activity and former and recent climate changes are the major factors that have led to the formation of genetically diverse relief types, from different morphostructural relief elements to genetically various exogenic landscapes.",
publisher = "Springer, Cham",
journal = "The Geography of Serbia: Nature, People, Economy",
booktitle = "Geomorphological Characteristics of Serbia",
pages = "85-98",
doi = "10.1007/978-3-030-74701-5_7"
}

Đurović, P.. (2022). Geomorphological Characteristics of Serbia. in The Geography of Serbia: Nature, People, Economy
Springer, Cham., 85-98.
https://doi.org/10.1007/978-3-030-74701-5_7

Đurović P. Geomorphological Characteristics of Serbia. in The Geography of Serbia: Nature, People, Economy. 2022;:85-98.
doi:10.1007/978-3-030-74701-5_7 .

Đurović, Predrag, "Geomorphological Characteristics of Serbia" in The Geography of Serbia: Nature, People, Economy (2022):85-98,
https://doi.org/10.1007/978-3-030-74701-5_7 . .

TY  - JOUR
AU  - Đurović, Mirela
AU  - Đurović, Predrag
PY  - 2021
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1140
AB  - The most significant caves in Montenegro were distinguished in response to their physical-geographic, biological, archeological and morphometric characteristics (length and depth). Caves distribute in four distinctive regions: coastal karst, karst plateau (relict valley system), fluvial karst (recent hydrologic systems) and the high mountainous karst area. The most outstanding within the last, due to abundances of the major caves with depths from a few hundred meters to 1,162 m, are four mountain regions: Mt. Durmitor, Mt. Lovcen-Orjen, Mt. Maganik and Mt. Bjelic.
PB  - Slovenian Academy of Sciences and Arts
PB  - ZRC SAZU Karst Research Institute, Slovenia
T2  - Acta Carsologica
T1  - Review of the most significant caves in Montenegro
VL  - 50
IS  - 1
SP  - 49
EP  - 65
DO  - 10.3986/ac.vi.7182
UR  - https://hdl.handle.net/21.15107/rcub_gery_1140
ER  - 

@article{
author = "Đurović, Mirela and Đurović, Predrag",
year = "2021",
abstract = "The most significant caves in Montenegro were distinguished in response to their physical-geographic, biological, archeological and morphometric characteristics (length and depth). Caves distribute in four distinctive regions: coastal karst, karst plateau (relict valley system), fluvial karst (recent hydrologic systems) and the high mountainous karst area. The most outstanding within the last, due to abundances of the major caves with depths from a few hundred meters to 1,162 m, are four mountain regions: Mt. Durmitor, Mt. Lovcen-Orjen, Mt. Maganik and Mt. Bjelic.",
publisher = "Slovenian Academy of Sciences and Arts, ZRC SAZU Karst Research Institute, Slovenia",
journal = "Acta Carsologica",
title = "Review of the most significant caves in Montenegro",
volume = "50",
number = "1",
pages = "49-65",
doi = "10.3986/ac.vi.7182",
url = "https://hdl.handle.net/21.15107/rcub_gery_1140"
}

Đurović, M.,& Đurović, P.. (2021). Review of the most significant caves in Montenegro. in Acta Carsologica
Slovenian Academy of Sciences and Arts., 50(1), 49-65.
https://doi.org/10.3986/ac.vi.7182
https://hdl.handle.net/21.15107/rcub_gery_1140

Đurović M, Đurović P. Review of the most significant caves in Montenegro. in Acta Carsologica. 2021;50(1):49-65.
doi:10.3986/ac.vi.7182
https://hdl.handle.net/21.15107/rcub_gery_1140 .

Đurović, Mirela, Đurović, Predrag, "Review of the most significant caves in Montenegro" in Acta Carsologica, 50, no. 1 (2021):49-65,
https://doi.org/10.3986/ac.vi.7182 .,
https://hdl.handle.net/21.15107/rcub_gery_1140 .

TY  - CHAP
AU  - Đurović, Predrag
AU  - Đurović, Mirela
PY  - 2016
UR  - https://gery.gef.bg.ac.rs/handle/123456789/761
AB  - The Debeli Namet glacier is located on the Durmitor Mountain in Montenegro. It is considered to be the southern most glaciers in Europe and the only modern glacier in overall area of Dinarids. In size is micro, i.e., embryonic glacier. The significant role in its origin and evolution had its macro, and particularly micro positioning respect to large relief landforms. Pleistocene cirques were recently under karst processes modified and transformed into karst forms (uvalas). Such closed forms considerably supported the accumulation of snow and formation of numerous snow patches as well as the Debeli Namet glacier. Geomorphological factors that supported the development of the Debeli Namet glacier are lowtemperatures (cryogenic), huge amounts of snow (nival) and carbonate basement (karst). In the highest elevations of the Durmitor Mt., as well as at other high mountains in Montenegro dominates periglacial process. On carbonate basement formed recent protalus ramparts, while those formed during the Little Ice Age survived. At non-carbonate basement persisted rock glaciers. According to recent morphology and climate conditions the hypothetical boundary of glacial process has been established to beneath the highest mountain peaks on Durmitor. As glacial process takes part above a periglacial zone, the glacier Debeli Namet represents the out of zone occurrence. Certain variations in glacier size were noted during instrumental observations. Analyses of two main climate factors (air temperature and precipitation) for the last four decades reflected on certain climate changes that had positive and negative influence on size of the Debeli Namet glacier. The most important changes were in its thickness while the length and the areal extent remained less affected due to its specific position.
PB  - Nova Science Publishers, Inc.
T2  - Glaciers: Formation, Climate Change and their Effects
T1  - Physical-geographical factors of origin and evolution of the debeli namet glacier (Montenegro)
SP  - 25
EP  - 52
EP  - 978-163484941-8
UR  - https://hdl.handle.net/21.15107/rcub_gery_761
ER  - 

@inbook{
author = "Đurović, Predrag and Đurović, Mirela",
year = "2016",
abstract = "The Debeli Namet glacier is located on the Durmitor Mountain in Montenegro. It is considered to be the southern most glaciers in Europe and the only modern glacier in overall area of Dinarids. In size is micro, i.e., embryonic glacier. The significant role in its origin and evolution had its macro, and particularly micro positioning respect to large relief landforms. Pleistocene cirques were recently under karst processes modified and transformed into karst forms (uvalas). Such closed forms considerably supported the accumulation of snow and formation of numerous snow patches as well as the Debeli Namet glacier. Geomorphological factors that supported the development of the Debeli Namet glacier are lowtemperatures (cryogenic), huge amounts of snow (nival) and carbonate basement (karst). In the highest elevations of the Durmitor Mt., as well as at other high mountains in Montenegro dominates periglacial process. On carbonate basement formed recent protalus ramparts, while those formed during the Little Ice Age survived. At non-carbonate basement persisted rock glaciers. According to recent morphology and climate conditions the hypothetical boundary of glacial process has been established to beneath the highest mountain peaks on Durmitor. As glacial process takes part above a periglacial zone, the glacier Debeli Namet represents the out of zone occurrence. Certain variations in glacier size were noted during instrumental observations. Analyses of two main climate factors (air temperature and precipitation) for the last four decades reflected on certain climate changes that had positive and negative influence on size of the Debeli Namet glacier. The most important changes were in its thickness while the length and the areal extent remained less affected due to its specific position.",
publisher = "Nova Science Publishers, Inc.",
journal = "Glaciers: Formation, Climate Change and their Effects",
booktitle = "Physical-geographical factors of origin and evolution of the debeli namet glacier (Montenegro)",
pages = "25-52-978-163484941-8",
url = "https://hdl.handle.net/21.15107/rcub_gery_761"
}

Đurović, P.,& Đurović, M.. (2016). Physical-geographical factors of origin and evolution of the debeli namet glacier (Montenegro). in Glaciers: Formation, Climate Change and their Effects
Nova Science Publishers, Inc.., 25-52.
https://hdl.handle.net/21.15107/rcub_gery_761

Đurović P, Đurović M. Physical-geographical factors of origin and evolution of the debeli namet glacier (Montenegro). in Glaciers: Formation, Climate Change and their Effects. 2016;:25-52.
https://hdl.handle.net/21.15107/rcub_gery_761 .

Đurović, Predrag, Đurović, Mirela, "Physical-geographical factors of origin and evolution of the debeli namet glacier (Montenegro)" in Glaciers: Formation, Climate Change and their Effects (2016):25-52,
https://hdl.handle.net/21.15107/rcub_gery_761 .

TY  - CHAP
AU  - Đurović, Predrag
AU  - Đurović, Mirela
PY  - 2015
UR  - https://gery.gef.bg.ac.rs/handle/123456789/678
AB  - Montenegro is located in the Balkan Penninsula, which is extremely mountainous country. More than two thirds of the total area is mountainous. There are four macro relief units in the mountain area: mountain plains, valleys (canyons and gorges), basins, and mountains. A very dynamic physical geographic basis (geology, geomorphology, climate, hydrology) enabled the diversity and rich natural potential resorts to be formed in the mountain area in Montenegro. In the past 50 years, new industries have appeared: mining, metallurgy, energy production, traffic, and tourism, and their development has led to endangered, devastated, and polluted environments in the mountain area of Montenegro.
PB  - Springer International Publishing
T2  - Sustainable Development in Mountain Regions: Southeastern Europe
T1  - Physical geographic characteristics and sustainable development of the mountain area in Montenegro
SP  - 93
EP  - 111
DO  - 10.1007/978-3-319-20110-8_8
UR  - https://hdl.handle.net/21.15107/rcub_gery_678
ER  - 

@inbook{
author = "Đurović, Predrag and Đurović, Mirela",
year = "2015",
abstract = "Montenegro is located in the Balkan Penninsula, which is extremely mountainous country. More than two thirds of the total area is mountainous. There are four macro relief units in the mountain area: mountain plains, valleys (canyons and gorges), basins, and mountains. A very dynamic physical geographic basis (geology, geomorphology, climate, hydrology) enabled the diversity and rich natural potential resorts to be formed in the mountain area in Montenegro. In the past 50 years, new industries have appeared: mining, metallurgy, energy production, traffic, and tourism, and their development has led to endangered, devastated, and polluted environments in the mountain area of Montenegro.",
publisher = "Springer International Publishing",
journal = "Sustainable Development in Mountain Regions: Southeastern Europe",
booktitle = "Physical geographic characteristics and sustainable development of the mountain area in Montenegro",
pages = "93-111",
doi = "10.1007/978-3-319-20110-8_8",
url = "https://hdl.handle.net/21.15107/rcub_gery_678"
}

Đurović, P.,& Đurović, M.. (2015). Physical geographic characteristics and sustainable development of the mountain area in Montenegro. in Sustainable Development in Mountain Regions: Southeastern Europe
Springer International Publishing., 93-111.
https://doi.org/10.1007/978-3-319-20110-8_8
https://hdl.handle.net/21.15107/rcub_gery_678

Đurović P, Đurović M. Physical geographic characteristics and sustainable development of the mountain area in Montenegro. in Sustainable Development in Mountain Regions: Southeastern Europe. 2015;:93-111.
doi:10.1007/978-3-319-20110-8_8
https://hdl.handle.net/21.15107/rcub_gery_678 .

Đurović, Predrag, Đurović, Mirela, "Physical geographic characteristics and sustainable development of the mountain area in Montenegro" in Sustainable Development in Mountain Regions: Southeastern Europe (2015):93-111,
https://doi.org/10.1007/978-3-319-20110-8_8 .,
https://hdl.handle.net/21.15107/rcub_gery_678 .

TY  - JOUR
AU  - Mustafić, Sanja
AU  - Manojlović, Predrag
AU  - Đurović, Predrag
AU  - Dragićević, Slavoljub
AU  - Tošić, Radislav
AU  - Petrović, Aleksandar S.
PY  - 2014
UR  - https://gery.gef.bg.ac.rs/handle/123456789/633
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Našim profesorima - Povodom 90 i 80 godina života i rada
VL  - 94
IS  - 4
SP  - 2
EP  - 34
DO  - 10.2298/GSGD1404002M
UR  - https://hdl.handle.net/21.15107/rcub_gery_633
ER  - 

@article{
author = "Mustafić, Sanja and Manojlović, Predrag and Đurović, Predrag and Dragićević, Slavoljub and Tošić, Radislav and Petrović, Aleksandar S.",
year = "2014",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Našim profesorima - Povodom 90 i 80 godina života i rada",
volume = "94",
number = "4",
pages = "2-34",
doi = "10.2298/GSGD1404002M",
url = "https://hdl.handle.net/21.15107/rcub_gery_633"
}

Mustafić, S., Manojlović, P., Đurović, P., Dragićević, S., Tošić, R.,& Petrović, A. S.. (2014). Našim profesorima - Povodom 90 i 80 godina života i rada. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 94(4), 2-34.
https://doi.org/10.2298/GSGD1404002M
https://hdl.handle.net/21.15107/rcub_gery_633

Mustafić S, Manojlović P, Đurović P, Dragićević S, Tošić R, Petrović AS. Našim profesorima - Povodom 90 i 80 godina života i rada. in Glasnik Srpskog geografskog društva. 2014;94(4):2-34.
doi:10.2298/GSGD1404002M
https://hdl.handle.net/21.15107/rcub_gery_633 .

Mustafić, Sanja, Manojlović, Predrag, Đurović, Predrag, Dragićević, Slavoljub, Tošić, Radislav, Petrović, Aleksandar S., "Našim profesorima - Povodom 90 i 80 godina života i rada" in Glasnik Srpskog geografskog društva, 94, no. 4 (2014):2-34,
https://doi.org/10.2298/GSGD1404002M .,
https://hdl.handle.net/21.15107/rcub_gery_633 .

TY  - JOUR
AU  - Đurović, Mirela
AU  - Đurović, Predrag
PY  - 2014
UR  - https://gery.gef.bg.ac.rs/handle/123456789/613
AB  - This paper provides the insight into morpho-hydrologic characteristics and speleogenesis of the Jankova pećina cave and the evolution of karst in the nearby vicinity. Phases in cave evolution, which represents the alternation of accumulative and erosion processes, were analysed. Clogging of existed conduits during the first accumulative phase leads to displacement of the Janko's creek abyss and formation of another entrance along with new, deeper storaged conduits. The strewed parts of the cave were exposed to partial removal of sediments what resulted in exhumation of its oldest products. The opening of the quite new entrance (vigled) during the opposite process and phase of clogging the endure air circulation inside the cave has been changed. As the consequence, the asymmetric forms of stalactites and stalagmites formed. Study of the Jankova pecina cave represents a contribution to better knowledge of accumulative processes as a significant speleogenetic factor.
AB  - У раду су представљенe морфо-хидролошке карактеристике и спелеогенеза Јанкове пећине и еволуцијa краса ближег окружења. Анализиране су фазе у еволуцији пећине током којих су се смењивали ерозивни и акумулативни процеси. У току прве акумулативне фазе засипају се постојећи канали, што доводи до померања понора Јанковог потока формирања другог улаза и стварања нових, нижих канала. У засутим деловима пећине врши се делимично одношење седимената и долази до ексхумације најстаријих делова пећине. У фази обурвавања отвара се нови улаз (виглед) што битно утиче на промену постојеће циркулације ваздуха у пећини. Последица овог процеса огледа се у стварању асиметричних форми сталагмита и сталактита. Проучавање Јанкове пећине представља допринос бољем познавању акумулатвиних процеса као значајаног спелогенетског фактора.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Speleogenesis of the Jankova pecina cave and karst in it's nearby vicinity
T1  - Спелеогенеза Јанкове пећине са приказом краса ближе околине
VL  - 94
IS  - 4
SP  - 77
EP  - 90
DO  - 10.2298/GSGD1404077D
UR  - https://hdl.handle.net/21.15107/rcub_gery_613
ER  - 

@article{
author = "Đurović, Mirela and Đurović, Predrag",
year = "2014",
abstract = "This paper provides the insight into morpho-hydrologic characteristics and speleogenesis of the Jankova pećina cave and the evolution of karst in the nearby vicinity. Phases in cave evolution, which represents the alternation of accumulative and erosion processes, were analysed. Clogging of existed conduits during the first accumulative phase leads to displacement of the Janko's creek abyss and formation of another entrance along with new, deeper storaged conduits. The strewed parts of the cave were exposed to partial removal of sediments what resulted in exhumation of its oldest products. The opening of the quite new entrance (vigled) during the opposite process and phase of clogging the endure air circulation inside the cave has been changed. As the consequence, the asymmetric forms of stalactites and stalagmites formed. Study of the Jankova pecina cave represents a contribution to better knowledge of accumulative processes as a significant speleogenetic factor., У раду су представљенe морфо-хидролошке карактеристике и спелеогенеза Јанкове пећине и еволуцијa краса ближег окружења. Анализиране су фазе у еволуцији пећине током којих су се смењивали ерозивни и акумулативни процеси. У току прве акумулативне фазе засипају се постојећи канали, што доводи до померања понора Јанковог потока формирања другог улаза и стварања нових, нижих канала. У засутим деловима пећине врши се делимично одношење седимената и долази до ексхумације најстаријих делова пећине. У фази обурвавања отвара се нови улаз (виглед) што битно утиче на промену постојеће циркулације ваздуха у пећини. Последица овог процеса огледа се у стварању асиметричних форми сталагмита и сталактита. Проучавање Јанкове пећине представља допринос бољем познавању акумулатвиних процеса као значајаног спелогенетског фактора.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Speleogenesis of the Jankova pecina cave and karst in it's nearby vicinity, Спелеогенеза Јанкове пећине са приказом краса ближе околине",
volume = "94",
number = "4",
pages = "77-90",
doi = "10.2298/GSGD1404077D",
url = "https://hdl.handle.net/21.15107/rcub_gery_613"
}

Đurović, M.,& Đurović, P.. (2014). Speleogenesis of the Jankova pecina cave and karst in it's nearby vicinity. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 94(4), 77-90.
https://doi.org/10.2298/GSGD1404077D
https://hdl.handle.net/21.15107/rcub_gery_613

Đurović M, Đurović P. Speleogenesis of the Jankova pecina cave and karst in it's nearby vicinity. in Glasnik Srpskog geografskog društva. 2014;94(4):77-90.
doi:10.2298/GSGD1404077D
https://hdl.handle.net/21.15107/rcub_gery_613 .

Đurović, Mirela, Đurović, Predrag, "Speleogenesis of the Jankova pecina cave and karst in it's nearby vicinity" in Glasnik Srpskog geografskog društva, 94, no. 4 (2014):77-90,
https://doi.org/10.2298/GSGD1404077D .,
https://hdl.handle.net/21.15107/rcub_gery_613 .

TY  - JOUR
AU  - Đurović, Predrag
AU  - Živković, Nenad
PY  - 2013
UR  - https://gery.gef.bg.ac.rs/handle/123456789/540
AB  - Morphological and hydrological analyses of the characteristics of the Serbian border zone towards Bulgaria were performed. The morphological analysis included the mountain (Stara Planina, Tupižnica, Svrljiške Planine, Suva Planina and Vidlič), structural basin (Zaječar, Knjaževac, Svrljig and Bela Palanka) and valley (Veliki Timok, Beli Timok, Visočica, Dragovištica) parts. Within the hydrological analysis, the areas with the highest and lowest annual amount of precipitation were identified, as well as the hottest and coldest areas. The change of river basins runoff was analysed, as well as the distribution of waters throughout the year in the studied area. The most important elements of the water balance were shown and the hydrological characteristics of the karst terrain were analysed.
AB  - Извршена је морфолошко-хидролошка анализа одлика пограничног појаса Србије према Бугарској. Морфолошка анализа обухватила је планинске (Стара планина, Тупижница, Сврљишке планине, Сува планина и Видлич), котлинске (Зајечарска, Књажевачка, Сврљишка и Белопаланачка котлина) и долинске (Велики Тимок, Бели Тимок, Височица, Драговиштица) делове. У оквиру хидролошке анализе издвојени су простори са највећом и најмањом годишњом количином падавина, као и најтоплији и најхаднији делови. Анализирана је промена водности сливова, као и расподела вода током године на проучаваном простору. Приказани су најважнији елеменати водног биланса и анализиране хидролошке одлике крашких терена.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Morphological and hydrological characteristics of the Serbian border zone towards Bulgaria
T1  - Морфолошко-хидролошке одлике пограничног појаса Србије према Бугарској
VL  - 93
IS  - 4
SP  - 51
EP  - 82
DO  - 10.2298/GSGD1304051D
UR  - https://hdl.handle.net/21.15107/rcub_gery_540
ER  - 

@article{
author = "Đurović, Predrag and Živković, Nenad",
year = "2013",
abstract = "Morphological and hydrological analyses of the characteristics of the Serbian border zone towards Bulgaria were performed. The morphological analysis included the mountain (Stara Planina, Tupižnica, Svrljiške Planine, Suva Planina and Vidlič), structural basin (Zaječar, Knjaževac, Svrljig and Bela Palanka) and valley (Veliki Timok, Beli Timok, Visočica, Dragovištica) parts. Within the hydrological analysis, the areas with the highest and lowest annual amount of precipitation were identified, as well as the hottest and coldest areas. The change of river basins runoff was analysed, as well as the distribution of waters throughout the year in the studied area. The most important elements of the water balance were shown and the hydrological characteristics of the karst terrain were analysed., Извршена је морфолошко-хидролошка анализа одлика пограничног појаса Србије према Бугарској. Морфолошка анализа обухватила је планинске (Стара планина, Тупижница, Сврљишке планине, Сува планина и Видлич), котлинске (Зајечарска, Књажевачка, Сврљишка и Белопаланачка котлина) и долинске (Велики Тимок, Бели Тимок, Височица, Драговиштица) делове. У оквиру хидролошке анализе издвојени су простори са највећом и најмањом годишњом количином падавина, као и најтоплији и најхаднији делови. Анализирана је промена водности сливова, као и расподела вода током године на проучаваном простору. Приказани су најважнији елеменати водног биланса и анализиране хидролошке одлике крашких терена.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Morphological and hydrological characteristics of the Serbian border zone towards Bulgaria, Морфолошко-хидролошке одлике пограничног појаса Србије према Бугарској",
volume = "93",
number = "4",
pages = "51-82",
doi = "10.2298/GSGD1304051D",
url = "https://hdl.handle.net/21.15107/rcub_gery_540"
}

Đurović, P.,& Živković, N.. (2013). Morphological and hydrological characteristics of the Serbian border zone towards Bulgaria. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 93(4), 51-82.
https://doi.org/10.2298/GSGD1304051D
https://hdl.handle.net/21.15107/rcub_gery_540

Đurović P, Živković N. Morphological and hydrological characteristics of the Serbian border zone towards Bulgaria. in Glasnik Srpskog geografskog društva. 2013;93(4):51-82.
doi:10.2298/GSGD1304051D
https://hdl.handle.net/21.15107/rcub_gery_540 .

Đurović, Predrag, Živković, Nenad, "Morphological and hydrological characteristics of the Serbian border zone towards Bulgaria" in Glasnik Srpskog geografskog društva, 93, no. 4 (2013):51-82,
https://doi.org/10.2298/GSGD1304051D .,
https://hdl.handle.net/21.15107/rcub_gery_540 .

TY  - JOUR
AU  - Đurović, Predrag
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/460
AB  - The Debeli Namet glacier is one of two recent glaciers located in the south western Balkans, located on Durmitor Mountain in the south eastern Dinarides mountain range in Montenegro and is considered to be a small glacier. The size of the glacier from 1954 to 1981 was estimated based on aerial photographs. According to glaciological research, geomorphologic studies of the nearby relief and analyses of climate change (temperature and precipitation) within the last 50 years, new data on the glacier have been obtained. The Debeli Namet glacier is reducing at a rate slower than that of other southern European glaciers. The Debeli Namet glacier did not significantly fluctuate in size (surface and thickness) in response to temperature increases that occurred at the end of the 20st and at the beginning of the 21st centuries. Here, we present partially revised data accompanied by recent results related to the glacier's recent behaviour, its surroundings and its associated climate.
PB  - Ljubljana: Geografski inštitut Antona Melika ZRC SAZU
T2  - Acta Geographica Slovenica - Geografski zbornik
T1  - The debeli namet glacier from the second half of the 20th century to the present
VL  - 52
IS  - 2
SP  - 277
EP  - 293
DO  - 10.3986/AGS52201
UR  - https://hdl.handle.net/21.15107/rcub_gery_460
ER  - 

@article{
author = "Đurović, Predrag",
year = "2012",
abstract = "The Debeli Namet glacier is one of two recent glaciers located in the south western Balkans, located on Durmitor Mountain in the south eastern Dinarides mountain range in Montenegro and is considered to be a small glacier. The size of the glacier from 1954 to 1981 was estimated based on aerial photographs. According to glaciological research, geomorphologic studies of the nearby relief and analyses of climate change (temperature and precipitation) within the last 50 years, new data on the glacier have been obtained. The Debeli Namet glacier is reducing at a rate slower than that of other southern European glaciers. The Debeli Namet glacier did not significantly fluctuate in size (surface and thickness) in response to temperature increases that occurred at the end of the 20st and at the beginning of the 21st centuries. Here, we present partially revised data accompanied by recent results related to the glacier's recent behaviour, its surroundings and its associated climate.",
publisher = "Ljubljana: Geografski inštitut Antona Melika ZRC SAZU",
journal = "Acta Geographica Slovenica - Geografski zbornik",
title = "The debeli namet glacier from the second half of the 20th century to the present",
volume = "52",
number = "2",
pages = "277-293",
doi = "10.3986/AGS52201",
url = "https://hdl.handle.net/21.15107/rcub_gery_460"
}

Đurović, P.. (2012). The debeli namet glacier from the second half of the 20th century to the present. in Acta Geographica Slovenica - Geografski zbornik
Ljubljana: Geografski inštitut Antona Melika ZRC SAZU., 52(2), 277-293.
https://doi.org/10.3986/AGS52201
https://hdl.handle.net/21.15107/rcub_gery_460

Đurović P. The debeli namet glacier from the second half of the 20th century to the present. in Acta Geographica Slovenica - Geografski zbornik. 2012;52(2):277-293.
doi:10.3986/AGS52201
https://hdl.handle.net/21.15107/rcub_gery_460 .

Đurović, Predrag, "The debeli namet glacier from the second half of the 20th century to the present" in Acta Geographica Slovenica - Geografski zbornik, 52, no. 2 (2012):277-293,
https://doi.org/10.3986/AGS52201 .,
https://hdl.handle.net/21.15107/rcub_gery_460 .

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 .

TY  - JOUR
AU  - Đurović, Predrag
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/457
PB  - Pergamon-Elsevier Science Ltd, Oxford
T2  - Quaternary Science Reviews
T1  - Comment on: "The glacial history of the Dinaric Alps, Montenegro" by P.D. Hughes, J.C. Woodward, P.C. van Calsteren, L.E. Thomas [Quaternary Science Reviews 30 (2011), 3393-3412]
VL  - 49
SP  - 109
EP  - 110
DO  - 10.1016/j.quascirev.2012.05.016
UR  - https://hdl.handle.net/21.15107/rcub_gery_457
ER  - 

@article{
author = "Đurović, Predrag",
year = "2012",
publisher = "Pergamon-Elsevier Science Ltd, Oxford",
journal = "Quaternary Science Reviews",
title = "Comment on: "The glacial history of the Dinaric Alps, Montenegro" by P.D. Hughes, J.C. Woodward, P.C. van Calsteren, L.E. Thomas [Quaternary Science Reviews 30 (2011), 3393-3412]",
volume = "49",
pages = "109-110",
doi = "10.1016/j.quascirev.2012.05.016",
url = "https://hdl.handle.net/21.15107/rcub_gery_457"
}

Đurović, P.. (2012). Comment on: "The glacial history of the Dinaric Alps, Montenegro" by P.D. Hughes, J.C. Woodward, P.C. van Calsteren, L.E. Thomas [Quaternary Science Reviews 30 (2011), 3393-3412]. in Quaternary Science Reviews
Pergamon-Elsevier Science Ltd, Oxford., 49, 109-110.
https://doi.org/10.1016/j.quascirev.2012.05.016
https://hdl.handle.net/21.15107/rcub_gery_457

Đurović P. Comment on: "The glacial history of the Dinaric Alps, Montenegro" by P.D. Hughes, J.C. Woodward, P.C. van Calsteren, L.E. Thomas [Quaternary Science Reviews 30 (2011), 3393-3412]. in Quaternary Science Reviews. 2012;49:109-110.
doi:10.1016/j.quascirev.2012.05.016
https://hdl.handle.net/21.15107/rcub_gery_457 .

Đurović, Predrag, "Comment on: "The glacial history of the Dinaric Alps, Montenegro" by P.D. Hughes, J.C. Woodward, P.C. van Calsteren, L.E. Thomas [Quaternary Science Reviews 30 (2011), 3393-3412]" in Quaternary Science Reviews, 49 (2012):109-110,
https://doi.org/10.1016/j.quascirev.2012.05.016 .,
https://hdl.handle.net/21.15107/rcub_gery_457 .

TY  - JOUR
AU  - Đurović, Predrag
AU  - Petrović, Aleksandar S.
AU  - Simić, Sava
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/347
AB  - The alternation of glacial and carts processes as the consequence of frequent changes of glacial and interglacial phases could be recognized at the mountains Durmitor and Žijovo. Re-modeling of glacial morphology (cirques and trough valleys) carved currently karst topography with domination of uvalas. Their size and shape vary considerably as the consequence of differences within the preexisting glacial forms. Duration and intensity of kartification, which re-modeled former glacial forms into karst landforms, determine the degree of uvalas development and formation of three distinct evolution types of high-mountainous uvalas: glacial, glacial-karst and glaciofluvial.
AB  - Kao posledica čestih smena glacijalnih i interglacijalnih faza na planinama Durmitor i Žijovo dolazi do smena glacijalnog i kraškog procesa. Premodeliranjem glacijalne morfologije (cirkovi i valovi) izgrađuje se savremeni kraški reljef u kome dominiraju uvale. Različita veličina i oblik uvala posledica je različitosti glacijalnih oblika koji su im prethodili. Trajanje i intenzitet kraškog procesa, kojima su nekadašnji glacijalni oblici premodelirani u kraške, odredili su stepen razijenosti uvala i izgradnju tri evolutivna tipa visokoplaninskih uvala: glacijalne, glacijalno-kraške i glacijalno-fluvijalne uvale.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - The overall impact of Pleistocene glaciation on morphological diversity of uvalas at Durmitor and Žijovo
T1  - Uticaj pleistocenske glacijacije na morfološku raznolikost uvala Durmitora i Žijova
VL  - 90
IS  - 1
SP  - 17
EP  - 34
UR  - https://hdl.handle.net/21.15107/rcub_gery_347
ER  - 

@article{
author = "Đurović, Predrag and Petrović, Aleksandar S. and Simić, Sava",
year = "2010",
abstract = "The alternation of glacial and carts processes as the consequence of frequent changes of glacial and interglacial phases could be recognized at the mountains Durmitor and Žijovo. Re-modeling of glacial morphology (cirques and trough valleys) carved currently karst topography with domination of uvalas. Their size and shape vary considerably as the consequence of differences within the preexisting glacial forms. Duration and intensity of kartification, which re-modeled former glacial forms into karst landforms, determine the degree of uvalas development and formation of three distinct evolution types of high-mountainous uvalas: glacial, glacial-karst and glaciofluvial., Kao posledica čestih smena glacijalnih i interglacijalnih faza na planinama Durmitor i Žijovo dolazi do smena glacijalnog i kraškog procesa. Premodeliranjem glacijalne morfologije (cirkovi i valovi) izgrađuje se savremeni kraški reljef u kome dominiraju uvale. Različita veličina i oblik uvala posledica je različitosti glacijalnih oblika koji su im prethodili. Trajanje i intenzitet kraškog procesa, kojima su nekadašnji glacijalni oblici premodelirani u kraške, odredili su stepen razijenosti uvala i izgradnju tri evolutivna tipa visokoplaninskih uvala: glacijalne, glacijalno-kraške i glacijalno-fluvijalne uvale.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "The overall impact of Pleistocene glaciation on morphological diversity of uvalas at Durmitor and Žijovo, Uticaj pleistocenske glacijacije na morfološku raznolikost uvala Durmitora i Žijova",
volume = "90",
number = "1",
pages = "17-34",
url = "https://hdl.handle.net/21.15107/rcub_gery_347"
}

Đurović, P., Petrović, A. S.,& Simić, S.. (2010). The overall impact of Pleistocene glaciation on morphological diversity of uvalas at Durmitor and Žijovo. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 90(1), 17-34.
https://hdl.handle.net/21.15107/rcub_gery_347

Đurović P, Petrović AS, Simić S. The overall impact of Pleistocene glaciation on morphological diversity of uvalas at Durmitor and Žijovo. in Glasnik Srpskog geografskog društva. 2010;90(1):17-34.
https://hdl.handle.net/21.15107/rcub_gery_347 .

Đurović, Predrag, Petrović, Aleksandar S., Simić, Sava, "The overall impact of Pleistocene glaciation on morphological diversity of uvalas at Durmitor and Žijovo" in Glasnik Srpskog geografskog društva, 90, no. 1 (2010):17-34,
https://hdl.handle.net/21.15107/rcub_gery_347 .

TY  - JOUR
AU  - Đurović, Predrag
AU  - Đurović, Mirela
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/376
AB  - The main principles and methodology of establishing the inventory of geoheritage sites are analyzed. Special attention is given to theoretical and practical problems related to application of the established principles. Geoheritage sites in Montenegro, classified according to international standards (ProGeo) were presented, including their valorization based on the aspects of tourism valorization. Possibilities and limitations of geotourism development in Montenegro were emphasized, too. .
PB  - Novi Sad : Univerzitet u Novom Sadu - Prirodno-matematički fakultet, Departman za geografiju, turizam i hotelijerstvo
T2  - Geographica Pannonica
T1  - Inventory of geoheritage sites: The base of geotourism development in Montenegro
VL  - 14
IS  - 4
SP  - 126
EP  - 132
DO  - 10.5937/GeoPan1004126D
UR  - https://hdl.handle.net/21.15107/rcub_gery_376
ER  - 

@article{
author = "Đurović, Predrag and Đurović, Mirela",
year = "2010",
abstract = "The main principles and methodology of establishing the inventory of geoheritage sites are analyzed. Special attention is given to theoretical and practical problems related to application of the established principles. Geoheritage sites in Montenegro, classified according to international standards (ProGeo) were presented, including their valorization based on the aspects of tourism valorization. Possibilities and limitations of geotourism development in Montenegro were emphasized, too. .",
publisher = "Novi Sad : Univerzitet u Novom Sadu - Prirodno-matematički fakultet, Departman za geografiju, turizam i hotelijerstvo",
journal = "Geographica Pannonica",
title = "Inventory of geoheritage sites: The base of geotourism development in Montenegro",
volume = "14",
number = "4",
pages = "126-132",
doi = "10.5937/GeoPan1004126D",
url = "https://hdl.handle.net/21.15107/rcub_gery_376"
}

Đurović, P.,& Đurović, M.. (2010). Inventory of geoheritage sites: The base of geotourism development in Montenegro. in Geographica Pannonica
Novi Sad : Univerzitet u Novom Sadu - Prirodno-matematički fakultet, Departman za geografiju, turizam i hotelijerstvo., 14(4), 126-132.
https://doi.org/10.5937/GeoPan1004126D
https://hdl.handle.net/21.15107/rcub_gery_376

Đurović P, Đurović M. Inventory of geoheritage sites: The base of geotourism development in Montenegro. in Geographica Pannonica. 2010;14(4):126-132.
doi:10.5937/GeoPan1004126D
https://hdl.handle.net/21.15107/rcub_gery_376 .

Đurović, Predrag, Đurović, Mirela, "Inventory of geoheritage sites: The base of geotourism development in Montenegro" in Geographica Pannonica, 14, no. 4 (2010):126-132,
https://doi.org/10.5937/GeoPan1004126D .,
https://hdl.handle.net/21.15107/rcub_gery_376 .

TY  - JOUR
AU  - Simić, Sava
AU  - Gavrilović, Ljiljana
AU  - Đurović, Predrag
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/346
AB  - Incomplete definitions of geodiversity and geoheritage caused the domination of clearly geological approach to these scientific problems. That is the reason why some of the integral elements of geographical environment were neglected. Wrong theoretical assumptions reflected negatively the determination and advancement of this scientific discipline. The reasons for such condition are mentioned in the paper, as well as the necessity of different and more comprehensive perspective of geodiversity and geoheritage, by which the directions of the future development are implied. .
AB  - Nepotpune definicije geodiverziteta i geonasleđa uzrokovale su dominaciju čisto geološkog pristupa ovim naučnim problemima. To je razlog što su neki od sastavnih segmenata geografske sredine bili zanemareni. Pogrešne teorijske postavke negativno su se odrazile na utvrđivanje i unapređenje ove naučne oblasti. U radu su navedeni razlozi ovakvog stanja, ukazano je na potrebu drugačijeg i obuhvatnijeg sagledavanja geodiverziteta i geonasleđa, čime se nagoveštavaju pravci budućeg razvoja. .
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Geodiversity and geoheritage: New approach to the interpretation of the terms
T1  - Geodiverzitet i geonasleđe - novi pristup tumačenju pojmova
VL  - 90
IS  - 2
SP  - 1
EP  - 14
UR  - https://hdl.handle.net/21.15107/rcub_gery_346
ER  - 

@article{
author = "Simić, Sava and Gavrilović, Ljiljana and Đurović, Predrag",
year = "2010",
abstract = "Incomplete definitions of geodiversity and geoheritage caused the domination of clearly geological approach to these scientific problems. That is the reason why some of the integral elements of geographical environment were neglected. Wrong theoretical assumptions reflected negatively the determination and advancement of this scientific discipline. The reasons for such condition are mentioned in the paper, as well as the necessity of different and more comprehensive perspective of geodiversity and geoheritage, by which the directions of the future development are implied. ., Nepotpune definicije geodiverziteta i geonasleđa uzrokovale su dominaciju čisto geološkog pristupa ovim naučnim problemima. To je razlog što su neki od sastavnih segmenata geografske sredine bili zanemareni. Pogrešne teorijske postavke negativno su se odrazile na utvrđivanje i unapređenje ove naučne oblasti. U radu su navedeni razlozi ovakvog stanja, ukazano je na potrebu drugačijeg i obuhvatnijeg sagledavanja geodiverziteta i geonasleđa, čime se nagoveštavaju pravci budućeg razvoja. .",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Geodiversity and geoheritage: New approach to the interpretation of the terms, Geodiverzitet i geonasleđe - novi pristup tumačenju pojmova",
volume = "90",
number = "2",
pages = "1-14",
url = "https://hdl.handle.net/21.15107/rcub_gery_346"
}

Simić, S., Gavrilović, L.,& Đurović, P.. (2010). Geodiversity and geoheritage: New approach to the interpretation of the terms. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 90(2), 1-14.
https://hdl.handle.net/21.15107/rcub_gery_346

Simić S, Gavrilović L, Đurović P. Geodiversity and geoheritage: New approach to the interpretation of the terms. in Glasnik Srpskog geografskog društva. 2010;90(2):1-14.
https://hdl.handle.net/21.15107/rcub_gery_346 .

Simić, Sava, Gavrilović, Ljiljana, Đurović, Predrag, "Geodiversity and geoheritage: New approach to the interpretation of the terms" in Glasnik Srpskog geografskog društva, 90, no. 2 (2010):1-14,
https://hdl.handle.net/21.15107/rcub_gery_346 .

TY  - JOUR
AU  - Đurović, Predrag
PY  - 2009
UR  - https://gery.gef.bg.ac.rs/handle/123456789/296
AB  - Mount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Throughout the Pleistocene there were many glaciers there, which descended to adjacent karst plateau. Types of glaciers, their number and direction of moving were mostly affected by geological structure (carbonate basis) and pre-glacial relief (karst and fluvial relief). During two phases of intensive glaciation, the surface that had been seized by glacial changes also changed. Over 54% of the surface of Durmitor was exposed to the glacial process of the stronger phase and about 36% of the weaker phase. Cirque type of glaciation dominated the third phase.
PB  - Ljubljana: Geografski inštitut Antona Melika ZRC SAZU
T2  - Acta Geographica Slovenica - Geografski zbornik
T1  - Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro
VL  - 49
IS  - 2
SP  - 263
EP  - 279
DO  - 10.3986/AGS49202
UR  - https://hdl.handle.net/21.15107/rcub_gery_296
ER  - 

@article{
author = "Đurović, Predrag",
year = "2009",
abstract = "Mount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Throughout the Pleistocene there were many glaciers there, which descended to adjacent karst plateau. Types of glaciers, their number and direction of moving were mostly affected by geological structure (carbonate basis) and pre-glacial relief (karst and fluvial relief). During two phases of intensive glaciation, the surface that had been seized by glacial changes also changed. Over 54% of the surface of Durmitor was exposed to the glacial process of the stronger phase and about 36% of the weaker phase. Cirque type of glaciation dominated the third phase.",
publisher = "Ljubljana: Geografski inštitut Antona Melika ZRC SAZU",
journal = "Acta Geographica Slovenica - Geografski zbornik",
title = "Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro",
volume = "49",
number = "2",
pages = "263-279",
doi = "10.3986/AGS49202",
url = "https://hdl.handle.net/21.15107/rcub_gery_296"
}

Đurović, P.. (2009). Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro. in Acta Geographica Slovenica - Geografski zbornik
Ljubljana: Geografski inštitut Antona Melika ZRC SAZU., 49(2), 263-279.
https://doi.org/10.3986/AGS49202
https://hdl.handle.net/21.15107/rcub_gery_296

Đurović P. Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro. in Acta Geographica Slovenica - Geografski zbornik. 2009;49(2):263-279.
doi:10.3986/AGS49202
https://hdl.handle.net/21.15107/rcub_gery_296 .

Đurović, Predrag, "Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro" in Acta Geographica Slovenica - Geografski zbornik, 49, no. 2 (2009):263-279,
https://doi.org/10.3986/AGS49202 .,
https://hdl.handle.net/21.15107/rcub_gery_296 .

TY  - JOUR
AU  - Đurović, Predrag
AU  - Menković, Ljubomir
PY  - 2008
UR  - https://gery.gef.bg.ac.rs/handle/123456789/283
AB  - The Duboka drains the eastern side of Kopaonik Mountain. Geomorphology and geology of the area indicate, and the office and field researches confirm, that the Duboka was formerly in the Rasina basin and now belongs to the Toplica system. A minor Toplica tributary captured the Duboka headwater and diverted it into its drainage system. Capturing and captured s of the two systems are a geomorphologic rarity; the headwaters of the Rasina are diverted into the Toplica system, and the middle course of the Toplica (Blatašnica) captures the Rasina.
PB  - Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić"
T2  - Zbornik radova Geografskog instituta "Jovan Cvijić", SANU
T1  - The Duboka piracy
IS  - 58
SP  - 17
EP  - 27
UR  - https://hdl.handle.net/21.15107/rcub_gery_283
ER  - 

@article{
author = "Đurović, Predrag and Menković, Ljubomir",
year = "2008",
abstract = "The Duboka drains the eastern side of Kopaonik Mountain. Geomorphology and geology of the area indicate, and the office and field researches confirm, that the Duboka was formerly in the Rasina basin and now belongs to the Toplica system. A minor Toplica tributary captured the Duboka headwater and diverted it into its drainage system. Capturing and captured s of the two systems are a geomorphologic rarity; the headwaters of the Rasina are diverted into the Toplica system, and the middle course of the Toplica (Blatašnica) captures the Rasina.",
publisher = "Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić"",
journal = "Zbornik radova Geografskog instituta "Jovan Cvijić", SANU",
title = "The Duboka piracy",
number = "58",
pages = "17-27",
url = "https://hdl.handle.net/21.15107/rcub_gery_283"
}

Đurović, P.,& Menković, L.. (2008). The Duboka piracy. in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU
Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić".(58), 17-27.
https://hdl.handle.net/21.15107/rcub_gery_283

Đurović P, Menković L. The Duboka piracy. in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU. 2008;(58):17-27.
https://hdl.handle.net/21.15107/rcub_gery_283 .

Đurović, Predrag, Menković, Ljubomir, "The Duboka piracy" in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU, no. 58 (2008):17-27,
https://hdl.handle.net/21.15107/rcub_gery_283 .

TY  - JOUR
AU  - Đurović, Predrag
PY  - 2008
UR  - https://gery.gef.bg.ac.rs/handle/123456789/265
AB  - Results of paleogeographic studies were presented in numerous scientific works in publications of the Faculty of Geography in Belgrade. Works of paleogeographic contents relate to certain general themes such as: paleoabrasion relief, pale volcanic relief, establishing the age of speleological objects, establishing the age of phases in the relief development, pale climate reconstructions, etc. This analysis has been done on the occasion of the thirtieth anniversary of introducing Paleogeography into regular instruction at the Faculty of Geography. .
AB  - U brojnim naučnim radovima koji su objavljeni u publikacijama Geografskog fakulteta u Beogradu izloženi su i rezultati paleogeografskih proučavanja. Radovi sa paleogeogrfskim sadržajem vezani su za određene opšte teme kao što su: paleoabrazioni i paleovulkanski reljef, utvrđivanje starosti speleoloških objekata, utvrđivanje starosti faza u razvoju reljefa, paleoklimatske rekonstrukcije i sl. Izvršena analiza urađena je povodom 30-godišnjice od uvođenja predmeta Paleogeografija u redovnu nastavu na Geografskom fakultetu.
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
T2  - Zbornik radova - Geografski fakultet Univerziteta u Beogradu
T1  - Paleogeographic contents in publications of Faculty of Geography in Belgrade: On the thirtieth anniversary of introducing Paleogeography into regular instruction
T1  - Paleogeografski sadržaji u publikacijama Geografskog fakulteta u Beogradu - povodom 30-godišnjice od uvođenja predmeta Paleogeografija u redovnu nastavu
IS  - 56
SP  - 5
EP  - 24
UR  - https://hdl.handle.net/21.15107/rcub_gery_265
ER  - 

@article{
author = "Đurović, Predrag",
year = "2008",
abstract = "Results of paleogeographic studies were presented in numerous scientific works in publications of the Faculty of Geography in Belgrade. Works of paleogeographic contents relate to certain general themes such as: paleoabrasion relief, pale volcanic relief, establishing the age of speleological objects, establishing the age of phases in the relief development, pale climate reconstructions, etc. This analysis has been done on the occasion of the thirtieth anniversary of introducing Paleogeography into regular instruction at the Faculty of Geography. ., U brojnim naučnim radovima koji su objavljeni u publikacijama Geografskog fakulteta u Beogradu izloženi su i rezultati paleogeografskih proučavanja. Radovi sa paleogeogrfskim sadržajem vezani su za određene opšte teme kao što su: paleoabrazioni i paleovulkanski reljef, utvrđivanje starosti speleoloških objekata, utvrđivanje starosti faza u razvoju reljefa, paleoklimatske rekonstrukcije i sl. Izvršena analiza urađena je povodom 30-godišnjice od uvođenja predmeta Paleogeografija u redovnu nastavu na Geografskom fakultetu.",
publisher = "Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova - Geografski fakultet Univerziteta u Beogradu",
title = "Paleogeographic contents in publications of Faculty of Geography in Belgrade: On the thirtieth anniversary of introducing Paleogeography into regular instruction, Paleogeografski sadržaji u publikacijama Geografskog fakulteta u Beogradu - povodom 30-godišnjice od uvođenja predmeta Paleogeografija u redovnu nastavu",
number = "56",
pages = "5-24",
url = "https://hdl.handle.net/21.15107/rcub_gery_265"
}

Đurović, P.. (2008). Paleogeographic contents in publications of Faculty of Geography in Belgrade: On the thirtieth anniversary of introducing Paleogeography into regular instruction. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu
Beograd : Univerzitet u Beogradu - Geografski fakultet.(56), 5-24.
https://hdl.handle.net/21.15107/rcub_gery_265

Đurović P. Paleogeographic contents in publications of Faculty of Geography in Belgrade: On the thirtieth anniversary of introducing Paleogeography into regular instruction. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu. 2008;(56):5-24.
https://hdl.handle.net/21.15107/rcub_gery_265 .

Đurović, Predrag, "Paleogeographic contents in publications of Faculty of Geography in Belgrade: On the thirtieth anniversary of introducing Paleogeography into regular instruction" in Zbornik radova - Geografski fakultet Univerziteta u Beogradu, no. 56 (2008):5-24,
https://hdl.handle.net/21.15107/rcub_gery_265 .

TY  - JOUR
AU  - Đurović, Predrag
AU  - Petrović, Aleksandar S.
PY  - 2007
UR  - https://gery.gef.bg.ac.rs/handle/123456789/233
AB  - Montenegro occupies relatively small, southeastern part of the Dinaric mountains. Geological composition, which is predominantly carbonate, enabled formation of a great number of deep canyons and gorges. Canyons of Montenegro were formed in several ways, during multiple phases. Regardless of polygenetic and polymorphic character of the canyons, they can be classified into three main groups. By incision of melt-water rivers of Pleistocene glaciers, deep and particularly narrow canyons of small width were formed. The rivers that presently flow through these canyons have a nival regime - during the summer, their discharge is minimal, or they completely dry out. Depths of these canyons are up to 500 m. Rivers that directly feed into the Adriatic sea are of torrential character. They have pluvial regime, and dry out during the summer. Their canyons are short, several hundreds of meters deep. Deepest and longest canyons have been formed by incision of rivers that have changed their regimes during a longer period of time. Melt-water of Pleistocene glaciers has incised the greatest parts of canyons at the beginning of Holocene. Presently, river courses have nival-pluvial regime. In this group, single-phase and multiple-phase canyons can be distinguished (alteration of erosional and accumulation processes). Depths of these canyons exceed 1000 m.
PB  - Novi Sad : Univerzitet u Novom Sadu - Prirodno-matematički fakultet, Departman za geografiju, turizam i hotelijerstvo
T2  - Geographica Pannonica
T1  - Large canyons in Dinaric and Prokletije mountains region of Montenegro
IS  - 11
SP  - 14
EP  - 18
DO  - 10.5937/GeoPan0711014D
UR  - https://hdl.handle.net/21.15107/rcub_gery_233
ER  - 

@article{
author = "Đurović, Predrag and Petrović, Aleksandar S.",
year = "2007",
abstract = "Montenegro occupies relatively small, southeastern part of the Dinaric mountains. Geological composition, which is predominantly carbonate, enabled formation of a great number of deep canyons and gorges. Canyons of Montenegro were formed in several ways, during multiple phases. Regardless of polygenetic and polymorphic character of the canyons, they can be classified into three main groups. By incision of melt-water rivers of Pleistocene glaciers, deep and particularly narrow canyons of small width were formed. The rivers that presently flow through these canyons have a nival regime - during the summer, their discharge is minimal, or they completely dry out. Depths of these canyons are up to 500 m. Rivers that directly feed into the Adriatic sea are of torrential character. They have pluvial regime, and dry out during the summer. Their canyons are short, several hundreds of meters deep. Deepest and longest canyons have been formed by incision of rivers that have changed their regimes during a longer period of time. Melt-water of Pleistocene glaciers has incised the greatest parts of canyons at the beginning of Holocene. Presently, river courses have nival-pluvial regime. In this group, single-phase and multiple-phase canyons can be distinguished (alteration of erosional and accumulation processes). Depths of these canyons exceed 1000 m.",
publisher = "Novi Sad : Univerzitet u Novom Sadu - Prirodno-matematički fakultet, Departman za geografiju, turizam i hotelijerstvo",
journal = "Geographica Pannonica",
title = "Large canyons in Dinaric and Prokletije mountains region of Montenegro",
number = "11",
pages = "14-18",
doi = "10.5937/GeoPan0711014D",
url = "https://hdl.handle.net/21.15107/rcub_gery_233"
}

Đurović, P.,& Petrović, A. S.. (2007). Large canyons in Dinaric and Prokletije mountains region of Montenegro. in Geographica Pannonica
Novi Sad : Univerzitet u Novom Sadu - Prirodno-matematički fakultet, Departman za geografiju, turizam i hotelijerstvo.(11), 14-18.
https://doi.org/10.5937/GeoPan0711014D
https://hdl.handle.net/21.15107/rcub_gery_233

Đurović P, Petrović AS. Large canyons in Dinaric and Prokletije mountains region of Montenegro. in Geographica Pannonica. 2007;(11):14-18.
doi:10.5937/GeoPan0711014D
https://hdl.handle.net/21.15107/rcub_gery_233 .

Đurović, Predrag, Petrović, Aleksandar S., "Large canyons in Dinaric and Prokletije mountains region of Montenegro" in Geographica Pannonica, no. 11 (2007):14-18,
https://doi.org/10.5937/GeoPan0711014D .,
https://hdl.handle.net/21.15107/rcub_gery_233 .

TY  - JOUR
AU  - Đurović, Predrag
PY  - 2007
UR  - https://gery.gef.bg.ac.rs/handle/123456789/228
AB  - Because of the similar appearance of certain alluvial fans and glacial landforms, during the reconstruction of accumulative landforms of the glacial process, some errors may occur regarding the determination of the genetic type, leading to the inaccurate conclusions about the size of glaciations. The key for genetic determination of landforms is their altitude. Landforms of the same genetic type (alluvial fans) depending on their altitude, can be determined and classified into different genetic categories - fluvial and glacial ones. This article researches morphological similarity and genesis of the alluvial fan in Dabarsko polje at the altitude of 500 m, as well as the series of stadial moraines at the Durmitor Mountain, at the altitude of 1800 m.
AB  - Zbog sličnog izgleda pojedinih plavina sa glacijalnim oblicima, prilikom rekonsturkcije akumulativnih oblika glacijalnog procesa mogu se načiniti greške u određivanju genetskog tipa, što ima za posledicu pogrešno određenje obima glacijacije. Ključ za genetsku determinaciju oblika je nadmorska visina na kojoj se oni nalaze. Oblici istog genetskog tipa (plavine), u zavisnosti od nadmorske visine na kojoj se nalaze, determinišu se i svrstavaju u različite genetske kategorije - fluvijalne i glacijalne. Analiziran je izgled, morfološka sličnost i nastanak plavine u Dabarskom polju na visini od oko 500 m i serija stadijalnih morene na Durmitoru na visini od oko 1800 m.
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
T2  - Zbornik radova - Geografski fakultet Univerziteta u Beogradu
T1  - Supplement to solving the issue of determination of moraines and alluvial fans
T1  - Prilog rešavanju problema determinisanja morena i plavina
IS  - 55
SP  - 5
EP  - 12
UR  - https://hdl.handle.net/21.15107/rcub_gery_228
ER  - 

@article{
author = "Đurović, Predrag",
year = "2007",
abstract = "Because of the similar appearance of certain alluvial fans and glacial landforms, during the reconstruction of accumulative landforms of the glacial process, some errors may occur regarding the determination of the genetic type, leading to the inaccurate conclusions about the size of glaciations. The key for genetic determination of landforms is their altitude. Landforms of the same genetic type (alluvial fans) depending on their altitude, can be determined and classified into different genetic categories - fluvial and glacial ones. This article researches morphological similarity and genesis of the alluvial fan in Dabarsko polje at the altitude of 500 m, as well as the series of stadial moraines at the Durmitor Mountain, at the altitude of 1800 m., Zbog sličnog izgleda pojedinih plavina sa glacijalnim oblicima, prilikom rekonsturkcije akumulativnih oblika glacijalnog procesa mogu se načiniti greške u određivanju genetskog tipa, što ima za posledicu pogrešno određenje obima glacijacije. Ključ za genetsku determinaciju oblika je nadmorska visina na kojoj se oni nalaze. Oblici istog genetskog tipa (plavine), u zavisnosti od nadmorske visine na kojoj se nalaze, determinišu se i svrstavaju u različite genetske kategorije - fluvijalne i glacijalne. Analiziran je izgled, morfološka sličnost i nastanak plavine u Dabarskom polju na visini od oko 500 m i serija stadijalnih morene na Durmitoru na visini od oko 1800 m.",
publisher = "Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova - Geografski fakultet Univerziteta u Beogradu",
title = "Supplement to solving the issue of determination of moraines and alluvial fans, Prilog rešavanju problema determinisanja morena i plavina",
number = "55",
pages = "5-12",
url = "https://hdl.handle.net/21.15107/rcub_gery_228"
}

Đurović, P.. (2007). Supplement to solving the issue of determination of moraines and alluvial fans. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu
Beograd : Univerzitet u Beogradu - Geografski fakultet.(55), 5-12.
https://hdl.handle.net/21.15107/rcub_gery_228

Đurović P. Supplement to solving the issue of determination of moraines and alluvial fans. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu. 2007;(55):5-12.
https://hdl.handle.net/21.15107/rcub_gery_228 .

Đurović, Predrag, "Supplement to solving the issue of determination of moraines and alluvial fans" in Zbornik radova - Geografski fakultet Univerziteta u Beogradu, no. 55 (2007):5-12,
https://hdl.handle.net/21.15107/rcub_gery_228 .

TY  - JOUR
AU  - Đurović, Predrag
AU  - Mijović, Dušan
PY  - 2006
UR  - https://gery.gef.bg.ac.rs/handle/123456789/178
AB  - The objects of geoheritage in Serbia represent the overall national geodiversity. Through the short history of the geosite conservation, these sites were given different names, mostly as school examples. The conservation activities expanded since the mid-20th century, but modern methods of the geosite designation and assessment have been applied only from the nineties on the basis of the Pro-GEO principles. In result, an inventory of the geosites of Serbia was made that lists 650 sites, and equalizes the status of geodiversity with that of biodiversity in many social fields.
AB  - Objekti geonasleđa u Srbiji predstavljaju njen ukupni geodiverzitet, a u dosadašnjem razvoju ideje geonasleđa oni su se javljali pod različitim imenima. Od polovine 20. veka rad na ovoj oblasti se proširuje, a tek 90-ih godina se ustanovljava savremena metodologija izdvajanja i vrednovanja objekata geonasleđa na principima ProGEO organizacije. Kao rezultat toga nastaje Inventar objekata geonasleđa Srbije koji ima 650 objekata. Tako geodiverzitet, a u okviru njega i geonasleđe, dobija ravnopravan status sa biodiverzitetom.
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
T2  - Zbornik radova - Geografski fakultet Univerziteta u Beogradu
T1  - Geoheritage of Serbia: Representative of its total geodiversity
T1  - Geonasleđe Srbije - reprezent njenog ukupnog geodiverziteta
IS  - 54
SP  - 5
EP  - 18
UR  - https://hdl.handle.net/21.15107/rcub_gery_178
ER  - 

@article{
author = "Đurović, Predrag and Mijović, Dušan",
year = "2006",
abstract = "The objects of geoheritage in Serbia represent the overall national geodiversity. Through the short history of the geosite conservation, these sites were given different names, mostly as school examples. The conservation activities expanded since the mid-20th century, but modern methods of the geosite designation and assessment have been applied only from the nineties on the basis of the Pro-GEO principles. In result, an inventory of the geosites of Serbia was made that lists 650 sites, and equalizes the status of geodiversity with that of biodiversity in many social fields., Objekti geonasleđa u Srbiji predstavljaju njen ukupni geodiverzitet, a u dosadašnjem razvoju ideje geonasleđa oni su se javljali pod različitim imenima. Od polovine 20. veka rad na ovoj oblasti se proširuje, a tek 90-ih godina se ustanovljava savremena metodologija izdvajanja i vrednovanja objekata geonasleđa na principima ProGEO organizacije. Kao rezultat toga nastaje Inventar objekata geonasleđa Srbije koji ima 650 objekata. Tako geodiverzitet, a u okviru njega i geonasleđe, dobija ravnopravan status sa biodiverzitetom.",
publisher = "Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova - Geografski fakultet Univerziteta u Beogradu",
title = "Geoheritage of Serbia: Representative of its total geodiversity, Geonasleđe Srbije - reprezent njenog ukupnog geodiverziteta",
number = "54",
pages = "5-18",
url = "https://hdl.handle.net/21.15107/rcub_gery_178"
}

Đurović, P.,& Mijović, D.. (2006). Geoheritage of Serbia: Representative of its total geodiversity. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu
Beograd : Univerzitet u Beogradu - Geografski fakultet.(54), 5-18.
https://hdl.handle.net/21.15107/rcub_gery_178

Đurović P, Mijović D. Geoheritage of Serbia: Representative of its total geodiversity. in Zbornik radova - Geografski fakultet Univerziteta u Beogradu. 2006;(54):5-18.
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