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  - 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  - 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 .