TY  - JOUR
AU  - Nešić, Dragan
AU  - Milinčić, Uroš V.
AU  - Milinčić, Miroljub A.
PY  - 2023
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1731
AB  - In the medium-high mountains of Serbia (1,000-2,000 m.a.s.l), sporadic periglacial relief forms occur, which is also the case with Mount Vardenik (1,876 m.high), a mountain in the southeast of Serbia. During reconnaissance, certain relict and sub-recent periglacial phenomena and landforms in the highest part of the mountain have been identified: block slides, rock flows, thermogenic landslides in springs, nivation-induced relief and in one location cryoplanation terraces. Sparsely clustered and individual occurrences of frost splitting and solifluction of the land surface and small areas with grass turf indicate contemporary signs of sporadically present seasonal frost and freeze-thaw cycles. Periglacial morphology and its processes have been recorded and investigated using a qualitative geomorphological procedure. The main problem is the origin of periglacial phenomena (occurrences and landforms) of the relief, considering that the analysis of the contemporary climate, geoecological properties and anthropogenic activities indicate that there are no condi-tions for the existence and development of a contemporary periglacial environment on the mountain. The problem was analyzed considering the climate change in general and, in particular, geoecological conditions created under the influence of human activities. Due to the observed sporadic relict and sub-recent periglacial relief on Mount Vardenik, in contemporary conditions the periglacial environment of this area can be consid-ered as relict or as a phenomenon bordering the limits of differentiation. The relict property also results from the fact that on the mountain, due to the contemporary climate and changed geoecological conditions, the transition zone of the periglacial environment cannot be distinguished.
PB  - Baia Mare : North University of Baia Mare
T2  - Carpathian Journal of Earth and Environmental Sciences
T1  - Periglacial Relief Phenomena on Mount Vardenik (Southeastern Serbia)
VL  - 18
IS  - 1
SP  - 127
EP  - 138
DO  - 10.26471/cjees/2023/018/246
ER  - 

@article{
author = "Nešić, Dragan and Milinčić, Uroš V. and Milinčić, Miroljub A.",
year = "2023",
abstract = "In the medium-high mountains of Serbia (1,000-2,000 m.a.s.l), sporadic periglacial relief forms occur, which is also the case with Mount Vardenik (1,876 m.high), a mountain in the southeast of Serbia. During reconnaissance, certain relict and sub-recent periglacial phenomena and landforms in the highest part of the mountain have been identified: block slides, rock flows, thermogenic landslides in springs, nivation-induced relief and in one location cryoplanation terraces. Sparsely clustered and individual occurrences of frost splitting and solifluction of the land surface and small areas with grass turf indicate contemporary signs of sporadically present seasonal frost and freeze-thaw cycles. Periglacial morphology and its processes have been recorded and investigated using a qualitative geomorphological procedure. The main problem is the origin of periglacial phenomena (occurrences and landforms) of the relief, considering that the analysis of the contemporary climate, geoecological properties and anthropogenic activities indicate that there are no condi-tions for the existence and development of a contemporary periglacial environment on the mountain. The problem was analyzed considering the climate change in general and, in particular, geoecological conditions created under the influence of human activities. Due to the observed sporadic relict and sub-recent periglacial relief on Mount Vardenik, in contemporary conditions the periglacial environment of this area can be consid-ered as relict or as a phenomenon bordering the limits of differentiation. The relict property also results from the fact that on the mountain, due to the contemporary climate and changed geoecological conditions, the transition zone of the periglacial environment cannot be distinguished.",
publisher = "Baia Mare : North University of Baia Mare",
journal = "Carpathian Journal of Earth and Environmental Sciences",
title = "Periglacial Relief Phenomena on Mount Vardenik (Southeastern Serbia)",
volume = "18",
number = "1",
pages = "127-138",
doi = "10.26471/cjees/2023/018/246"
}

Nešić, D., Milinčić, U. V.,& Milinčić, M. A.. (2023). Periglacial Relief Phenomena on Mount Vardenik (Southeastern Serbia). in Carpathian Journal of Earth and Environmental Sciences
Baia Mare : North University of Baia Mare., 18(1), 127-138.
https://doi.org/10.26471/cjees/2023/018/246

Nešić D, Milinčić UV, Milinčić MA. Periglacial Relief Phenomena on Mount Vardenik (Southeastern Serbia). in Carpathian Journal of Earth and Environmental Sciences. 2023;18(1):127-138.
doi:10.26471/cjees/2023/018/246 .

Nešić, Dragan, Milinčić, Uroš V., Milinčić, Miroljub A., "Periglacial Relief Phenomena on Mount Vardenik (Southeastern Serbia)" in Carpathian Journal of Earth and Environmental Sciences, 18, no. 1 (2023):127-138,
https://doi.org/10.26471/cjees/2023/018/246 . .

TY  - JOUR
AU  - Nešić, Dragan
AU  - Milinčić, Uroš
PY  - 2019
UR  - https://gery.gef.bg.ac.rs/handle/123456789/976
AB  - The morphostructural relief of the highest parts of the central Kopaonik Mt was altered by exogenous agents, by denudation as a primary and periglacial processes as a secondary agent. Previous geomorphological studies were mostly focused on the traces of the Pleistocene glaciation, although no reliable evidence was found for this. Recent research, in the part of the mountain above 1,700 m of absolute height, points to geomorphological phenomena resulting from more recent processes within the periglacial environment. By means of geomorphological reconnaissance, analysis and mapping of the highest part of the Kopaonik mountain massif, forms of relief were studied, the ones that according to their morphology correspond to the periglacial forms and processes described in the conditions of high latitudes and high mountains. Determining the spatial coverage of the periglacial belt, especially its lower limit on Kopaonik Mt, is important for understanding the distribution of this climatic morphology both in Serbia and in South East Europe. The research contributes to one of the primary aims of exploring the concept of the periglacial zone, in terms of the regional distribution of its specific relief forms.
AB  - Morfostrukturni reljef najviših delova centralnog Kopaonika je izmenjen egzogenim agensima, dominantno denudacijom, a sekundarno i periglacijalnim procesima. Ranija geomorfološka istraživanja su najčešće bila usmerena na tragove pleistocene glacijacije, iako za to nisu nađeni pouzdani dokazi. Novija istraživanja, na delu planine iznad 1.700 m apsolutne visine upućuju na geomorfološke pojave koje su posledica recentnih procesa periglacijalne sredine. Postupkom geomorfološkog rekognosciranja, analiziranja i kartiranja najvišeg dela planinskog masiva Kopaonika tretirani su oblici reljefa koji prema svojoj morfologiji odgovaraju periglacijalnim oblicima i procesima opisanim u uslovima velikih geografskih širina i visokih planina. Determinisanje prostornog obuhvata periglacijalnog pojasa, posebno njegove donje granice na Kopaoniku, značajno je za poznavanje rasprostranjenja ove klimatogene morfologije kako u Srbiji tako i u Jugoistočnoj Evropi. Istraživanje predstavlja doprinos jednom od primarnih ciljeva istraživanja koncepta periglacijalne zone, u smislu regionalnog rasprostranjenja njenih specifičnih formi reljefa.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - The lower altitudinal limit of the periglacial climazonal belt on Kopaonik mountain (Serbia)
T1  - Donja granica periglacijalnog klimazonalnog pojasa na planini Kopaonik (Crbija)
VL  - 99
IS  - 1
SP  - 1
EP  - 18
DO  - 10.2298/GSGD1901001N
UR  - https://hdl.handle.net/21.15107/rcub_gery_976
ER  - 

@article{
author = "Nešić, Dragan and Milinčić, Uroš",
year = "2019",
abstract = "The morphostructural relief of the highest parts of the central Kopaonik Mt was altered by exogenous agents, by denudation as a primary and periglacial processes as a secondary agent. Previous geomorphological studies were mostly focused on the traces of the Pleistocene glaciation, although no reliable evidence was found for this. Recent research, in the part of the mountain above 1,700 m of absolute height, points to geomorphological phenomena resulting from more recent processes within the periglacial environment. By means of geomorphological reconnaissance, analysis and mapping of the highest part of the Kopaonik mountain massif, forms of relief were studied, the ones that according to their morphology correspond to the periglacial forms and processes described in the conditions of high latitudes and high mountains. Determining the spatial coverage of the periglacial belt, especially its lower limit on Kopaonik Mt, is important for understanding the distribution of this climatic morphology both in Serbia and in South East Europe. The research contributes to one of the primary aims of exploring the concept of the periglacial zone, in terms of the regional distribution of its specific relief forms., Morfostrukturni reljef najviših delova centralnog Kopaonika je izmenjen egzogenim agensima, dominantno denudacijom, a sekundarno i periglacijalnim procesima. Ranija geomorfološka istraživanja su najčešće bila usmerena na tragove pleistocene glacijacije, iako za to nisu nađeni pouzdani dokazi. Novija istraživanja, na delu planine iznad 1.700 m apsolutne visine upućuju na geomorfološke pojave koje su posledica recentnih procesa periglacijalne sredine. Postupkom geomorfološkog rekognosciranja, analiziranja i kartiranja najvišeg dela planinskog masiva Kopaonika tretirani su oblici reljefa koji prema svojoj morfologiji odgovaraju periglacijalnim oblicima i procesima opisanim u uslovima velikih geografskih širina i visokih planina. Determinisanje prostornog obuhvata periglacijalnog pojasa, posebno njegove donje granice na Kopaoniku, značajno je za poznavanje rasprostranjenja ove klimatogene morfologije kako u Srbiji tako i u Jugoistočnoj Evropi. Istraživanje predstavlja doprinos jednom od primarnih ciljeva istraživanja koncepta periglacijalne zone, u smislu regionalnog rasprostranjenja njenih specifičnih formi reljefa.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "The lower altitudinal limit of the periglacial climazonal belt on Kopaonik mountain (Serbia), Donja granica periglacijalnog klimazonalnog pojasa na planini Kopaonik (Crbija)",
volume = "99",
number = "1",
pages = "1-18",
doi = "10.2298/GSGD1901001N",
url = "https://hdl.handle.net/21.15107/rcub_gery_976"
}

Nešić, D.,& Milinčić, U.. (2019). The lower altitudinal limit of the periglacial climazonal belt on Kopaonik mountain (Serbia). in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 99(1), 1-18.
https://doi.org/10.2298/GSGD1901001N
https://hdl.handle.net/21.15107/rcub_gery_976

Nešić D, Milinčić U. The lower altitudinal limit of the periglacial climazonal belt on Kopaonik mountain (Serbia). in Glasnik Srpskog geografskog društva. 2019;99(1):1-18.
doi:10.2298/GSGD1901001N
https://hdl.handle.net/21.15107/rcub_gery_976 .

Nešić, Dragan, Milinčić, Uroš, "The lower altitudinal limit of the periglacial climazonal belt on Kopaonik mountain (Serbia)" in Glasnik Srpskog geografskog društva, 99, no. 1 (2019):1-18,
https://doi.org/10.2298/GSGD1901001N .,
https://hdl.handle.net/21.15107/rcub_gery_976 .

TY  - JOUR
AU  - Nešić, Dragan
AU  - Milinčić, Miroljub
AU  - Lukić, Bogdan
PY  - 2017
UR  - https://gery.gef.bg.ac.rs/handle/123456789/808
AB  - The paper deals with cryoplanation terraces on Kopaonik Mountain (2017m) which had been formed for the first time as a relict relief probably during the last glacial maximum (LGM) of Late Pleistocene. Four sites on the slopes of the southern and eastern exposure of the central part of the mountain range at the altitude between 1390 and 1910 m have been studied. Qualitative geomorphological research has dominated. Quantitative research has not been possible due to the properties of the relict formations and genetic inactivity of this relief, which is also typical for modern periglacial environments. Distinction of cryoplanation terraces on Kopaonik is important for understanding the distribution of this relict morphology both in Serbia and South East Europe. The research presents a contribution to one of the primary goals of the concept of cryoplanation in terms of regional distribution of cryoplanation relief.
PB  - Baia Mare : North University of Baia Mare
T2  - Carpathian Journal of Earth and Environmental Sciences
T1  - Relict cryoplanation terraces of central Kopaonik (Serbia)
VL  - 12
IS  - 1
SP  - 61
EP  - 68
UR  - https://hdl.handle.net/21.15107/rcub_gery_808
ER  - 

@article{
author = "Nešić, Dragan and Milinčić, Miroljub and Lukić, Bogdan",
year = "2017",
abstract = "The paper deals with cryoplanation terraces on Kopaonik Mountain (2017m) which had been formed for the first time as a relict relief probably during the last glacial maximum (LGM) of Late Pleistocene. Four sites on the slopes of the southern and eastern exposure of the central part of the mountain range at the altitude between 1390 and 1910 m have been studied. Qualitative geomorphological research has dominated. Quantitative research has not been possible due to the properties of the relict formations and genetic inactivity of this relief, which is also typical for modern periglacial environments. Distinction of cryoplanation terraces on Kopaonik is important for understanding the distribution of this relict morphology both in Serbia and South East Europe. The research presents a contribution to one of the primary goals of the concept of cryoplanation in terms of regional distribution of cryoplanation relief.",
publisher = "Baia Mare : North University of Baia Mare",
journal = "Carpathian Journal of Earth and Environmental Sciences",
title = "Relict cryoplanation terraces of central Kopaonik (Serbia)",
volume = "12",
number = "1",
pages = "61-68",
url = "https://hdl.handle.net/21.15107/rcub_gery_808"
}

Nešić, D., Milinčić, M.,& Lukić, B.. (2017). Relict cryoplanation terraces of central Kopaonik (Serbia). in Carpathian Journal of Earth and Environmental Sciences
Baia Mare : North University of Baia Mare., 12(1), 61-68.
https://hdl.handle.net/21.15107/rcub_gery_808

Nešić D, Milinčić M, Lukić B. Relict cryoplanation terraces of central Kopaonik (Serbia). in Carpathian Journal of Earth and Environmental Sciences. 2017;12(1):61-68.
https://hdl.handle.net/21.15107/rcub_gery_808 .

Nešić, Dragan, Milinčić, Miroljub, Lukić, Bogdan, "Relict cryoplanation terraces of central Kopaonik (Serbia)" in Carpathian Journal of Earth and Environmental Sciences, 12, no. 1 (2017):61-68,
https://hdl.handle.net/21.15107/rcub_gery_808 .

TY  - JOUR
AU  - Nešić, Dragan
AU  - Milinčić, Miroljub
PY  - 2004
UR  - https://gery.gef.bg.ac.rs/handle/123456789/91
AB  - In central area of Kopaonik (2017 m), in source parts of Samokovska, Velika and Duboka rivers, in altitude zone of more than 1770 m above the sea level specific appearance of landslides have been pronoticed. The characteristics of their positions, morphology, genesis, lithological attributes of landslides masses etc. are presented in this article. At present level of qualitative research process, these landslides are defined as specific phenomena of high mountain region of Kopaonik, which correspond to complex thermo-morphogenic landslides. The particular importance of the research of these landslides is in solving problems of the presence of glacial morphology and sediments in source area of Duboka, and their defining as shapes and appearances with colluviums genetic origin. One of the conclusions of this article is necessity of further research of these phenomena, as well.
AB  - Na centralnom delu Kopaonika (2017 m) u izvorišnim delovima Samokovske Velike i Duboke reke u visinskom pojasu iznad 1770 m n.v. konstatovane su specifične pojave klizišta. U radu su iznete odlike njihovih položaja morfologije, geneze, litološka svojstva kliznih masa i drugo. Na sadašnjem nivou kvalitativnog istraživačkog postupka ova klizišta su definisana kao specifične pojave visokoplaninskog regiona Kopaonika koje odgovaraju složenim termogeno-morfogenim klizištima. Poseban značaj istraživanja ovih klizišta je u rešavanju problema zastupljenosti glacijalne morfologije i sedimenata u izvorištu Duboke, sa njihovim definisanjem kao oblika i pojava koluvijalnog genetskog porekla. Jedan od zaključaka rada je i potreba daljih proučavanja ovih pojava.
PB  - Zavod za zaštitu prirode, Beograd
T2  - Zaštita prirode
T1  - The specifics of high-mountain landslides in example of NP Kopaonik
T1  - Specifičnosti visokoplaninskih klizišta na primeru NP Kopaonik
VL  - 55
IS  - 1-2
SP  - 5
EP  - 14
UR  - https://hdl.handle.net/21.15107/rcub_gery_91
ER  - 

@article{
author = "Nešić, Dragan and Milinčić, Miroljub",
year = "2004",
abstract = "In central area of Kopaonik (2017 m), in source parts of Samokovska, Velika and Duboka rivers, in altitude zone of more than 1770 m above the sea level specific appearance of landslides have been pronoticed. The characteristics of their positions, morphology, genesis, lithological attributes of landslides masses etc. are presented in this article. At present level of qualitative research process, these landslides are defined as specific phenomena of high mountain region of Kopaonik, which correspond to complex thermo-morphogenic landslides. The particular importance of the research of these landslides is in solving problems of the presence of glacial morphology and sediments in source area of Duboka, and their defining as shapes and appearances with colluviums genetic origin. One of the conclusions of this article is necessity of further research of these phenomena, as well., Na centralnom delu Kopaonika (2017 m) u izvorišnim delovima Samokovske Velike i Duboke reke u visinskom pojasu iznad 1770 m n.v. konstatovane su specifične pojave klizišta. U radu su iznete odlike njihovih položaja morfologije, geneze, litološka svojstva kliznih masa i drugo. Na sadašnjem nivou kvalitativnog istraživačkog postupka ova klizišta su definisana kao specifične pojave visokoplaninskog regiona Kopaonika koje odgovaraju složenim termogeno-morfogenim klizištima. Poseban značaj istraživanja ovih klizišta je u rešavanju problema zastupljenosti glacijalne morfologije i sedimenata u izvorištu Duboke, sa njihovim definisanjem kao oblika i pojava koluvijalnog genetskog porekla. Jedan od zaključaka rada je i potreba daljih proučavanja ovih pojava.",
publisher = "Zavod za zaštitu prirode, Beograd",
journal = "Zaštita prirode",
title = "The specifics of high-mountain landslides in example of NP Kopaonik, Specifičnosti visokoplaninskih klizišta na primeru NP Kopaonik",
volume = "55",
number = "1-2",
pages = "5-14",
url = "https://hdl.handle.net/21.15107/rcub_gery_91"
}

Nešić, D.,& Milinčić, M.. (2004). The specifics of high-mountain landslides in example of NP Kopaonik. in Zaštita prirode
Zavod za zaštitu prirode, Beograd., 55(1-2), 5-14.
https://hdl.handle.net/21.15107/rcub_gery_91

Nešić D, Milinčić M. The specifics of high-mountain landslides in example of NP Kopaonik. in Zaštita prirode. 2004;55(1-2):5-14.
https://hdl.handle.net/21.15107/rcub_gery_91 .

Nešić, Dragan, Milinčić, Miroljub, "The specifics of high-mountain landslides in example of NP Kopaonik" in Zaštita prirode, 55, no. 1-2 (2004):5-14,
https://hdl.handle.net/21.15107/rcub_gery_91 .