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The specifics of high-mountain landslides in example of NP Kopaonik

Specifičnosti visokoplaninskih klizišta na primeru NP Kopaonik

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Nešić, Dragan
Milinčić, Miroljub
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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.
Keywords:
relief / sloping ground process / landslide / sediments / reljef / padinski proces / klizište / koluvijum / sedimenti
Source:
Zaštita prirode, 2004, 55, 1-2, 5-14
Publisher:
  • Zavod za zaštitu prirode, Beograd

ISSN: 0514-5899

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URI
https://gery.gef.bg.ac.rs/handle/123456789/91
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  • Radovi istraživača
Institution/Community
Geografski fakultet
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  - conv_623
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 = "conv_623"
}
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.
conv_623
Nešić D, Milinčić M. The specifics of high-mountain landslides in example of NP Kopaonik. in Zaštita prirode. 2004;55(1-2):5-14.
conv_623 .
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,
conv_623 .

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