The specifics of high-mountain landslides in example of NP Kopaonik
Specifičnosti visokoplaninskih klizišta na primeru NP Kopaonik
Апстракт
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.
Кључне речи:
relief / sloping ground process / landslide / sediments / reljef / padinski proces / klizište / koluvijum / sedimentiИзвор:
Zaštita prirode, 2004, 55, 1-2, 5-14Издавач:
- Zavod za zaštitu prirode, Beograd
Колекције
Институција/група
Geografski fakultetTY - 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 .