A Reconstruction of the Pleistocene Glacial Maximum in the Žijovo Range (Prokletije Mountains, Montenegro)
DOI:
https://doi.org/10.3986/AGS54202Ključne besede:
geography, glaciations, glacier reconstruction, Pleistocene, Žijovo Range, Prokletije Mountains, MontenegroPovzetek
The Žijovo Range belongs to the Prokletije Mountains of Montenegro and is located in the extreme southeast, on the border with Albania. Glacial processes were intensively active in this range during the Pleistocene. This is indicated by erosive and accumulative glacial features of relief that have been preserved due to the favorable geologic structure. The glacial maximum in the Žijovo Range is characterized by a unique glacier on the entire area of the range. Preglacial relief prevented the formation of a typical icecap glacier. Due to drainage of the central glacial mass in the direction of the preglacial valleys, there was a transection glacier in the central, northern, and northwestern parts, and an icefield glacier in the eastern and southeastern parts of the Žijovo Range. These glaciers covered an area of 180 km during the glacial maximum.
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Literatura
Benn, D. I., Evans, D. J. A. 1998: Glaciers and Glaciation. London.
Blott, S. J., Pye, K. 2001: Gradistat: A grain size distribution and statistics package for the analysis of unconsolidated sediments. Earth surface processes and landforms 26-11. DOI: http://dx.doi.org/10.1002/esp.261
Correggiari, A., Roveri, M., Tricardi, F. 1996: Late Plaistocene and Holocene evolution of the north Adriatic Sea. Il Quaternario 9-2. DOI: http://dx.doi.org/10.1016/0025-3227(79)90130-0
Cvijić, J. 1899: Glacijalne i morfološke studije o planinama Bosne, Hercegovine i Crne Gore. Glas Srpske kraljevske akademije 57.
Cvijić, J. 1903: Novi rezultati o glacijalnoj eposi Balkanskog poluostrva. Glasnik Srpske kraljevske akademije nauka 65.
Cvijić, J. 1913: Ledeno doba u Prokletijama i okolnim planinama. Glas Srpske kraljevske akademije nauka 91.
Djokić, V., Živaljević, M., Petrović, Z. 1968: Tumać za osnovnu geološku kartu Gusinje (1 : 100,000). Beograd.
Djurović, P. 1996: Visokoplaninski kras Durmitora – geomorfološka studija. Ph. D. thesis. Geografski fakultet Univerziteta u Beogradu. Beograd.
Djurović, P., Petrović, A. S. 2007: Large canyons in Dinaric and Prokletije mountain regions of Montenegro. Geographica Pannonica 11.
Djurović, P. 2009: Reconstruction of Pleistocene glaciers of Mount Durmitor in Montenegro. Acta Geographica Slovenica 49-2. DOI: http://dx.doi.org/10.3986/AGS49202
Djurović, P., Petrović, A. S., Simić, S. 2010: The overall impact of Pleistocene glaciation on morphological diversity of uvalas at Durmitor and Žijovo. Glasnik Srpskog geografskog društva 90-1. DOI: http://dx.doi.org/10.2298/GSGD1001017D
Flint, R. F. 1971: Glacial and Quaternary geology. New York.
Hassert, K. 1901: Gletscherspuren in Montenegro. Vortrag gehalten auf dem XIII. Deutschen Geographentag, Brelau.
Hubbard, B., Glasser, N. 2005: Field technique in glaciology and glacial geomorphology. Chichester.
Hughes, P. D., Gibbard, P. L., Woodward, J. C. 2005: Quaternary glacial records in mountain regions: A formal stratigraphical approach. Episodes 28-2.
Hughes, P. D., Woodward, J. C., Gibbard, P. L. 2006: Quaternary glacial history of the Mediterranean mountains. Progress in physical geography 30. DOI: http://dx.doi.org/10.1191/0309133306pp481ra
Hughes, P. D., Gibbard, P. L., Woodward, J. C. 2007: Geological controls on Pleistocene glaciations and cirque form in Greece. Geomorphology 88. DOI: http://dx.doi.org/10.1016/j.geomorph.2006.11.008
Hughes, P. D., Woodward, J. C., van Calsteren, P. C., Thomas, L. E., Adamson, L. E. 2010: Pleistocene ice caps on the coastal mountains of the Adriatic Sea. Quaternary science reviews 29. DOI: http://dx.doi.org/101.1016/j.quascirev.2010.06.032
Kuhlemann, J., Milivojević, M., Krumrei, I., Kubik, P. W. 2009: Last glaciations of Šara range (Balkan peninsula): increasing dryness from the LGM to the Holocene. Austrian journal of Earth science 102.
Martelli, A. 1908: Studio geologico sul Montenegro sud-orientale e littoraneo. Memorie della R. Accademia dei Lincei. Classe di scienze fisiche, matematiche e naturali 6.
Meierding, T. C. 1982: Late pleistocene glacial equilibrium-line altitudes in the Colorado Front Range: A comparison of methods. Quaternary research 18-3. DOI: http://dx.doi.org/10.1016/00335894(82)90076-X
Milivojević, M. 2004: Glacijalna morfologija Komova. Glasnik Srpskog Geografskog Društva 84-2.
Milivojević, M., Menković, Lj., Ćalić, J. 2008: Pleistocene glacial relief of the central part of Mt. Prokletije (Albanian Alps). Quaternary international 190. DOI: http://dx.doi.org/10.1016/j.quaint.2008.04.006
Petrović, A. S. 2007: Pleistocena glacijacija gornjeg toka Veruše. Zbornik radova Geografskog fakulteta Univerziteta u Beogradu 55.
Petrović, A. S. 2009: Pleistoceni glacijalni reljef Žijova. M. Sc. thesis, Univerziteta u Beogradu, Geografski fakultet, Beograd.
Porter, S. C. 2001: Snowline depression in the tropics during the last glaciation. Quaternary science reviews 20-10. DOI: http://dx.doi.org/10.1016/S0277-3791(00)00178-5
Stepišnik, U., Ferk, M., Kodelja, B., Medenjak, G., Mihevc, A., Natek, K., Žebre, M. 2010: Glaciokras of western Orjen, Montenegro. Cave and karst science 36-1.
Stepišnik, U. and Žebre, M. 2011: Glaciokras Lovčena. E-GeograFF 2. Ljubljana.
Vinassa de Regny, P. 1901: Tracce glaciali net Montenegro. Reale accademia del Lincei 10. Roma.
Vojnogeografski institut, 1982. Orto-foto snimci Žijova 1 : 50,000. Beograd.
Živaljević, M., Đokić, V., Pajović, M. 1967: Tumač za osnovnu geološku kartu Titograd (1 : 100,000). Beograd.
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