Glacial morphology of the Šara Mountains

The paper defines and presents the forms of glacial relief formed, most likely, during the last Pleistocene glacial maximum (LGM). A graphic and textual presentation of almost all glacial forms is given on the entire territory of the Šara Mountains, on both sides of their main ridge, from...

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Main Authors: Menković Ljubomir, Milivojević Milovan
Format: Article
Language:English
Published: Serbian Geographical Society 2021-01-01
Series:Glasnik Srpskog Geografskog Društva
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/0350-3593/2021/0350-35932101001M.pdf
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author Menković Ljubomir
Milivojević Milovan
author_facet Menković Ljubomir
Milivojević Milovan
author_sort Menković Ljubomir
collection DOAJ
description The paper defines and presents the forms of glacial relief formed, most likely, during the last Pleistocene glacial maximum (LGM). A graphic and textual presentation of almost all glacial forms is given on the entire territory of the Šara Mountains, on both sides of their main ridge, from Ljuboten in the NE to the source tributaries of the Radika River in the SW. Based on the height position and spatial development of glacial forms, the height of the snow line (ELA) was determined, glacier types were determined and defined, which is shown on two overview maps representing Pleistocene glacial morphology and reconstructed Pleistocene glaciers referring to the last Pleistocene glacial (MIS-2). Since these are the youngest glacial morphological traces on the Šara Mountains, they are the best preserved today.
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spelling doaj.art-d90ff4af20234787a59ee7f56ae057d92022-12-21T22:28:45ZengSerbian Geographical SocietyGlasnik Srpskog Geografskog Društva0350-35932406-078X2021-01-01101112910.2298/GSGD2101001M0350-35932101001MGlacial morphology of the Šara MountainsMenković Ljubomir0Milivojević Milovan1Geographical Institute "Jovan Cvijić", SASA, Belgrade, SerbiaGeographical Institute "Jovan Cvijić", SASA, Belgrade, SerbiaThe paper defines and presents the forms of glacial relief formed, most likely, during the last Pleistocene glacial maximum (LGM). A graphic and textual presentation of almost all glacial forms is given on the entire territory of the Šara Mountains, on both sides of their main ridge, from Ljuboten in the NE to the source tributaries of the Radika River in the SW. Based on the height position and spatial development of glacial forms, the height of the snow line (ELA) was determined, glacier types were determined and defined, which is shown on two overview maps representing Pleistocene glacial morphology and reconstructed Pleistocene glaciers referring to the last Pleistocene glacial (MIS-2). Since these are the youngest glacial morphological traces on the Šara Mountains, they are the best preserved today.http://www.doiserbia.nb.rs/img/doi/0350-3593/2021/0350-35932101001M.pdfthe šara mountainstypes of glacierscirquesglacial valleysmoraines
spellingShingle Menković Ljubomir
Milivojević Milovan
Glacial morphology of the Šara Mountains
Glasnik Srpskog Geografskog Društva
the šara mountains
types of glaciers
cirques
glacial valleys
moraines
title Glacial morphology of the Šara Mountains
title_full Glacial morphology of the Šara Mountains
title_fullStr Glacial morphology of the Šara Mountains
title_full_unstemmed Glacial morphology of the Šara Mountains
title_short Glacial morphology of the Šara Mountains
title_sort glacial morphology of the sara mountains
topic the šara mountains
types of glaciers
cirques
glacial valleys
moraines
url http://www.doiserbia.nb.rs/img/doi/0350-3593/2021/0350-35932101001M.pdf
work_keys_str_mv AT menkovicljubomir glacialmorphologyofthesaramountains
AT milivojevicmilovan glacialmorphologyofthesaramountains