Reconstruction of the pleistocene glaciers of Mt. Durmitor in Montenegro
Mount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Throughout the Pleistocene there were many glaciers there, which descended to adjacent karst plateau. Types of glaciers, their number and direction of moving were mostly affected by geological structure...
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Format: | Article |
Language: | English |
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ZRC SAZU, Založba ZRC
2009-12-01
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Series: | Acta Geographica Slovenica |
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Online Access: | https://ojs.zrc-sazu.si/ags/article/view/1286 |
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author | Predrag Djurović |
author_facet | Predrag Djurović |
author_sort | Predrag Djurović |
collection | DOAJ |
description | Mount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Throughout the Pleistocene there were many glaciers there, which descended to adjacent karst plateau. Types of glaciers, their number and direction of moving were mostly affected by geological structure (carbonate basis) and pre-glacial relief (karst and fluvial relief). During two phases of intensive glaciation, the surface that had been seized by glacial changes also changed. Over 54% of the surface of Durmitor was exposed to the glacial process of the stronger phase and about 36% of the weaker phase. Cirque type of glaciation dominated the third phase. |
first_indexed | 2024-04-12T07:01:18Z |
format | Article |
id | doaj.art-bf835eb419974d16818fe97f352bf821 |
institution | Directory Open Access Journal |
issn | 1581-6613 1581-8314 |
language | English |
last_indexed | 2024-04-12T07:01:18Z |
publishDate | 2009-12-01 |
publisher | ZRC SAZU, Založba ZRC |
record_format | Article |
series | Acta Geographica Slovenica |
spelling | doaj.art-bf835eb419974d16818fe97f352bf8212022-12-22T03:43:00ZengZRC SAZU, Založba ZRCActa Geographica Slovenica1581-66131581-83142009-12-0149226328910.3986/AGS492021011Reconstruction of the pleistocene glaciers of Mt. Durmitor in MontenegroPredrag DjurovićMount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Throughout the Pleistocene there were many glaciers there, which descended to adjacent karst plateau. Types of glaciers, their number and direction of moving were mostly affected by geological structure (carbonate basis) and pre-glacial relief (karst and fluvial relief). During two phases of intensive glaciation, the surface that had been seized by glacial changes also changed. Over 54% of the surface of Durmitor was exposed to the glacial process of the stronger phase and about 36% of the weaker phase. Cirque type of glaciation dominated the third phase.https://ojs.zrc-sazu.si/ags/article/view/1286geographyglaciationglacier reconstructionpleistocenedurmitordinaric mountainsmontenegro |
spellingShingle | Predrag Djurović Reconstruction of the pleistocene glaciers of Mt. Durmitor in Montenegro Acta Geographica Slovenica geography glaciation glacier reconstruction pleistocene durmitor dinaric mountains montenegro |
title | Reconstruction of the pleistocene glaciers of Mt. Durmitor in Montenegro |
title_full | Reconstruction of the pleistocene glaciers of Mt. Durmitor in Montenegro |
title_fullStr | Reconstruction of the pleistocene glaciers of Mt. Durmitor in Montenegro |
title_full_unstemmed | Reconstruction of the pleistocene glaciers of Mt. Durmitor in Montenegro |
title_short | Reconstruction of the pleistocene glaciers of Mt. Durmitor in Montenegro |
title_sort | reconstruction of the pleistocene glaciers of mt durmitor in montenegro |
topic | geography glaciation glacier reconstruction pleistocene durmitor dinaric mountains montenegro |
url | https://ojs.zrc-sazu.si/ags/article/view/1286 |
work_keys_str_mv | AT predragdjurovic reconstructionofthepleistoceneglaciersofmtdurmitorinmontenegro |