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 |
| Summary: | 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. |
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| ISSN: | 1581-6613 1581-8314 |