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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Main Author: Predrag Djurović
Format: Article
Language:English
Published: ZRC SAZU, Založba ZRC 2009-12-01
Series:Acta Geographica Slovenica
Subjects:
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.
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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