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.
TY - JOUR
AU - Đurović, Predrag
PY - 2009
UR - https://gery.gef.bg.ac.rs/handle/123456789/296
AB - 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.
PB - Geografski Inst Antona Melika Zrc Sazu, Ljubljana
T2 - Acta Geographica Slovenica - Geografski zbornik
T1 - Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro
VL - 49
IS - 2
SP - 263
EP - 279
DO - 10.3986/AGS49202
UR - conv_823
ER -
@article{
author = "Đurović, Predrag",
year = "2009",
abstract = "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.",
publisher = "Geografski Inst Antona Melika Zrc Sazu, Ljubljana",
journal = "Acta Geographica Slovenica - Geografski zbornik",
title = "Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro",
volume = "49",
number = "2",
pages = "263-279",
doi = "10.3986/AGS49202",
url = "conv_823"
}
Đurović, P.. (2009). Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro. in Acta Geographica Slovenica - Geografski zbornik
Geografski Inst Antona Melika Zrc Sazu, Ljubljana., 49(2), 263-279.
https://doi.org/10.3986/AGS49202
conv_823
Đurović P. Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro. in Acta Geographica Slovenica - Geografski zbornik. 2009;49(2):263-279.
doi:10.3986/AGS49202
conv_823 .
Đurović, Predrag, "Reconstruction of the pleistocene glaciers of mount Durmitor in Montenegro" in Acta Geographica Slovenica - Geografski zbornik, 49, no. 2 (2009):263-279,
https://doi.org/10.3986/AGS49202 .,
conv_823 .
