The paper presents the glacial relief on Mt. Komovi in Montenegro. The most common are the macro-glacial forms, which are the best preserved - cirques and moraines. By the analysis of topographic maps and survey in the field the situation, orientation and morphometric data on these forms are given. The analysis of impact of exposures on the cirque bottom elevation is given. Furthermore, the level of preservation of glacial relief forms, depending on geological settings, is analyzed. Finally, there is the reconstruction of Pleistocene snow line elevation and spread of glaciations
Identification of the remnant traces of paleo-glaciers provides important proxies to understand the ...
Glaciokarst is a landscape which combines karst features and hydrology as well as inherited glacial ...
The area of the eastern Kamnik-Savinja Alps was glaciated in the time of the Last Pleistocene Glacia...
There are several amphitheatrical valley heads in the Hrubý Jeseník mountains. Velká kotlina is situ...
The submitted diploma thesis is concerned with the geomorphological analysis of specific landforms i...
Although glacial landforms on the Balkan Peninsula have been studied since the 19th century, only sc...
The Žijovo Range belongs to the Prokletije Mountains of Montenegro and is located in the extreme sou...
Despite the large variability of landforms in Montenegro, no attempts have yet been made to regional...
U ovome radu analiziran je glacijalni reljef planine Šator u Bosni i Hercegovini. Takav reljef nasta...
The Zijovo Range belongs to the Prokletije Mountains of Montenegro and is located in the extreme sou...
The area of the Risnjak mountain massif is a submorphological region - part of the mesomorphological...
Mount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Th...
The paper deals with cryoplanation terraces on Kopaonik Mountain (2017m) which had been formed for t...
Mount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Th...
<div><p>The geomorphological map of the northeastern Durmitor Mountains and the plateau Jezerska Pov...
Identification of the remnant traces of paleo-glaciers provides important proxies to understand the ...
Glaciokarst is a landscape which combines karst features and hydrology as well as inherited glacial ...
The area of the eastern Kamnik-Savinja Alps was glaciated in the time of the Last Pleistocene Glacia...
There are several amphitheatrical valley heads in the Hrubý Jeseník mountains. Velká kotlina is situ...
The submitted diploma thesis is concerned with the geomorphological analysis of specific landforms i...
Although glacial landforms on the Balkan Peninsula have been studied since the 19th century, only sc...
The Žijovo Range belongs to the Prokletije Mountains of Montenegro and is located in the extreme sou...
Despite the large variability of landforms in Montenegro, no attempts have yet been made to regional...
U ovome radu analiziran je glacijalni reljef planine Šator u Bosni i Hercegovini. Takav reljef nasta...
The Zijovo Range belongs to the Prokletije Mountains of Montenegro and is located in the extreme sou...
The area of the Risnjak mountain massif is a submorphological region - part of the mesomorphological...
Mount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Th...
The paper deals with cryoplanation terraces on Kopaonik Mountain (2017m) which had been formed for t...
Mount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Th...
<div><p>The geomorphological map of the northeastern Durmitor Mountains and the plateau Jezerska Pov...
Identification of the remnant traces of paleo-glaciers provides important proxies to understand the ...
Glaciokarst is a landscape which combines karst features and hydrology as well as inherited glacial ...
The area of the eastern Kamnik-Savinja Alps was glaciated in the time of the Last Pleistocene Glacia...