Glacial morphology of the Sara Mountains

The paper defines and presents the forms of glacial relief formed, most likely, during the last Pleistocene glacial maximum (LGM). A graphic and textual presentation of almost all glacial forms is given on the entire territory of the Sara Mountains, on both sides of their main ridge, from Ljuboten in the NE to the source tributaries of the Radika River in the SW. Based on the height position and spatial development of glacial forms, the height of the snow line (ELA) was determined, glacier types were determined and defined, which is shown on two overview maps representing Pleistocene glacial morphology and reconstructed Pleistocene glaciers referring to the last Pleistocene glacial (MIS-2). Since these are the youngest glacial morphological traces on the Sara Mountains, they are the best preserved today.