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The lower altitudinal limit of the periglacial climazonal belt on Kopaonik Mountain (Serbia)

The morphostructural relief of the highest parts of the central Kopaonik Mt
 was altered by exogenous agents, by denudation as a primary and periglacial
 processes as a secondary agent. Previous geomorphological studies were
 mostly focused on the traces of the Pleistocene glaciation, although no
 reliable evidence was found for this. Recent research, in the part of the
 mountain above 1,700 m of absolute height, points to geomorphological
 phenomena resulting from more recent processes within the periglacial
 environment. By means of geomorphological reconnaissance, analysis and
 mapping of the highest part of the Kopaonik mountain massif, forms of relief
 were studied, the ones that according to their morphology correspond to the
 periglacial forms and processes described in the conditions of high
 latitudes and high mountains. Determining the spatial coverage of the
 periglacial belt, especially its lower limit on Kopaonik Mt, is important
 for understan-ding the distribution of this climatic morphology both in
 Serbia and in South East Europe. The research contributes to one of the
 primary aims of exploring the concept of the periglacial zone, in terms of
 the regional distribution of its specific relief forms.