The study propound the results of the authors' investigations about the morphostructure of the Rila-Pirin Mountains Range. Here are analyzed morphological characteristics of positive regional landforms as a real criterion of the nature and evolution of its morphogenesis. For this purpose were studied and compared species, morphological traits, spatial dimensions, vertical displacement and relationships between the morphographic units within the research area. Conducting of such research in the future would be an important criterion for assessing of the near-surface lithospheric geodynamic processes and trends in the changes to the local relief.
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