The Babia Góra ridge (Outer Western Carpathians) exhibits one of the most complex landslide relief in the Carpathians. The aim of this research was to create a new interpretation of the Babia Góra range morphology, using the combined LiDAR data analysis, field mapping and the Schmidt hammer relative age dating. The general approach consisted of generation and automatic analysis of high-resolution DEM, interpretation of DTM-derived maps, manual vectorization of landforms and identification of ambiguous locations, in-situ investigation and Schmidt-hammer measurements, and completion of geomorphological data for the Babia Góra ridge. As a result, two generations of glaciofluvial levels were distinguished at the foothills of Diablak and Cyl, and for the first time three flow-like landforms were recognized at the foothills of the Sokolica peak. Above them the colluvial covers were located that formed two altitudinal complexes of landslide covers. In the uppermost Babia Góra slope section, the dominant features were sliding landforms, partially shaped by glacial and periglacial processes and debris flows activity.