Fig. 5 | Scientific Reports

Fig. 5

From: Development and optimization of a morphodiversity model for mountainous areas using supervised classification and artificial neural networks

Fig. 5

Geological cross-section of the Pieniny Klippen Belt along the Kraków–Zakopane transect (located approximately 10 km west of the study area). After Birkenmajer82, simplified. Outer Carpathian units: 1—Grajcarek Unit (Jurassic–Maastrichtian); 2—Cenomanian–Maastrichtian; 3—Paleogene. Pieniny Klippen Belt units: 4—Czorsztyn Unit (Jurassic–Lower Cretaceous); 5—Czorsztyn and Niedzica units (?) (incompetent Upper Cretaceous marls and flysch-like rocks); 6—Branisko and Pieniny units; 7—Jarmuta Formation (Maastrichtian molasse and flysch); 8—Maruszyna Thrust Sheet (Upper Santonian–Middle Eocene). Inner Carpathian units: 9—basal conglomerate (Sulov Conglomerate) and nummulitic limestone (Paleogene); 10—Zakopane Formation (Paleogene flysch). Orava–Nowy Targ Basin: 11—Neogene and Quaternary deposits.

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