Soil processes in rendzinas are primarily influenced by the calcareous bedrock, which constitutes the soil substrate. In sloping terrain, these processes are further modified by slope denudation and colluvial deposition, involving the erosion of convex slope sections and the deposition of solimovic materials in concave areas and at the base of the slope. This dynamic shapes both the slope's geomorphological profile and the associated soil development. Four soil profiles were analyzed in the southern Beskid Foothills near Prešov, Slovakia, along a 500-meter east-facing slope with a 67-meter elevation difference. Specific sampling locations included a flat hilltop, a convex slope section, a transition zone from convex to concave slope, and the slope base. Under agricultural cultivation, a deep, skeletic, Calcaric Cambic Leptosol was developed on the flat hilltop. On the 11° inclined convex slope section, a 25-cm-thick arable-humus Ap horizon directly overlies solid rock, resulting in a skeletic Rendzic Leptosol. At the slope base, Endogleyic Cambisol was developed from non-skeletic solimovic deposits. The top-down decalcification of detritus, accompanied by the emergence of low hydrolytic acidity, was observed in the slope soils. The sorption complex exhibited a high degree of saturation with alkaline cations, exceeding 93.7%, with calcium being the dominant cation. Notably, exchangeable sodium accounted for approximately 10% of the cation-exchange capacity (CEC). A distinctive characteristic of the soils within this transect was their high total iron content, ranging from 1.82 to 4.50 % Fe, contributing to the red coloration (2.5 YR).