Abstract
The morphologic configuration of the P aglajhora slump valley is controlled by geologic structure and remodelled by the hydro-geomorphic processes. The slope forms exhibit a com- bination of convex - concave - irregular profiles with highly variable inclination (10° to 35°). Overland flow feeding the uppermost niche during heavy rains transformed into concentrated sub-surface flow over the permeable colluvium. The observed rills and cracks facilitate the piping and deep drainage towards the slumped areas. The high intensity of the processes as well as the relative heights and steep gradients are the limiting factors in the stabilization of the Paglajhora slumps. At present, the form reached quasi-unstable equilibrium. Each extreme rainfall (above 300 mm/day) causes substantial changes in its morphology.
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