摘要：A relief that is strongly modelled by
extensive erosion processes (sheet erosion, rills and
gullies) characterizes the Alpine level of the Bucegi
Mountains. All processes are favoured by the geological
structure represented by conglomerates, limestone with
grit stone intrusions, by strongly degraded podzolic soils
with a loamy-sandy texture in the first layer and by
some economic activities, such as the overgrazing and
the tourism.
We have identified an area with large-scale erosion
forms in the sector comprised between Furnica Peak and
Piatra Arsă Peak.
This paper analyses the genesis and the manifestation
conditions of the erosion processes, as well as the
climate, making use of the temperature and the
precipitation data provided by the meteorological
stations in the region.
Using the Péltier diagram, we framed the region to
various seasons. By subsequently using the Péguy
diagram, we framed the region to the morphoclimatic
conditions and to the river processes. On the other hand,
by using GIS, we created geology, slope, soil and
vegetation Boolean maps and then the risk map to the
erosion processes.
