标题：FEATURES OF THE RELIEF FRAGMENTATION WITHIN THE BLAHNIŢA BASIN.
THE PIEDMONT SECTOR
CARACTERISTICI ALE FRAGMENTĂRII RELIEFULUI ÎN BAZINUL BLAHNIŢEI. SECTORUL PIEMONTAN
摘要：The piedmont sector of the Blahniţa basin presents a longitudinal location, a character of subsequent valley and an asymmetrical shape. Most of the basin surface is represented by slopes developed on sedimentary detritic rocks, with high friability, which makes the modeling processes present a wide range of action ways and different intensities.
The values of the drainage density characteristic to the piedmont basin of the Blahniţa oscillate between 0 and 6.61 km/sq km, which resembles to the values specific to the Bălăciţa Piedmont, overall. The relief intensity registers the highest values, 145 m, in the Eastern side of the basin, while the lowest values, 15 m, can be noticed downstream the settlement of Livezile, where the Blahniţa enters the plain. From the correlation energy – density, it resulted a determination coefficient of 9.16% and an unexplained variation of 90.84%.
关键词：drainage density, relief intensity, drainage density - relief intensity correlation, the Blahniţa.
