Soil Resources of Interfluve Garda Seaca-Ordancusa from the Apuseni Mountains…

Pedogenetic conditions of interfluve Garda Seaca - Ordancusa northern part of the Bihor Massif in the Apuseni Mountains are characterized by a less complex geological constitution, the largest share (80%) having limestone (white and black) and dolomites, which became material support of morphogenesis and pedogenesis. Physiognomy current territory is due to the coexistence of lithologic and hydr…