![]() ![]() ![]() ![]() This paper focuses on the explanation of hydrogeological relations in the zone where losses of water occur in the riverbed, relationship to the neighbouring Una River catchment, as well as possibilities of relocating the source of water supply from the Kozjak Lake (Plitvice Lakes) to the new site in the sinking zone of the Korana River. The sinking zone in that area is built of high permeable carbonate rocks and with the appearance of less permeable dolomite rocks, about 17 km downstream, the Korana River becomes a permanent river. A few hundred meters downstream of the source zone, during the summer dry periods, there are losses of water in the riverbed resulting in its total drying. 1 COBISS: 1.02 Hydrogeology of the sinking zone of the Korana River downstream of the Plitvice Lakes, Croatia Hidrogeologija ponornega območja reke Korane dolvodno od Plitviških jezer, Hrvaška Ranko Biondić 1, Hrvoje Meaški 1 & Božidar Biondić 1 Abstract UDC 556.3(497.56) Ranko Biondić, Hrvoje Meaški & Božidar Biondić: Hydrogeology of the sinking zone of the Korana River downstream of the Plitvice Lakes, Croatia Downstream of the Plitvice Lakes National Park, water that pass through the water system of the lakes begins its flow as the Korana River. ![]()
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