Plitvice Lakes National Park of Croatia

Plitvice Lakes National Park

Land of Falling Lakes

Plitvice Lakes National Park holds a plan of phenomenal lakes, clasps and waterfalls. These have been molded by methods common of karst scenes, for instance the testimony of travertine controls, making trademark dams. These land procedures continue today. 

See the Land of falling Lakes

The Plitvice Lakes dish is a geomorphologic station of regular origin, a karst conduit bowl of limestone and dolomite, with give or take 20 lakes, put forth by the expression of calcium carbonate heartened in water through the conglomeration of greenery, green development and land and water proficient minute living beings. These make odd, trademark shapes and hold travertine-roofed and vaulted hollows. The carbonates date from the Upper Trias, Juras and Cretaceous Ages and are needy upon 4,000 m thick. With a particular final objective to keep up and spare the regular parts of the lakes, the whole of surface and the lion's share of the subterranean waste skeleton must be grasped by increasing the authoritative edge of the diversion focus. The new domains include layers of karstified limestone with dolomites of Jurassic age. 

Plitvice Lake in Winters

Lake in winter

Same Area of Lake

in Summer

There are 16 interlinked lakes between Mala Kapela Mountain and Pljesevica Mountain. The lake structure is disengaged into the upper and more level lakes: the upper lakes lie in a dolomite valley and are incorporated by thick woodlands and interlinked by different waterfalls; the more level lakes, more unobtrusive and shallower, lie on the limestone bedrock and are enveloped simply by lacking underbrush.

Same Area of Lake

in Winter

The upper lakes are separated by dolomite restrictions, which advance with the forming of travertine, organizing appropriately travertine obstacles. Travertine is fundamentally organized on the spots where water tumbles from a stature, by the incrustation of green development and greenery with calcium carbonate. The more level lakes were surrounded by dividing and caving in of the vaults above subterranean pits through which water of the upper lakes vanished. 

Canoeing 1

Canoeing 2

The timberland, that includes impeccable stands of beech at simpler rises and mixed stands of beech and fir at additional hoisted measures, can similarly be amassed noticing underlying strata of dolomite and limestone edifices. The dolomite assemblies typify tertiary pine, hornbeam, spruce and beech-fir boondocks. The limestone gatherings have a tinier number of woodland sorts yet front a greater extend with neighborhoods of spruce and plant, spruce in beech, coppiced hornbeam with sumac, maple and heather. Hydrophytic neighborhoods of dull birch, light dark ivy, willow, reeds and bulrush neighborhoods are revealed. There are an extensive mosaic of meadow neighborhoods, dependent upon stature, geology soils and other characteristic segments. The locale is fauna-rich, consolidating European tan bear, wolf, hawk owl and capercaillie. There are records of 126 sorts of winged creature, of which 70 breed. 

Canoeing 3