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According to UNESCO: Plitvice Lakes National Park contains a series of beautiful lakes, caves and waterfalls. These have been formed by processes typical of karst landscapes such as the deposition of travertine barriers, creating natural dams. These geological processes continue today.
The Plitvice Lakes basin has approximately 20 lakes, created by the deposition of calcium carbonate precipitated in water through the agency of moss, algae and aquatic bacteria. These create strange, characteristic shapes and contain travertine-roofed and vaulted caves.
There are 16 interlinked lakes between Mala Kapela Mountain and Pljesevica Mountain. The lake
system is divided into the upper and lower lakes: the upper lakes lie in a dolomite valley and are surrounded by thick forests and interlinked by numerous waterfalls; the lower lakes, smaller and shallower, lie on the limestone bedrock and are surrounded only by sparse underbrush. The upper lakes are separated by dolomite barriers, which grow with the formation of travertine, forming thus travertine barriers. The lower lakes were formed by crumbling and caving-in of the vaults above subterranean cavities through which water of the upper lakes disappeared..
The area is fauna-rich, including European brown bear, wolf, eagle owl and capercaillie. There are records of 126 species of bird, of which 70 breed.
The area was the cradle of the prehistoric Illyrian tribe of Japuds dating from 1000 BC. The Japudic culture was followed by the Romans and from the 8th century AD was occupied by Slavs. Archaeological remains include a prehistoric settlement on the site of the current Plitvice village, fortifications, Bronze Age tools and ceramics.


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