The Pliva valley is located in the northern part of central Bosnia and Herzegovina and known for its tranquil mountains rich in forests and abundance of nature, wildlife and especially bodies of water. The valley is dominated by two unique rivers, the Pliva and the
Janj and two natural lakes on the Pliva river.
Hydrography and sectioning The Pliva river flows from West to East, is 26.8 kilometers long, and has an average discharge artificially set for a biological minimum of 3.0 m3 near town of
Jajce at the
waterfall site. Total watershed area of the Pliva is 1,326 km2. Its
source is some 8 kilometers upstream of the town of
Šipovo near
Pljeva at the foot of the mountain of
Smiljevac-
Jastrebnjak, where the Pliva springs out from two very strong
karstic springwells at 483 meters above sea level. The main tributary of the Pliva is the
Janj, that flows into the Pliva from the right, in the center of the town of
Šipovo. At the confluence, both the Janj and the Pliva are approximately the same size, and both rivers have the same amount of water. Some 12 kilometers downstream, at the village of
Jezero, the Pliva flows into the largest of three lakes,
Veliko Plivsko Lake, then into two smaller lakes:
Malo Plivsko Lake and
Okruglo Lake. After the Pliva river passed through the towns of
Šipovo and
Jezero, and through both Plivska lakes, it reaches the town of
Jajce where it meets with the
Vrbas river. The Pliva river is a left tributary of the Vrbas that, on its way north, flows into the
Sava river, therefore the Pliva is part of the Sava river basin.
Geo-hydrology The river Pliva is characterized by the specific
geological nature of the
terrain and distinctive
morphological and
hydrological features, very similar as nearby
Una River. The river bed of the Pliva, from the village of
Jezero to its confluence with the
Vrbas, consists of
tufa also known as
travertine which forms
travertine barriers. In this area the Pliva river has created three natural lakes,
Veliko Plivsko Lake,
Malo Plivsko Lake and
Okruglo Lake, with countless low cascades and travertine barriers (
tufa barriers), which causing these lakes to form, slowing the river and deepening it. == Pliva lakes ==