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Map of Plitvice Lakes National Park View of the lakes on a satellite image

Plitvice Lakes National Park (: Nacionalni park Plitvička jezera, colloquial Plitvice, pronounced ) is one of the oldest and the largest national parks in . In 1979, Plitvice Lakes National Park was added to the register.

The national park was founded in 1949 and is situated in the mountainous area of central Croatia, at the border to . The important north-south road connection, which passes through the national park area, connects the Croatian inland with the coastal region.

The protected area extends over 296.85 square kilometres (73,350 acres). About 90% of this area is part of , while the remaining 10% is part of .

Each year, more than 1 million visitors are recorded. Entrance is subject to variable charges, up to 250 or around 34 per adult per day in summer 2018.


The national park is world-famous for its lakes arranged in cascades. Sixteen lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of , which is deposited by the action of , , and . The particularly sensitive barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.

The 16 lakes are separated into an upper and lower cluster formed by from the mountains, descending from an altitude of 636 to 503 m (2,087 to 1,650 ) over a distance of some eight km, aligned in a south-north direction. The lakes collectively cover an area of about two square kilometres (0.77 square miles), with the water exiting from the lowest lake forming the .

The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.[]


The name Plitvice was first mentioned in a written document in 1777 by , the of . This name was designated due to natural phenomena that have created the lakes. Nature formed shallow basins (Croatian pličina or plitvak, plitko means shallow), which have been filled with water. For centuries, water has changed the limestone and thus the landscape of this area. The emerging travertine barriers decelerated and retained the flowing water. These dams are continuously growing in height.

Some scientists refer to the river as origin of the name. This little river flows into the Plitvice Lakes at the lower and final part of the lakes. A nearby village bears the same name. The water masses of the Plitvice Lakes continue as river in northern direction.

The national park became famous during the 1960s and 1970s through several of novels. Many scenes have been shot at the lakes or waterfalls.


Routes and distances[]

The Plitvice Lakes have formed in a depression between the mountain in the west and the mountain in the east amidst the . The national park is located at the national route D1 Zagreb–Split between and in the vicinity of . Other larger municipalities within the surrounding area are , , , and in Bosnia.

The shortest linear distance between the Adriatic coast and the national park is 55 km (34 ). By road from the coastal town of the distance is about 110 km (68 ). After traversing the mountain range travelers reach the Croatian karst plains of . These plains are characterized by many karst (e.g. the Gacko polje).

The fastest north-south road connection within Croatia, the highway is distanced about 50 km (31 ) west of the national park and thus circumvents the protected area. Plitvice Lakes National Park can be reached from Karlovac exit in the north, from Otočac exit in the west or Gornja Ploča exit in the south.

The nearest airports are , and . The nearest train stations are and , although no direct bus connection from these train stations to the lakes exists. Using public transport the lakes can easily be reached by direct bus lines from Zagreb, Karlovac, Zadar or Split.


Galovac waterfall Cross-section Paths between the lakes Lower lakes canyon

The area of Plitvice Lakes National Park extends across two political subdivisions or counties (Croatian županija). Its 296.85 square kilometres (114.61 sq mi) area is divided between (90.7 percent) and (9.3 percent). Hence the national park authority is under national jurisdiction. The overall water body area is about 2 km2 (0.77 sq mi). The two largest lakes, Prošćansko jezero and Kozjak, cover about 80 percent of the overall water body area. These lakes are also the deepest, with a depth of 37 and 47 metres (121 and 154 ft) respectively. On Lake Kozjak, low-noise and ecologically-friendly electric boats are being used. None of the other lakes in the park exceeds 25 metres (82 feet) in depth. The altitude drop from the first lake to the last is 133 metres (436 feet).

The 16 lakes that can be seen from the surface are grouped into the 12 Upper Lakes (Gornja jezera) and the four Lower Lakes (Donja jezera).

Lake altitude (m) area () depth (m) Group Prošćansko jezero 636 69.0 37 Upper Lakes Ciginovac 625 7.5 11 Upper Lakes Okrugljak 613 4.1 15 Upper Lakes Batinovac 610 1.5 6 Upper Lakes Veliko jezero 607 1.5 8 Upper Lakes Malo jezero 605 2.0 10 Upper Lakes Vir 599 0.6 5 Upper Lakes Galovac 585 12.5 25 Upper Lakes Milinovo jezero 576 1.0 1 Upper Lakes Gradinsko jezero 553 8.1 10 Upper Lakes Buk 545 0.1 2 Upper Lakes Kozjak 535 81.5 47 Upper Lakes Milanovac 523 3.2 19 Lower Lakes Gavanovac 519 1.0 10 Lower Lakes Kaluđerovac 505 2.1 13 Lower Lakes Novakovića brod 503 0.4 5 Lower Lakes Plitvice Lakes   217.0    

The highest waterfalls are the Large Waterfall (kroat. Veliki slap) at the end of the Lower Lakes, over which the Plitvica river falls, and Galovački buk at the Upper Lakes.

Waterfall height Veliki slap (Large Waterfall) 78 m Galovački buk (Galovac Waterfall) 25 m

Within the national park area there are 19 small settlements. Altogether they form the Plitvice Lakes municipality (Croatian općina ). The municipality is part of . The seat is located in .

The Plitvice Lakes area has always been regarded as part of the historic regions of and . During the , the region was part of the that was under direct control of the .

Topography and geology[]


The particular geographic position of the Plitvice Lakes and the specific climate features contributed to the emergence of many natural phenomena and a rich biodiversity within this area. Despite the vicinity to the Mediterranean climatic region, a moderate mountainous climate prevails at the Plitvice Lakes. These climatic conditions prevail due to the mountain range, which acts as a climatic separator between the coastal region and the Lika . For centuries, legends have been created about this mythic mountain range.

The availability of water, influenced by the configuration of the terrain, has a great impact on the biodiversity of this area. The Plitvice Lakes are surrounded by various mountains. The western side of the national park area is enclosed by the mountain, while the eastern side is enclosed by the mountain, which also represents the border to Bosnia and Hercegovina. Plitvice Lakes National Park is situated in the Plitvice plateau which is surrounded by three mountains that are part of the : mountain (Gornja Plješevica peak 1,640 m), mountain (Seliški Vrh peak at 1,280 m), and Medveđak (884 m).

The afforested mountain slopes serve as water reservoirs. They are also a refuge for many animal species. The large difference in altitude in a narrow space between the mountains in the south and the Korana river in the north also represents a significant criterion for biodiversity in this region. The overall difference in altitude within the national park area is 912 m (the highest elevation is Seliški vrh at 1279 m, the lowest elevation is reached at 367 m at the bridge across the Korana river).[14]

The national Park is underlain by rock, mainly and with associated lakes and , this has given rise to the most distinctive feature of the lakes. Right at the lakes, the Golubnjača Cave (145 m) before the second Korana waterfall and Šupljara Cave (68 m) above Lake Kaluđerovac can be visited. Other caves e.g. are Mračna Cave (160 m), Vila Jezerkinje Cave (104 m) and Golubnjača at Homoljačko Field (153 m). Within the national park, several exist, such as the Čudinka pit-cave (-203 m) or Jama on Vršić (-154 m, length 110 m). In Rodića Cave at and in Mračna Cave at the Lower Lakes, cave bear bones were found, so these sites may be considered paleontologically significant.


The Plitvice Lakes originate in the south of the park area at the confluence of Bijela Rijeka (English White River) and Crna Rijeka (English Black River). These rivers originate south of the municipality of and unite at one of the bridges in this village. From this place onwards to the lakes, the water masses are referred to as Matica (English for water current, can also mean root or origin). At the bay of Liman (also called Limun), a part of Prošćansko jezero, another little river flows into the lakes. This river is fed by permanent springs; the water quantity, however, varies. Temporarily, water from other, usually dead creeks reaches Prošćansko jezero from the west.

The river reaches the Plitvice lake chain at the northern end via the Large Waterfall. This place is called Sastavci (English confluence or composition). The water masses of the Plitvice Lakes and the river Plitvice form the river.

Properties of the underground[]

The Lower Lakes canyon

The underground configuration of the Plitvice Lakes consists of various geologic features. Generally, the whole area of Plitvice Lakes National Park can be attributed to the South-East European . The typical feature of this karst area is brittle or porous rock, mostly or . This configuration creates different phenomena being referred to as dolina (), , , , etc.

In the future, the analysis of underground water courses could be an interesting field of research for . Up to now, little has been known about these unexplored courses. At first sight, a lack of water in the karst region could be ascertained. However, this is only the case on the surface. The major part of natural phenomena takes place underground, where an abundance of water exists.

Due to the features of limestone, many rivers drain away into the rock. Therefore, extensive underground river systems exist. Upon reaching hard rock, rivers emerge on the surface. This phenomenon of underground karst rivers (Croatian rijeka ponornica) can also be observed at the Plitvice Lakes.

sediments have been formed from the onwards in sinkholes or depressed areas between the surrounding mountains. Generally seen, the underground of the Plitvice Lakes could be categorized into two zones. The Upper Lakes in the south predominantly consist of rock. The Lower lakes in the north predominantly consist of rock. Dolomite rock is slightly harder than limestone. Though fragile upon physical influence, dolomite rock has lower water permeability properties. In contrast, limestone rock is more compact and massive, but has a higher water permeability.

From an aerial perspective, significant differences between the terrain of the Upper and the Lower Plitvice Lakes can be observed. At the Upper Lakes several little lakes have formed parallel to each other and a rather shallow water flow can be observed. The Lower Lakes, however, are much larger and virtually drill their path through the rock. Furthermore, there are only a few lakes at the Lower Lakes. They have formed a , which continues as river Korana.


On average, the annual precipitation rate at the Plitvice Lakes is 1,500 mm (59.06 ). Usually, in spring and fall (autumn) the largest rain quantities are measured. The average relative is 81.8 percent. In January, the average temperature is 2.2 °C (36 °F). During the summer months of July and August, the temperature rises to 17.4 °C (63 °F). The general average annual temperature is 7.9 °C (46 °F). Snow falls from November until March. Usually, the lakes are frozen during December and January.

The water temperature at the springs is usually below 10 °C (50 °F). Within the rivers and lakes, the water temperature rises up to 20 °C (68 °F). The following example for different water temperatures measured on July 7, 1954 demonstrates large temperature differences within the lakes: Within lake Kozjak at the depth of 4 m a temperature of 18.9 °C (66 °F) has been measured. At a depth of 20 m, 5 °C (41 °F) have been measured. At 44 m depth, virtually at the bottom of the lake, a temperature of 4.1 °C (39 °F) has been measured.

The dissolution and creation of rock[]

The lakes of Plitvice are a result of century-old processes and the sedimentation of , which is abundantly available in the waters of this karst area. These sedimentations are called or (both are called sedra or tuf in the , apart from many other names like bigar or vapneni mačak).

A distinctive feature of the Plitvice lakes is the fact that they do not represent separated, stationary waters. The lakes altogether have always been seen as one composed system of lakes. Due to constant changes it is not even possible to pursue individual analyses of single lakes. The water masses reaching the lakes at the upper or lower part of the system are continuously changing the outlook of the lakes and the surrounding landscape. They finally exit the lakes as river Korana. On the one hand, chalk tufa is being washed away partly. On the other hand, new sediments are continuously being formed. Thus, new waterfalls are being formed while others run dry. Nature itself is continuously adapting to these new conditions. As a whole, the complex of lakes represents a very sensitive and labile (liable to change) ecosystem.

Alteration processes[]

In geological terms, the actual phenomena molding the Plitvice Lakes are quite young. The complex processes of dissolution and sedimentation of limestone require specific climatic preconditions. These have only existed since the end of the ice age about 12,000 to 15,000 years ago, according to tufa .

Apart from weather and temperature factors, the water quality and other natural factors are significant for the creation of these natural phenomena, prevailing at the Plitvice Lakes. By passing through the limestone underground the karst rivers dissolve chalk (calcite), which concentrates in the water. The saturation level of calcite within the frontal flows is thus very high. The water becomes significantly mineralized, super-saturated with calcium and magnesium-hydrogencarbonate.

The dissolution of limestone happens through alteration processes and the effects of . In a natural environment, carbonic acid (H2CO3) is formed by the dissolution of (CO2) from the air or from rainwater (H2O). Limestone or (CaMg(CO3)2) mainly consists of calcite (CaCO3), which is not very soluble in water. Calcite, however, is dissolved by carbonic acid, thus creating (Ca(HCO3)2). This is shown by the following formulas:

H2O + CO2 ↔ H2CO3 ↔ H+ + HCO3− ↔ 2 H+ + CO32− CaCO3 + H2CO3 → Ca(HCO3)2 CaCO3 + H+ + HCO3− ↔ Ca2+ + 2 HCO3− ↔ Ca(HCO3)2

The quantity of calcium hydrogencarbonate (also called calcium bicarbonate) dissolved in water depends on the quantity of dissolved carbon dioxide in the water. Generally, the following could be said: The colder the water, the higher the quantity of dissolved calcium hydrogencarbonate. Depending on the conditions for the alteration processes, scientists identified limestone dissolution rates of 0.01 to 4 millimeters a year. (It is possible that by the effect of rainwater about 1 m3 of limestone is dissolved in about 10,000 years.)

Sedimentation processes[]

The waterfall Galovački buk at the Upper Lakes

The previously mentioned mechanical and chemical dissolution processes are regularly occurring natural phenomena. A unique process occurring at the Plitvice Lakes, however, is the sedimentation of water-bound chalk at certain places. With regard to other similar phenomena in the world, at Plitvice Lakes the sedimentation of chalk and the formation of tufa happens dynamically all along the watercourse and in various forms (fluviatile sedimentation). It is thus not a static phenomenon occurring at only single places.

Another unique and distinctive feature are the natural factors, particularly the influences of the vegetation in the process of sedimentation. While passing the vegetation, barriers are being created by foaming water. These naturally created barriers decelerate and dam the waters, thus forming lakes. At Plitvice, this constant interplay between water, air, rock and vegetation can easily be observed. The foaming water creates ever growing and impressive waterfalls. The thresholds grown up above the water level, create cataracts.

About 30 km (18.64 ) north of the lakes at the conflux of the and rivers, right in the center of the town of , similar phenomena occur. This part of the town, called , is often being referred to as "the Small Lakes of Plitvice."

Preconditions for sedimentation[]

The large waterfall (78 m) of the river at the Lower Lakes.

Measurements of carbon dioxide quantities in the water show that they correspond with continuous sedimentation processes in the Plitvice Lakes area. Carbon dioxide quantities at the springs are about twenty times higher than in the atmosphere. The quantity of carbon dioxide decreases along the water route. The Plitvica river for example loses even up to 97 percent of its original quantity of carbon dioxide along its route.

The sedimentation of calcium carbonate from the water occurs only at certain temperature conditions (only above 14 °C), e.g. when the water warms up or by evaporation or by another loss of carbon dioxide, additionally fostered by water plants and moss. Since sedimentation only occurs under warm, humid climate conditions, these phenomena have only been occurring since the end of the last ice age. Since then, a layer of hardened tufa, also called travertine, has been formed on the limestone ground.

The area of a river, in which the formation of tufa occurs, is called precipitation area. Along the Korana river for example, measured from its origins tufa is being formed only along the first 10 to 15 km (9.32 ), even if according to pH measurements the conditions would be favorable further down the river. At the ground of Lake Kozjak a constant yearly sedimentation of 0,8 millimeters during the past 3,000 years has been ascertained. Yearly, the barriers are growing up to 13 millimeters in height. Tufa formation processes thus surpass erosion activities, which would destroy the sensitive barriers of the lakes. It is estimated that the tufa sedimentations at the ground of the lakes date back 6,000 or even 7,000 years.

The precipitation of calcium carbonate, however, does not occur right at the springs of the rivers that flow into the Plitvice Lakes. For the precipitation of carbonate chalk (calcium carbonate) the water needs to reach a certain mineral saturation level. At the springs this saturation level is about 1. For the precipitation, the water saturation level needs to be higher than 3. At the same time, the pH value of the water needs to be above 8,0 (slightly alkaline).

Thresholds become barriers[]

Cross-section of a barrier

Tufa barriers are the result of continuous sedimentation processes along natural thresholds. As the water flows in thin layers over thresholds, it is splashed up. This disturbs the chemical balance and causes precipitation of the carbonates, which then creates sedimentary deposits. Since the water forms larger surfaces at these places, increased quantities of carbon dioxide (CO2) are released. Calcium carbonate is secreted in the form of microcrystals that are deposited, eventually creating tufa sediments (CaCO3). This phenomenon particularly occurs on abundantly available mosses, enabling better adherence of the crystals.

In the course of time, older barriers can be flooded by rising water levels since other barriers have outgrown the older ones. 400 years ago, there were two lakes in the place of today's Kozjak lake. In the lowest third of the lake, at the level of Matijaševića draga, a crown of an underwater barrier that is 40 m high, is stretching 4 m below the water surface. This barrier certainly formed a magnificent waterfall in the past. The travertine barrier at the Kozjak bridges (at the current end of the Kozjak lake), however, grew faster. Thus, 400 years ago two lakes merged in one. That is why the greatest depths of Kozjak lake are in its lower basin (north from the little island).

Influence of vegetation[]

Calcium-carbonate-encrusted, yet growing moss, early stage of porous formation as in Plitvice.

Mosses, algae and water plants play a major role in forming the unique landscape of the Plitvice Lakes and its barriers. Up until the 21st century, it was supposed that plants extract carbon dioxide from the water for photosynthesis purposes and that in return oxygen is released, thus resulting in the sedimentation of hydrogen carbonate (). The leading scientist arguing for this theory was . Thanks to his efforts the Plitvice Lakes are now under national protection.

Recent scientific evidence indicates that vegetation is not primarily responsible for the extraction of carbonate from the flowing water. However, plants indirectly contribute to formation. For sedimentation to occur it is essential that the water be decelerated, aerated and sprayed. The mosses of the Plitvice Lakes waterfalls provide a for sedimentation, generating travertine (). Depending on the species found locally, various biological types of can be differentiated.

Photosynthesis activities of algae and mosses in conjunction with the water, however, foster the crystallization of sediments due to the extraction of carbon dioxide. These effects are fostered by the millions of microscopically-small bacteria and algae that grow on such plants. They secrete mucus to which the first microcrystals of calcite adhere. The most significant plants of this kind are mosses of the species and .

The young shoots of mosses are green and soft. They are mostly without travertine, while older shoots are encrusted by a thin and fragile yellow layer, completely covered and petrified by plant-formed travertine. The mosses foster not only the creation of tufa barriers, but also become part of the barrier. The moss becomes encrusted with travertine and fresh moss grows further out. First a crag is formed but later a cave roof forms under the crag. If the water continues flowing, the cave becomes progressively bigger. Older travertine is filled with fossilized algae and mosses. This type of tufa rock typical of the Plitvice Lakes is called "phytogeneous tufa."

Factors impeding tufa formation[]

Even though the vegetation has beneficial effects for the formation of tufa, excessive concentrations of organic substances within the water impede its formation. Excessive plant cover has adverse effects on mineral sedimentation. Along the course of Korana River from the Korana bridge, for example, travertine creation ends quite quickly, in spite of its supersaturation with calcium bicarbonate, as a result of the increased concentration of organic matter in the water. The park authorities have therefore begun systematic removal of excessive vegetation along the barriers. Water purity is the decisive factor for tufa formation. The water at the influx to the Plitvice Lakes is defined as pure from an analytical point of view. The Dissolved Organic Carbon (DOC) value of the water barely exceeds 2.5 mg/L at the influx to the Upper Lakes (Matica). At the Lower Lakes higher concentrations are measured (5.15 mg/L). At the springs of other Croatian rivers in the karst region similar concentrations have been recorded.

During the 20th century, uncontrolled tourism and water pollution caused by waste water from hotels and agricultural activities in the surrounding area have led to damage. This has led to increasing of the lakes (increased concentrations of organic substances within the water). For the sustainable formation of tufa it is therefore imperative to protect this extremely sensitive area from excessively harmful human influence. Since 2006, it has been strictly forbidden to bathe or swim in the lakes. Previously, swimming had been allowed in Lake Kozjak.

Types of rock[]

Cellular rock Porous rock that has been exposed to external effects, for example rainwater ( or ) Sedimentations of minerals from the water that typically consolidate on moss or on the underground of the lakes. These sediments are the results of century-old sedimentation processes. Year after year, new layers of sediments are being added. Consolidated tufa. Older, hardened sediments. This porous type of rock is very sensitive to physical impacts.

Flora and Fauna[]

Barrier between the lakes Gavanovac and Kaluđerovac , and various species of insects gather in lush meadows

With regard to plant and animal diversity, the area of the Plitvice Lakes is one of the most significant areas of Croatia, due to climatic conditions and its relatively remote location, since the lakes are at a fair distance from polluted and noisy cities and industrial plants. As a result of the low level of industrial development in this region and the early introduction of protective measures, a nearly untouched landscape has been preserved. In the partially primeval beech and fir forests various rare species, such as the have survived.


The Plitvice Lakes national park is heavily forested, mainly with , , and trees, and features a mixture of Alpine and Mediterranean vegetation. It has a notably wide variety of plant communities, due to its range of microclimates, differing soils and varying levels of altitude.

Scientists have so far identified 1,267 different types of plants belonging to the 109 species so far recorded in the area of the national park. 75 species of plants are , which means that they were first defined and classified in this area of the world or nearby. A great number of these plants and species are protected by law. Within the national park area 55 different species of can be found.

Examples of endemic plants to be found in the national park:

Examples of other rare plants:

The great plant diversity creates a fascinating interplay of colours that change with the seasons. The lake area is surrounded by dense forests. The national park has an area of 29,842 hectares, of which some 22,308 hectares are forests (74.75 percent), 6,957 ha are meadows (23.31 percent) in village areas and 217 ha (0.72 percent) are water areas. A unique area is the forest of Čorkova uvala, a 79.50 ha large virgin forest in the northwestern part of the park. The beech and fir trees in this area of the park are up to 700 years old. 


The area of the national park is home to an extremely wide variety of animal and bird species. Rare fauna such as the European , , , , , , and can be found there, along with many more common species.

The wider area of the national park is one of the last areas in Europe in which a great number of wild and can be found. The rich fauna of the Plitvice Lakes includes some 50 species of mammals. Scientists have so far discovered 321 different kinds of butterflies, of which 76 are day-flying butterflies, and 245 are nocturnal moths. Scientists, however, estimate that up until now only about 40 percent of the whole population of butterflies has been identified. Furthermore, 12 amphibian species, as well as some species of reptiles have been recorded, including the (Lacerta vivipara), the (Lacerta viridis), the (Natrix tessellata), , and the (Emys orbicularis).

As regards bird species, the Plitvice Lakes rank third among the Croatian national parks for diversity. Some 157 species have been counted, of which 70 have been recorded as breeding there. The Plitvice Lakes are also home to many kinds of . Recent findings list about 20 different kinds of bat species, among them the rare species of .

Among original species the brown trout ( and ) can be mentioned. Salmo trutta fario is found mostly in the Upper Lakes, while Salmo trutta lacustris is mainly found in Lake Kozjak. These species developed in different life conditions independently from each other within the various lakes.

Due to the spreading growth of vegetation at the barriers, allochthonous (species that originate elsewhere and do not belong to this ecosystem) fish species spread quickly and thus endanger autochthonous trout species. Apart from the trout, (Phoxinus phoxinus) are also found. As a result of human interference the species alpinus and the North American have been introduced to this ecosystem. Recently, even (Squalius cephalus) and (Scardinius erythropthalmus), species whose emergence may be attributed to climate change, have been discovered. The number of , which were almost extinct, is now again increasing. Even rare (Proteus anguinus) can be found in the karst caves of this region.

Examples of some animals found in the national park:


Main article:

While other nature protection areas are located far away from any interference by man, the Plitvice Lakes have permanently been exposed to human influence in the course of history. The Plitvice Lakes do not represent an abandoned or lonely nature reserve. They are located along an important transport route and have always been a meeting place of and cultural influences.

Early History and Medieval Age[]

Gradinsko jezero

Humans have inhabited the Plitvice Lakes area for thousands of years. It has been settled in turn by , , , , , , and . Under the region was incorporated as the province of into the . The areas of the neighborly tribes of the , the and were united into the . Successively, the took over the rule. After the in 454, the Ostrogoths were rewarded with a federation agreement with the Roman Empire.

During the 6th century, settled in this region, which were accompanied by the . The Croats eventually defied Avar control and settled permanently in this region. In medieval times, frequent attacks by posed a permanent threat to the settled population. The lakes formed part of the which in 1102 elected to be in .

Croat rule and particularly the rule of the noble families and led to economic recovery in the wider area. On the remnants of an ancient settlement of the Japods and Romans a monastery was built at the lakes. Presumably, this monastery belonged to the (Croatian pavlinci) or the . Today, only ancient wall remnants of this building (Croatian gradina) exist. The foundation was made of travertine rock.

Ottoman Wars and the Habsburgs[]

In 1493, not far away from the Plitvice Lakes a decisive battle in Croatian history between the and took place. During the almost the entire Croatian nobility was killed. The Ottomans advanced far into Western lands up to and . In 1527, the the Habsburg monarch as the new king of Croatia in the hope of resources to ward of the Ottoman advance. In 1528, the area fell to the and was retaken by the 150 years later.

In 1538, king ordered the establishment of the as a borderland of Habsburg Austria to the Ottoman Empire. The laws that prevailed in this area under special jurisdiction had formative impact on the local population for centuries. As a consequence of the establishment of this special regime, people abandoned these areas in great masses towards the West.

In addition to the native already inhabiting the region and serving in the Austrian military, many central Europeans migrated to the region as did refugees fleeing Ottoman repression, who were given refuge in the abandoned areas in exchange for military service. The entire population of the military frontier, particularly the so-called frontiersmen, had the duty to protect this area of permanent unrest and terrible destruction. The region once also used to be called the garden of the devil ().

The Ottomans succeeded several times to gain control over the area of the Plitvice Lakes for shorter periods. In 1788, this area permanently fell back under Habsburg rule. When the Ottoman threat subsided, the Military Frontier was reverted to the civilian control of the (Ban). The area then formed part of within the and then part of the within the . Today, it is part of the .

In 1805, another major rule change happened, which created an economic upturn. and fell under the rule of , who founded the . After 1814, the area of the Plitvice Lakes came back under Habsburg rule. Since 1850, only professional soldiers served in the Military Frontier. This was also a time of national awakening in Croatia. In 1871, the famous Croatian politician was killed north of the lakes at . The Croatian rebellion was put down by Austrian authorities. Kvaternik propagated the rule of law and argued for the liberation from Austrian-Hungarian predominance.

Farmlands becoming an area of recreation[]

Prošćansko jezero

In former times, the local population lacked the proper comprehension of the natural values of the Plitvice Lakes. Farmers had to focus on securing the daily bread for their families in these dour times, which was accompanied by grave changes to nature. For example, smaller lakes were filled up with earth or people adapted the flow of the rivers to their individual needs.

Already in 1861, an accommodation for travelers was erected at Velika Poljana. The local population called this accommodation the Emperor's house, since imperial military officers used to reside in this location. For the visit of , the wife of in 1888, the Plitvice Lakes and their surroundings were arranged for tourist purposes for the first time in history. Two paths still bear the names of the daughters of the : " Path" (Croatian Štefanijin put) and " Path" (: Dorotejin put).

In 1890, the tradesman from built the first hotel with a restaurant at Prošćansko jezero. However, he exaggerated in his efforts and also caused partly irreparable damage on the nature. For example, he constructed canals across the travertine barriers for his saw mill that are visible even today.

At the same place, today called Labudovac, , a Czech from Zagreb, built a restaurant and accommodation. In 1893, Janeček founded the Society for the preservation of the Plitvice Lakes (Croatian Društvo za uređenje i poljepšanje Plitvičkih jezera), with the aim of preserving the lakes after all negative influence they have been exposed to. The society also built a hotel at the lakes. In 1898, one of the waterfalls was named after Croatian opera singer . She gave money from concerts to preserve the park, upgrade tracks and build pathways.

During the First World War, the Croatian parliament in Zagreb passed the Law on the Protection of the Plitvice Lakes in 1916. However, this law did not contain adequate measures of protection and is thus not regarded as official founding declaration of the national park.

During the following decades, preservation efforts reached a deadlock. However, some very significant meetings took place at the Plitvice Lakes during the Second World War, as for example the first secret regional conference of the (Croatian: Savez komunista Hrvatske, SKH) in 1940. On June 14, 1943 one of the founding sessions of the took place at Plitvice Lakes. This was the highest governing organ of the anti-fascist movement in Croatia during World War II. The former Secretary General of the Communist Party of Croatia, , was born in at the Plitvice Lakes in 1911.

The Lakes as National Park[]

Okrugljak Bus connection offered to visitors of the national park

After the end of the Second World War, the unique natural phenomena of this area were acknowledged permanently. On April 8, 1949, the Plitvice Lakes were declared as a national park area and rigorous nature protection measures were established.

During the 1960s, a modern road connection to the Plitvice Lakes was constructed, which led to increasing traffic volumes. During these years, several hotels and other objects were erected according to innovative plans of Croatian architects. However, some buildings that would fit current standards were already demolished during the 1980s by the Communist authorities.

Between 1962 and 1968, many of novels have been shot at the Plitvice Lakes (mainly German-French-Yugoslav cooperations). The most successful film of this series, was also produced at some locations within the national park. (Lake Kaluđerovac served as scenery for the Silver Lake.)

During the 1970s, detailed of the national park were recorded. The park was inscribed on the List in 1979 in recognition of its "outstanding natural beauty, and the undisturbed production of travertine (tufa) through chemical and biological action".

During the 1980s, tourism was booming in Yugoslavia. Plitvice Lakes National Park soon became one of Yugoslavia's most popular tourist attractions. The beginning of the 1990s, however, marked another great turning point in the history of this national park. In March 1991 it became the scene of the (also called the "Plitvice Bloody Easter"), the first armed confrontation of the that resulted in fatalities. The park was held by local Serb rebels backed by and the (JNA) as part of the self-proclaimed "" during the conflict and suffered some damage in the process, with hotels and other facilities being used as barracks. During the period under the control of Serb forces loyal to Belgrade, Croats were ethnically cleansed from the region systematically. The region was retaken by the in August 1995 during , and majority of Serb population was expelled.

Year Number of visitors 1894 1,000 1989 500,000 1996 238,401 2000 482,275 2001 597,884 2002 665,108 2003 721,265 2004 749,209 2005 855,866 2006 866,218 2007 927,661 2008 948,891 2009 939,747 2010 980,033 2011 1,083,638 2014 1,184,449 2015 1,367,304 2016 1,429,228

During the war from 1991 until 1995, many buildings in the national park were destroyed or burnt down. Due to the apparent risk of mines, the park was even put on the UNESCO List of World Heritage in Danger during the war years. After the war, the Plitvice Lakes were among the first areas to be cleared of mines and renovated. In 1998, the national park was removed from the List of World Heritage in Danger. In 2000, the national park was expanded by a further 102 square kilometres (39 sq mi) in order to protect the underground tributary streams.

Within the national park continuous scientific research projects are being carried out. The national park administration currently endeavors to introduce new, progressive protection measures. There is a proposal to replace the wooden bridges and paths by floating . The existing wooden paths are anchored within the travertine sediments, creating the danger of seepage and cracks of the weak travertine.

The Plitvice Lakes are today one of the most frequently visited tourist attractions in Croatia. Due to their high natural, cultural and tourist significance they have become a motor for the local economy. About 1,000,000 visitors per year greatly contribute to the economic development of the wider region.

Due to high tourism and illegal construction around lakes, with faecal waste flowing down to surrounding woods and lakes without any treatment, the water in the lakes is polluted and no longer drinkable. In current state UNESCO threatens to remove parks status as World Natural Heritage site.

Local customs and traditions[]

The preservation of old customs and traditions is of high significance for the local population. The local culture has also been detected as an important factor for tourism. As regards architecture, the region of is well known for its low wooden houses with roofs made of rye straw or shingles. Many features of the ancient living style are mirrored in local costumes. They tell a lot about regional affiliations or social standings of those who have worn those costumes. Under French rule, men were allowed to wear their costumes during military service.

Up until the 20th century, social gatherings during the winter months, when no agricultural activities could be performed, called "" represented a typical tradition of this region. These gatherings served for the joint production of textiles or butter or for the further processing of harvest products (production of flour, etc.). These activities used to be accompanied by drinks and dances, particularly during the evenings. A well-known dance of this region is the (Croatian kolo).

Local cuisine consists of drinks, such as (Croatian šljivovica), wine and coffee or dishes, such as (Croatian vrhnje), , , paprika sausage, roasted (Croatian: odojak) or lamb (Croatian: janjetina).

Lake names and anecdotes[]

Each of the Plitvice Lakes has a story or legend to tell. Most lake names stem from true events.

Lake Other names Approximate translation Explanation Prošćansko jezero Prošće Scrub Lake
Crave Lake The name is due to the fences that have been built by farmers as delimitation between the farmlands and the lakes. The farmers used stakes (Croatian prošće), poles, scrub and earth to build these fences.

The Legend of the Black Queen, the legend on "prošnja" (praying the black Queen for water) says that the inhabitants of this region were craving for water and thus called upon the magic queen to help them, which she did. According to the legend, this is the reason why Prošćansko jezero and the other lakes have emerged.

Ciginovac Cigino jezero
Ciganovac jezero
Gypsy's Lake According to a legend, a roma (gypsy) drowned in this lake while fishing. Okrugljak Okruglić
Round Lake The name stems from its round shape. Batinovac Batin
Lake Batin/Batić's Lake People reported that a villager named Batinić used to dwell at this lake. Others say that a grandmother (Croatian baka) might have drowned in this lake. Veliko jezero Jovinovac veliki Large Lake Malo jezero Jovinovac mali
Veliko jezerce
Small Lake Vir Whirlpool The name originates from water whirling downward in the middle of the lake. Galovac Galov's/Galović's Lake Allegedly, a bandit chief named captain Gal, who defeated the Turks, was shot down at this lake. It could also have been named after a brig and Galović. Milinovo jezero Milino Jezerce Mile's Lake According to a legend, a man named Mile Marić from Stropina drowned in this lake. Gradinsko jezero Jezerce
Lake Gradina The lake is named after a building (Croatian gradina) or monastery which had once been situated on the peak between Kozjak lake and this one. Bukovi Burgeti
Gush Lakes A chain of small shallow lakes separated by travertine barriers, and covered by low vegetation. The name comes from agitated waterflow in small scars which make noise or "boil". Kozjak Kozje Jezero Goat Lake On the island in the middle of the lake (today Štefanijin otok, Stephanie's Lake) farmers used to protect their goats from wolves. The name originates from a legend, according to which 30 young goats were running away from wolves during winter. They drowned in the lake as the thin ice layer cracked. Milanovac Milanovo Jezero Milan's Lake According to a legend, the lake was named after a shepherd called Mile who drowned in it, or after the miller Mile Perišić who owned a mill at the lake. Gavanovac Gavanovo Jezero
Osredak Jezero
Okrugljak Donji
Gavan's Lake Allegedly, the treasure of a man named Gavan (the Gavanovo treasure) lies hidden in this lake. Kaluđerovac Kaluđerovo Jezero Monk Lake or Hermit Lake According to reports, a monk or hermit (Croatian kaluđer) used to live either in Šupljara Cave just next to the water or in Golubnjača Cave at the canyon edge. People used to seek advice from this monk. Novakovića brod Novaković's crossing According to a tale, a named Novaković was thrown off his horse into this lake. Other reports say that a man named Novaković used to offer boat rides across this lake.

Comparable phenomena worldwide[]

Comparable phenomena to those prevailing at the Plitvice Lakes exist at (Slunj), at the or at the rivers and the in Bosnia and Herzegovina. The lakes within the mountain range form a similar system of lakes and dams, though diverging tufa formation processes prevail. Calc-sinter formation processes that have not emerged along a river flow can be observed at the within (USA) or at in Turkey. is a nature reserve and national park located in the north of Sichuan, China. Also inscribed by UNESCO as a World Heritage Site, its landscape of cascading lakes is made up of high-altitude karsts shaped by glacial, hydrological and tectonic activity.The area around Ocho Rios Jamaica is another region famous for its calc-sinter rivers. Most popular, particularly with cruise ships, is .


  • Water paving its way along many small waterfalls

  • Water flowing across mossy cascades

  • Water being splashed by cascades

  • Water flowing across mossy cascades

  • The continuous flow of water

  • Wooden paths

  • Wooden paths along turquoise-colored lakes

  • Turquoise-colored lakes

  • Waterfall at the upper lakes

  • Lower Plitvice Lakes

  • Waterfalls during summer

  • Walking on wooden footbridges

  • Waterfall

  • View from Šupljara cave at the Lower Lakes

  • Park map

  • Lake behind a waterfall

  • Turquoise water along the unpaved route

  • Turquoise-colored lakes

  • Turquoise-colored lakes

  • Distant waterfalls

  • Turquoise-colored lake

  • Fishes in lake

  • Turquoise-colored lake

  • View of lake in evening


  1. ^ . 
  2. There are seven other national parks in Croatia, as well as ten nature parks.
  3. UNESCO World Heritage Centre (2000-11-30). . Retrieved 2013-09-08. 
  4. ^ . 
  5. March 28, 2009, at the .
  6. ^ . Retrieved 2013-09-08. 
  7. ^ Franić, D. (1910) Plitvička jezera i njihova okolica, Zagreb, Tisak kraljevske zemaljske tiskare
  8. . Retrieved 2013-09-08. 
  9. Vgl.
  10. Vgl.
  11. , p. 11
  12. ^ Meridijani, 3/2002, 30. Šafarek, G. Plitvička jezera - 16 srebrnih stepenica
  13. First permanent shelter at Plitvice Lakes have been constructed by officers of the Otočac Regiment in 1861/2 for rare chance travelers, who meet unexpectedly with that romantic but unknown, almost wild and insecure area. This was the way in which the first traveler's house was built in simple Swiss style, which served for a few decades for tourist and public purpose, until the construction of the first hotel inside villa "Devčićevac" in 1890.
  14. ^ March 2, 2009, at the .
  15. December 16, 2008, at the .
  16. ^ Gušić, B. & Marković, M. (ed.) (1974) Plitvička jezera - čovjek i priroda, Zagreb, Nacionalni park Plitvice
  17. ^ Horvatinčić, N. (1999) Starost sedre Plitvičkih jezera. Priroda: mjesečnik za popularizaciju prirodnih znanosti i ekologije, 89, 20-22
  18. ^ Stilinović, Božidar. . Plitvice Lakes National Park. Retrieved 2 June 2011. 
  19. (in German). 2013-08-09. Retrieved 2013-09-08. 
  20. ^ . Retrieved 2013-09-08. 
  21. Zdunić, D. & Movčan, J. (ed.) (1985) Plitvice, Zagreb, Nacionalni park Plitvička jezera, Spektar
  22. December 16, 2008, at the .
  23. (in German). 2010-09-24. Retrieved 2013-09-08. 
  24. December 16, 2008, at the .
  25. December 16, 2008, at the .
  26. March 2, 2009, at the .
  27. ^ December 16, 2008, at the .
  28. ^ March 2, 2009, at the .
  29. Darko Zubrinic (1995). . Retrieved 2013-09-08. 
  30. . Archived from on 2010-09-26. Retrieved 2013-09-08. 
  31. . Retrieved 2013-09-08. 
  32. , Review of World Heritage Nomination, April 1979
  33. . Retrieved 2013-09-08. 
  34. (PDF). Retrieved 2013-09-08. 
  35. ^ (PDF) (in Croatian). II.a. Zagreb: Ministry of Construction and Spatial Planning (Croatia). 2014. p. 89. Retrieved 21 March 2018. 
  36. ^ Retrieved 31 March 2015. 
  37. . 2013-08-25. Retrieved 2013-09-08. []
  38. . Croatian Ministry of Culture. 2013-07-23. Retrieved 2013-09-08. 
  39. Božičević, Srećko. . Plitvice Lakes National Park. Retrieved 2 June 2011. 
  40. Božičević, Srećko. . Plitvice Lakes National Park. Retrieved 2 June 2011. 
  41. in Croatian


  • Mato Njavro (ed.): Plitvice Lakes, Turistička naklada d.o.o., Zagreb 2005,  
  • Josip Movčan, Drago Zdunić: Plitvice, Grafički zavod Hrvatske, Spektar, Zagreb 1985 (German, Croatian, English, French)
  • Dragutin Franić: Plitvička jezera i njihova okolica, Tisak kraljevske zemaljske tiskare, Zagreb 1910 (Croatian)
  • Branimir Gušić, Mirko Marković (ed.): Plitvička jezera – čovjek i priroda, Grafički zavod Hrvatske, Zagreb 1974 (Croatian)
  • Jeanne Oliver, Lonely Planet Croatia, pp. 164–166 (Lonely Planet, 2005)
  • Radovan Radovinović (ed.), The Croatian Adriatic (Naklada Naprijed, Zagreb)
  • Šikić, Zoran, ed. (October 2007). [Plitvice Lakes National Park Management Plan] (PDF) (in Croatian). .  . Archived from (PDF) on 1 July 2014. Retrieved 31 March 2015. 

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