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703:(9.3 percent), hence the national park authority is under national jurisdiction. The overall water body area is about 2 km (0.77 sq mi). The two largest lakes, ProÅ”Äansko 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).
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1952:
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1725:), 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.
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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.
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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
57:
1800:, 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).
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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."
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cleared of mines and renovated, although some of the more remote areas in the park are suspected still to contain landmines. 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.
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1172:. 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
3103:" 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
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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
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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
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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.
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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
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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.
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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
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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
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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
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The great plant diversity creates an interesting interplay of colours that change with the seasons. The national park has an area of 29,842 hectares, of which some 22,308 hectares consists of forests (74.75 percent), 6,957 hectares are meadows (23.31 percent) (mainly in village areas), and
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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,
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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
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The water temperature at the springs is usually below 10 Ā°C (50 Ā°F). Within the rivers and lakes, the water temperature rises up to 20 Ā°C (68 Ā°F). The following example for different water temperatures measured on July 7, 1954 demonstrates large temperature differences within the
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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
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First permanent shelter at Plitvice Lakes have been constructed by officers of the OtoÄac 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
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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
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The fauna of the Plitvice Lakes includes some 50 species of mammals. Scientists have so far discovered 321 different species of lepidoptera, of which 76 are day-flying butterflies, and 245 are nocturnal moths. However, they estimate that only about 40 percent of the lepidopteran population has been
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Photosynthesis by algae and mosses, however, fosters the crystallization of sediments because of the extraction of carbon dioxide. These effects are fostered by the millions of microscopically-small bacteria and algae that grow on such plants, which secrete mucus to which the first microcrystals of
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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
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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
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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
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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
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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
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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
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Because of high tourism and illegal construction around the 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 its current state, UNESCO threatens to remove the park's status as a World Natural
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During the war from 1991 until 1995, many buildings in the national park were destroyed or burnt down. Because of the apparent risk of mines, the park was placed 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
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The area of the Plitvice Lakes is one of the most significant areas of Croatia for plant and animal diversity, mainly because of climatic conditions and its relatively remote location. The low level of industrial development in the surrounding area, along with the early introduction of protective
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is 81.8 percent. In January, the average temperature is 2.2 Ā°C (36 Ā°F). During the summer months of July and August, the temperature rises to 17.4 Ā°C (63 Ā°F). The general average annual temperature is 7.9 Ā°C (46 Ā°F). Snow falls from November until March. Usually, the
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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
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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
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A distinctive feature of the Plitvice lakes is the fact that they do not represent separated, stationary waters. The lakes have always been seen as one composed system of lakes. Because of constant changes it is not possible to analyse individual lakes. The water masses reaching the lakes at the
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trees, and features a mixture of Alpine and Mediterranean vegetation. It has a notably wide variety of plant communities, because of 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
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from the water occurs only at certain temperature conditions (only above 14 Ā°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
3209:, the legend on "proÅ”nja" (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 ProÅ”Äansko jezero and the other lakes have emerged.
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The quantity of calcium hydrogencarbonate (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
1365:. 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.
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lakes: Within lake Kozjak at the depth of 4 m a temperature of 18.9 Ā°C (66 Ā°F) has been measured. At a depth of 20 m, 5 Ā°C (41 Ā°F) have been measured. At 44 m depth, virtually at the bottom of the lake, a temperature of 4.1 Ā°C (39 Ā°F) has been measured.
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The Plitvice Lakes are one of the most frequently visited tourist attractions in Croatia. Their natural, cultural and tourist significance has become a motor for the local economy. About 1,000,000 visitors per year greatly contribute to the economic development of the wider region.
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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
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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
1881:(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.
455:. The particularly sensitive travertine 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.
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built the first hotel with a restaurant at ProÅ”Äansko 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.
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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
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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
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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
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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.
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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.
2674:. 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
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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.
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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 m of limestone is dissolved in about 10,000 years.)
3428:, 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.
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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
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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.
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Because of the growth of vegetation at the barriers, allochthonous fish species (species that originate elsewhere and do not belong to this ecosystem) spread quickly and thus endanger autochthonous trout species. Apart from trout,
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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
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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.
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Because limestone is soluble, many rivers drain away into the rock, forming extensive underground river systems. Upon reaching hard rock, rivers emerge on the surface. This phenomenon of underground karst rivers (Croatian
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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
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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.
2002:, 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
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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
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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
2778:), 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
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Plitvice Lakes rank third among the Croatian national parks for avian diversity. Some 157 species have been counted, of which 70 have been recorded as breeding there. Recent findings list about 20 species of
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466:) over a distance of some 8 kilometres (5.0 mi), aligned in a southānorth direction. The lakes collectively cover an area of about 0.77 square miles, the water exiting from the lowest lake forming the
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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
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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
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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
656:, 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.
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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
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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,
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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.
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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
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within this area. Despite the vicinity to the Mediterranean climatic region, a moderate mountainous climate prevails at the Plitvice Lakes. These climatic conditions prevail because of the
426:
Each year, more than 1 million visitors are recorded, making the national park the most popular tourist attraction in Croatia. Entrance is subject to variable charges, between 10 and 40
1287:, another small river flows into the lakes. This river is fed by permanent springs; the water quantity, however, varies. Temporarily, water from other, usually dry, creeks reaches
1836:
Recent scientific evidence indicates that vegetation is not primarily responsible for the extraction of carbonate from the flowing water. However, plants indirectly contribute to
3406:
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".
1738:
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According to a tale, a hajduk named NovakoviÄ was thrown off his horse into this lake. Other reports say that a man named NovakoviÄ used to offer boat rides across this lake.
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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.
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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
2682:. The Croatian rebellion was put down by Austrian authorities. Kvaternik propagated the rule of law and argued for the liberation from Austrian-Hungarian predominance.
1729:
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).
102:
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2018:
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and thus the landscape of this area. The emerging travertine barriers decelerated and retained the flowing water. These dams are continuously growing in height.
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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
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List in 1979 in recognition of its "outstanding natural beauty, and the undisturbed production of travertine (tufa) through chemical and biological action".
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The particular geographic position of the Plitvice Lakes and the specific climate features contributed to the emergence of many natural phenomena and a rich
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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.
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According to a legend, the lake was named after a shepherd called Mile who drowned in it, or after the miller Mile PeriÅ”iÄ who owned a mill at the lake.
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2104:, a 79.50 ha virgin forest in the northwestern part of the park. Some of the beech and fir trees in this area of the park are up to 700 years old.
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The name comes from the fences that have been built by farmers as delimitation between the farmlands and the lakes. The farmers used stakes (Croatian
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style, which served for a few decades for tourist and public purpose, until the construction of the first hotel inside villa "DevÄiÄevac" in 1890.
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is mainly found in Lake Kozjak. These species developed in different life conditions independently from each other within the various lakes.
1830:
4083:"Kreiszeitung.de. "Kroatien: Schatz hinterm Silbersee", 25. September 2010: The penalty for bathing in the lakes was about 70 euros in 2010"
3074:. The existing wooden paths are anchored within the travertine sediments, creating the danger of seepage and cracks of the weak travertine.
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measures, means an almost untouched landscape has been preserved. The partially primeval beech and fir forests host species such as the
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HorvatinÄiÄ, N. (1999) Starost sedre PlitviÄkih jezera. Priroda: mjeseÄnik za popularizaciju prirodnih znanosti i ekologije, 89, 20-22
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was also produced at some locations within the national park. (KaluÄerovac in the lower lakes served as scenery for the Silver Lake.)
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Up until the 20th century, social gatherings during the winter months, when no agricultural activities could be performed, called "
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novels were shot at the Plitvice Lakes (mainly German-French-Yugoslav coproductions). The most successful film of this series,
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mountain, which also represents the border to Bosnia and Hercegovina. Plitvice Lakes National Park is situated in the Plitvice
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route. The Plitvica river for example loses even up to 97 percent of its original quantity of carbon dioxide along its route.
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Within the national park area there are 19 small settlements. Altogether they form the Plitvice Lakes municipality (Croatian
4035:"Sedra PlitviÄkih jezera, K. KovaÄ (zit. n. Hrvoje IvekoviÄ, "Kemija na PlitviÄkim jezerima, Priroda 47 (1960) 10; 376-379)"
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virtually drill their path through the rock. Furthermore, there are only a few lakes at the Lower Lakes. They have formed a
498:. This name was designated because of natural phenomena that have created the lakes. Nature formed shallow basins (Croatian
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2499:. The Croats eventually defied Avar control and settled permanently in this region. In medieval times, frequent attacks by
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and unite at one of the bridges in this village. From this place onwards to the lakes, the water masses are referred to as
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already inhabiting the region and serving in the Austrian military, many central Europeans migrated to the region as did
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621:) west of the national park and thus circumvents the protected area. Plitvice Lakes National Park can be reached from
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People reported that a villager named BatiniÄ used to dwell at this lake. Others say that a grandmother (Croatian
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as the new king of Croatia in the hope of resources to ward of the Ottoman advance. In 1528, the area fell to the
1792:). This phenomenon particularly occurs on abundantly available mosses, enabling better adherence of the crystals.
408:. The important northāsouth road that passes through the national park area connects the Croatian inland with the
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4422:"PlitviÄka jezera pucaju po Å”avovima: HoÄemo li postati generacija koja je uspjela "ubiti" biser hrvatskog krÅ”a?"
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4370:(in Croatian). Vol. II.a. Zagreb: Ministry of Construction and Spatial Planning (Croatia). 2014. p. 89
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GuÅ”iÄ, B. & MarkoviÄ, M. (ed.) (1974) PlitviÄka jezera - Äovjek i priroda, Zagreb, Nacionalni park Plitvice
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The area of the national park is home to a wide variety of animal and bird species. Fauna such as the European
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Mosses, algae and water plants play a major role in forming the unique landscape of the Plitvice Lakes and its
1306:(English "confluence" or "composition"). The waterbodies of the Plitvice Lakes and the River Plitvice form the
17:
3344:, who defeated the Turks, was shot down at this lake. It could also have been named after a brig and GaloviÄ.
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Consolidated tufa. Older, hardened sediments. This porous type of rock is very sensitive to physical impacts.
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The protected area extends over 296.85 square kilometres (73,350 acres). About 90% of this area is part of
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The area of Plitvice Lakes National Park extends across two political subdivisions or counties (Croatian
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1428:). Usually, in spring and fall (autumn) the largest rain quantities are measured. The average relative
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In the future, the analysis of underground water courses could be an interesting field of research for
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1545:), which is not very soluble in water. Calcite, however, is dissolved by carbonic acid, thus creating
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Humans have inhabited the Plitvice Lakes area for thousands of years. It has been settled in turn by
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The shortest linear distance between the Adriatic coast and the national park is 55 km (34
4054:
ZduniÄ, D. & MovÄan, J. (ed.) (1985) Plitvice, Zagreb, Nacionalni park PlitviÄka jezera, Spektar
5592:
4186:
2569:
almost the entire Croatian nobility was killed. The Ottomans advanced far into Western lands up to
1878:
209:
4950:
4803:
4288:
3858:
1453:, which is abundantly available in the waters of this karst area. These sedimentations are called
3160:
Each of the Plitvice Lakes has a story or legend to tell. Most lake names stem from true events.
2886:
2878:
2616:
2264:), whose emergence may be attributed to climate change, have also been discovered. The number of
1109:
381:
3805:
FraniÄ, D. (1910) PlitviÄka jezera i njihova okolica, Zagreb, Tisak kraljevske zemaljske tiskare
4999:
4966:
4879:
3466:
Allegedly, the treasure of a man named Gavan (the Gavanovo treasure) lies hidden in this lake.
2578:
2566:
2213:
560:
405:
3933:"Plitvice Lakes National Park, Sixteen Pearls of the Plitvice Lakes, Dr. sc. SreÄko BožiÄeviÄ"
3600:"Mrak TaritaÅ” i ZmajloviÄ odobrili betonizaciju Plitvica: UNESCO Hrvatskoj dao rok do veljaÄe"
5655:
5212:
5144:
3573:
2870:
2640:
2355:
2157:
2054:
1978:
1424:
On average, the annual precipitation rate at the Plitvice Lakes is 1,500 mm (59.06
706:
The sixteen lakes that can be seen from the surface are grouped into the twelve Upper Lakes (
390:
5468:
5313:
5217:
3839:
2557:
In 1493, not far away from the Plitvice Lakes a decisive battle in Croatian history between
1195:, this has given rise to the most distinctive feature of the lakes. Right at the lakes, the
1176:
at 1279 m, the lowest elevation is reached at 367 m at the bridge across the Korana river).
5763:
5544:
4323:"International Criminal Tribunal for the Former Yugoslavia, Judgement against Milan MartiÄ"
3572:
region famous for its calc-sinter rivers. Most popular, particularly with cruise ships, is
2367:
2181:
2148:
identified. Twelve amphibian and several reptile species have been recorded, including the
2141:
1133:
mountain range, which acts as a climatic separator between the coastal region and the Lika
5358:
4850:
4122:"Plitvice Lakes National Park, Äorkova uvala Virgin Forest (Prof. dr. sc. Branimir PrpiÄ)"
3386:) or monastery which had once been situated on the peak between Kozjak lake and this one.
2770:, a Czech from Zagreb, built a restaurant and accommodation. In 1893, JaneÄek founded the
510:
means "shallow"), which have been filled with water. For centuries, water has changed the
462:
from the mountains, descending from an altitude of 636 to 503 m (2,087 to 1,650
8:
5836:
5640:
5539:
4861:
4760:
4034:
3936:
3556:
2636:
2071:
179:
5353:
4761:
Explore Plitvice Lakes National Park in the UNESCO collection on Google Arts and Culture
4322:
4247:
3362:
According to a legend, a man named Mile MiriÄ from MiriÄ Stropina drowned in this lake.
2782:. She gave money from concerts to preserve the park, upgrade tracks and build pathways.
2488:
in 454, the Ostrogoths were rewarded with a federation agreement with the Roman Empire.
1409:
1077:
5610:
5504:
5119:
3531:
2671:
2551:
2388:
2311:
2207:
2129:
2061:
2034:
1495:
4222:
683:
5729:
5650:
5583:
4899:
4685:
4654:
4585:
2739:
2712:, since imperial military officers used to reside in this location. For the visit of
2590:
2149:
1713:
1505:
The dissolution of limestone happens through alteration processes and the effects of
1470:
1450:
365:
46:
5448:
2690:
1972:
1092:
The Plitvice Lakes area has always been regarded as part of the historic regions of
659:
345:
64:
5791:
5428:
4884:
4301:
2410:
2323:
2177:
2137:
2079:
1998:
species so far recorded in the area of the national park. 75 species of plants are
1856:
calcite adhere. The most significant plants of this kind are mosses of the species
1701:
1351:
1327:
1295:
1082:
696:
518:
416:
82:
5796:
5645:
5318:
4808:
4268:
2810:
2503:
posed a permanent threat to the settled population. The lakes formed part of the
1951:
1243:
bones were found, so these sites may be considered paleontologically significant.
5831:
5826:
5368:
5023:
4929:
Ancient and Primeval Beech Forests of the Carpathians and Other Regions of Europe
3862:
3843:
2903:
2881:(also called the "Plitvice Bloody Easter"), the first armed confrontation of the
2849:
2846:
2821:
2675:
2531:
2492:
2485:
2437:
2100:
217 hectares (0.72 percent) are water areas. A unique area is the forest of
2088:
1904:
1784:
forms larger surfaces at these places, increased quantities of carbon dioxide (CO
1530:
1385:
1335:
1251:
1184:
700:
695:). Its 296.85 square kilometres (114.61 sq mi) area is divided between
420:
86:
5816:
5698:
5600:
5559:
4594:
1649:
1259:
The Plitvice Lakes originate in the south of the park area at the confluence of
5488:
5293:
5283:
5197:
5007:
4875:
4364:
Prostorni plan podruÄja posebnih obilježja Nacionalnog parka "PlitviÄka Jezera"
3543:
3071:
2658:
In 1805, another major rule change happened, which created an economic upturn.
2586:
2562:
2449:
1885:
1518:
1275:(English for "water current", can also mean "root" or "origin"). At the bay of
645:
641:
459:
5673:
5625:
5172:
2885:
that resulted in fatalities. The park was held by local Serb rebels backed by
2806:
1903:
Porous rock that has been exposed to external effects, for example rainwater (
1841:
5856:
5811:
5801:
5688:
5683:
5678:
5635:
5338:
5182:
5062:
4658:
3772:
3744:
3616:
There are seven other national parks in Croatia, as well as ten nature parks.
3599:
3539:
2899:
2866:
2779:
2453:
2395:
2249:
2245:
2230:
2133:
1772:
1506:
1446:
1339:
1137:. For centuries, legends have been created about this mythic mountain range.
637:
551:. The national park is located at the national route D1 ZagrebāSplit between
253:
117:
104:
5620:
5509:
3888:
Meridijani, 3/2002, 30. Å afarek, G. PlitviÄka jezera - 16 srebrnih stepenica
3327:
The name originates from water whirling downward in the middle of the lake.
2803:
National Anti-Fascist Council of the People's Liberation of Croatia (ZAVNOH)
1158:
1146:
544:
5821:
5786:
5781:
5773:
5750:
5605:
5483:
5478:
5458:
5433:
5388:
5348:
5328:
3141:
3104:
2461:
2433:
2333:
2173:
1750:
1429:
1330:. The typical feature of this karst area is brittle or porous rock, mostly
1154:
1126:
1101:
614:
548:
467:
409:
5443:
4733:
3230:
According to a legend, a roma (gypsy) drowned in this lake while fishing.
2701:
earth or people adapted the flow of the rivers to their individual needs.
1674:
1039:) at the end of the Lower Lakes, over which the Plitvica river falls, and
5806:
5413:
5408:
5228:
5047:
4894:
3547:
3123:
2785:
During the First World War, the Croatian parliament in Zagreb passed the
2632:
2546:
2345:
2257:
1861:
1380:
1162:
1142:
540:
463:
5403:
4794:
High resolution photos of lakes and waterfalls in Plitvice National Park
4770:
4743:
3526:
Comparable phenomena to those prevailing at the Plitvice Lakes exist at
1165:
mountain (SeliÅ”ki Vrh peak at 1,280 m), and MedveÄak (884 m).
667:
5841:
5615:
5473:
5373:
5343:
5298:
5187:
4970:
3568:
3551:
3535:
2842:
were already demolished during the 1980s by the Communist authorities.
2481:
2469:
2465:
2239:
2165:
2121:
2112:
1961:
1927:
1849:
1848:). Depending on the species found locally, various biological types of
1813:
1458:
1413:
1362:
440:
5564:
5383:
4916:
4649:[Removing Phosphates from Water Bodies with the Aid of Slag].
4104:"NP PlitviÄka jezera, Endemske vrste (Prof. dr. sc. Nedeljka Å egulja)"
2829:
1808:
1767:
5693:
5134:
4938:
4855:
4755:
3564:
3115:
2519:
2421:
2301:
2125:
1908:
1833:. whose efforts contributed to the national protection of the lakes.
1812:
Calcium-carbonate-encrusted, yet growing moss: early stage of porous
1761:
1389:
1331:
1267:("Black River"). These rivers originate south of the municipality of
1240:
1188:
1169:
511:
458:
The 16 lakes are separated into an upper and lower cluster formed by
167:
5519:
5393:
4889:
4778:
4401:"Broj posjetitelja u NP PlitviÄka jezera u razdoblju 2006.-2011. g."
4289:
International Union for Conservation of Nature and Natural Resources
1756:
1745:
1445:
The lakes of Plitvice are a result of century-old processes and the
653:
576:
572:
495:
221:
5524:
5039:
5035:
5003:
3633:. United Nations Educational, Scientific, and Cultural Organization
3626:
2853:
2667:
2659:
2473:
2265:
2198:
1999:
1343:
1216:
1203:(68 m) above Lake KaluÄerovac can be visited. Other caves e.g. are
1086:
649:
556:
452:
5308:
4865:
4183:"The living world in the lakes and around them, Milorad MrakovÄiÄ"
3136:
2869:
of the national park were recorded. The park was inscribed on the
1985:
The Plitvice Lakes national park is heavily forested, mainly with
580:
5569:
5549:
5418:
5260:
5207:
5177:
5162:
5114:
5109:
5051:
5031:
5015:
4995:
4991:
4987:
3527:
3131:
2652:
2574:
2570:
2515:
2500:
2003:
1682:
1150:
1134:
1130:
727:
599:
386:
90:
56:
5202:
2801:) in 1940. On June 14, 1943 one of the founding sessions of the
2237:) are also found. As a result of human interference the species
1318:
400:
The national park was founded in 1949 and is in the mountainous
5898:
Register of Protected Natural Values of the Republic of Croatia
5514:
5453:
5363:
5323:
5167:
5027:
5011:
4974:
4906:
4721:
4498:"Croatia: Pristine Nature in Peril | DW | 24.05.2018"
3500:
at the canyon edge. People used to seek advice from this monk.
2802:
2704:
Already in 1861, an accommodation for travelers was erected at
2609:
2534:. Today, only ancient wall remnants of this building (Croatian
2496:
2445:
2425:
2399:
1990:
1737:
1670:
1417:
1398:
1307:
1097:
564:
523:
491:
5288:
3745:"Five Things You May Not Know About Plitvice Lakes in Croatia"
563:. Other larger municipalities within the surrounding area are
5554:
5534:
5529:
5463:
5423:
5398:
5333:
5303:
5192:
5124:
5043:
5019:
4980:
4921:
4065:"Plitvice Lakes National Park, Otvorenje ZSC-a "Ivo Pevalek""
2613:
2441:
2429:
1986:
1857:
1776:
1696:
1678:
1355:
1347:
1192:
1180:
675:
607:
552:
448:
401:
389:. In 1979, Plitvice Lakes National Park was inscribed on the
1388:
rock. The Lower lakes in the north predominantly consist of
1298:
reaches the Plitvice lake chain at the northern end via the
1153:
which is surrounded by three mountains that are part of the
613:
The fastest northāsouth road connection within Croatia, the
602:
mountain range travelers reach the Croatian karst plains of
5438:
5378:
4651:
Priroda: popularni Äasopis hrvatskog prirodoslovnog druÅ”tva
3092:
2755:
2685:
2663:
2514:
Croat rule and particularly the rule of the noble families
2268:, which were almost extinct, is now again increasing. Rare
1955:
Bees, dragonflies and other insects gather in lush meadows.
1916:
1845:
1837:
1821:
1722:
1666:
1454:
1425:
1376:
1093:
618:
603:
595:
591:
587:
539:
The Plitvice Lakes have formed in a depression between the
444:
427:
394:
353:
249:
4475:
3773:"Lika-Senj County Tourist Association, The Plitvice Lakes"
4912:
Venetian Works of Defence between 15th and 17th centuries
2269:
2193:
1994:
1681:, similar phenomena occur. This part of the town, called
1035:
The highest waterfalls are the Large Waterfall (Croatian
2906:, and the majority of the Serb population was expelled.
2559:
Kingdom of Croatia (then in personal union with Hungary)
2217:) are indigenous subspecies of fish found in the lakes.
4302:"UNESCO World Heritage Committee report, December 1998"
3855:
3815:
3677:"Plitvice Lakes: the Ultimate Guide to Visiting (2023)"
2833:
Bus connection offered to visitors of the national park
1440:
2495:
settled in this region, which were accompanied by the
2010:
Examples of endemic plants found in the national park:
1889:
Previously, swimming had been allowed in Lake Kozjak.
3978:
3976:
3836:
2708:. The local population called this accommodation the
2538:) exist. The foundation was made of travertine rock.
2279:
Examples of some animals found in the national park:
1829:). The leading scientist arguing for this theory was
486:
was first mentioned in a written document in 1777 by
385:) is one of the oldest and largest national parks in
4512:"Video. The Custom of Social Gathering. LiÄko prelo"
4007:"Logo Science Magazine, Author: Dr. Alexander Stahr"
1145:
mountain, while the eastern side is enclosed by the
393:
list, for its outstanding and picturesque series of
327:
4838:
4782:(in Croatian, English, German, Italian, and French)
4774:(in Croatian, English, German, Italian, and French)
4669:
Plan upravljanja Nacionalnog parka PlitviÄka Jezera
4612:, Tisak kraljevske zemaljske tiskare, Zagreb 1910 (
4009:(in German). Tk-logo.de. 2013-08-09. Archived from
2776:
DruÅ”tvo za ureÄenje i poljepÅ”anje PlitviÄkih jezera
1947:
Barrier between the Gavanovac and KaluÄerovac lakes
335:
Location of Plitvice Lakes National Park in Croatia
3973:
3884:
3882:
3767:
3765:
3659:"PlitviÄka jezera s rekordnim brojem posjetitelja"
2772:Society for the preservation of the Plitvice Lakes
2276:) can be found in the karst caves of this region.
2196:in the area, among them rare species in the genus
1871:
1691:
4601:, GrafiÄki zavod Hrvatske, Spektar, Zagreb 1985 (
4291:, Review of World Heritage Nomination, April 1979
4204:"Plitvice Lakes National Park, cultural heritage"
3703:"Price list - Nacionalni park "PlitviÄka jezera""
3521:
3488:According to reports, a monk or hermit (Croatian
3203:), poles, scrub and earth to build these fences.
2541:
2405:
2144:can be found there, along with commoner species.
5854:
4779:Official Website of Plitvice Lakes Tourist Board
4771:Official Website of Plitvice Lakes National Park
1653:The Veliki PrŔtavac waterfall at the Upper Lakes
1313:
1161:mountain (Gornja PljeŔevica peak 1,640 m),
3879:
3762:
3424:On the island in the middle of the lake (today
3085:
2456:the region was incorporated as the province of
1199:(145 m) before the second Korana waterfall and
606:. These plains are characterized by many karst
161:Javna ustanova Nacionalni park PlitviÄka jezera
5092:
4495:
4220:
3966:
3964:
3962:
3898:Plitvice Lakes National ParkāBasic Information
3727:"Plitvice Lakes National Park, protected area"
3652:
3650:
3648:
2394:route and have always been a meeting place of
1433:lakes are frozen during December and January.
1373:) can also be observed at the Plitvice Lakes.
38:
5244:
5078:
4824:
4440:"Safety and security - Croatia travel advice"
3382:The lake is named after a building (Croatian
3096:wear their costumes during military service.
2816:
1732:
4799:Plitvice Lakes National Park Picture gallery
4674:Plitvice Lakes National Park Management Plan
4653:. Vol. 74, no. 9ā10. p. 242.
4177:
4175:
2464:. The areas of the neighborly tribes of the
2248:have been introduced to this ecosystem. The
1557:). This is shown by the following formulas:
1509:. In a natural environment, carbonic acid (H
4548:
4525:
4029:
4027:
3959:
3645:
3155:
2787:Law on the Protection of the Plitvice Lakes
1677:rivers, right in the center of the town of
1669:) north of the lakes at the conflux of the
1215:(153 m). Within the national park, several
594:the distance is about 110 km (68
145:367 m (Korana bridge), 1279 m (SeliŔki vrh)
5258:
5251:
5237:
5085:
5071:
4831:
4817:
4647:"Uklanjanje fosfata iz voda pomoÄu troske"
4644:
4584:, TuristiÄka naklada d.o.o., Zagreb 2005,
4514:. Croatian Ministry of Culture. 2013-07-23
4198:
4196:
3114:Local cuisine consists of drinks, such as
2221:is found mostly in the Upper Lakes, while
1844:for sedimentation, generating travertine (
1803:
1644:
430:per adult per day in summer (as of 2024).
404:area of central Croatia, at the border to
55:
4172:
3801:
3799:
3797:
3795:
3793:
3791:
3789:
1115:
4634:, pp. 164ā166 (Lonely Planet, 2005)
4623:, GrafiÄki zavod Hrvatske, Zagreb 1974 (
4357:
4355:
4353:
4351:
4349:
4347:
4345:
4343:
4341:
4246:. Getaway.ninemsn.com.au. Archived from
4085:(in German). Kreiszeitung.de. 2010-09-24
4024:
3952:
3950:
3948:
3946:
3909:
3907:
3340:Allegedly, a bandit chief named captain
2828:
2820:
2689:
2686:Farmlands becoming an area of recreation
2545:
2409:
2111:
1971:
1950:
1942:
1807:
1766:
1755:
1744:
1736:
1695:
1648:
1408:
1317:
1255:Bridge over a river with small waterfall
1250:
1168:The afforested mountain slopes serve as
682:
674:
666:
658:
397:lakes, caves, and connected waterfalls.
352:
344:
4193:
3657:portal, SEEbiz eu-regionalni poslovni.
3594:
3592:
3590:
3588:
1700:The large waterfall (78 m) of the
1488:
1342:phenomena being referred to as dolina (
1338:. This configuration creates different
534:
14:
5855:
4619:Branimir GuÅ”iÄ, Mirko MarkoviÄ (ed.):
4395:
4393:
4391:
4389:
4387:
4385:
4048:
3982:
3786:
3122:), wine and coffee or dishes, such as
443:, which is deposited by the action of
357:View of the lakes on a satellite image
5232:
5066:
4812:
4766:Plitvice Lakes Management Plan (2007)
4665:
4554:
4531:
4338:
4162:"Plitvice Lakes National Park, Fauna"
3943:
3915:"Plitvice Lakes National Park, Flora"
3904:
3873:
3619:
3542:in Bosnia and Herzegovina and at the
3252:The name stems from its round shape.
2893:(JNA) as part of the self-proclaimed
1108:that was under direct control of the
419:, while the remaining 10% is part of
380:
3585:
2635:(Ban). The area then formed part of
2524:Order of Saint Paul the First Hermit
1441:The dissolution and creation of rock
1379:sediments have been formed from the
1227:on VrÅ”iÄ (-154 m, length 110 m). In
590:). By road from the coastal town of
5893:Protected areas of Lika-Senj County
5883:Protected areas established in 1949
4804:Plitvice lakes winter photo gallery
4621:PlitviÄka jezera ā Äovjek i priroda
4382:
3719:
3276:) might have drowned in this lake.
2714:Crown Princess StƩphanie of Belgium
1525:) from the air or from rainwater (H
1473:, apart from many other names like
1401:, which continues as river Korana.
517:Some scientists refer to the river
349:Map of Plitvice Lakes National Park
24:
5888:Protected areas of Karlovac County
4949:
4787:
4666:Å ikiÄ, Zoran, ed. (October 2007).
4610:PlitviÄka jezera i njihova okolica
4142:. Nacionalni park PlitviÄka jezera
3656:
1938:
1541:) mainly consists of calcite (CaCO
1517:) is formed by the dissolution of
1179:The national Park is underlain by
284:Protected Natural Value of Croatia
25:
5924:
4749:
4714:
4603:German, Croatian, English, French
2678:was killed north of the lakes at
2600:ordered the establishment of the
1771:Fish in the crystal-clear water;
648:. The nearest train stations are
617:, runs about 50 km (31
5582:
4732:
4720:
4476:"VeÄernji list, August 29, 2007"
2762:At the same place, today called
1892:
1685:, is often being referred to as
1057:Veliki slap ("Large Waterfall")
547:mountain in the east amidst the
370:Nacionalni park PlitviÄka jezera
326:
319:
294:Nacionalni park PlitviÄka jezera
63:
40:Nacionalni park PlitviÄka jezera
5903:World Heritage Sites in Croatia
5863:Dinaric Mountains mixed forests
4851:Cathedral of St. James, Å ibenik
4840:World Heritage Sites in Croatia
4574:
4504:
4489:
4468:
4450:
4432:
4414:
4315:
4294:
4282:
4261:
4236:
4214:
4154:
4132:
4114:
4096:
4075:
4057:
3999:
3925:
3891:
3867:
3848:
3829:
3808:
2813:at the Plitvice Lakes in 1911.
2795:League of Communists of Croatia
2507:which in 1102 elected to be in
1872:Factors impeding tufa formation
1692:Preconditions for sedimentation
1081:). The municipality is part of
5913:1949 establishments in Croatia
5908:World Heritage Sites in Danger
4934:Northern Velebit National Park
4559:. Plitvice Lakes National Park
4536:. Plitvice Lakes National Park
4496:Welle (www.dw.com), Deutsche.
3987:. Plitvice Lakes National Park
3816:"Map24.de, distance measuring"
3737:
3695:
3669:
3627:"Plitvice Lakes National Park"
3610:
3522:Comparable phenomena worldwide
2730:Path" (Croatian Å tefanijin put
2718:Crown Prince Rudolf of Austria
2583:Ferdinand, Archduke of Austria
2542:Ottoman Wars and the Habsburgs
2484:took over the rule. After the
2406:Early history and medieval age
2046:Examples of other rare plants:
1687:"the Small Lakes of Plitvice."
1213:GolubnjaÄa at HomoljaÄko Field
13:
1:
3579:
3496:just next to the water or in
2871:UNESCO World Natural Heritage
2799:Savez komunista Hrvatske, SKH
2645:Socialist Republic of Croatia
1665:About 30 km (18.64
1314:Properties of the underground
1104:, the region was part of the
543:mountain in the west and the
526:river in northern direction.
4756:UNESCO World Heritage Centre
4740:travel guide from Wikivoyage
4727:Plitvice Lakes National Park
4682:Croatian Ministry of Culture
3631:UNESCO World Heritage Centre
3086:Local customs and traditions
2883:Croatian War of Independence
2845:Between 1962 and 1968, many
710:) and the four Lower Lakes (
477:
362:Plitvice Lakes National Park
33:Plitvice Lakes National Park
7:
4637:Radovan RadovinoviÄ (ed.),
3985:"Nature creates waterfalls"
3140:, paprika sausage, roasted
2895:Republic of Serbian Krajina
2865:During the 1970s, detailed
2859:Treasure of the Silver Lake
2651:. Today, it is part of the
2579:Croatian Parliament elected
2509:personal union with Hungary
2505:medieval kingdom of Croatia
2262:Scardinius erythropthalmus
529:
10:
5929:
5735:Large waterfall (Plitvice)
5094:Protected areas of Croatia
4641:(Naklada Naprijed, Zagreb)
4223:"Croatian classical music"
2817:The lakes as national park
2608:In addition to the native
2602:Croatian Military Frontier
2386:
2382:
1976:The lady's-slipper orchid
1741:Cross-section of a barrier
1733:Thresholds become barriers
1404:
1191:with associated lakes and
1120:
1106:Croatian Military Frontier
180:UNESCO World Heritage Site
168:www.np-plitvicka-jezera.hr
5878:National parks of Croatia
5772:
5743:
5707:
5664:
5591:
5580:
5497:
5276:
5267:
5218:Žumberak-Samoborsko gorje
5153:
5100:
4961:
4947:
4860:Episcopal Complex of the
4846:
4478:. Vecernji.hr. 2013-08-25
3681:The World Is A Playground
3561:Yellowstone National Park
3492:) used to live either in
3207:Legend of the Black Queen
2622:the garden of the devil (
1547:calcium hydrogencarbonate
1246:
1085:. The seat is located in
636:The nearest airports are
314:
310:
306:
298:
290:
281:
277:
269:
261:
247:
243:
235:
227:
217:
202:
194:
186:
177:
173:
163:HR-53231 PlitviÄka jezera
157:
149:
141:
133:
96:
78:
74:
54:
37:
32:
3837:Croatian Motorways (HAC)
3172:Approximate translation
3156:Lake names and anecdotes
2491:During the 6th century,
2107:
1967:
1879:Dissolved Organic Carbon
1816:formation as in Plitvice
1704:river at the Lower Lakes
610:(e.g. the Gacko polje).
598:). After traversing the
153:1,367,304 (in 2015)
27:National park in Croatia
4500:– via www.dw.com.
4221:Darko Zubrinic (1995).
3268:Lake Batin/BatiÄ's Lake
2879:Plitvice Lakes incident
2750:In 1890, the tradesman
2666:fell under the rule of
2620:also used to be called
2589:and was retaken by the
2565:took place. During the
2244:and the North American
2019:Edraianthus tenuifolius
1852:can be differentiated.
1804:Influence of vegetation
1645:Sedimentation processes
1302:. This place is called
1110:Habsburg Council of War
679:Paths between the lakes
433:
165:Tel. +385 (0)53 751 015
5873:Lake groups of Croatia
5000:Bosnia and Herzegovina
4967:Bosnia and Herzegovina
4955:
4744:Maps of Plitvice Lakes
4738:Plitvice National Park
3856:Croatian Railways (HŽ)
3707:np-plitvicka-jezera.hr
3337:Galov's/GaloviÄ's Lake
3119:
2902:in August 1995 during
2891:Yugoslav People's Army
2834:
2826:
2743:
2697:
2567:Battle of Krbava Field
2554:
2417:
2214:Salmo trutta lacustris
2117:
1982:
1956:
1948:
1817:
1780:
1764:
1753:
1742:
1705:
1654:
1421:
1323:
1322:The Lower Lakes canyon
1256:
1116:Topography and geology
688:
680:
672:
664:
561:Bosnia and Herzegovina
406:Bosnia and Herzegovina
369:
358:
350:
39:
4953:
4639:The Croatian Adriatic
4632:Lonely Planet Croatia
4244:"Lake-lustre Croatia"
4225:. Croatianhistory.net
4189:on December 16, 2008.
4128:on December 16, 2008.
4110:on December 16, 2008.
4071:on December 16, 2008.
3983:StilinoviÄ, Božidar.
3939:on December 16, 2008.
2832:
2824:
2693:
2643:and then part of the
2641:Kingdom of Yugoslavia
2581:the Habsburg monarch
2549:
2476:were united into the
2413:
2402:cultural influences.
2356:White-throated dipper
2158:european green lizard
2115:
2055:Cypripedium calceolus
1979:Cypripedium calceolus
1975:
1954:
1946:
1811:
1770:
1759:
1748:
1740:
1712:The sedimentation of
1699:
1652:
1412:
1321:
1263:("White River'") and
1254:
1223:pit-cave (-203 m) or
686:
678:
670:
662:
391:UNESCO World Heritage
356:
348:
118:44.88056Ā°N 15.61611Ā°E
5764:Sava-Odra-Sava Canal
5665:Valleys, estuaries,
4880:Palace of Diocletian
4729:at Wikimedia Commons
4269:"Rialto Film Berlin"
4037:. Eskola.chem.pmf.hr
3511:NovakoviÄ's crossing
2722:Emperor Franz Joseph
2649:Socialist Yugoslavia
2480:. Successively, the
2478:province of Dalmatia
2368:European pond turtle
2182:european pond turtle
1489:Alteration processes
1239:at the Lower Lakes,
1209:Vila Jezerkinje Cave
1043:at the Upper Lakes.
535:Routes and distances
61:The large waterfall
5837:St. Anthony Channel
4862:Euphrasian Basilica
4645:UredniŔtvo (1986).
4580:Mato Njavro (ed.):
4555:BožiÄeviÄ, SreÄko.
4532:BožiÄeviÄ, SreÄko.
3557:Mammoth Hot Springs
2915:Number of visitors
2653:Republic of Croatia
2637:Banovina of Croatia
2072:Pinguicula vulgaris
2069:Common butterwort (
2026:Ranunculus scutatus
1496:radiocarbon datings
1269:PlitviÄki Ljeskovac
1219:exist, such as the
699:(90.7 percent) and
625:in the north, from
559:in the vicinity of
382:[plĆ®tŹitse]
114: /
5868:Forests of Croatia
4956:
3861:2013-10-31 at the
3842:2018-12-08 at the
3775:. Lickosenjska.com
3733:on March 28, 2009.
3574:Dunn's River Falls
3532:Krka National Park
2887:Slobodan MiloÅ”eviÄ
2835:
2827:
2698:
2672:Illyrian provinces
2670:, who founded the
2555:
2552:Lika-Krbava County
2550:Map of the former
2418:
2389:History of Croatia
2350:Triturus alpestris
2312:Eurasian eagle-owl
2208:Salmo trutta fario
2118:
2062:Ligularia sibirica
2035:Scilla litardierei
1983:
1957:
1949:
1818:
1798:MatijaÅ”eviÄa draga
1781:
1765:
1754:
1743:
1706:
1655:
1422:
1420:north of the lakes
1324:
1257:
741:ProÅ”Äansko jezero
689:
687:Lower lakes canyon
681:
673:
665:
359:
351:
218:Reference no.
123:44.88056; 15.61611
5850:
5849:
5757:Danube-Sava Canal
5667:canyons, wetlands
5578:
5577:
5226:
5225:
5060:
5059:
4725:Media related to
4691:978-953-6240-83-8
4608:Dragutin FraniÄ:
4557:"The lower lakes"
4534:"The upper lakes"
4210:on March 2, 2009.
4168:on March 2, 2009.
3921:on March 2, 2009.
3550:lakes within the
3546:in Bulgaria. The
3519:
3518:
3475:KaluÄerovo Jezero
3180:ProÅ”Äansko jezero
3063:
3062:
2695:ProÅ”Äansko jezero
2593:150 years later.
2380:
2379:
2338:Aquila chrysaetos
2254:Squalius cephalus
2235:Phoxinus phoxinus
2170:Natrix tessellata
2150:viviparous lizard
2097:
2096:
2043:
2042:
1936:
1935:
1775:are driving away
1714:calcium carbonate
1638:
1637:
1529:O). Limestone or
1461:(both are called
1289:ProÅ”Äansko jezero
1285:ProÅ”Äansko jezero
1072:
1071:
1033:
1032:
894:Gradinsko jezero
663:Galovac waterfall
631:Gornja PloÄa exit
488:Dominik VukasoviÄ
343:
342:
213:
16:(Redirected from
5920:
5792:Bay of Mali Ston
5656:Vrana (Dalmatia)
5586:
5274:
5273:
5253:
5246:
5239:
5230:
5229:
5130:Northern Velebit
5087:
5080:
5073:
5064:
5063:
4885:Stari Grad Plain
4833:
4826:
4819:
4810:
4809:
4783:
4775:
4736:
4724:
4710:
4708:
4706:
4700:
4694:. Archived from
4679:
4662:
4597:, Drago ZduniÄ:
4569:
4568:
4566:
4564:
4552:
4546:
4545:
4543:
4541:
4529:
4523:
4522:
4520:
4519:
4508:
4502:
4501:
4493:
4487:
4486:
4484:
4483:
4472:
4466:
4465:
4458:"Plitvice Lakes"
4454:
4448:
4447:
4436:
4430:
4429:
4418:
4412:
4411:
4409:
4407:
4397:
4380:
4379:
4377:
4375:
4369:
4359:
4336:
4335:
4333:
4332:
4327:
4319:
4313:
4312:
4310:
4309:
4304:. Whc.unesco.org
4298:
4292:
4286:
4280:
4279:
4277:
4276:
4265:
4259:
4258:
4256:
4255:
4240:
4234:
4233:
4231:
4230:
4218:
4212:
4211:
4206:. Archived from
4200:
4191:
4190:
4185:. Archived from
4179:
4170:
4169:
4164:. Archived from
4158:
4152:
4151:
4149:
4147:
4136:
4130:
4129:
4124:. Archived from
4118:
4112:
4111:
4106:. Archived from
4100:
4094:
4093:
4091:
4090:
4079:
4073:
4072:
4067:. Archived from
4061:
4055:
4052:
4046:
4045:
4043:
4042:
4031:
4022:
4021:
4019:
4018:
4003:
3997:
3996:
3994:
3992:
3980:
3971:
3968:
3957:
3954:
3941:
3940:
3935:. Archived from
3929:
3923:
3922:
3917:. Archived from
3911:
3902:
3895:
3889:
3886:
3877:
3871:
3865:
3852:
3846:
3833:
3827:
3826:
3824:
3823:
3812:
3806:
3803:
3784:
3783:
3781:
3780:
3769:
3760:
3759:
3757:
3756:
3741:
3735:
3734:
3729:. Archived from
3723:
3717:
3716:
3714:
3713:
3699:
3693:
3692:
3690:
3688:
3673:
3667:
3666:
3654:
3643:
3642:
3640:
3638:
3623:
3617:
3614:
3608:
3607:
3596:
3534:, at the rivers
3530:(Slunj), at the
3367:Gradinsko jezero
3285:Jovinovac veliki
3221:Ciganovac jezero
3163:
3162:
2909:
2908:
2850:film productions
2633:Croatian viceroy
2532:Knights Templars
2415:Gradinsko jezero
2372:Emys orbicularis
2328:Mustela putorius
2324:European polecat
2282:
2281:
2274:Proteus anguinus
2186:Emys orbicularis
2178:Vipera ammodytes
2154:Lacerta vivipara
2138:European wildcat
2080:Telekia speciosa
2050:
2049:
2014:
2013:
1897:
1896:
1749:The cascades of
1560:
1559:
1371:rijeka ponornica
1340:geomorphological
1170:water reservoirs
1083:Lika-Senj County
1078:PlitviÄka Jezera
1065:Veliki PrŔtavac
1046:
1045:
996:NovakoviÄa brod
717:
716:
697:Lika-Senj County
417:Lika-Senj County
412:coastal region.
384:
379:
330:
329:
323:
207:
129:
128:
126:
125:
124:
119:
115:
112:
111:
110:
107:
83:Lika-Senj County
67:
59:
50:
42:
30:
29:
21:
5928:
5927:
5923:
5922:
5921:
5919:
5918:
5917:
5853:
5852:
5851:
5846:
5832:Vinodol Channel
5827:Velebit Channel
5768:
5739:
5703:
5666:
5660:
5587:
5574:
5493:
5277:Black Sea Basin
5263:
5259:Hydrography of
5257:
5227:
5222:
5149:
5096:
5091:
5061:
5056:
5024:North Macedonia
4957:
4954:Flag of Croatia
4945:
4842:
4837:
4790:
4788:Photo galleries
4781:
4773:
4752:
4717:
4704:
4702:
4698:
4692:
4680:(in Croatian).
4677:
4630:Jeanne Oliver,
4577:
4572:
4562:
4560:
4553:
4549:
4539:
4537:
4530:
4526:
4517:
4515:
4510:
4509:
4505:
4494:
4490:
4481:
4479:
4474:
4473:
4469:
4456:
4455:
4451:
4438:
4437:
4433:
4420:
4419:
4415:
4405:
4403:
4399:
4398:
4383:
4373:
4371:
4367:
4361:
4360:
4339:
4330:
4328:
4325:
4321:
4320:
4316:
4307:
4305:
4300:
4299:
4295:
4287:
4283:
4274:
4272:
4271:. Rialtofilm.de
4267:
4266:
4262:
4253:
4251:
4242:
4241:
4237:
4228:
4226:
4219:
4215:
4202:
4201:
4194:
4181:
4180:
4173:
4160:
4159:
4155:
4145:
4143:
4138:
4137:
4133:
4120:
4119:
4115:
4102:
4101:
4097:
4088:
4086:
4081:
4080:
4076:
4063:
4062:
4058:
4053:
4049:
4040:
4038:
4033:
4032:
4025:
4016:
4014:
4005:
4004:
4000:
3990:
3988:
3981:
3974:
3969:
3960:
3955:
3944:
3931:
3930:
3926:
3913:
3912:
3905:
3896:
3892:
3887:
3880:
3872:
3868:
3863:Wayback Machine
3853:
3849:
3844:Wayback Machine
3834:
3830:
3821:
3819:
3814:
3813:
3809:
3804:
3787:
3778:
3776:
3771:
3770:
3763:
3754:
3752:
3743:
3742:
3738:
3725:
3724:
3720:
3711:
3709:
3701:
3700:
3696:
3686:
3684:
3675:
3674:
3670:
3655:
3646:
3636:
3634:
3625:
3624:
3620:
3615:
3611:
3598:
3597:
3586:
3582:
3524:
3505:NovakoviÄa brod
3498:GolubnjaÄa Cave
3459:Okrugljak Donji
3458:
3456:
3455:Gavanovo Jezero
3437:Milanovo Jezero
3426:Å tefanijin otok
3396:
3372:
3349:Milinovo jezero
3303:
3262:
3242:
3240:
3220:
3193:
3191:
3158:
3088:
3082:Heritage site.
3072:pontoon bridges
2904:Operation Storm
2819:
2710:Emperor's house
2688:
2676:Eugen Kvaternik
2624:hortus diabolus
2591:Habsburg Empire
2577:. In 1527, the
2544:
2486:Battle of Nedao
2408:
2391:
2385:
2360:Cinclus cinclus
2285:Eurasian lynx (
2223:S. t. lacustris
2162:Lacerta viridis
2110:
2089:Daphne laureola
1970:
1941:
1939:Flora and fauna
1895:
1874:
1806:
1791:
1787:
1735:
1694:
1647:
1634:
1630:
1626:
1622:
1618:
1610:
1606:
1602:
1598:
1594:
1586:
1582:
1578:
1574:
1570:
1566:
1556:
1552:
1544:
1540:
1536:
1528:
1524:
1516:
1512:
1491:
1443:
1416:of the city of
1407:
1316:
1300:Large Waterfall
1291:from the west.
1249:
1197:GolubnjaÄa Cave
1123:
1118:
1041:Veliki PrŔtavac
701:Karlovac County
629:in the west or
615:A1 ZagrebāSplit
537:
532:
480:
436:
421:Karlovac County
377:
372:, colloquially
339:
338:
337:
336:
333:
332:
331:
286:
257:
182:
166:
164:
162:
122:
120:
116:
113:
108:
105:
103:
101:
100:
87:Karlovac County
70:
44:
28:
23:
22:
15:
12:
11:
5:
5926:
5916:
5915:
5910:
5905:
5900:
5895:
5890:
5885:
5880:
5875:
5870:
5865:
5848:
5847:
5845:
5844:
5839:
5834:
5829:
5824:
5819:
5814:
5809:
5804:
5799:
5794:
5789:
5784:
5778:
5776:
5770:
5769:
5767:
5766:
5761:
5753:
5747:
5745:
5741:
5740:
5738:
5737:
5732:
5727:
5722:
5720:Skradinski buk
5717:
5711:
5709:
5705:
5704:
5702:
5701:
5696:
5691:
5686:
5681:
5676:
5670:
5668:
5662:
5661:
5659:
5658:
5653:
5648:
5643:
5638:
5633:
5628:
5623:
5618:
5613:
5608:
5603:
5597:
5595:
5589:
5588:
5581:
5579:
5576:
5575:
5573:
5572:
5567:
5562:
5557:
5552:
5547:
5542:
5537:
5532:
5527:
5522:
5517:
5512:
5507:
5501:
5499:
5498:Adriatic Basin
5495:
5494:
5492:
5491:
5486:
5481:
5476:
5471:
5466:
5461:
5456:
5451:
5446:
5441:
5436:
5431:
5426:
5421:
5416:
5411:
5406:
5401:
5396:
5391:
5386:
5381:
5376:
5371:
5366:
5361:
5356:
5351:
5346:
5341:
5336:
5331:
5326:
5321:
5316:
5311:
5306:
5301:
5296:
5291:
5286:
5280:
5278:
5271:
5265:
5264:
5256:
5255:
5248:
5241:
5233:
5224:
5223:
5221:
5220:
5215:
5210:
5205:
5200:
5195:
5190:
5185:
5180:
5175:
5173:KopaÄevo Marsh
5170:
5165:
5159:
5157:
5151:
5150:
5148:
5147:
5142:
5140:Plitvice Lakes
5137:
5132:
5127:
5122:
5117:
5112:
5106:
5104:
5102:National parks
5098:
5097:
5090:
5089:
5082:
5075:
5067:
5058:
5057:
5055:
5054:
5008:Czech Republic
4984:
4983:and Montenegro
4977:
4962:
4959:
4958:
4948:
4946:
4944:
4943:
4942:
4941:
4936:
4926:
4925:
4924:
4919:
4909:
4904:
4903:
4902:
4897:
4887:
4882:
4873:
4871:Plitvice Lakes
4868:
4858:
4853:
4847:
4844:
4843:
4836:
4835:
4828:
4821:
4813:
4807:
4806:
4801:
4796:
4789:
4786:
4785:
4784:
4776:
4768:
4763:
4758:
4751:
4750:Official links
4748:
4747:
4746:
4741:
4730:
4716:
4715:External links
4713:
4712:
4711:
4701:on 1 July 2014
4690:
4663:
4642:
4635:
4628:
4617:
4606:
4592:
4582:Plitvice Lakes
4576:
4573:
4571:
4570:
4547:
4524:
4503:
4488:
4467:
4449:
4431:
4413:
4381:
4337:
4314:
4293:
4281:
4260:
4235:
4213:
4192:
4171:
4153:
4131:
4113:
4095:
4074:
4056:
4047:
4023:
3998:
3972:
3958:
3942:
3924:
3903:
3890:
3878:
3866:
3847:
3828:
3807:
3785:
3761:
3736:
3718:
3694:
3668:
3644:
3618:
3609:
3583:
3581:
3578:
3544:Krushuna Falls
3523:
3520:
3517:
3516:
3513:
3508:
3506:
3502:
3501:
3486:
3477:
3472:
3468:
3467:
3464:
3461:
3457:Osredak Jezero
3452:
3448:
3447:
3444:
3439:
3434:
3430:
3429:
3422:
3417:
3412:
3408:
3407:
3404:
3399:
3392:
3388:
3387:
3380:
3375:
3368:
3364:
3363:
3360:
3355:
3353:Milino Jezerce
3350:
3346:
3345:
3338:
3335:
3333:
3329:
3328:
3325:
3320:
3318:
3314:
3313:
3311:
3306:
3304:Veliko jezerce
3302:Jovinovac mali
3299:
3295:
3294:
3292:
3287:
3282:
3278:
3277:
3270:
3265:
3258:
3254:
3253:
3250:
3245:
3236:
3232:
3231:
3228:
3223:
3216:
3212:
3211:
3197:
3186:
3181:
3177:
3176:
3173:
3170:
3167:
3157:
3154:
3087:
3084:
3061:
3060:
3057:
3053:
3052:
3049:
3045:
3044:
3041:
3037:
3036:
3033:
3029:
3028:
3025:
3021:
3020:
3017:
3013:
3012:
3009:
3005:
3004:
3001:
2997:
2996:
2993:
2989:
2988:
2985:
2981:
2980:
2977:
2973:
2972:
2969:
2965:
2964:
2961:
2957:
2956:
2953:
2949:
2948:
2945:
2941:
2940:
2937:
2933:
2932:
2929:
2925:
2924:
2921:
2917:
2916:
2913:
2867:land registers
2818:
2815:
2809:, was born in
2768:Gustav JaneÄek
2716:, the wife of
2706:Velika Poljana
2687:
2684:
2596:In 1538, king
2563:Ottoman Empire
2543:
2540:
2407:
2404:
2387:Main article:
2384:
2381:
2378:
2377:
2375:
2364:
2363:
2353:
2342:
2341:
2331:
2320:
2319:
2309:
2298:
2297:
2290:
2231:common minnows
2109:
2106:
2095:
2094:
2092:
2084:
2083:
2076:
2066:
2065:
2058:
2041:
2040:
2038:
2030:
2029:
2022:
2006:can be found.
1969:
1966:
1940:
1937:
1934:
1933:
1930:
1924:
1923:
1919:
1913:
1912:
1901:
1900:Cellular rock
1894:
1891:
1886:eutrophication
1873:
1870:
1805:
1802:
1789:
1785:
1734:
1731:
1693:
1690:
1646:
1643:
1636:
1635:
1632:
1628:
1624:
1620:
1616:
1612:
1611:
1608:
1604:
1600:
1596:
1592:
1588:
1587:
1584:
1580:
1576:
1572:
1568:
1564:
1554:
1550:
1542:
1538:
1534:
1526:
1522:
1519:carbon dioxide
1514:
1510:
1490:
1487:
1442:
1439:
1406:
1403:
1315:
1312:
1248:
1245:
1233:SertiÄ Poljana
1122:
1119:
1117:
1114:
1070:
1069:
1066:
1062:
1061:
1058:
1054:
1053:
1050:
1031:
1030:
1027:
1024:
1019:
1016:
1014:Plitvice Lakes
1010:
1009:
1006:
1003:
1000:
997:
993:
992:
989:
986:
983:
980:
976:
975:
972:
969:
966:
963:
959:
958:
955:
952:
949:
946:
942:
941:
938:
935:
932:
929:
925:
924:
921:
918:
915:
912:
911:Veliki Burget
908:
907:
904:
901:
898:
895:
891:
890:
887:
884:
881:
878:
877:Milino jezero
874:
873:
870:
867:
864:
861:
857:
856:
853:
850:
847:
844:
840:
839:
836:
833:
830:
827:
823:
822:
819:
816:
813:
810:
809:Veliko jezero
806:
805:
802:
799:
796:
793:
789:
788:
785:
782:
779:
776:
772:
771:
768:
765:
762:
759:
755:
754:
751:
748:
745:
742:
738:
737:
734:
731:
724:
721:
633:in the south.
536:
533:
531:
528:
479:
476:
435:
432:
341:
340:
334:
325:
324:
318:
317:
316:
315:
312:
311:
308:
307:
304:
303:
300:
296:
295:
292:
288:
287:
282:
279:
278:
275:
274:
271:
267:
266:
263:
259:
258:
248:
245:
244:
241:
240:
237:
233:
232:
229:
225:
224:
219:
215:
214:
204:
200:
199:
196:
192:
191:
188:
184:
183:
178:
175:
174:
171:
170:
159:
158:Governing body
155:
154:
151:
147:
146:
143:
139:
138:
135:
131:
130:
98:
94:
93:
80:
76:
75:
72:
71:
60:
52:
51:
35:
34:
26:
18:Plitvice Lakes
9:
6:
4:
3:
2:
5925:
5914:
5911:
5909:
5906:
5904:
5901:
5899:
5896:
5894:
5891:
5889:
5886:
5884:
5881:
5879:
5876:
5874:
5871:
5869:
5866:
5864:
5861:
5860:
5858:
5843:
5840:
5838:
5835:
5833:
5830:
5828:
5825:
5823:
5820:
5818:
5815:
5813:
5812:Gulf of Piran
5810:
5808:
5805:
5803:
5802:Split Channel
5800:
5798:
5797:Novsko Ždrilo
5795:
5793:
5790:
5788:
5785:
5783:
5780:
5779:
5777:
5775:
5771:
5765:
5762:
5760:
5758:
5754:
5752:
5749:
5748:
5746:
5742:
5736:
5733:
5731:
5728:
5726:
5723:
5721:
5718:
5716:
5715:GalovaÄki buk
5713:
5712:
5710:
5706:
5700:
5697:
5695:
5692:
5690:
5689:Neretva Delta
5687:
5685:
5684:Lonjsko Polje
5682:
5680:
5677:
5675:
5672:
5671:
5669:
5663:
5657:
5654:
5652:
5649:
5647:
5644:
5642:
5639:
5637:
5634:
5632:
5629:
5627:
5624:
5622:
5619:
5617:
5614:
5612:
5609:
5607:
5604:
5602:
5599:
5598:
5596:
5594:
5590:
5585:
5571:
5568:
5566:
5563:
5561:
5558:
5556:
5553:
5551:
5548:
5546:
5543:
5541:
5538:
5536:
5533:
5531:
5528:
5526:
5523:
5521:
5518:
5516:
5513:
5511:
5508:
5506:
5503:
5502:
5500:
5496:
5490:
5487:
5485:
5482:
5480:
5477:
5475:
5472:
5470:
5467:
5465:
5462:
5460:
5457:
5455:
5452:
5450:
5447:
5445:
5442:
5440:
5437:
5435:
5432:
5430:
5427:
5425:
5422:
5420:
5417:
5415:
5412:
5410:
5407:
5405:
5402:
5400:
5397:
5395:
5392:
5390:
5387:
5385:
5382:
5380:
5377:
5375:
5372:
5370:
5367:
5365:
5362:
5360:
5357:
5355:
5352:
5350:
5347:
5345:
5342:
5340:
5337:
5335:
5332:
5330:
5327:
5325:
5322:
5320:
5317:
5315:
5312:
5310:
5307:
5305:
5302:
5300:
5297:
5295:
5292:
5290:
5287:
5285:
5282:
5281:
5279:
5275:
5272:
5270:
5266:
5262:
5254:
5249:
5247:
5242:
5240:
5235:
5234:
5231:
5219:
5216:
5214:
5211:
5209:
5206:
5204:
5201:
5199:
5196:
5194:
5191:
5189:
5186:
5184:
5183:Lonjsko Polje
5181:
5179:
5176:
5174:
5171:
5169:
5166:
5164:
5161:
5160:
5158:
5156:
5152:
5146:
5143:
5141:
5138:
5136:
5133:
5131:
5128:
5126:
5123:
5121:
5118:
5116:
5113:
5111:
5108:
5107:
5105:
5103:
5099:
5095:
5088:
5083:
5081:
5076:
5074:
5069:
5068:
5065:
5053:
5049:
5045:
5041:
5037:
5033:
5029:
5025:
5021:
5017:
5013:
5009:
5005:
5001:
4997:
4993:
4989:
4985:
4982:
4978:
4976:
4972:
4968:
4964:
4963:
4960:
4952:
4940:
4937:
4935:
4932:
4931:
4930:
4927:
4923:
4920:
4918:
4915:
4914:
4913:
4910:
4908:
4905:
4901:
4898:
4896:
4893:
4892:
4891:
4888:
4886:
4883:
4881:
4877:
4874:
4872:
4869:
4867:
4863:
4859:
4857:
4854:
4852:
4849:
4848:
4845:
4841:
4834:
4829:
4827:
4822:
4820:
4815:
4814:
4811:
4805:
4802:
4800:
4797:
4795:
4792:
4791:
4780:
4777:
4772:
4769:
4767:
4764:
4762:
4759:
4757:
4754:
4753:
4745:
4742:
4739:
4735:
4731:
4728:
4723:
4719:
4718:
4697:
4693:
4687:
4683:
4675:
4671:
4670:
4664:
4660:
4656:
4652:
4648:
4643:
4640:
4636:
4633:
4629:
4626:
4622:
4618:
4615:
4611:
4607:
4604:
4600:
4596:
4593:
4591:
4590:953-215-212-1
4587:
4583:
4579:
4578:
4558:
4551:
4535:
4528:
4513:
4507:
4499:
4492:
4477:
4471:
4463:
4462:Atlas Obscura
4459:
4453:
4445:
4441:
4435:
4427:
4423:
4417:
4402:
4396:
4394:
4392:
4390:
4388:
4386:
4366:
4365:
4358:
4356:
4354:
4352:
4350:
4348:
4346:
4344:
4342:
4324:
4318:
4303:
4297:
4290:
4285:
4270:
4264:
4250:on 2010-09-26
4249:
4245:
4239:
4224:
4217:
4209:
4205:
4199:
4197:
4188:
4184:
4178:
4176:
4167:
4163:
4157:
4141:
4135:
4127:
4123:
4117:
4109:
4105:
4099:
4084:
4078:
4070:
4066:
4060:
4051:
4036:
4030:
4028:
4013:on 2007-09-27
4012:
4008:
4002:
3986:
3979:
3977:
3967:
3965:
3963:
3953:
3951:
3949:
3947:
3938:
3934:
3928:
3920:
3916:
3910:
3908:
3899:
3894:
3885:
3883:
3875:
3870:
3864:
3860:
3857:
3851:
3845:
3841:
3838:
3832:
3817:
3811:
3802:
3800:
3798:
3796:
3794:
3792:
3790:
3774:
3768:
3766:
3750:
3746:
3740:
3732:
3728:
3722:
3708:
3704:
3698:
3683:. 12 May 2019
3682:
3678:
3672:
3664:
3663:www.seebiz.eu
3660:
3653:
3651:
3649:
3632:
3628:
3622:
3613:
3605:
3601:
3595:
3593:
3591:
3589:
3584:
3577:
3575:
3570:
3566:
3562:
3558:
3553:
3549:
3545:
3541:
3537:
3533:
3529:
3514:
3512:
3509:
3507:
3504:
3503:
3499:
3495:
3494:Å upljara Cave
3491:
3487:
3485:
3481:
3478:
3476:
3473:
3470:
3469:
3465:
3462:
3460:
3453:
3450:
3449:
3445:
3443:
3440:
3438:
3435:
3432:
3431:
3427:
3423:
3421:
3418:
3416:
3413:
3410:
3409:
3405:
3403:
3400:
3398:
3393:
3390:
3389:
3385:
3381:
3379:
3376:
3374:
3369:
3366:
3365:
3361:
3359:
3356:
3354:
3351:
3348:
3347:
3343:
3339:
3336:
3334:
3331:
3330:
3326:
3324:
3321:
3319:
3316:
3315:
3312:
3310:
3307:
3305:
3300:
3297:
3296:
3293:
3291:
3288:
3286:
3283:
3281:Veliko jezero
3280:
3279:
3275:
3271:
3269:
3266:
3264:
3259:
3256:
3255:
3251:
3249:
3246:
3244:
3237:
3234:
3233:
3229:
3227:
3224:
3222:
3219:Cigino jezero
3217:
3214:
3213:
3210:
3208:
3202:
3198:
3196:
3190:
3187:
3185:
3182:
3179:
3178:
3174:
3171:
3168:
3165:
3164:
3161:
3153:
3151:
3147:
3143:
3139:
3138:
3133:
3129:
3125:
3121:
3117:
3112:
3110:
3106:
3102:
3097:
3094:
3083:
3079:
3075:
3073:
3067:
3058:
3055:
3054:
3050:
3047:
3046:
3042:
3039:
3038:
3034:
3031:
3030:
3026:
3023:
3022:
3018:
3015:
3014:
3010:
3007:
3006:
3002:
2999:
2998:
2994:
2991:
2990:
2986:
2983:
2982:
2978:
2975:
2974:
2970:
2967:
2966:
2962:
2959:
2958:
2954:
2951:
2950:
2946:
2943:
2942:
2938:
2935:
2934:
2930:
2927:
2926:
2922:
2919:
2918:
2914:
2911:
2910:
2907:
2905:
2901:
2900:Croatian Army
2896:
2892:
2888:
2884:
2880:
2874:
2872:
2868:
2863:
2861:
2860:
2855:
2851:
2848:
2843:
2839:
2831:
2823:
2814:
2812:
2811:KonÄarev Kraj
2808:
2804:
2800:
2796:
2790:
2788:
2783:
2781:
2780:Milka Ternina
2777:
2773:
2769:
2765:
2760:
2757:
2753:
2748:
2746:
2745:
2744:Dorotejin put
2741:
2737:
2731:
2729:
2723:
2719:
2715:
2711:
2707:
2702:
2696:
2692:
2683:
2681:
2677:
2673:
2669:
2665:
2661:
2656:
2654:
2650:
2646:
2642:
2638:
2634:
2628:
2626:
2625:
2618:
2615:
2611:
2606:
2603:
2599:
2594:
2592:
2588:
2584:
2580:
2576:
2572:
2568:
2564:
2560:
2553:
2548:
2539:
2537:
2533:
2529:
2525:
2521:
2517:
2512:
2510:
2506:
2502:
2498:
2494:
2489:
2487:
2483:
2479:
2475:
2471:
2467:
2463:
2459:
2455:
2454:Julius Caesar
2451:
2447:
2443:
2439:
2435:
2431:
2427:
2423:
2416:
2412:
2403:
2401:
2397:
2390:
2376:
2373:
2369:
2366:
2365:
2361:
2357:
2354:
2351:
2347:
2344:
2343:
2339:
2335:
2332:
2329:
2325:
2322:
2321:
2317:
2313:
2310:
2307:
2303:
2300:
2299:
2295:
2291:
2288:
2284:
2283:
2280:
2277:
2275:
2271:
2267:
2263:
2259:
2255:
2251:
2250:European chub
2247:
2246:rainbow trout
2243:
2241:
2236:
2232:
2226:
2224:
2220:
2216:
2215:
2210:
2209:
2205:Brown trout (
2203:
2201:
2200:
2195:
2189:
2187:
2183:
2179:
2175:
2171:
2167:
2163:
2159:
2155:
2151:
2145:
2143:
2139:
2135:
2134:Eurasian lynx
2131:
2127:
2123:
2114:
2105:
2103:
2102:Äorkova uvala
2093:
2091:
2090:
2086:
2085:
2081:
2077:
2074:
2073:
2068:
2067:
2064:
2063:
2059:
2057:
2056:
2052:
2051:
2048:
2047:
2039:
2037:
2036:
2032:
2031:
2028:
2027:
2023:
2021:
2020:
2016:
2015:
2012:
2011:
2007:
2005:
2001:
1996:
1992:
1988:
1981:
1980:
1974:
1965:
1963:
1953:
1945:
1931:
1929:
1926:
1925:
1920:
1918:
1915:
1914:
1910:
1906:
1902:
1899:
1898:
1893:Types of rock
1890:
1887:
1882:
1880:
1869:
1865:
1863:
1859:
1853:
1851:
1847:
1843:
1839:
1834:
1832:
1828:
1823:
1815:
1810:
1801:
1799:
1793:
1778:
1774:
1773:European chub
1769:
1763:
1758:
1752:
1747:
1739:
1730:
1726:
1724:
1718:
1715:
1710:
1703:
1698:
1689:
1688:
1684:
1680:
1676:
1672:
1668:
1663:
1659:
1651:
1642:
1614:
1613:
1590:
1589:
1562:
1561:
1558:
1548:
1532:
1520:
1508:
1507:carbonic acid
1503:
1499:
1497:
1486:
1482:
1480:
1479:vapneni maÄak
1476:
1472:
1468:
1464:
1460:
1456:
1452:
1448:
1447:sedimentation
1438:
1434:
1431:
1427:
1419:
1415:
1411:
1402:
1400:
1394:
1391:
1387:
1382:
1378:
1374:
1372:
1366:
1364:
1363:speleologists
1359:
1357:
1353:
1349:
1345:
1341:
1337:
1333:
1329:
1320:
1311:
1309:
1305:
1301:
1297:
1292:
1290:
1286:
1283:), a part of
1282:
1279:(also called
1278:
1274:
1270:
1266:
1262:
1261:Bijela Rijeka
1253:
1244:
1242:
1238:
1234:
1230:
1226:
1222:
1218:
1214:
1210:
1206:
1202:
1201:Å upljara Cave
1198:
1194:
1190:
1186:
1183:rock, mainly
1182:
1177:
1175:
1171:
1166:
1164:
1160:
1156:
1152:
1148:
1144:
1138:
1136:
1132:
1128:
1113:
1111:
1107:
1103:
1100:. During the
1099:
1095:
1090:
1088:
1084:
1080:
1079:
1067:
1064:
1063:
1059:
1056:
1055:
1051:
1048:
1047:
1044:
1042:
1038:
1028:
1025:
1023:
1020:
1017:
1015:
1012:
1011:
1007:
1004:
1001:
998:
995:
994:
990:
987:
984:
981:
978:
977:
973:
970:
967:
964:
961:
960:
956:
953:
950:
947:
944:
943:
939:
936:
933:
930:
927:
926:
922:
919:
916:
913:
910:
909:
905:
902:
899:
896:
893:
892:
888:
885:
882:
879:
876:
875:
871:
868:
865:
862:
859:
858:
854:
851:
848:
845:
842:
841:
837:
834:
831:
828:
825:
824:
820:
817:
814:
811:
808:
807:
803:
800:
797:
794:
791:
790:
786:
783:
780:
777:
774:
773:
769:
766:
763:
760:
757:
756:
752:
749:
746:
743:
740:
739:
735:
732:
729:
725:
723:altitude (m)
722:
719:
718:
715:
713:
709:
708:Gornja jezera
704:
702:
698:
694:
685:
677:
671:Cross-section
669:
661:
657:
655:
651:
647:
643:
639:
634:
632:
628:
624:
623:Karlovac exit
620:
616:
611:
609:
605:
601:
597:
593:
589:
584:
582:
578:
574:
570:
566:
562:
558:
554:
550:
546:
542:
527:
525:
520:
515:
513:
509:
505:
501:
497:
493:
489:
485:
475:
471:
469:
465:
461:
456:
454:
450:
446:
442:
431:
429:
424:
422:
418:
413:
411:
407:
403:
398:
396:
392:
388:
383:
375:
371:
367:
363:
355:
347:
322:
313:
309:
305:
302:April 8, 1949
301:
297:
293:
291:Official name
289:
285:
280:
276:
272:
268:
264:
260:
255:
254:National Park
252:Category II (
251:
246:
242:
238:
234:
230:
226:
223:
220:
216:
211:
205:
201:
198:vii, viii, ix
197:
193:
189:
185:
181:
176:
172:
169:
160:
156:
152:
148:
144:
140:
136:
132:
127:
99:
95:
92:
88:
84:
81:
77:
73:
68:
66:
58:
53:
48:
41:
36:
31:
19:
5822:Hvar Channel
5817:BraÄ Channel
5787:Bay of Bakar
5782:Kvarner Gulf
5774:Adriatic Sea
5755:
5751:Bobota Canal
5734:
5730:Å trbaÄki buk
5714:
5699:SpaÄva basin
5651:Vrana (Cres)
5630:
5479:Veliki Strug
5155:Nature parks
5139:
4895:Cista Velika
4870:
4703:. Retrieved
4696:the original
4673:
4668:
4650:
4638:
4631:
4624:
4620:
4613:
4609:
4602:
4598:
4595:Josip MovÄan
4581:
4575:Bibliography
4561:. Retrieved
4550:
4538:. Retrieved
4527:
4516:. Retrieved
4506:
4491:
4480:. Retrieved
4470:
4461:
4452:
4443:
4434:
4425:
4416:
4372:. Retrieved
4363:
4329:. Retrieved
4317:
4306:. Retrieved
4296:
4284:
4273:. Retrieved
4263:
4252:. Retrieved
4248:the original
4238:
4227:. Retrieved
4216:
4208:the original
4187:the original
4166:the original
4156:
4144:. Retrieved
4134:
4126:the original
4116:
4108:the original
4098:
4087:. Retrieved
4077:
4069:the original
4059:
4050:
4039:. Retrieved
4015:. Retrieved
4011:the original
4001:
3989:. Retrieved
3937:the original
3927:
3919:the original
3893:
3876:, p. 11
3869:
3850:
3831:
3820:. Retrieved
3810:
3777:. Retrieved
3753:. Retrieved
3751:. 2013-07-01
3748:
3739:
3731:the original
3721:
3710:. Retrieved
3706:
3697:
3685:. Retrieved
3680:
3671:
3662:
3635:. Retrieved
3630:
3621:
3612:
3604:www.index.hr
3603:
3563:(USA) or at
3525:
3510:
3497:
3493:
3489:
3483:
3479:
3474:
3463:Gavan's Lake
3454:
3442:Milan's Lake
3441:
3436:
3425:
3419:
3415:Kozje Jezero
3414:
3401:
3394:
3383:
3378:Lake Gradina
3377:
3370:
3357:
3352:
3341:
3322:
3308:
3301:
3289:
3284:
3273:
3267:
3260:
3247:
3238:
3226:Gypsy's Lake
3225:
3218:
3206:
3204:
3200:
3194:
3188:
3183:
3175:Explanation
3169:Other names
3159:
3149:
3145:
3142:suckling pig
3135:
3127:
3113:
3108:
3098:
3089:
3080:
3076:
3068:
3064:
2875:
2864:
2857:
2844:
2840:
2836:
2798:
2791:
2786:
2784:
2775:
2771:
2763:
2761:
2749:
2733:
2725:
2709:
2705:
2703:
2699:
2694:
2657:
2629:
2621:
2607:
2595:
2556:
2535:
2527:
2513:
2490:
2462:Roman Empire
2419:
2414:
2392:
2371:
2359:
2349:
2337:
2334:Golden eagle
2327:
2315:
2305:
2294:Ursus arctos
2293:
2292:Brown bear (
2286:
2278:
2273:
2261:
2253:
2238:
2234:
2227:
2222:
2218:
2212:
2206:
2204:
2197:
2190:
2185:
2174:Vipera berus
2169:
2161:
2153:
2146:
2142:capercaillie
2119:
2101:
2098:
2087:
2070:
2060:
2053:
2045:
2044:
2033:
2024:
2017:
2009:
2008:
1984:
1977:
1958:
1883:
1875:
1866:
1854:
1835:
1827:phytogenesis
1819:
1797:
1794:
1782:
1751:Milka Trnina
1727:
1719:
1711:
1707:
1686:
1664:
1660:
1656:
1639:
1623:ā Ca + 2 HCO
1504:
1500:
1492:
1483:
1478:
1474:
1466:
1462:
1444:
1435:
1430:air humidity
1423:
1395:
1375:
1370:
1367:
1360:
1325:
1303:
1299:
1293:
1288:
1284:
1280:
1276:
1272:
1264:
1260:
1258:
1236:
1228:
1224:
1220:
1212:
1211:(104 m) and
1208:
1204:
1200:
1196:
1178:
1173:
1167:
1155:Dinaric Alps
1139:
1135:high plateau
1127:biodiversity
1124:
1102:Ottoman Wars
1091:
1075:
1073:
1040:
1036:
1034:
1021:
1013:
1008:Lower Lakes
991:Lower Lakes
979:KaluÄerovac
974:Lower Lakes
957:Lower Lakes
940:Upper Lakes
923:Upper Lakes
906:Upper Lakes
889:Upper Lakes
872:Upper Lakes
855:Upper Lakes
838:Upper Lakes
826:Malo jezero
821:Upper Lakes
804:Upper Lakes
787:Upper Lakes
770:Upper Lakes
753:Upper Lakes
712:Donja jezera
711:
707:
705:
692:
690:
635:
630:
626:
622:
612:
585:
549:Dinaric Alps
538:
516:
507:
503:
499:
483:
481:
472:
468:Korana River
457:
437:
425:
414:
399:
373:
361:
360:
62:
5807:Split Gates
5674:KopaÄki Rit
5048:Switzerland
3687:17 November
3567:in Turkey.
3548:Band-e Amir
3484:Hermit Lake
3471:KaluÄerovac
3358:Mile's Lake
3298:Malo jezero
3148:) or lamb (
3124:soft cheese
3118:(Croatian:
3105:round dance
2807:Rade KonÄar
2797:(Croatian:
2752:Ante DevÄiÄ
2728:Stephanie's
2647:within the
2639:within the
2598:Ferdinand I
2346:Alpine newt
2306:Canis lupus
2258:common rudd
2219:S. t. fario
1862:cratoneuron
1831:Ivo Pevalek
1721:(9.32
1381:Pleistocene
1265:Crna Rijeka
1237:MraÄna Cave
1229:RodiÄa Cave
1205:MraÄna Cave
1174:SeliŔki vrh
1163:Mala Kapela
1143:Mala Kapela
1037:Veliki slap
627:OtoÄac exit
583:in Bosnia.
541:Mala Kapela
121: /
97:Coordinates
5857:Categories
5842:Zavratnica
5759:(proposed)
5725:RoŔki slap
5708:Waterfalls
5510:BoljunÄica
5344:Glogovnica
5299:Bjelovacka
5213:Lake Vrana
5188:Medvednica
4971:Montenegro
4518:2013-09-08
4482:2013-09-08
4426:Dnevnik.hr
4404:Retrieved
4331:2013-09-08
4308:2013-09-08
4275:2013-09-08
4254:2013-09-08
4229:2013-09-08
4089:2013-09-08
4041:2013-09-08
4017:2013-09-08
3874:Å ikiÄ 2007
3822:2013-09-08
3818:. Map24.de
3779:2013-09-08
3755:2018-12-19
3749:LandLopers
3712:2024-04-24
3580:References
3569:Jiuzhaigou
3552:Hindu Kush
3402:Gush Lakes
3309:Small Lake
3290:Large Lake
3248:Round Lake
3243:Kruginovac
3195:Crave Lake
3189:Scrub Lake
3120:Ŕljivovica
3107:(Croatian
3059:1,429,228
3051:1,367,304
3043:1,184,449
3035:1,083,638
2774:(Croatian
2736:Dorothea's
2526:(Croatian
2482:Ostrogoths
2474:Dalmatians
2470:Liburnians
2466:Pannonians
2396:occidental
2240:Salvelinus
2166:dice snake
2122:brown bear
2116:Brown bear
1962:brown bear
1928:Travertine
1850:travertine
1814:travertine
1583:ā 2 H + CO
1459:travertine
1414:Climograph
1328:karst area
1294:The river
1159:PljeŔevica
1147:PljeŔevica
1068:28 m
1060:78 m
1049:Waterfall
962:Gavanovac
945:Milanovac
792:Batinovac
775:Okrugljak
758:Ciginovac
733:depth (m)
545:PljeŔevica
441:travertine
378:pronounced
299:Designated
270:Designated
236:Endangered
228:Extensions
203:Designated
109:15Ā°36ā²58ā³E
106:44Ā°52ā²50ā³N
5694:Paklenica
5641:TrakoÅ”Äan
5444:SlunjÄica
5198:TelaÅ”Äica
5135:Paklenica
4939:Paklenica
4878:with the
4856:Dubrovnik
4659:0351-0662
3565:Pamukkale
3480:Monk Lake
3451:Gavanovac
3433:Milanovac
3420:Goat Lake
3323:Whirlpool
3263:Bakinovac
3257:Batinovac
3241:Okrugljaj
3235:Okrugljak
3215:Ciginovac
3150:janjetina
3116:slivovitz
2825:Okrugljak
2764:Labudovac
2530:) or the
2520:Frankopan
2460:into the
2458:Illyricum
2422:Illyrians
2316:Bubo bubo
2302:Grey wolf
2287:Lynx lynx
2130:eagle owl
2126:grey wolf
1909:limestone
1842:substrate
1675:SlunjÄica
1619:+ H + HCO
1579:ā H + HCO
1390:limestone
1332:limestone
1241:cave bear
1217:pit-caves
1207:(160 m),
1189:limestone
512:limestone
482:The name
478:Etymology
239:1992ā1997
142:Elevation
137:296.85 km
69:Park logo
5646:Varaždin
5636:Prokljan
5631:Plitvice
5611:KruÅ”Äica
5525:Dragonja
5429:Plitvica
5404:Mrežnica
5359:KaraŔica
5354:KaraŔica
5040:Slovenia
5036:Slovakia
5004:Bulgaria
4900:Dubravka
4705:31 March
4625:Croatian
4614:Croatian
4599:Plitvice
4406:31 March
4374:21 March
3859:Archived
3840:Archived
3538:and the
3239:OkrugliÄ
3027:980,033
3019:939,747
3011:948,891
3003:927,661
2995:866,218
2987:855,866
2979:749,209
2971:721,265
2963:665,108
2955:597,884
2947:482,275
2939:238,401
2931:500,000
2889:and the
2854:Karl May
2740:Croatian
2680:Rakovica
2668:Napoleon
2660:Dalmatia
2617:Orthodox
2587:Ottomans
2528:pavlinci
2452:. Under
2400:oriental
2266:crayfish
2199:Plecotus
2180:and the
1905:dolomite
1762:cascades
1702:Plitvica
1627:ā Ca(HCO
1603:ā Ca(HCO
1533:(CaMg(CO
1531:dolomite
1471:Croatian
1386:dolomite
1344:sinkhole
1336:dolomite
1304:Sastavci
1296:Plitvica
1185:dolomite
1087:Korenica
860:Galovac
693:županija
650:Josipdol
569:Rakovica
557:Korenica
530:Location
519:Plitvica
484:Plitvice
453:bacteria
439:dams of
410:Adriatic
374:Plitvice
366:Croatian
195:Criteria
150:Visitors
79:Location
47:Croatian
5606:Dubrava
5570:Zrmanja
5565:RjeÄina
5550:Neretva
5434:RaÄaÄka
5419:Orljava
5384:KupÄina
5369:Krapina
5261:Croatia
5208:Velebit
5178:Lastovo
5163:Biokovo
5145:Risnjak
5115:Kornati
5110:Brijuni
5052:Ukraine
5032:Romania
5016:Germany
4996:Belgium
4992:Austria
4988:Albania
4917:Å ibenik
4146:15 June
4140:"Fauna"
3559:within
3528:Rastoke
3490:kaluÄer
3395:Burgeti
3391:Burgeti
3384:gradina
3373:Jezerac
3371:Jezerce
3332:Galovac
3132:polenta
2847:Western
2738:Path" (
2575:Hungary
2571:Croatia
2536:gradina
2516:Zrinski
2501:Mongols
2383:History
2242:alpinus
2164:), the
2156:), the
2004:orchids
2000:endemic
1683:Rastoke
1549:(Ca(HCO
1405:Climate
1358:, etc.
1310:river.
1235:and in
1221:Äudinka
1181:karstic
1151:plateau
1131:Velebit
1121:Terrain
1076:opÄina
1052:height
1029:
1026:
1018:
928:Kozjak
600:Velebit
504:plitvak
500:pliÄina
387:Croatia
265:Natural
210:Session
190:Natural
91:Croatia
5744:Canals
5626:PeruÄa
5601:BaÄina
5520:Äikola
5515:Cetina
5505:Bijela
5489:Zelina
5469:Trnava
5454:Studva
5449:SpaÄva
5394:Londža
5364:Korana
5324:Danube
5294:Bijela
5284:Bednja
5269:Rivers
5168:Dinara
5028:Poland
5012:France
4975:Serbia
4907:Trogir
4890:SteÄak
4688:
4676:]
4657:
4588:
4563:2 June
4540:2 June
4444:GOV.UK
3991:2 June
3637:22 May
3411:Kozjak
3397:Bugeti
3201:proÅ”Äe
3184:ProÅ”Äe
3146:odojak
3128:vrhnje
2923:1,000
2732:) and
2610:Croats
2605:West.
2497:Croats
2468:, the
2446:Croats
2434:Romans
2426:Japods
2256:) and
2140:, and
1993:, and
1991:spruce
1760:Small
1671:Korana
1567:O + CO
1418:Ogulin
1399:canyon
1308:Korana
1273:Matica
1247:Rivers
1098:Kordun
736:Group
726:area (
654:PlaŔki
646:Rijeka
642:Zagreb
608:poljes
577:GospiÄ
573:OtoÄac
565:Ogulin
524:Korana
508:plitko
496:OtoÄac
492:priest
490:, the
460:runoff
451:, and
43:
5621:Ormož
5616:Lokve
5593:Lakes
5555:Ombla
5545:Mirna
5535:Jadro
5530:Gacka
5464:Sutla
5459:Sunja
5424:Pakra
5399:Lonja
5349:Ilova
5339:Glina
5334:Drava
5329:Dobra
5319:Ärnec
5314:Ärnec
5309:Äesma
5304:Bosut
5193:Papuk
5125:Mljet
5044:Spain
5020:Italy
4986:with
4981:Italy
4979:with
4965:with
4922:Zadar
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3101:prelo
2912:Year
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2450:Turks
2442:Slavs
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2430:Celts
2108:Fauna
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1968:Flora
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2928:1989
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