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The ten counties and Zagreb cover 28,337 square kilometres 10,941 square miles of land, corresponding to 50% of the territory of Croatia, and have a population of 2,418,214 yielding a population density of 85. The contemporary of the cut off the flow of water to the , and the formed in the basin. In past five years, film production in Croatia produced up to five feature films and 10 to 51 short films, with an additional 76 to 112 TV films. In total, there are 55 institutions of higher education in Croatia, attended by more than 157 thousand students. The New York Times. Indigenous sorts of cultivated plants and breeds of domesticated animals are also numerous. The is headed by the , who has four deputy prime ministers and 16 ministers in charge of particular sectors of activity. Retrieved 3 January 2009. The Yugoslav government retained control of defence, internal security, foreign affairs, trade, and transport while other matters were left to the Croatian Sabor and a crown-appointed Ban. Following the death of Yugoslav president Josip Broz Tito in 1980, the political situation in Yugoslavia deteriorated, with national tension fanned by the 1986 Serbian and the. Since the end of the Croatian War of Independence, the tourist industry has grown rapidly, recording a fourfold rise in tourist numbers, with more than 11 million tourists each year. Serbs have been only partially re-settled in the regions they previously inhabited while some of the settlements previously inhabited by Serbs were settled by Croat refugees from Bosnia and Herzegovina, mostly from.

Top up vouchers can be bought for 16. A vipme SIM is sold for 10 kn in mini, for 20 kn in micro and for 50 kn in nano size without credit. Following the death of Yugoslav president Josip Broz Tito in 1980, the political situation in Yugoslavia deteriorated, with national tension fanned by the 1986 Serbian and the.

Calendar for Year 2018 (Croatia) - Archived from on 29 April 2012.

Croatia proper ; : Hrvatska pronounced is one of the four of the , together with , , and. It is located between Slavonia in the east, the in the west, and Dalmatia to the south. The region is not officially defined, and its borders and extent are described differently by various sources. Croatia proper is the most significant economic area of the country, contributing well over 50% of Croatia's. The capital of both Croatia proper, and the Republic of Croatia, Zagreb, is the largest city and most important economic centre in the region. It only became Croatia proper in 1522, when the capital of Croatia was moved from Dalmatia to. Croatia proper comprises several smaller regions of its own: , , , the , , , , , , , , and. The region covers 28,337 square kilometres 10,941 square miles of land and has a population of 2,418,214. Croatia proper straddles the boundary between the and the. The boundary of these two units runs from to , along the River. The Dinaric Alps area is typified by topography, while the Pannonian Basin exhibits plains, especially in the river valleys—along the Sava, , and —interspersed with hills and mountains developed as and structures. Lika and Gorski Kotar are part of the , and contain five out of eight higher than 1,500 metres 4,900 feet. Most of the region has a moderately warm and rainy , although there is considerable seasonal snow at greater elevations. The region belongs almost exclusively to the and includes most of the. The boundaries of Croatia proper were shaped by territorial losses of to the and the starting in the 15th century. In effect, Croatia proper loosely corresponds to what was termed reliquiae reliquiarum olim magni et inclyti regni Croatiae the relics of the relics of the formerly great and glorious Kingdom of Croatia and the subsequent within the. The region contains most of the 180 preserved or restored , as it was spared any large-scale war damage throughout its history. The west of the region represents a natural barrier between the and the , and this, along with and resulting status, has contributed to the relatively poor development of the economy and infrastructure of that area. See also: , , and Croatia proper is a geographic region of that encompasses territory around , located between in the east and the in the west. Its exact borders are determined ambiguously, and the extent of the region is defined differently by various sources. The border with Slavonia to the east was variously defined throughout history, depending on the political divisions of Croatia. Croatia proper roughly corresponds to the area of Zagreb and ten : , , , , , , , , , and. Most of the region, excluding Primorje-Gorski Kotar and Lika-Senj counties, is part of the along with all of Slavonia. Primorje-Gorski Kotar and Lika-Senj are included in the NUTS unit. The ten counties and Zagreb cover 28,337 square kilometres 10,941 square miles of land, corresponding to 50% of the territory of Croatia, and have a population of 2,418,214 yielding a population density of 85. Croatia proper comprises several smaller regions of its own: the , , , , , , , , , , , and. The western areas of Lika and suffered from population depletion during and the , and the 2001 census indicated a large proportion of elderly. The Ogulin-Plaški Valley contains the largest settlement of the area, , with a population of 8,216. The second-largest settlement in Mountainous Croatia, and the largest in Lika, is See also: and Croatia proper straddles the boundary between the and the , two of three major parts of Croatia. The boundary runs from the 1,181-metre 3,875 ft Žumberak range to the Banovina area, along the River. The Dinaric Alps are linked to a active from the Late to recent times, and is itself part of the that extends southeast from the southern. The Pannonian Basin took shape through thinning and of crust structures formed during the Late. Paleozoic and structures are visible in and other Slavonian mountains. The processes also led to the formation of a chain in the basin 12—17 ; intensified subsidence was observed until 5 Mya as well as at about 7. The contemporary of the cut off the flow of water to the , and the formed in the basin. Ultimately up to 3,000 metres 9,800 ft of sediment was deposited in the basin, and the sea eventually drained through the gorge. The result is large plains, particularly in river valleys, and especially along the Sava, , and rivers. The plains are interspersed with and structures, believed to have broken the Pannonian Sea's surface as. The tallest among these landforms are 1,059-metre 3,474 ft and 1,035-metre 3,396 ft , north of. Parts of 489-metre 1,604 ft , along with on and mountains in Slavonia to the east, are possibly remnants of a from the same collision that caused the Dinaric Alps. The Dinaric Alps in Croatia encompass the entire Gorski Kotar and Lika regions, as well as considerable parts of , with their northeastern edge running from 1,181-metre 3,875 ft to the , along the Sava River, and their westernmost landforms being 1,272-metre 4,173 ft and 1,396-metre 4,580 ft mountains in Istria. The Mountainous Croatia contains five out of eight higher than 1,500 metres 4,900 feet : , , , and. Karst topography makes up about and is especially prominent in the Dinaric Alps and in turn, the Mountainous Croatia. The longest cave in Croatia and in the entire Dinaric Alps, 20,656-metre 67,769 ft , is located in southern Velebit area of the Mountainous Croatia. Hydrology and climate See also: and The vast majority of the region is encompassed by the Black Sea. The area includes all the largest rivers flowing in the country—Sava, Drava, , and Kupa—except the. The largest lakes in Croatia proper are 17. Croatia proper has a wealth of wetlands. Two out of the four Croatian wetlands included in the are located in the region— along the Sava and rivers near , and near. A high degree of karstification of the terrain in the Dinaric Alps has resulted in an increased permeability of soil and rocks and the formation of barriers and waterfalls. The finest examples of the interaction of watercourses and karst are the , listed as a , and , to the north of the Plitvice Lakes. Those are the , tracing the northern boundary of the region, , and the —forming barriers and waterfalls before discharging into Kupa in area of , as well as , in the eastern part of the region, at the border of Bosnia and Herzegovina. Furthermore, there are such as , and rivers, reflecting a high degree of karstification of the terrain in the region, resulting in increased permeability of soil and rocks. Ingress of water underground resulted in formation of subterranean watercourses and lakes. Probably the finest example of interaction of karst terrain and watercourses in the area are —16 interlinked lakes between Mala Kapela and Plješevica, through which Korana River flows. The area is abundant in travertine barriers, waterfalls and caves of biological origin—created through deposition of through agency of moss, algae and aquatic bacteria. The Plitvice Lakes are listed as a , and they are a part of one of three located in the Mountainous Croatia, along with and. Croatia proper has a moderately warm and rainy as defined by the. Temperature peaks are pronounced in the region compared to parts of Croatia closer to the , because of the absence of its moderating effect. Gorski Kotar and Lika represent the coldest parts of Croatia as mean annual temperature there ranges between 8 and 10 46 and 50 at lower elevations and 2 and 4 36 and 39 at greater elevations. Gorski Kotar mountain peaks of Risnjak and Snježnik receive the greatest precipitation in Croatia—3,500 millimetres 140 inches per year. Overall, the region has no arid periods of the year. Gorski Kotar also receives the least sunlight—1,700 hours per year on average. Demographics See also: According to the 2011 census, the total population of the ten counties of Croatia proper, together with that of the city of Zagreb, is 2,418,214—representing 56. The largest proportion of the total population lives in the city of Zagreb, followed by Zagreb County. Lika-Senj County is the least populous county of Croatia proper. The population density of the counties ranges from 156. The highest population density is recorded in the city of Zagreb area, at 1,236. Zagreb is the largest city in Croatia proper, followed by , Karlovac, Varaždin, , and. Other cities in Croatia proper have populations below 30,000. According to the 2001 census, account for 92. The largest proportion of the Serb minority was recorded in the Sisak-Moslavina and Karlovac counties 11. The most populous urban areas in Croatia proper Rank City County Urban population Municipal population 1 686,568 792,875 2 128,624 213,666 3 46,827 55,981 4 38,746 47,055 5 33,049 47,699 6 31,341 63,511 7 27,099 40,443 8 23,896 30,872 9 Zagreb 19,574 25,226 10 Zagreb 15,867 37,607 Sources: , 2011 Census See also: The lowland regions of Croatia proper are the most significant economic area of Croatia in terms of its contribution to the national GDP. The city of Zagreb alone contributes 30. By 2011, the national GDP share increased further for the city of Zagreb and Zagreb County, reaching 31. The economy of the city of Zagreb represents the bulk of the economy of Croatia proper. Its most significant components are and trade, accounting for 38. Further industries, by income share, are the —the supply of , , steam, and 7. These account for 91. The economy of the Zagreb County, largely contiguous with Zagreb's metropolitan area, is dominated by wholesale and retail trade 53. Unlike the economy of the city of Zagreb, the county's economic income is largely generated by small and medium businesses 64. The city of Zagreb and the Zagreb County dominate the economy of the Croatia proper and Croatia as a whole: nearly 91% of all Croatia's wholesale and retail trade companies and 45% of the Croatian processing industry is headquartered there. In 2010, nine companies headquartered in the Croatia proper ranked among the largest by income among , and 27 out of the top 30 companies were based in the region. The largest were , a part of , , and —all of them headquartered in Zagreb. Deloitte ranks Agrokor as the largest business among Croatia's enterprises. The largest company by income in the Varaždin County is the 15th-ranked industry company , while the 17th-ranked plant , based in , is the largest company in the Sisak-Moslavina County. The largest company by income in the Zagreb County is , a company headquartered in , which ranks 36th in Croatia. It ranks 115th in Croatia. The main source of income in the area was , and. Forests represent a development potential of the area as 45% of Lika and as much as 83% of Gorski Kotar is forested. Industrialisation of the region started after the World War II, with a particular emphasis on development of wood processing industry in Gorski Kotar and other industries elsewhere in the region, but it did not create sufficient jobs to prevent economic migrations. Furthermore, the economic structure of the area sustained great downturn in the 1990s during the Croatian War of Independence. Since the 2000s, an increasing prominence is given to tourism sector, especially. Infrastructure See also: Three run through Croatia proper. The corridor Vb encompasses the , spanning from Zagreb to Varaždin and the border of , and a section of the and , extending south of Zagreb towards Karlovac and. The transport corridor also contains a parallel railway line connecting the and via Zagreb. The second major transport route is the corridor X, represented as the and a double-track railway spanning the region from west to east, as well as the —the Xa branch of the corridor X. The three routes form junctions near Zagreb. The region is also home to the largest airport in Croatia—the. In April 2012, a 30-year contract to develop and manage the airport as a regional transport centre was signed by the and. The only navigable river in the region is the Sava, downstream of Sisak. The navigable route became disused after onset of the in 1991, and it has not been fully restored since the end of the war, limiting the size of vessels that may reach Sisak. The JANAF system also includes a pipeline to a fuel handling terminal in Zagreb. The region forms a center of Croatia's supply system, based on an located approximately 50 kilometres 31 miles east of Zagreb. The Dinaric mountain ranges of and in the region's western reaches represent a natural barrier between the to its west and the and to its east, traversed by few high-performance transport routes until recently. The region was first spanned by a trading route between and in and later in , but the first modern road in the area was the , completed in 1732 connecting and via , , and , and named after who ordered its construction. The same emperor commissioned construction of a narrow road between and Gospić—the first to span Velebit. Those first roads were replaced by the more modern connecting Karlovac to Senj, largely tracing the Roman trading route across the , and the following a different route between Karlobag and Gospić, completed in 1779 and 1784 respectively. In 1789, a road to Dalmatia, branching from the Josephine road at towards via Gospić. The first railway built in the region was the — Rijeka railway, completed in 1875. Since the 2000s, the region is spanned by modern. See also: Most of Croatia proper is distinguished in Croatia by its relatively high population density — a consequence of the fact that the region was spared from large-scale war damage. This also allowed preservation of numerous sites, including medieval city cores, , , castles, palaces, and churches. Because the was governed by rulers based further south, in areas closer to the coast, there are few and monuments preserved in the region—most of them date back to the and later periods. There are, however, with from and. The most significant prehistoric site in the region is a site. The region contains most the 180 preserved or restored —most of the best preserved-ones were built in the 17th and 18th centuries, when the was no longer a threat. A substantial number of buildings were destroyed in the Second World War. The largest number of preserved castles and manor houses are situated in Hrvatsko Zagorje, including the —the most beautiful castle in Croatia. Its construction started in the 14th century, and it has been substantially expanded and rebuilt since. Another example is the —the best-preserved castle in Croatia—completed in the second half of the 15th century. Among the cities in the region, Varaždin and Zagreb occupy particularly prominent places in terms of culture. Varaždin is often considered the most significant centre of culture and heritage in Croatia. That claim is reflected in the city's historical architecture and cultural events, based on traditions of the city from the era. Zagreb, on the other hand, is the largest cultural centre, not only in the region, but also in Croatia as a whole. It is home to dozens of galleries, museums, and theatres as well as being the site of numerous. The landmarks include the , founded in 1093 and rebuilt numerous times since, the last major reconstruction being after the. The cathedral is the tallest structure in Croatia. Zagreb is the most significant centre of scientific work and education in the region and the entire country. It is the site of the —the oldest place of in Croatia and , operating continuously since 1669. It is also home to the —the leading Croatia's scientific —and to the. See also: Croatia proper as a region has defined itself historically through territorial losses of the to the and conquest starting in the 15th century. In response, was established under direct imperial rule. By 1528, nearly all of was under Ottoman control. Venice seized the area of present-day as the Ottomans advanced, winning the decisive in 1493 and the in 1526. This led to the loss of Slavonia and the defeat of the , to which Croatia was tied through a. The extent of the Ottoman conquest still marks the southern and eastern boundaries of Croatia proper as a geographical region. In effect, Croatia proper loosely corresponds to what was termed the relics of the relics of the formerly great and glorious Kingdom of Croatia : reliquiae reliquiarum olim magni et inclyti regni Croatiae and subsequent within the. The was gradually established in the second half of the 16th century, removing further territory from the Kingdom of Croatia and placing the military zone under direct imperial rule. Ottoman advances into Croatian territory continued until the 1593 , the first decisive Ottoman defeat, which led to a more lasting stabilisation of the frontier. As the Ottoman control of the area waned, the Military Frontier expanded to include the entirety of Lika. In 1881, that region was incorporated into the , together with , which remained a part of the throughout the. After the Ottoman defeat in the and the 1699 , a separate was formed out of the regained territories, confirming the established borders of the Kingdom of Croatia. Pursuant to provisions of the of 1868, Slavionia was added to the —the territory ruled from Zagreb—and the military frontier was abolished. Following World War I and the , Hungary lost Rijeka and , as well as other territories, to the newly established. The defined the country as a and abolished the historical administrative divisions, effectively ending Croatia's autonomy. Međimurje was assigned to in 1947—when all the borders of the former were defined by demarcation commissions, pursuant to decisions of the of 1943 and 1945. After the and in 1991, the RSK was proclaimed in parts of Croatia, including parts of the Croatia—Banovina and Kordun—encompassing areas east of Karlovac and south of Sisak, marking the start of the. After the January 1992 ceasefire, a was deployed to the area. 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