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Veliki Kozjak
Veliki Kozjak or just Kozjak is a mountain cliff in Croatia, located inland of Dalmatian Zagora. It belongs to Dinaric Alps, and stretches over the small village Kijevo between the towns of Vrlika and Knin Knin () is a city in the Šibenik-Knin County of Croatia, located in the Dalmatian hinterland near the source of the river Krka (Croatia), Krka, an important traffic junction on the rail and road routes between Zagreb and Split, Croatia, Split. .... The highest peak of this cliff is ''Bat'' (1,207 m), and its southeast peak is ''Kunica'' (1,101 m), over the small village of Maovice. Gallery Kozjak north.jpg, Kozjak from the north in winter See also * List of mountains in Croatia Mountains of Croatia Cliffs of Europe Landforms of Šibenik-Knin County {{Dalmatia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dalmatia
Dalmatia (; ; ) is a historical region located in modern-day Croatia and Montenegro, on the eastern shore of the Adriatic Sea. Through time it formed part of several historical states, most notably the Roman Empire, the Kingdom of Croatia (925–1102), Kingdom of Croatia, the Republic of Venice, the Austrian Empire, and presently the Croatia, Republic of Croatia. Dalmatia is a narrow belt stretching from the island of Rab (island), Rab in the north to the Bay of Kotor in the south. The Dalmatian Hinterland ranges in width from fifty kilometres in the north, to just a few kilometres in the south; it is mostly covered by the rugged Dinaric Alps. List of islands of Croatia, Seventy-nine islands (and about 500 islets) run parallel to the coast, the largest (in Dalmatia) being Brač, Pag (island), Pag, and Hvar. The largest city is Split, Croatia, Split, followed by Zadar, Šibenik, and Dubrovnik. The name of the region stems from an Illyrians, Illyrian tribe called the Dalmatae, w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Croatia
Croatia, officially the Republic of Croatia, is a country in Central Europe, Central and Southeast Europe, on the coast of the Adriatic Sea. It borders Slovenia to the northwest, Hungary to the northeast, Serbia to the east, Bosnia and Herzegovina and Montenegro to the southeast, and shares a maritime border with Italy to the west. Its capital and largest city, Zagreb, forms one of the country's Administrative divisions of Croatia, primary subdivisions, with Counties of Croatia, twenty counties. Other major urban centers include Split, Croatia, Split, Rijeka and Osijek. The country spans , and has a population of nearly 3.9 million. The Croats arrived in modern-day Croatia, then part of Illyria, Roman Illyria, in the late 6th century. By the 7th century, they had organized the territory into Duchy of Croatia, two duchies. Croatia was first internationally recognized as independent on 7 June 879 during the reign of Duke Branimir of Croatia, Branimir. Tomislav of Croatia, Tomis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dinaric Alps
The Dinaric Alps (), also Dinarides, are a mountain range in Southern Europe, Southern and Southcentral Europe, separating the continental Balkan Peninsula from the Adriatic Sea. They stretch from Italy in the northwest through Slovenia, Croatia, Bosnia and Herzegovina, Serbia, Montenegro, and Kosovo to Albania in the southeast. The Dinaric Alps extend for approximately along the western Balkan Peninsula from the Julian Alps of the northeast Italy, downwards to the Šar Mountains, Šar and Korab (mountain), Korab massif, where their direction changes. The Accursed Mountains are the highest section of the entire Dinaric Alps; this section stretches from Albania to Kosovo and eastern Montenegro. Maja Jezercë, standing at Metres above the Adriatic, above the Adriatic, is the highest peak and is located in Albania. The Dinaric Alps are one of the most rugged and extensive mountainous areas of Europe, alongside the Caucasus Mountains, Alps, Pyrenees, Carpathian Mountains and Scand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zagora (Croatia)
The Dalmatian Hinterland () is the southern inland hinterland in the historical Croatian region of Dalmatia. The name means 'beyond (the) hills', which is a reference to the fact that it is the part of Dalmatia that is not coastal and the existence of the concordant coastline where hills run parallel to the coast. Geography Dalmatian Zagora, in the strict sense, spans from the hinterland east of Šibenik to the border with Bosnia and Herzegovina and continues south to Vrgorac, just north of the Neum corridor. Its borders are present in two counties: Split-Dalmatia County, Split-Dalmatia and Šibenik-Knin County, Šibenik-Knin. The terrain in Zagora is fairly rugged: in the region immediately bordering the coastline, it is mostly flat but dry, mainly covered with maquis shrubland, ''makija'' (maquis, macchia). More inland, greener pastures can be seen, as the climate and elevations change. Karst topography dominates the landscape. The land is interspersed with river canyons, of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kijevo, Croatia
Kijevo is a village and the only settlement in the eponymous municipality of Kijevo in Dalmatia, southeast of Knin in the Šibenik-Knin County of Croatia. The population of the municipality is 417 (2011), with 100% declaring themselves as Croats and Roman Catholics. Kijevo is an underdeveloped municipality which is statistically classified as the First Category Area of Special State Concern by the Government of Croatia. Location Kijevo lies underneath the Dinara mountain, near the source of the river Cetina. It is located on the State route D1 between the towns of Vrlika and Knin. History Thirty-four people from Kijevo died in World War I.Ante Kovačević. ''Kijevo i okolica : kulturnopovijesna, etnografska i prirodna baština Hrvatskog podinarja''. Kijevo : Općinsko poglavarstvo, 2000. (pg. 18) In World War II, Kijevo became part of the Independent State of Croatia fascist puppet state ruled by Nazi Germany and Italy. In the spring of 1942, the town was liberated by Yugosla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vrlika
Vrlika is a small town in inland Split-Dalmatia County, Croatia. The closest large towns are Sinj, Knin, and Drniš. Vrlika was given the status of town in 1997. Vrlika is an underdeveloped municipality which is statistically classified as the Areas of Special State Concern (Croatia), First Category Area of Special State Concern by the Government of Croatia. Location Vrlika is located in the Cetinska Krajina region in Split-Dalmatia County. It is 40 km northwest of the town of Sinj on the State route D1 road (Croatia), D1 between the towns of Sinj and Knin and on the regional route which connects Vrlika and Drniš. History The oldest evidence for human life in this region is from 30,000 BC. During the Bronze Age, between 1900 and 1600 BC, there was the so-called Cetina culture on the territory of Vrlika municipality. Archaeologists have found ancient graves, a Bronze Age sword and other smaller items dating back to that period. These findings made it clear that in the past t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Knin
Knin () is a city in the Šibenik-Knin County of Croatia, located in the Dalmatian hinterland near the source of the river Krka (Croatia), Krka, an important traffic junction on the rail and road routes between Zagreb and Split, Croatia, Split. Knin rose to prominence twice in history, as the capital of both the Kingdom of Croatia (925–1102), medieval Kingdom of Croatia and briefly of the self-proclaimed Republic of Serbian Krajina within the newly independent Croatia, Republic of Croatia for the duration of the Croatian War of Independence from 1991 to 1995. Etymology The name is likely derived from the Illyrian language, Illyrian ''Ninia''. According to an alternative explanation, offered by Franz Miklosich and Petar Skok, the name - derived from a Slavic root ''*tьn-'' ("to cut", "to chop") - means "cleared forest". The medieval names of Knin include ; ; . The Latin name is still used as a titular see, titular episcopal see, the Diocese of Tinum. History Ancient The are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maovice
Maovice is a small village in Split-Dalmatia county, Croatia. Maovice is a settlement in the Vrlika municipality, and has a population of 494. The majority of the population are Croats. Location Located in inland Dalmatia, west from the town of Vrlika, on the route between towns of Drniš and Vrlika, Maovice spread on 27.57 km2 mainly on plateau Maovičko field ''(Maovičko polje)'', at an altitude of approximate 640–700 m, just under the north base of mountain Svilaja. History In the 17th century, Maovice was largely settled by new inhabitants from Croatia and Bosnia. Austrians gave to the new inhabitants land in exchange for fighting against the Ottomans. From 1869 to 1889 the settlement was called ''Mahovice'', and from 1890 to 1910 ''Mavice''. It consists of two villages, Gornje Maovice and Donje Maovice. Parts of a settlement are hamlets: * Bijuk * Donje Maovice * Gornje Maovice * Pod Umcem * Radinje * Svilaja Between Gornje and Donje Maovice there is a small Cat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In Croatia
This is a list of mountains () in Croatia. The highest mountains in Croatia belong to the Dinarides range that is sometimes also called Dinaric Alps, of which Dinara is the highest mountain in Croatia. Together with the easternmost parts of the Alps, these mountains span most of the country, and their orogenic activity started in the Paleozoic with the Variscan orogeny and continued in the Mesozoic and Cenozoic with the Alpine orogeny. The mountains in the northeastern part of the country, in the Pannonian plain, are considerably older than the rest as their orogeny happened in the Paleozoic. Mountains in the list are ordered by height. See also * Geography of Croatia * List of rivers in Croatia * List of lakes in Croatia * Croatian Mountaineering Association Notes Sources * Further reading * Dr. Željko Poljak "Hrvatske planine" Zagreb, 2001. * Greater Geographical Atlas of Yugoslavia, University Press "Liber", Zagreb (Croatia), 1987. * Geographical Atla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Croatia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are inselberg, isolated summits, but most occur in mountain ranges. mountain formation, Mountains are formed through tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosystems of mountains: different elevations hav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of Europe
In geography and geology, a cliff or rock face is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
