The Carpathians are a wide, crescent-shaped mountain ridge located in Central and Eastern Europe, extending for about 1450 km in a system of parallel structural ranges eastward from the Danube Gap near Bratislava in Slovakia, southward to...
moreThe Carpathians are a wide, crescent-shaped mountain ridge located in Central and Eastern Europe, extending for about 1450 km in a system of parallel structural ranges eastward from the Danube Gap near Bratislava in Slovakia, southward to Brasov in Romania, and southeastward to a part of the Danube Valley, called the Iron Gate near Orsova in Romania and covering the area of 209,256 square km. Bojnansky and Fargasova 2007), over parts of the territories of the Czech Republic, Slovakia, Hungary, Poland, Ukraine, Romania, and Serbia . The Carpathians comprise of several geologically and orographically distinct mountain ridges. The highest part is the Tatra Massif, characterized by typical alpine relief, which has more than 50 peaks with an elevation above 2000 m, the highest one is Gerlachovsky stit (Mount Gerlach), 2655 m ASL, located in Slovakia. In the Eastern Carpathians, Chornohora is the highest ridge, with six peaks exceeding 2000 m (Hoverla 2061 m ASL) ). The name "Carpathians" was first mentioned as Karpates oros in the second century by the Greek geographer Ptolemy . The Carpathians are designated by a mid-mountainous relief shaped by rivers and slope erosion. Pleistocene glaciations occurred in the Tatras . Despite the fact that commonly referred to as a mountain chain, the Carpathians do not actually form an uninterrupted chain. Rather, they are formed of several orographically and geologically distinctive groups, presenting as great a structural diversity as the Alps. The Carpathians, which only in few locations exceed an altitude 2500 m, lack the bold peaks, extensive snowfields and glaciers, high waterfalls, and the various large lakes which are common in the Alps. The Carpathians are split up into several mountain blocks separated by basins. Water runoff from the mountain chain escapes for its most part into the Black Sea through the rivers Danube and Dniester. From the northern slopes and the large Big Poland Lowland, it falls into the Baltic Sea through the Vistula River (Bojnansky and Fargasova 2007). The Carpathians play a significant role in Romania (40.1% of national territory) and Slovakia (77.8%). In the latter case, three hills represent the mountains in the country's state symbol . No consistent geomorphologic division of the Carpathians exists currently. In the Czech Republic, Slovakia, and Poland, the division into the Western, Eastern, and Southern Carpathians is accepted. In Romania, they are classified as Northern, Eastern, Southern, and Western Carpathians. The Predeal Pass is considered as the division between the Eastern and Southern Carpathians . Similarly to the Alps, the Carpathians have risen from a Mesozoic geosynclinal sea. The curved shape of the range is caused by occurrence of older, more resistant parts of crust, representing the Bohemian Massif in the northwest, the Ukrainian shield in the northeast, and the Moesian Platform in the southeast, known as Tisia Massif (in the Danube basin). The folding had several stages and was completed in the Tertiary. The Southern Carpathians were formed during the final phase ).