|Elevation||2,655 m (8,711 ft)|
|Length||1,700 km (1,100 mi)|
|Countries||Czech Republic, Poland, Austria, Slovakia, Hungary, Ukraine, Romania and Serbia|
The Carpathian Mountains or Carpathians ( // ) are a range of mountains forming an arc throughout Central and Eastern Europe. Roughly 1,500 km (932 mi) long, it is the third-longest European mountain range after the Urals at 2,500 km (1,553 mi) and the Scandinavian Mountains at 1,700 km (1,056 mi). The range stretches from the far eastern Czech Republic (3%) in the northwest through Slovakia (17%), Poland (10%), Hungary (4%), Ukraine (10%), Romania (50%) to Serbia (5%) in the south. The highest range within the Carpathians is known as the Tatra mountains in Slovakia and Poland, where the highest peaks exceed 2,600 m (8,530 ft). The second-highest range is the Southern Carpathians in Romania, where the highest peaks range between 2,500 m (8,202 ft) and 2,550 m (8,366 ft).
The divisions of the Carpathians are usually in three major sections:
The term Outer Carpathians is frequently used to describe the northern rim of the Western and Eastern Carpathians.
The Carpathians provide habitat for the largest European populations of brown bears, wolves, chamois, and lynxes, with the highest concentration in Romania,as well as over one third of all European plant species. The mountains and their foothills also have many thermal and mineral waters, with Romania having one-third of the European total. Romania is likewise home to the second-largest surface of virgin forests in Europe after Russia, totaling 250,000 hectares (65%), most of them in the Carpathians, with the Southern Carpathians constituting Europe's largest unfragmented forest area. Deforestation rates due to illegal logging in the Carpathians are high.
In modern times, the range is called Karpaty in Czech, Polish and Slovak and Карпати (Karpaty) in Ukrainian, Карпати / Karpati in Serbian, Carpați [karˈpat͡sʲ] ( listen ) in Romanian, Карпаты in Rusyn, Karpaten in German and Kárpátok in Hungarian. Although the toponym was recorded already by Ptolemy in the second century of the Christian era, the modern form of the name is a neologism in most languages. For instance, Havasok ("Snowy Mountains") was its medieval Hungarian name; Russian chronicles referred to it as "Hungarian Mountains". Later sources, such as Dimitrie Cantemir and the Italian chronicler Giovanandrea Gromo, referred to the range as "Transylvania's Mountains", while the 17th-century historian Constantin Cantacuzino translated the name of the mountains in an Italian-Romanian glossary to "Rumanian Mountains".
The name "Carpates" is highly associated with the old Dacian tribes called "Carpes" or "Carpi" who lived in a large area from the east, north-east of the Black Sea to Transylvanian plains on the present day Romania and Moldova. The name Carpates may ultimately be from the Proto Indo-European root *sker-/*ker-, from which comes the Albanian word karpë (rock), and the Slavic word skála (rock, cliff), perhaps via a Dacian cognate[ which? ] which meant mountain, rock, or rugged (cf. Germanic root *skerp-, Old Norse harfr "harrow", Gothic skarpo, Middle Low German scharf "potsherd", and Modern High German Scherbe "shard", Old English scearp and English sharp, Lithuanian kar~pas "cut, hack, notch", Latvian cìrpt "to shear, clip"). The archaic Polish word karpa meant "rugged irregularities, underwater obstacles/rocks, rugged roots, or trunks". The more common word skarpa means a sharp cliff or other vertical terrain. The name may instead come from Indo-European *kwerp "to turn", akin to Old English hweorfan "to turn, change" (English warp) and Greek καρπόςkarpós "wrist", perhaps referring to the way the mountain range bends or veers in an L-shape.
In late Roman documents, the Eastern Carpathian Mountains were referred to as Montes Sarmatici (meaning Sarmatian Mountains). [ citation needed ]The Western Carpathians were called Carpates, a name that is first recorded in Ptolemy's Geographia (second century AD).
In the Scandinavian Hervarar saga , which relates ancient Germanic legends about battles between Goths and Huns, the name Karpates appears in the predictable Germanic form as Harvaða fjöllum (see Grimm's law).
"Inter Alpes Huniae et Oceanum est Polonia" ("Between the Hunic Alps and the ocean lies Poland") by Gervase of Tilbury, has described in his Otia Imperialia ("Recreation for an Emperor") in 1211.Thirteenth- to fifteenth-century Hungarian documents named the mountains Thorchal, Tarczal, or less frequently Montes Nivium ("Snowy Mountains").
The northwestern Carpathians begin in Slovakia and southern Poland. They surround Transcarpathia and Transylvania in a large semicircle, sweeping towards the southeast, and end on the Danube near Orşova in Romania. The total length of the Carpathians is over 1,500 km (932 mi) and the mountain chain's width varies between 12 and 500 km (7 and 311 mi). The highest altitudes of the Carpathians occur where they are widest. The system attains its greatest breadth in the Transylvanian plateau and in the southern Tatra Mountains group – the highest range, in which Gerlachovský štít in Slovakia is the highest peak at 2,655 m (8,711 ft) above sea level. The Carpathians cover an area of 190,000 km2 (73,359 sq mi), and after the Alps, form the next-most extensive mountain system in Europe.
Although commonly referred to as a mountain chain, the Carpathians do not actually form an uninterrupted chain of mountains. Rather, they consist of several orographically and geologically distinctive groups, presenting as great a structural variety as the Alps. The Carpathians, which attain an altitude over 2,500 m (8,202 ft) in only a few places, lack the bold peaks, extensive snowfields, large glaciers, high waterfalls, and numerous large lakes that are common in the Alps. It was believed that no area of the Carpathian range was covered in snow all year round and there were no glaciers, but recent research by Polish scientists discovered one permafrost and glacial area in the Tatra Mountains. The Carpathians at their highest altitude are only as high as the middle region of the Alps, with which they share a common appearance, climate, and flora. The Carpathians are separated from the Alps by the Danube. The two ranges meet at only one point: the Leitha Mountains at Bratislava. The river also separates them from the Balkan Mountains at Orşova in Romania. The valley of the March and Oder separates the Carpathians from the Silesian and Moravian chains, which belong to the middle wing of the great Central Mountain System of Europe. Unlike the other wings of the system, the Carpathians, which form the watershed between the northern seas and the Black Sea, are surrounded on all sides by plains, namely the Pannonian plain to the southwest, the Lower Danubian Plain to the south, with the southern part being in Bulgaria, and the northern - in (Romania), and the Galician plain to the northeast.
Important cities and towns in or near the Carpathians are, in approximate descending order of population:
This is an (incomplete) list of the peaks of the Carpathians having summits over 2,500 metres (8,200 ft), with their heights, geologic divisions, and locations.
|Peak||Geologic divisions||Nation (Nations)||County (Counties)||Height (m)|
|Gerlachovský štít||High Tatras||Slovakia||Prešov Region||2,655|
|Gerlachovská veža||High Tatras||Slovakia||Prešov Region||2,642|
|Lomnický štít||High Tatras||Slovakia||Prešov Region||2,633|
|Ľadový štít||High Tatras||Slovakia||Prešov Region||2,627|
|Pyšný štít||High Tatras||Slovakia||Prešov Region||2,623|
|Zadný Gerlach||High Tatras||Slovakia||Prešov Region||2,616|
|Lavínový štít||High Tatras||Slovakia||Prešov Region||2,606|
|Malý Ľadový štít||High Tatras||Slovakia||Prešov Region||2,602|
|Kotlový štít||High Tatras||Slovakia||Prešov Region||2,601|
|Lavínová veža||High Tatras||Slovakia||Prešov Region||2,600|
|Malý Pyšný štít||High Tatras||Slovakia||Prešov Region||2,591|
|Veľká Litvorová veža||High Tatras||Slovakia||Prešov Region||2,581|
|Strapatá veža||High Tatras||Slovakia||Prešov Region||2,565|
|Kežmarský štít||High Tatras||Slovakia||Prešov Region||2,556|
|Vysoká||High Tatras||Slovakia||Prešov Region||2,547|
|Viştea Mare||Făgăraş Mountains||Romania||Brașov||2,527|
|Parângu Mare||Parâng Mountains||Romania||Alba, Gorj, Hunedoara||2,519|
|Vânătoarea lui Buteanu||Făgăraș Mountains||Romania||Argeș||2,507|
|Omu (mountain)||Bucegi Mountains||Romania||Prahova, Brașov, Dâmbovița||2,505|
|Cornul Călțunului||Făgăraș Mountains||Romania||Sibiu||2,505|
|Ocolit (Bucura)||Bucegi Mountains||Romania||Prahova, Brașov, Dâmbovița||2,503|
|Rysy||High Tatras||Poland, Slovakia||Lesser Poland Voivodeship, Prešov Region||2,503|
This is a list of the highest national peaks of the Carpathians, their heights, geologic divisions, and locations. Excluding mountains located in two countries (on the border).
|Peak||Geologic divisions||Nation (Nations)||County (Counties)||Height (m)|
|Gerlachovský štít||High Tatras||Slovakia||Prešov Region||2,655|
|Rysy||Fatra-Tatra Area||Poland||Tatra County||2,503|
|Hoverla||Eastern Beskids (Chornohora)||Ukraine||Nadvirna Raion, Rakhiv Raion||2,061|
|Rtanj||Serbian Carpathians||Serbia||Zaječar District||1,565|
|Lysá hora||Moravian-Silesian Beskids||Czech Republic||Moravian-Silesian Region||1,323|
|Kékes||North Hungarian Mountains||Hungary||Heves County||1,014|
In the Romanian part of the main chain of the Carpathians, mountain passes include Prislop Pass, Tihuța Pass, Bicaz Canyon, Ghimeș Pass, Buzău Pass, Predeal Pass (crossed by the railway from Braşov to Bucharest), Turnu Roșu Pass (1,115 ft., running through the narrow gorge of the Olt River and crossed by the railway from Sibiu to Bucharest), Vulcan Pass, and the Iron Gate (both crossed by the railway from Timișoara to Craiova).
The area now occupied by the Carpathians was once occupied by smaller ocean basins. The Carpathian mountains were formed during the Alpine orogeny in the Mesozoicand Tertiary by moving the ALCAPA (Alpine-Carpathian-Pannonian), Tisza and Dacia plates over subducting oceanic crust. The mountains take the form of a fold and thrust belt with generally north vergence in the western segment, northeast to east vergence in the eastern portion and southeast vergence in the southern portion.
The external, generally northern, portion of the orogenic belt is a Tertiary accretionary wedge of a so-called Flysch belt (the Carpathian Flysch Belt) created by rocks scraped off the sea bottom and thrust over the North-European plate. The Carpathian accretionary wedge is made of several thin skinned nappes composed of Cretaceous to Paleogene turbidites. Thrusting of the Flysch nappes over the Carpathian foreland caused the formation of the Carpathian foreland basin.The boundary between the Flysch belt and internal zones of the orogenic belt in the western segment of the mountain range is marked by the Pieniny Klippen Belt, a narrow complicated zone of polyphase compressional deformation, later involved in a supposed strike-slip zone. Internal zones in western and eastern segments contain older Variscan igneous massifs reworked in Mesozoic thick and thin-skinned nappes. During the Middle Miocene this zone was affected by intensive calc-alkaline arc volcanism that developed over the subduction zone of the flysch basins. At the same time, the internal zones of the orogenic belt were affected by large extensional structure of the back-arc Pannonian Basin. The last volcanic activity occurred at Ciomadul about 30,000 years ago.
Iron, gold and silver were found in great quantities in the Western Carpathians. After the Roman emperor Trajan's conquest of Dacia, he brought back to Rome over 165 tons of gold and 330 tons of silver.
The ecology of the Carpathians varies with altitude, ranging from lowland forests to alpine meadows. Foothill forests are primarily of broadleaf deciduous trees, including oak, hornbeam, and linden. European beech is characteristic of the montane forest zone. Higher-elevation subalpine forests are characterized by Norway spruce (Picea abies). Krummholtz and alpine meadows occur above the treeline.
Wildlife in the Carpathians includes brown bear (Ursus arctos), wolf (Canis lupus), Eurasian lynx (Lynx lynx), European wildcat (Felis silvestris), Tatra chamois (Rupicapra rupicapra tatrica), European bison (Bison bonasus), and golden eagle (Aquila chrysaetos).
The largest range is the Tatras in Slovakia and Poland. A major part of the western and northeastern Outer Eastern Carpathians in Poland, Ukraine, and Slovakia is traditionally called the Eastern Beskids.
The geological border between the Western and Eastern Carpathians runs approximately along the line (south to north) between the towns of Michalovce, Bardejov, Nowy Sącz and Tarnów. In older systems the border runs more in the east, along the line (north to south) along the rivers San and Osława (Poland), the town of Snina (Slovakia) and river Tur'ia (Ukraine). Biologists shift the border even further to the east.
The border between the eastern and southern Carpathians is formed by the Predeal Pass, south of Braşov and the Prahova Valley.
In geopolitical terms, Carpathian Mountains are often grouped and labeled according to national or regional borders, but such division has turned out to be relative, since it was, and still is dependent on frequent historical, political and administrative changes of national or regional borders. According to modern geopolitical division, Carpathians can be grouped as: Serbian, Romanian, Ukrainian, Polish, Slovakian, Czech, Austrian, and Hungarian. Within each nation, specific classifications of the Carpathians have been developing, often reflecting local traditions, and thus creating terminological diversity, that produces various challenges in the fields of comparative classification and international systematization.
The section of the Carpathians within the borders of Romania is commonly known as the Romanian Carpathians. In local use, Romanians sometimes denote as "Eastern Carpathians" only the Romanian part of the Eastern Carpathians, which lies on their territory (i.e., from the Ukrainian border or from the Prislop Pass to the south), which they subdivide into three simplified geographical groups (northern, central, southern), instead of Outer and Inner Eastern Carpathians. These groups are:
The section of the Carpathians within the borders of Ukraine is commonly known as the Ukrainian Carpathians. Classification of eastern sections of the Carpathians is particularly complex, since it was influenced by several overlapping traditions. Terms like Wooded Carpathians, Poloniny Mountains or Eastern Beskids are often used in varying scopes by authors belonging to different traditions.
The geography of Ukraine varies greatly from one region of the country to another, with the majority of the country lying within the East European Plain. Ukraine is the second-largest country by area in Europe. Its various regions have diverse geographic features ranging from highlands to lowlands, as well as climatic range and a wide variety in hydrography.
The Tatra Mountains, Tatras, or Tatra, is a mountain range that forms a natural border between Slovakia and Poland. They are the highest mountain range in the Carpathian Mountains. The Tatras are distinct from the Low Tatras, a separate Slovak mountain range further south.
The Beskids or Beskid Mountains are a series of mountain ranges in the Carpathians, stretching from the Czech Republic in the west along the border of Poland with Slovakia up to Ukraine in the east.
The Southern Carpathians are a group of mountain ranges located in southern Romania. They cover the part of the Carpathian Mountains located between the Prahova River in the east and the Timiș and Cerna Rivers in the west. To the south they are bounded by the Balkan mountain range in eastern Serbia.
The Pannonian Basin, or Carpathian Basin, is a large basin in Central Europe. The geomorphological term Pannonian Plain is more widely used for roughly the same region though with a somewhat different sense, with only the lowlands, the plain that remained when the Pliocene Epoch Pannonian Sea dried out.
Divisions of the Carpathians are a categorization of the Carpathian mountains system.
The High Tatras or High Tatra Mountains, are a mountain range along the border of northern Slovakia in the Prešov Region, and southern Poland in the Lesser Poland Voivodeship. They are a range of the Tatra Mountains chain.
The Alps cover a large area. This article describes the delimitation of the Alps as a whole and of subdivisions of the range, follows the course of the main chain of the Alps and discusses the lakes and glaciers found in the region.
The Western Carpathians are a mountain range and geomorphological province that forms the western part of the Carpathian Mountains.
Tatra(s) National Park is one of the nine national parks in Slovakia. It is situated in North Central Slovakia in the Tatra Mountains. The park is important for protecting a diverse variety of flora and fauna, with many endemic species, including the Tatra chamois.
The Pieniny Klippen Belt is in geology a tectonically and orographically remarkable zone in the Western Carpathians, with a very complex geological structure. It is a narrow and extremely long north banded zone of extreme shortening and sub-vertical strike-slip fault zone, with complex geological history, where only fragments of individual strata and facies are preserved. The Pieniny Klippen Belt is considered one of the main tectonic sutures of the Carpathians and forms the boundary between the Outer and Central Western Carpathians.
The Western Carpathians are an arc-shaped mountain range, the northern branch of the Alpine-Himalayan fold and thrust system called the Alpide belt, which evolved during the Alpine orogeny. In particular, their pre-Cenozoic evolution is very similar to that of the Eastern Alps, and they constitute a transition between the Eastern Alps and the Eastern Carpathians.
The regional geology of Serbia describes the geologic structure and history inside the borders of Serbia.
The Carpathian Flysch Belt is an arcuate tectonic zone included in the megastructural elevation of the Carpathians on the external periphery of the mountain chain. Geomorphologically it is a portion of Outer Carpathians. Geologically it is a thin-skinned thrust belt or accretionary wedge, formed by rootles nappes consisting of so-called flysch - alternating marine deposits of claystones, shales and sandstones which were detached from their substratum and moved tens of kilometers to the north (generally). The Flysch Belt is together with Neogene volcanic complexes only tectonic zone occurring along the whole Carpathian arc.
The geology of Romania is structurally complex, with evidence of past crustal movements and the incorporation of different blocks or platforms to the edge of Europe, driving recent mountain building of the Carpathian Mountains. Romania is a country located at the crossroads of Central, Eastern, and Southeastern Europe. It borders the Black Sea to the southeast, Bulgaria to the south, Ukraine to the north, Hungary to the west, Serbia to the southwest, and Moldova to the east.
The geology of Slovakia is structurally complex, with a highly varied array of mountain ranges and belts largely formed during the Paleozoic, Mesozoic and Cenozoic eras.
The Pannonian Biogeographic Region is a biogeographic region, as defined by the European Environment Agency. It covers the lowlands of the Pannonian Basin centered on Hungary.
The Krempachy Marl Formation is a geological formation in Poland and Slovakia, dating to about 179 million years ago, and covering the middle Toarcian stage of the Jurassic Period. It is among the most important formations of the Toarcian boundary on the Carpathian realm, being the regional equivalent of the Posidonia Shale.
The Carpathian montane conifer forests, also known as Carpathian montane forests, is a temperate coniferous forests ecoregion in the Carpathian Mountains of the Czech Republic, Poland, Slovakia, Ukraine, and Romania.
|Wikivoyage has a travel guide for Carpathian Mountains .|
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|Wikisource has the text of the 1911 Encyclopædia Britannica article Carpathian Mountains .|