The Carpathian Mountains or Carpathians (/kɑːrˈpeɪθiənz/) are a range of mountains forming an arc across Central Europe. Roughly 1,500 km (930 mi) long, it is the third-longest European mountain range after the Urals at 2,500 km (1,600 mi) and the Scandinavian Mountains at 1,700 km (1,100 mi). The range stretches from the far eastern Czech Republic (3%) and Austria (1%) in the northwest through Slovakia (21%), Poland (10%), Ukraine (10%), Romania (50%) to Serbia (5%) in the south.[1][2][3][4] The highest range within the Carpathians is known as the Tatra mountains in Poland and Slovakia, where the highest peaks exceed 2,600 m (8,500 ft). The second-highest range is the Southern Carpathians in Romania, where the highest peaks range between 2,500 m (8,200 ft) and 2,550 m (8,370 ft).
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,[6][7][8] as well as over one-third of all European plant species.[9] The mountains and their foothills also have many thermal and mineral waters, with Romania having one-third of the European total.[10][11] Romania is likewise home to the second-largest area of virgin forests in Europe after Russia, totaling 250,000 hectares (65%), most of them in the Carpathians,[12] with the Southern Carpathians constituting Europe's largest unfragmented forest area.[13] Deforestation rates due to illegal logging in the Carpathians are high.[14]
In modern times, the range is called Karpaty in Czech, Polish and Slovak and Карпати (Karpaty) in Ukrainian, Карпати / Karpati in Serbo-Croatian, Carpați[karˈpat͡sʲ]ⓘ in Romanian, Карпаты in Rusyn, KarpatenGerman pronunciation:[kaʁˈpaːtn̩]ⓘ in German and Kárpátok in Hungarian.[15][16] Although the toponym was recorded by Ptolemy in the second century AD, [17] the modern form of the name is a neologism in most languages.[15] For instance, Havasok ("Snowy Mountains") was its medieval Hungarian name. Russian chronicles referred to it as "Hungarian Mountains".[16][15] 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".[15]
The name "Carpates" is highly associated with the old Dacian tribes called "Carpes" or "Carpi" who lived in an area to the east of the Carpathians, from the east, northeast of the Black Sea to the Transylvanian Plain in the present day Romania and Moldova. Karpates is considered a Paleo-Balkan name, with evidence provided by the Albaniankárpë / kárpa, pl. kárpa / kárpat ('rock, stiff'), and the Messapickarpa 'tuff (rock), limestone' (preserved as càrpë 'tuff' in Bitonto dialect and càrparu 'limestone' in Salentino).[18][19][20][21][22][17] This connection is further supported by the fact that also the oronym Beskydy, a series of mountain ranges in the Carpathians, has a meaning in Albanian: bjeshkë / bjeshkët 'high mountains, mountain pastures' (cf. also the Albanian oronym Bjeshkët e Namuna, the Accursed Mountains / Albanian Alps).[21][22]
The name Carpates may ultimately be from the Proto Indo-European root *sker-/*ker-, which meant mountain, rock, or rugged (cf. Albanian kárpë, Germanic root *skerp-, Old Norse harfr "harrow", Gothic skarpo, Middle Low German scharf "potsherd", and Modern High German Scherbe "shard", Lithuanian kar~pas "cut, hack, notch", Latvian cìrpt "to shear, clip").[23] 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, cf..Old English scearp and English sharp. 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.[24]
In late Roman documents, the Eastern Carpathian Mountains were referred to as Montes Sarmatici (meaning Sarmatian Mountains).[25] The Western Carpathians were called Carpates, a name that is first recorded in Ptolemy's Geographia (second century AD).[26]
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, was described in his Otia Imperialia ("Recreation for an Emperor") in 1211.[27] Thirteenth- to fifteenth-century Hungarian documents named the mountains Thorchal, Tarczal, or less frequently Montes Nivium ("Snowy Mountains").[27]
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 Orșova in Romania. The total length of the Carpathians is over 1,500 km (930 mi). 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, is 2,655 m (8,711 ft) above sea level. The Carpathians cover an area of 190,000 km2 (73,000 sq mi). After the Alps, they form the next-most extensive mountain system in Europe.
Although commonly referred to as a mountain chain, the Carpathians do not 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 (8,200 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.[28]
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 Orșova 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. The Pannonian plain is 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.
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.
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).
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 Mesozoic[29] and Cenozoic by moving the ALCAPA (Alpine-Carpathian-Pannonian), Tisza and Dacia plates over subductingoceanic crust.[30]
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. Currently, the area is the most seismically active in Central Europe.[31]
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.[32] 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.[33]
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[34]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[35] of the back-arcPannonian Basin.[36] The last volcanic activity occurred at Ciomadul about 30,000 years ago.[34]
The mountains started to gain their current shape from the latest Miocene onward.[37] The slopes of the Carphartian contain at some locations solifluction deposits.[37]
Iron, gold and silver were found in great quantities[vague] 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.[38]
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). Krummholz and alpine meadows occur above the treeline.[39]
The range with the highest peaks 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. Romania comprises roughly 50% of the Carpathian chain where the rest of the highest peaks, above 2500m (in the Southern Carpathians) are found.
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 Brașov 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 and Austrian. 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:
Maramureș-Bukovinian Carpathians (Romanian: Carpații Maramureșului și ai Bucovinei)
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.
^ ab[1]Archived 12 October 2017 at the Wayback Machine "The Carpathians" European Travel Commission, in The Official Travel Portal of Europe, Retrieved 15 November 2016
^ ab[2]Archived 19 November 2016 at the Wayback Machine The Carpathian Project: Carpathian Mountains in Serbia, Institute for Spatial Planning, Faculty of Geography, University of Belgrade (2008), Retrieved: 15 November 2016
^[3]Archived 1 August 2019 at the Wayback Machine Bulletin of the Natural History Museum, pg. 54, Valuing the geological heritage of Serbia (UDC: 502.171:55(497.11), Aleksandra Maran (2010), Retrieved 15 November 2016
^ abÇabej, Eqrem. (1972). Studime Filologjike. universiteti shtetëror i Tiranës.
^ abÇabej, Eqrem (1985). "The Problem of the Place of Formation of the Albanian Language". The Albanians and their Territories. Academy of Sciences of Albania. Tiranë: 8 Nëntori. pp. 63–99. p. 67.
^Room, Adrian. Placenames of the World. London: MacFarland and Co., Inc., 1997.
^Room, Adrian. Placenames of the World. London: MacFarland and Co., Inc., 1997.
^Mantovani, E., Viti, M., Babbucci, D., Tamburelli, C., Albarello, D., 2006, Geodynamic connection between the indentation of Arabia and the Neogene tectonics of the central–eastern Mediterranean region. GSA Special Papers, v. 409, p. 15-41
^Nehyba, S., Šikula, J., 2007, Depositional architecture, sequence stratigraphy and geodynamic development of the Carpathian Foredeep (Czech Republic). Geologica Carpathica, 58, 1, pp. 53-69
^Mišík, M., 1997, The Slovak Part of the Pieniny Klippen Belt After the Pioneering Works of D. Andrusov. Geologica Carpathica, 48, 4, pp. 209-220
^ abPácskay, Z., Lexa, J., Szákacs, A., 2006, Geochronology of Neogene magmatism in the Carpathian arc and intra-Carpathian area. Geologica Carpathica, 57, 6, pp. 511 - 530
^Dolton, G.L., 2006, Pannonian Basin Province, Central Europe (Province 4808)—Petroleum geology, total petroleum systems, and petroleum resource assessment. U.S. Geological Survey Bulletin 2204–B, 47 p.
^Royden, L.H., Horváth, F., Rumpler, J., 1983, '"Evolution of the Pannonian basin system. 1. Tectionics." Tectonics, 2, pp. 61-90
^ abStarkel, Leszek (1969). "L'évolution des versants des Carpates à flysch au quaternaire". Biuletyn Peryglacjalny (in French). 18: 349–379.
Blazovich, László (1994). "Kárpátok [Carpathians]". In Kristó, Gyula; Engel, Pál; Makk, Ferenc (eds.). Korai magyar történeti lexikon (9-14. század) [Encyclopedia of the Early Hungarian History (9th-14th centuries)] (in Hungarian). Akadémiai Kiadó. p. 332. ISBN963-05-6722-9.
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