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14-729: The Gurghiu Mountains (Romanian: Munții Gurghiu [ m u n tsʲ i   ɡ u r ɡʲ u ] , Hungarian: Görgény [ɡørɡeːɲ] ) are a range in the Căliman-Harghita Mountains of the Eastern Carpathians , Romania , in the Transylvania region. They cover an area of 581.76 km (224.62 sq mi). The mountains are relatively low, but well-wooded and naturally beautiful. They are known for an abundance of wildlife, including deer, wild boar, wolves and bears. The highest peak, Vârful Saca Mare,

28-428: A list of the final units ( mountains etc.) from the west to the east and south, in a separate listing at the end. (CZ: Jihomoravské Karpaty , AT: Österreichisch-Südmährische Karpaten ) (CZ: Středomoravské Karpaty ) (CZ/SK: Slovensko-moravské Karpaty ) (CZ: Západobeskydské podhůří , PL: Pogórze Zachodniobeskidzkie ) (CZ: Západní Beskydy , SK: Západné Beskydy , PL: Beskidy Zachodnie ) Western section of

42-480: Is 1,776 m (5,827 ft). Notable peaks include Amza Peak at 1,695 m (5,561 ft), Saca Mică Peak at 1,731 m (5,679 ft), and Fâncelu at 1,684 m (5,525 ft). Average rainfall is about 1,200 mm (47 in) and average temperature 4 °C (39 °F). The Gurghiu Mountains are part of the volcanic mountain chain in the western side of the Eastern Carpathians. In

56-1090: Is denoted as "Eastern Carpathians" only the part basically on their territory (i.e.to the north of the Prislop Pass ), while in Romania sometimes use to call "Eastern Carpathians" ( Carpații Orientali ) only the other part, which lies on their territory (i.e. from the Ukrainian border or from the Prislop Pass to the south). In some Polish classifications, Central Beskids and Central Beskidian Piedmont belongs to Western Carpathians province and Outer Western Carpathians subprovince. Wooded Beskids (PL: Beskidy Lesiste; UA: Лісисті Бескиди): Polonynian Beskids (PL: Beskidy Połonińskie; UA: Полонинські Бескиди; SK: Poloniny): Criș Mountains ( Munții Criș ) : Seș-Meseș Mountains ( Munții Seș-Meseșului ): Bihor Massif ( Masivul Bihor ): Mureș Mountains ( Munții Mureșului ): (Note: sometimes considered part of

70-624: The Eastern Carpathians in Romanian territory into three formal groups (northern, central, southern), instead in Outer and Inner sections of Eastern Carpathians. The Romanian approach is shown by adding the following abbreviations to the names of units within Romania: A similar standard (grouping of outer and inner sections) is traditionally applied within broader use of the term " Wooded Carpathians ", that encompasses all mountain ranges within

84-708: The ISO 3166-1 alpha-2 country codes : The most confusing and diverse is the classification of the Beskids , including the Western Beskids , the Central Beskids and the Eastern Beskids . Their geologic features are fairly distinct, but multiple traditions, languages, and nationalities have developed overlapping variants for the divisions and names of these ranges. In Romania , it is usual to divide

98-722: The Western Beskids Northern section of the Western Beskids Eastern section of the Western Beskids (in Slovak terminology: Eastern Beskids , SK: Východné Beskydy ) Central section of the Western Beskids (in Slovak terminology: Central Beskids , SK: Stredné Beskydy ) Source: (SK: Podhôľno-magurská oblasť , PL: Obniżenie Orawsko-Podhalańskie ) Slovak : Slovenské rudohorie Clarification: In Ukraine sometimes

112-596: The Carpathians are a categorization of the Carpathian mountains system. Below is a detailed overview of the major subdivisions and ranges of the Carpathian Mountains . The Carpathians are a "subsystem" of a bigger Alps-Himalaya System that stretches from western Europe all the way to southern Asia, and are further divided into " provinces " and "subprovinces". The last level of the division, i.e.

126-663: The Southern Carpathians (together with the Banat Mountains ), sometimes not considered part of the Carpathians at all. They're included below. The regions of Outer Subcarpathia lay outside the broad arc of the entire formation and are usually listed as part of the individual divisions of the Carpathian Mountains, i.e. of Western Carpathians, Eastern Carpathians, etc. With the difficulty of finding their exact subdivisions, they are given only as

140-624: The Southern Carpathians) (Note: sometimes considered part of the Southern Carpathians) Transylvanian Plateau ( Podișul Transilvaniei ): The Outer Subcarpathian regions are divided into Western, Northern, etc. and are usually treated as part of the individual parts of the Carpathian Mountains, i.e. of Western Carpathians, Eastern Carpathians, etc. Since, however, it was impossible to find their exact subdivision, they are given only as

154-465: The actual mountain ranges and basins, is usually classified as "units". The main divisions are shown in the map on the right. To generalize, there are three major provinces (regions): Western Carpathians, Eastern Carpathians, and the Southern Carpathians. The division is largely (with many exceptions) undisputed at the lowest level (except for the Ukrainian part), but various divisions are given for

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168-572: The central section of Outer Eastern Carpathians , including Eastern Beskids with Polonynian Mountains , and also all mountains within the northern section of Inner Eastern Carpathians , including Vihorlat-Gutin Area and Maramureș-Rodna Area . The Transylvanian Plateau is encircled by, and geologically a part of, the Carpathians. But it is not a mountainous region and its inclusion is disputed in some sources. Its features are included below. The Serbian Carpathians are sometimes considered part of

182-420: The higher levels, especially for the penultimate level. A geomorphological division has been used as much as the data was available; other new physiogeographic divisions were used in other cases. Where the classification of a higher level "title" is known/sure, it is added at the end of the name in brackets, e.g. "(subprovince)". The names are also given in the language of the corresponding country and marked by

196-690: The north the Mureș River separates them from the Călimani Mountains . To the south are the Harghita Mountains and the Târnava River Valley. The mountains were formed during a period of volcanic activity between 9.4 and 5.4 million years ago, starting in the north and moving southwards. This Romanian location article is a stub . You can help Misplaced Pages by expanding it . Eastern Carpathians Divisions of

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