Choč Mountains
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Choč Mountains
The Choč Mountains (in Slovak, ''Chočské vrchy'') are a range of mountains in north-central Slovakia, a portion of the Fatra-Tatra Area of the Inner Western Carpathians. The range is 24 kilometers long and on average only 4 kilometers wide. Highest peak is Veľký Choč at 1 611 metres above sea level. Location Choč Mountains are bordered: * in the northwest by the Orava Highlands, * in the northeast by the valley of the Podtatranská Brázda, * in the east by the Western Tatras, * the south by the basin of the Podtatranská kotlina, * in the southwest by Greater Fatra Highest Peaks * Veľký Choč, 1611 metres * Malý Choč, 1465 metres * Prosečné, 1371 metres * Holica, 1340 metres * Lomná, 1278 metres See also * Tatra Mountains * Tourism in Slovakia Tourism in Slovakia offers natural landscapes, mountains, caves, medieval castles and towns, folk architecture, spas and ski resorts. More than 5 million people visited Slovakia in 2017, and the most attract ...
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Slovak Language
Slovak ( ; endonym: or ), is a West Slavic language of the Czech-Slovak languages, Czech–Slovak group, written in Latin script and formerly in Cyrillic script. It is part of the Indo-European languages, Indo-European language family, and is one of the Slavic languages, which are part of the larger Balto-Slavic languages, Balto-Slavic branch. Spoken by approximately 5 million people as a native language, primarily ethnic Slovaks, it serves as the official language of Slovakia and one of the 24 official languages of the European Union. Slovak is closely related to Czech language, Czech, to the point of very high mutual intelligibility, as well as to Polish language, Polish. Like other Slavic languages, Slovak is a fusional language with a complex system of morphology (linguistics), morphology and relatively flexible word order. Its vocabulary has been extensively influenced by Latin and German language, German, as well as other Slavic languages. History The Czech–Slovak gr ...
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Slovakia
Slovakia, officially the Slovak Republic, is a landlocked country in Central Europe. It is bordered by Poland to the north, Ukraine to the east, Hungary to the south, Austria to the west, and the Czech Republic to the northwest. Slovakia's mostly mountainous territory spans about , hosting a population exceeding 5.4 million. The capital and largest city is Bratislava, while the second largest city is Košice. The Slavs arrived in the territory of the present-day Slovakia in the 5th and 6th centuries. From the late 6th century, parts of modern Slovakia were incorporated into the Pannonian Avars, Avar Khaghanate. In the 7th century, the Slavs played a significant role in the creation of Samo's Empire. When the Avar Khaghanate dissolved in the 9th century, the Slavs established the Principality of Nitra before it was annexed by the Great Moravia, Principality of Moravia, which later became Great Moravia. When Great Moravia fell in the 10th century, the territory was integrated i ...
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Fatra-Tatra Area
The Fatra-Tatra Area (in geomorphology) or the Tatra-Fatra Belt of core mountains (in geology) is a part of the Inner Western Carpathians, a subprovince of the Western Carpathians. Most of the area lies in Slovakia with small parts reaching into Austria and Poland Poland, officially the Republic of Poland, is a country in Central Europe. It extends from the Baltic Sea in the north to the Sudetes and Carpathian Mountains in the south, bordered by Lithuania and Russia to the northeast, Belarus and Ukrai .... The highest summit of the whole Carpathians, the Gerlachovský štít at , lies in the High Tatras range which belongs to this area. The Fatra-Tatra Area is from the northern side bounded by Pieniny Klippen Belt. Mountains of the area are located in two ranges. The external range consists of Hainburg Hills, Malé Karpaty (Pezinok part), Považský Inovec, Strážovské vrchy, Malá Fatra, Tatras (Western Tatras, Western, High Tatras, High and Belianske Tatras). Inner r ...
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Inner Western Carpathians
Divisions of 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. 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. Naming conventions The division is largely (with many exceptions) undisputed at the lowest level (except for the Ukrainian part), but various divisions are given for the higher levels, especially for the penultimate level. A geomorphological division has been used as much as the data was available; other new physioge ...
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Orava Highlands
The Orava Highlands (in Slovak, ''Oravská vrchovina'') is a range of small mountains in the Žilina Region of north central Slovakia, part of the Outer Western Carpathians. In Slovakia these hills are considered part of the Central Beskids; in Poland they're considered Western Beskids. The highlands stretch along both sides of the Orava River, and cover an area about 220 square kilometers. It consists of two smaller areas: the ''Podchočská brázda'' (the Podchočská furrow) and the ''Veličnianska kotlina'' (Veličnianska basin). The highest of the relatively modest summits are ''Kopec'' (1251 meters), ''Machy'' (1202 meters) and ''Mnich'' (1110 meters), the last of which towers over the ski resort town of Zuberec. Geologically the highlands are composed of Carpathian flysch Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rap ...
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Sub-Tatra Trench
Sub-Tatra Trench (Polish language, Polish: Rów Podtatrzański; Slovakian language, Slovakian: Podtatranská brázda) (Regions of Poland, 514.14) is a Mesoregion (geomorphology), mesoregion located below the Tatra Mountains, part of the Podhale-Magura Area, Orava-Podhale Depression. The trench divides the Choč Mountains, Choč and Tatra Mountains from the Spiš–Gubałówka Highlands. The region has an elevation of between 700 and 1000 m.a.s.l. It is formed from Eocene marlstone slates (Podhalański Flysch). In Poland, the area has a total length of 20 km and a total surface area of 130 km². The regional valleys incline in the north, covered with alluvial fans, formed via upper course river flow. The Zakopane Valley has three gravel top soil coverings from three separate glacial periods. The western part and eastern borderlands of the Podtatrzański Trench are forested. The main brooks that drain through the valley are the Czarny Dunajec (river), Czarny Dunajec, as well as ...
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