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Čergov
Čergov is a mountain range in the central part of the Prešov Region of Slovakia. Geologically the range is part of the Outer Western Carpathians. The Polish name for the range is ''Góry Czerchowskie'', the Czerchów Mountains. In Polish terminology, it is classified within the eastern section of the Western Beskids. In Slovak terminology, the same region is known simply as the ''Eastern Beskids'' ( sk, Východné Beskydy). The entire range is composed of Carpathian flysch and is oriented from north to southeast. The major peaks include ''Minčol'' (1157 m), ''Veľká Javorina'' (1098 m), ''Bukový vrch'' (1010 m), and ''Lysá'' (1068 m). Čergov Peak itself stands at 1050 m. The Topľa River and many of its tributaries, creeks and rivers arise from its eastern slopes. The slopes are grown with mixed forests with a predominance of deciduous trees, mostly beech, maple, oak, and birch. At least five major nature reserves have been set aside for rare and protected s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topľa
Topľa ( hu, Tapoly, german: Töpl) is a river in eastern Slovakia and right tributary of the Ondava. It is long and its basin covers an area of . It rises in the Čergov mountains, flows through Ondava Highlands, Beskidian Piedmont, Eastern Slovak Hills and Eastern Slovak Flat and flows into the Ondava in the cadastral area of Parchovany. It flows through the towns of Bardejov, Giraltovce, Hanušovce nad Topľou and Vranov nad Topľou. Etymology The name come from Slavic ( Slovak) ''Teplá'': warm (river). The name was adopted by Hungarians and then it was adopted back (in the modified form) by Slovaks The Slovaks ( sk, Slováci, singular: ''Slovák'', feminine: ''Slovenka'', plural: ''Slovenky'') are a West Slavic ethnic group and nation native to Slovakia who share a common ancestry, culture, history and speak Slovak. In Slovakia, 4.4 mi ..., probably in the 13th century. References Rivers of Slovakia {{Slovakia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Section Of The Western Beskids
Eastern section of the Western Beskids ( cs, Východní část Západních Beskyd) are a set of mountain ranges spanning the southern Polish and northern Slovak border. They constitute an eastern section of the Western Beskids, within the Outer Western Carpathians. In geographic classification, the term ''Beskid Mountains'' has several definitions, related to distinctive historical and linguistic traditions. Depending on a particular classification, designation ''Eastern'' in relation to the Beskids is also used with different meanings. In Slovak terminology, the term ''Eastern Beskids'' ( sk, Východné Beskydy) is used to designate the eastern section of the Western Beskids. In Polish terminology, the same region is also classified as the eastern section of the Western Beskids, but not under the term ''Eastern Beskids'' ( pl, Beskidy Wschodnie), since that term is used to designate Eastern Beskids of the Outer Eastern Carpathians. Subdivisions The Eastern section of the Weste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prešov Region
The Prešov Region, also Priashiv Region ( sk, Prešovský kraj, ; hu, Eperjesi kerület; uk, Пряшівський край) is one of the eight Slovak administrative regions and consists of 13 districts (okresy) and 666 municipalities, 23 of which have town status. The region was established in 1996 and is the most populous of all the regions in Slovakia. Its administrative center is the city of Prešov. Geography It is located in the north-eastern Slovakia and has an area of 8,975 km2. The region has a predominantly mountainous landscape. The subdivisions of Tatras – High Tatras and Belianske Tatras lie almost entirely in the region and include the highest point of Slovakia – Gerlachovský štít (2,654 ASL). Other mountain ranges and highlands in the region are Šarišská vrchovina, Čergov, Ondavská vrchovina, Slanské vrchy, Pieniny, Levoča Hills, Laborecká vrchovina, Bukovské vrchy, Vihorlat Mountains and Eastern Slovak Lowland. The basins in Prešov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Outer 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 physiogeog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Outer Eastern 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 physiogeo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovakia
Slovakia (; sk, Slovensko ), officially the Slovak Republic ( sk, Slovenská republika, links=no ), 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 southwest, and the Czech Republic to the northwest. Slovakia's mostly mountainous territory spans about , with a population of over 5.4 million. The capital and largest city is Bratislava, while the second largest city is Košice. The Slavs arrived in the territory of present-day Slovakia in the fifth and sixth centuries. In the seventh century, they played a significant role in the creation of Samo's Empire. In the ninth century, they established the Principality of Nitra, which was later conquered by the Principality of Moravia to establish Great Moravia. In the 10th century, after the dissolution of Great Moravia, the territory was integrated into the Principality of Hungary, which then became the Kingdom of Hungary in 1000. In 1241 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polish Language
Polish (Polish: ''język polski'', , ''polszczyzna'' or simply ''polski'', ) is a West Slavic language of the Lechitic group written in the Latin script. It is spoken primarily in Poland and serves as the native language of the Poles. In addition to being the official language of Poland, it is also used by the Polish diaspora. There are over 50 million Polish speakers around the world. It ranks as the sixth most-spoken among languages of the European Union. Polish is subdivided into regional dialects and maintains strict T–V distinction pronouns, honorifics, and various forms of formalities when addressing individuals. The traditional 32-letter Polish alphabet has nine additions (''ą'', ''ć'', ''ę'', ''ł'', ''ń'', ''ó'', ''ś'', ''ź'', ''ż'') to the letters of the basic 26-letter Latin alphabet, while removing three (x, q, v). Those three letters are at times included in an extended 35-letter alphabet, although they are not used in native words. The traditional ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovak Language
Slovak () , is a West Slavic language of the Czech–Slovak group, written in Latin script. It is part of the Indo-European language family, and is one of the Slavic languages, which are part of the larger 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, to the point of mutual intelligibility to a very high degree, as well as Polish. Like other Slavic languages, Slovak is a fusional language with a complex system of morphology and relatively flexible word order. Its vocabulary has been extensively influenced by Latin and German and other Slavic languages. The Czech–Slovak group developed within West Slavic in the high medieval period, and the standardization of Czech and Slovak within the Czech–Slovak dialect continuum emerged in the early modern period. In the later mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Slovakia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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