Spiš Magura
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Spiš Magura
The Spiš Magura ( sk, Spišská Magura, hu, Szepesi-Magura) is a set of mountain ranges in northern Slovakia, part of the Podhale-Magura Area region of the Outer Western Carpathians. The western and northern boundaries of the Spiš Magura are the international border with Poland. Its highest point is Repisko (1259 meters). See also * Geography of Slovakia Slovakia is a landlocked Central European country with mountainous regions in the north and flat terrain in the south. During much of the Holocene, Slovakia was much more forested than today. Decline of the forest occurred in as consequence of t ... {{DEFAULTSORT:Spis Magura Mountain ranges of Slovakia Mountain ranges of the Western Carpathians ...
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Podhale-Magura Area
The Podhale-Magura Area ( sk, Podhôľno-magurská oblasť; known in Polish language, Polish as the Orava-Podhale Depression, ''Obniżenie Orawsko-Podhalańskie'') — is a Geomorphology, geomorfologic region of mountain ranges in northern Slovakia and southern Poland, belonging to the Outer Western Carpathians within the Carpathian Mountains system. Subdivision The Podhale-Magura Area consists of: * Skorušina Mountains (SK: ''Skorušinské vrchy'') + Spiš-Gubałówka Piedmont (PL: ''Pogórze Spisko-Gubałowskie'') * Sub-Tatra Furrow (SK: ''Podtatranská brázda'', PL: ''Rów Podtatrzański'') * Spiš Magura (SK: ''Spišská Magura'') + Spiš-Gubałówka Piedmont (PL: ''Pogórze Spisko-Gubałowskie'') * Levoča Mountains (SK: ''Levočské vrchy''), with its highest point, ''Čierna hora'' (Black Mountain), 1,289 metres * Bachureň (SK) * Spiš-Šariš Intermontane (SK: ''Spišsko-šarišské medzihorie'') * Šariš Highlands (SK: ''Šarišská vrchovina'') * Orava Basin (SK: ''O ...
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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 ...
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Geography Of Slovakia
Slovakia is a landlocked Central European country with mountainous regions in the north and flat terrain in the south. During much of the Holocene, Slovakia was much more forested than today. Decline of the forest occurred in as consequence of the Valachian colonization and the development of mining in the territory. Statistics Land use: ''agricultural land'': 40.1% ''arable land'': 28.9%; permanent crops: 0.4%; permanent pasture: 10.8% ''forest'': 40.2% ''other'': 19.7% (2011 est.) Natural resources: Lignite, small amounts of iron ore, copper and manganese ore; salt; arable land Natural Hazards: Flooding Environment-international agreements: ''Party to'': Air Pollution, Air Pollution-Nitrogen Oxides, Air Pollution-Persistent Organic Pollutants, Air Pollution-Sulfur 85, Air Pollution-Sulfur 94, Air Pollution-Volatile Organic Compounds, Antarctic Treaty, Biodiversity, Climate Change, Climate Change-Kyoto Protocol, Desertification, Endangered Species, Environmental Mod ...
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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 ...
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