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Równia Pod Śnieżką
The Równia pod Śnieżką (, , ; ) is a subalpine plateau in the Giant Mountains of Poland and the Czech Republic. The plateau is situated west from the peak of Sněžka, between the mountains of Smogornia and Sněžka at 1,390–1,446 m above sea level. Its area is approximately 9 km2, mostly covered in bogs, marshes and clumps of mountain pine. From both the Polish and Czech sides, the plateau is limited by glacial cirques. Tourism and hiking At the eastern side of the plateau there is an important junction for the main path Polish–Czech Friendship Trail. Four mountain hut A mountain hut is a building located at high elevation, in mountainous terrain, generally accessible only by foot, intended to provide food and shelter to mountaineering, mountaineers, climbing, climbers and Hiking, hikers. Mountain huts are us ...s in the proximity are ''Dom Śląski'', ''Samotnia'', ''Strzecha Akademicka'' in Poland and ''Luční Bouda'' in the Czech Republic. References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Giant Mountains
The Giant Mountains, Krkonoše, or Karkonosze (Czech: , , ), are a mountain range located in the north of the Czech Republic and the south-west of Poland, part of the Sudetes mountain system (part of the Bohemian Massif). The Czech–Polish border, which divides the historic regions of Bohemia and Silesia, runs along the main ridge. The highest peak, Sněžka (), is the Czech Republic's highest natural point with an elevation of . On both sides of the border, large areas of the mountains are designated national parks ( Krkonoše National Park in the Czech Republic and Karkonosze National Park in Poland), and these together comprise the Krkonoše/Karkonosze Transboundary Biosphere Reserve under the UNESCO Man and the Biosphere Programme. The source of the River Elbe is within the Giant Mountains. The range has a number of major ski resorts, and is a popular destination for tourists engaging in downhill and cross-country skiing, hiking, cycling and other activities. Names The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Ukraine to the east, Slovakia and the Czech Republic to the south, and Germany to the west. The territory has a varied landscape, diverse ecosystems, and a temperate climate. Poland is composed of Voivodeships of Poland, sixteen voivodeships and is the fifth most populous member state of the European Union (EU), with over 38 million people, and the List of European countries by area, fifth largest EU country by area, covering . The capital and List of cities and towns in Poland, largest city is Warsaw; other major cities include Kraków, Wrocław, Łódź, Poznań, and Gdańsk. Prehistory and protohistory of Poland, Prehistoric human activity on Polish soil dates to the Lower Paleolithic, with continuous settlement since the end of the Last Gla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Czech Republic
The Czech Republic, also known as Czechia, and historically known as Bohemia, is a landlocked country in Central Europe. The country is bordered by Austria to the south, Germany to the west, Poland to the northeast, and Slovakia to the southeast. The Czech Republic has a hilly landscape that covers an area of with a mostly temperate Humid continental climate, continental and oceanic climate. The capital and largest city is Prague; other major cities and urban areas include Brno, Ostrava, Plzeň and Liberec. The Duchy of Bohemia was founded in the late 9th century under Great Moravia. It was formally recognized as an Imperial Estate of the Holy Roman Empire in 1002 and became Kingdom of Bohemia, a kingdom in 1198. Following the Battle of Mohács in 1526, all of the Lands of the Bohemian Crown were gradually integrated into the Habsburg monarchy. Nearly a hundred years later, the Protestantism, Protestant Bohemian Revolt led to the Thirty Years' War. After the Battle of White ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subalpine
Montane ecosystems are found on the slopes of mountains. The alpine climate in these regions strongly affects the ecosystem because temperatures fall as elevation increases, causing the ecosystem to stratify. This stratification is a crucial factor in shaping plant community, biodiversity, metabolic processes and ecosystem dynamics for montane ecosystems. Dense montane forests are common at moderate elevations, due to moderate temperatures and high rainfall. At higher elevations, the climate is harsher, with lower temperatures and higher winds, preventing the growth of trees and causing the plant community to transition to montane grasslands and shrublands or alpine tundra. Due to the unique climate conditions of montane ecosystems, they contain increased numbers of endemic species. Montane ecosystems also exhibit variation in ecosystem services, which include carbon storage and water supply. Life zones As elevation increases, the climate becomes cooler, due to a decrease ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sněžka
Sněžka () or Śnieżka (, ) is a mountain on the border between the Czech Republic and Poland, the most prominent point of the Silesian Ridge in the Giant Mountains. At , its summit is the highest point in the Czech Republic, in the Lower Silesian Voivodeship, in the Giant Mountains and in the entire Sudetes. History Sněžka was one of the first European mountains visited by many tourists. This was mainly due to the relatively minor technical difficulties of the ascent and the fact that since the sixteenth century, many resort visitors flocked to the nearby Cieplice Śląskie-Zdrój, Bad Warmbrunn (today: Cieplice Śląskie-Zdrój) and the highly visible Sněžka, visually dominant over all Giant Mountains was for them an important attraction. The first historical account of an ascent to the peak is in 1456, by an unknown Republic of Venice, Venetian merchant searching for precious stones. The first settlements on the mountain soon appeared, being primarily mining communiti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Smogornia
Smogornia (, , , ) is a peak in the Giant Mountains, on the Czech-Polish border. It is situated in the eastern part of the main range. The peak is not accessible; the Main Sudetes Trail and Polish–Czech Friendship Trail traverse the mountain c. 300 m north from the peak. On the northern slope of the mountain there is a glacial cirque. The mountain has mild slopes and is mostly deforested, covered in mountain pine ''Pinus mugo'', known as dwarf mountain pine, mountain pine, scrub mountain pine, Swiss mountain pine, bog pine, creeping pine, or mugo pine, is a species of conifer, native to high elevation habitats from southwestern to Central Europe and So .... References {{Authority control Mountains of Poland Mountains and hills of the Czech Republic Czech Republic–Poland border International mountains of Europe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsh
In ecology, a marsh is a wetland that is dominated by herbaceous plants rather than by woody plants.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p More in general, the word can be used for any low-lying and seasonally waterlogged terrain. In Europe and in agricultural literature low-lying meadows that require draining and embanked polderlands are also referred to as marshes or marshland. Marshes can often be found at the edges of lakes and streams, where they form a transition between the aquatic and terrestrial ecosystems. They are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs, and the marsh is sometimes called a carr. This form of vegetation is what differentiates marshes from other types of wetland such as swamps, which are dominated by trees, and mires, which are wetlands that have accumulated deposits of acidic peat. Marshes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pinus Mugo
''Pinus mugo'', known as dwarf mountain pine, mountain pine, scrub mountain pine, Swiss mountain pine, bog pine, creeping pine, or mugo pine, is a species of conifer, native to high elevation habitats from southwestern to Central Europe and Southeast Europe. Description The tree has dark green leaves ("needles") in pairs, long. The cones are nut-brown, long. Custura Bucurei.jpg, ''Pinus mugo'' subsp. ''mugo'', Romania Pinus mugo uncinata trees.jpg, ''Pinus mugo'' subsp. ''uncinata'' Swiss National Park 007.JPG, ''Pinus mugo'' subsp. ''rotundata'', Swiss National Park Бор кривул 01.JPG, On Jakupica mountain, Republic of North Macedonia Taxonomy There are three subspecies: * ''Pinus mugo'' subsp. ''mugo'' — in the east and south of the range (southern & eastern Alps, Balkan Peninsula), a low, shrubby, often multi-stemmed plant to tall with matt-textured symmetrical cones, which are thin-scaled. * ''Pinus mugo'' subsp. ''uncinata'' — in the west and north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ) is an amphitheatre-like valley formed by Glacier#Erosion, glacial erosion. Alternative names for this landform are corrie (from , meaning a pot or cauldron) and ; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepening, overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (lake), tarn (small lake) behind a d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polish–Czech Friendship Trail
The Polish–Czech Friendship Trail (, ) is a public walking path in the Giant Mountains. The path runs on both sides of the Czech–Polish border, along the main ridge and crosses or traverses all its summits. The maintenance of the trail is performed by the staff of both adjacent national parks: the Polish Karkonosze National Park and the Czech Krkonoše National Park. The start point is located on Szrenica and the end in the Okraj pass / Pomezní boudy; the length of the trail is approx. 30 km; the level of difficulty is moderate. The trail partially overlaps with ski trails. The trail is marked with red stripe signs. Many places at the trail are equipped with two signposts parallelly: with Polish one in Polish language according to Polish standards, with distances in hours, and with Czech one in Czech language according to Czech standards, with distances in kilometers. History Background Until the Middle Ages, the peak area of Karkonosze remained untouched; the firs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Hut
A mountain hut is a building located at high elevation, in mountainous terrain, generally accessible only by foot, intended to provide food and shelter to mountaineering, mountaineers, climbing, climbers and Hiking, hikers. Mountain huts are usually operated by an Alpine Club or some organization dedicated to hiking or mountain recreation. They are known by many names, including alpine hut, mountain shelter, mountain refuge, mountain lodge, and mountain hostel. It may also be called a refuge hut, although these occur in lowland areas (e.g. lowland forests) too. Mountain huts can provide a range of services, starting with shelter and simple sleeping berths. Some, particularly in remote areas, are not staffed, but others have staff which prepare meals and drinks and can provide other services, including providing lectures and selling clothing and small items. Permanent staffing is not possible above the highest permanent human settlements, which are 5500m at the latitude of Everes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateaus Of Europe
In geology and physical geography, a plateau (; ; : plateaus or plateaux), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wider ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, plate tectonics movements, and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. They may be formed by upwelling of volcanic magma or extrusion of lava. The underlining mechanism in forming plateaus from up ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
