Kasprowy Wierch
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Kasprowy Wierch
Kasprowy Wierch (; Slovak; ''Kasprov vrch''; sometimes in ''Kasper Peak'') is a peak of a long crest (ridgeline) in the Western Tatras one of Poland's main winter ski areas. Its dominant southern crests, WSW and ESE, mark the border with Slovakia. It is accessible in most conditions by foot and daily by cablecar. History From 1910 onwards Kasprowy Wierch became very popular among ski tourists so much so an aerial tramway or téléphérique, reaching almost to the summit, was built between 1935 and 1936 as such it is one of the oldest in Europe. As part of its modernization, the cabin aerial ropeway was closed for a period until December 2007. In 1938 meteorological and astronomical observatories were built here. One of the faint Kordylewski clouds, at or circling the L4 and L5 Lagrange points of the moon, was first photographed here by Kazimierz Kordylewski in 1961. Geography The mountain is at the crossroads of four crests, two of which coincide with footpaths, incorporatin ...
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Giewont
The Giewont () is a mountain massif in the Tatra Mountains of Poland. Its highest peak, Great Giewont (''Wielki Giewont''), is 1,895 metres (6,217 ft) above sea level and the highest peak of the Western Tatras ( Polish: ''Tatry Zachodnie'') located entirely within Poland's borders. The mountain is regarded as the symbol of Zakopane, the Polish Tatras and Podhale, which throughout history has been the subject of many legends, poems and works of art. Geography Giewont lies in the area of the Polish Tatra National Park (''Tatrzański Park Narodowy''). It encompasses three peaks: Small Giewont ( Polish: ''Mały Giewont'', 1,728 m), Great Giewont (''Wielki Giewont'', 1,895 m) and Long Giewont (''Długi Giewont'', 1,867 m). There is a mountain pass located between Great and Long Giewont, known as Szczerba (1,823 m). It is located between the valleys (''doliny'') of Kondratowa, Małej Łąki and Strążyska. The 600-meter high northern face of Great Giewont is clearly visible from t ...
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Kazimierz Kordylewski
Kazimierz Kordylewski (born 11 October 1903 in Poznań – 11 March 1981 in Kraków, Poland) was a Polish astronomer. In 1956, he claimed the discovery of the Kordylewski clouds, large transient concentrations of dust at the Trojan points of the Earth–Moon system, which were reported to have been confirmed to exist in October 2018. He studied at University of Poznań A university () is an institution of higher (or tertiary) education and research which awards academic degrees in several academic disciplines. Universities typically offer both undergraduate and postgraduate programs. In the United States, th ... and Jagiellonian University, and earned a PhD degree in 1932. References External links A page about Kazimierz KordylewskiArchived
on 26 January 2005.
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Poland–Slovakia Border
The Poland–Slovakia border is the international border between Poland and Slovakia and has formally existed since 1 January 1993, following the dissolution of Czechoslovakia into two independent states. Before the dissolution of Czechoslovakia, its eastern border with Poland was practically identical to the present day border between Poland and Slovakia, with minor corrections made in later years. The length of the Poland–Slovakia border is Course of the border The border with Slovakia runs from Jaworzynka Trzycatek through the Zwardońska Pass, Wielka Racza, Wielki Rycea, the Glinka Pass, Pilsko, Babia Góra, Chyżne, crosses the Orava valley, the main ridge of the Tatra Mountains, runs along the Białka valley, along the Dunajec valley, through the Pieniny, the Poprad valley, through Muszyna, the Tylicka Pass, the Dukla Pass and the Łupków Pass, to the Uzhok pass. History When the Slovak Republic was established on March 14, 1939, under the auspices of Nazi ...
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Mountains 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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Mountains Of Poland
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 ...
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Weather Station
A weather station is a facility, either on land or sea, with instruments and equipment for measuring atmospheric conditions to provide information for weather forecasts and to study the weather and climate. The measurements taken include temperature, atmospheric pressure, humidity, wind speed, wind direction, and precipitation amounts. Wind measurements are taken with as few other obstructions as possible, while temperature and humidity measurements are kept free from direct solar radiation, or insolation. Manual observations are taken at least once daily, while automated measurements are taken at least once an hour. Weather conditions out at sea are taken by ships and buoys, which measure slightly different meteorological quantities such as sea surface temperature (SST), wave height, and wave period. Drifting weather buoys outnumber their moored versions by a significant amount. Weather instruments Typical weather stations have the following instruments: * Thermometer for ...
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Chairlift
An elevated passenger ropeway, or chairlift, is a type of aerial lift, which consists of a continuously circulating steel wire rope loop strung between two end terminals and usually over intermediate towers, carrying a series of chairs. They are the primary onhill transport at most ski areas (in such cases referred to as 'ski lifts'), but are also found at amusement parks, various tourist attractions, and increasingly in urban transport. Depending on carrier size and loading efficiency, a passenger ropeway can move up to 4000 people per hour, and the fastest lifts achieve operating speeds of up to or . The two-person double chair, which for many years was the workhorse of the ski industry, can move roughly 1200 people per hour at rope speeds of up to . The four person detachable chairlift ("high-speed quad") can transport 2400 people per hour with an average rope speed of . Some bi and tri cable elevated ropeways and reversible tramways achieve much greater operating speeds ...
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Alps
The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Switzerland, Italy, Liechtenstein, Austria, Germany, and Slovenia. The Alpine arch generally extends from Nice on the western Mediterranean to Trieste on the Adriatic and Vienna at the beginning of the Pannonian Basin. The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided. Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Mont Blanc and the Matterhorn. Mont Blanc spans the French–Italian border, and at is the highest mountain in the Alps. The Alpine region area contains 128 peaks higher than . The altitude and size of the range affect the climate in Europe; in the mountains, precipitation ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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Tundra
In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless mountain tract". There are three regions and associated types of tundra: Arctic tundra, alpine tundra, and Antarctic tundra. Tundra vegetation is composed of dwarf shrubs, sedges, grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone (or ecological boundary region) between the tundra and the forest is known as the tree line or timberline. The tundra soil is rich in nitrogen and phosphorus. The soil also contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide in the permafrost, making the tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained g ...
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Austria-Hungary
Austria-Hungary, often referred to as the Austro-Hungarian Empire,, the Dual Monarchy, or Austria, was a constitutional monarchy and great power in Central Europe between 1867 and 1918. It was formed with the Austro-Hungarian Compromise of 1867 in the aftermath of the Austro-Prussian War and was dissolved shortly after its defeat in the First World War. Austria-Hungary was ruled by the House of Habsburg and constituted the last phase in the constitutional evolution of the Habsburg monarchy. It was a multinational state and one of Europe's major powers at the time. Austria-Hungary was geographically the second-largest country in Europe after the Russian Empire, at and the third-most populous (after Russia and the German Empire). The Empire built up the fourth-largest machine building industry in the world, after the United States, Germany and the United Kingdom. Austria-Hungary also became the world's third-largest manufacturer and exporter of electric home appliances, ...
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Schengen Area
The Schengen Area ( , ) is an area comprising 27 European countries that have officially abolished all passport and all other types of border control at their mutual borders. Being an element within the wider area of freedom, security and justice policy of the EU, it mostly functions as a single jurisdiction under visa policies in the European Union, a common visa policy for international travel purposes. The area is named after the 1985 Schengen Agreement and the 1990 Schengen Convention, both signed in Schengen, Luxembourg. Of the 27 EU member states of the European Union, member states, 23 participate in the Schengen Area. Of the five EU members that are not part of the Schengen Area, three—Bulgaria and the European Union, Bulgaria, Cyprus and the European Union, Cyprus and Romania and the European Union, Romania—are legally obligated to join the area in the future; Croatia has been approved to join on January 1, 2023; Ireland and the European Union, Ireland maintains ...
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