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Piz Buin
Piz Buin () is a mountain in the Silvretta range of the Alps on the border between Austria and Switzerland. It forms the border between the Swiss canton of Graubünden and the Austrian state of Vorarlberg and is the highest peak in Vorarlberg. Its original name in the Romansh language is ''Piz Buin Grond''. A similar but smaller summit nearby is called ''Piz Buin Pitschen'' at 3,255 m (10,680 ft). Piz Buin was first climbed on 14 July 1865 by Joseph Anton Specht and Johann Jakob Weilenmann, guided by Jakob Pfitscher and Franz Pöll. Piz Buin Pitschen was climbed three years later. Piz Buin can be reached from the Wiesbadener hut, crossing the Vermunt glacier, climbing up the Wiesbadener ridge and hiking over the Ochsentaler Glacier to the Buin gap. From the gap there is a zigzag walk to the top, with only a 20 m (65 ft) steep step to surmount before reaching the relatively flat summit space, which has an old wooden cross on the very top. The border between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piz Buin Pitschen
Piz Buin Pitschen ( Rumantsch) or Kleiner Piz Buin (German) is a peak in the Silvretta Alps. The Piz Buin Pitschen lies western of his higher neighbor the Piz Buin Grond or Großer Piz Buin. The summit forms the border between Switzerland and Austria and is the second highest peak in Vorarlberg, a state of Austria, and the sixth highest peak of the mountain range after the Piz Linard, the Fluchthorn, the Piz Buin Grond, the Verstanclahorn and the Piz Fliana. The first ascent was made 1868 by O.W. Stein and his guide Christian Jann. Geography The Piz Buin Pitschen lies on the main ridge of the Silvretta alps. It is separated from its more famous neighbour by the Buinlücke (Fourcla Buin), a 3,056 m high mountain pass between the two summits. Piz Buin Pitschen separates two glacial valleys, the Ochsenthaler Glacier on the north and La Cudera on the southwest of the mountain. While the Ochsenthaler Glacier forms the origin of the River Ill, which first fills the Silvretta R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swisstopo
Swisstopo is the official name for the Swiss Federal Office of Topography (in German language, German: ''Bundesamt für Landestopografie''; French language, French: ''Office fédéral de topographie''; Italian language, Italian: ''Ufficio federale di topografia''; Romansh language, Romansh: ''Uffizi federal da topografia''), Switzerland's national mapping agency. The current name was made official in 2002. It had been in use as the domain name for the institute's homepage, swisstopo.ch, since 1997. Maps The main class of products produced by Swisstopo are topographical maps on seven different Scale (map), scales. Swiss maps have been praised for their accuracy and quality. Regular maps * 1:25.000. This is the most detailed map, useful for many purposes. Those are popular with tourists, especially for famous areas like Zermatt and St. Moritz. These maps cost CHF 13.50 each (2004). 208 maps on this scale are published at regular intervals. The first map published on this scale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austria–Switzerland Border
The modern states of Austria and Switzerland share a border with a length of () in two parts, separated by , the longer stretch running across the and the shorter one following the to its mouth at |
Mountains Of Graubünden
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 an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Switzerland
This article contains a sortable table of many of the major mountains and hills of Switzerland. The table only includes those summits that have a topographic prominence of at least above other points, and ranks them by height and prominence. Therefore it only includes mountains that might generally be regarded as 'independent' and covers most of the country, even lower areas. For a fuller list of mountains, including subsidiary points, see List of mountains of Switzerland above 3000 m and List of mountains of Switzerland above 3600 m. For a list of just the most isolated mountains, see List of most isolated mountains of Switzerland. Along with the lakes, mountains constitute a major natural feature of Switzerland with most of the cantons having summits exceeding and three of them having summits exceeding . The two main mountain ranges are the Alps (south and east) and the Jura (north and west), separated by the Swiss Plateau which also includes a large number of hills. Topo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Vorarlberg
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] |
Alpine Three-thousanders
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Alps
This page tabulates only the most prominent mountains of the Alps, selected for having a topographic prominence of ''at least'' , and all of them exceeding in height. Although the list contains 537 summits, some significant alpine mountains are necessarily excluded for failing to meet the stringent prominence criterion. The list of these most prominent mountains is continued down to 2500 m elevation at List of prominent mountains of the Alps (2500–2999 m) and down to 2000 m elevation on List of prominent mountains of the Alps (2000–2499 m). All such mountains are located in either France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these three lists include all 44 ultra-prominent peaks of the Alps, with 19 ultras over 3000m on this page. For a definitive list of all 82 the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to as the 'Alpi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of Switzerland
This article contains a sortable table of many of the major mountains and hills of Switzerland. The table only includes those summits that have a topographic prominence of at least above other points, and ranks them by height and prominence. Therefore it only includes mountains that might generally be regarded as 'independent' and covers most of the country, even lower areas. For a fuller list of mountains, including subsidiary points, see List of mountains of Switzerland above 3000 m and List of mountains of Switzerland above 3600 m. For a list of just the most isolated mountains, see List of most isolated mountains of Switzerland. Along with the lakes, mountains constitute a major natural feature of Switzerland with most of the cantons having summits exceeding and three of them having summits exceeding . The two main mountain ranges are the Alps (south and east) and the Jura (north and west), separated by the Swiss Plateau which also includes a large number of hills. Topo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Romansh Language
Romansh (; sometimes also spelled Romansch and Rumantsch; Sursilvan: ; Vallader, Surmiran, and Rumantsch Grischun: ; Putèr: ; Sutsilvan: , , ; Jauer: ) is a Gallo-Romance language spoken predominantly in the Swiss canton of the Grisons (Graubünden). Romansh has been recognized as a national language of Switzerland since 1938, and as an official language in correspondence with Romansh-speaking citizens since 1996, along with German, French, and Italian. It also has official status in the canton of the Grisons alongside German and Italian and is used as the medium of instruction in schools in Romansh-speaking areas. It is sometimes grouped by linguists with Ladin and Friulian as the Rhaeto-Romance languages, though this is disputed. Romansh is one of the descendant languages of the spoken Latin language of the Roman Empire, which by the 5th century AD replaced the Celtic and Raetic languages previously spoken in the area. Romansh retains a small number of words fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cantons Of Switzerland
The 26 cantons of Switzerland (german: Kanton; french: canton ; it, cantone; Sursilvan and Surmiran: ; Vallader and Puter: ; Sutsilvan: ; Rumantsch Grischun: ) are the member states of the Swiss Confederation. The nucleus of the Swiss Confederacy in the form of the first three confederate allies used to be referred to as the . Two important periods in the development of the Old Swiss Confederacy are summarized by the terms ('Eight Cantons'; from 1353–1481) and ('Thirteen Cantons', from 1513–1798).rendered "the 'confederacy of eight'" and "the 'Thirteen-Canton Confederation'", respectively, in: Each canton of the Old Swiss Confederacy, formerly also ('lieu/locality', from before 1450), or ('estate', from ), was a fully sovereign state with its own border controls, army, and currency from at least the Treaty of Westphalia (1648) until the establishment of the Swiss federal state in 1848, with a brief period of centralised government during the Helvetic Republic ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
