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Steinhüshorn
The Steinhüshorn (or ''Steinhaushorn'') is a mountain of the Urner Alps, overlooking Guttannen in the Bernese Oberland. It lies north of the Diechterhorn and west of the Trift Glacier The Trift Glacier (german: Triftgletscher) is a long glacier (2005) in the Urner Alps near Gadmen, in the extreme east of the canton Berne in Switzerland. Morphology In 1973 glacier was 5.75 km long, 3 km wide at the top and around 500 m w .... References External linksSteinhüshorn on Summitpost Mountains of the Alps Alpine three-thousanders [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Urner Alps
The Uri Alps (also known as ''Urner Alps'', german: Urner Alpen) are a mountain range in Central Switzerland and part of the Western Alps. They extend into the cantons of Obwalden, Valais, Bern, Uri and Nidwalden and are bordered by the Bernese Alps (Grimsel Pass) and the Emmental Alps to the west (the four lakes: Lungerersee, Sarnersee, Wichelsee, and Alpnachersee), the Schwyzer Alps to the north (Lake Lucerne), the Lepontine Alps to the south (the valley of Urseren with Andermatt) and the Glarus Alps to the east (Reuss). The Uri Alps are composed of two distinct groups separated by the Susten Pass. The Dammastock massif on the south is the most glaciated part while the northern part, which culminates on Titlis, has lower summits but greater extent. Geography The group south of the Susten Pass forms the dividing range between the head waters of the Aare (west) from those of the Reuss. In addition a small portion of the range (south-west) is located in the basin of the Rhone. Th ... [...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] |
Dammastock
The Dammastock (3,630 m) is the highest mountain in the Urner Alps in Switzerland and is part of the Winterberg massif. Its summit ridge forms the border between the cantons of Uri and the Valais. It is the highest summit in the canton of Uri. The tripoint between the cantons of Berne, Valais and Uri lies near the Eggstock, north of the Dammastock. Politically, the Dammastock is split between the municipalities of Göschenen (Uri) and Obergoms (Valais). The massif is almost completely covered by ice, the large Rhone Glacier on the west side, the smaller Damma Glacier on the east side and the Trift Glacier further on the north side. It was first climbed by Albert Hoffmann-Burkhardt with guides Johann Fischer and Andreas von Weissenfluh on 28 July 1864. Huts *Dammastock Hut (2,445 m) *Hotel Tiefenbach (2,109 m) See also * List of mountains of Uri *List of mountains of Switzerland *List of most isolated mountains of Switzerland A ''list'' is any set of items in a row. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canton Of Bern
The canton of Bern or Berne (german: Kanton Bern; rm, Chantun Berna; french: canton de Berne; it, Canton Berna) is one of the 26 cantons forming the Swiss Confederation. Its capital city, Bern, is also the ''de facto'' capital of Switzerland. The bear is the heraldic symbol of the canton, displayed on a red-yellow background. Comprising ten districts, Bern is the second-largest canton by both surface area and population. Located in west-central Switzerland, it is surrounded by eleven cantons. It borders the canton of Jura and the canton of Solothurn to the north. To the west lie the canton of Neuchâtel, the canton of Fribourg and canton of Vaud. To the south lies the canton of Valais. East of the canton of Bern lie the cantons of Uri, Nidwalden, Obwalden, Lucerne and Aargau. The geography of the canton includes a large share of all three natural regions of Switzerland: the Jura Mountains (the Bernese Jura), the Swiss Plateau (the Bernese Mittelland) and the Alps (th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Switzerland
). Swiss law does not designate a ''capital'' as such, but the federal parliament and government are installed in Bern, while other federal institutions, such as the federal courts, are in other cities (Bellinzona, Lausanne, Luzern, Neuchâtel, St. Gallen a.o.). , coordinates = , largest_city = Zürich , official_languages = , englishmotto = "One for all, all for one" , religion_year = 2020 , religion_ref = , religion = , demonym = , german: Schweizer/Schweizerin, french: Suisse/Suissesse, it, svizzero/svizzera or , rm, Svizzer/Svizra , government_type = Federalism, Federal assembly-independent Directorial system, directorial republic with elements of a direct democracy , leader_title1 = Federal Council (Switzerland), Federal Council , leader_name1 = , leader_title2 = , leader_name2 = Walter Thurnherr , legislature = Fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guttannen
Guttannen is a municipality in the Interlaken-Oberhasli administrative district in the canton of Bern in Switzerland. Origin of the name Guttannen is the name of a meadow, which became the name of the municipality. It comes from the phrase ''ze den guoten tannen'' (by the good firs). History Guttannen is first mentioned in 1377 as ''Guotentannon''. During the Middle Ages it was part of the Vogtei of Hasli and the parish of Meiringen. In 1334 the entire Vogtei was acquired by Bern. A chapel was built in the village in 1467 though it did not have a baptismal font. When the entire Canton accepted the new faith of the Protestant Reformation, the chapel was converted and remained under Meiringen. In 1713 it joined the parish of Innertkirchen where it remained until it became an independent parish in 1816. The old chapel was damaged in a fire in 1723 and replaced with a new chapel which became a parish church when Guttannen became a parish. Following the French invasion of S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bernese Oberland
The Bernese Oberland ( en, Bernese Highlands, german: Berner Oberland; gsw, Bärner Oberland; french: Oberland bernois), the highest and southernmost part of the canton of Bern, is one of the canton's five administrative regions (in which context it is referred to as ''Oberland'' without further specification). It constitutes the Alpine region of the canton and the northern side of the Bernese Alps, including many of its highest peaks, among which the Finsteraarhorn (), the highest in both range and canton. The region essentially coincides with the upper basin of the Aare, the latter notably comprehending Lake Thun and Lake Brienz, the two large lakes of the region. On the banks of the lakes or the Aare are the main settlements of Thun, Spiez, Interlaken, Brienz and Meiringen. The numerous side valleys of the Bernese Oberland include a large number of Alpine villages, many of them being tourist resorts and connected by mountain railways to Spiez and Interlaken. The Lötschbe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diechterhorn
The Diechterhorn is a mountain in the Urner Alps, overlooking the Haslital in the Bernese Oberland. At 3,389 metres above sea level it is the highest summit of the Urner Alps lying within the canton of Bern. On its east side lies the upper basin of the Trift Glacier, the summit of the Dammastock being located about five kilometres east. On its west side lies the Gelmersee Gelmersee (or Lake Gelmer) is a reservoir in Bernese Oberland, Switzerland. The hydroelectric reservoir was completed in 1932, at about the same time as the Grimselsee reservoir, and both are operated by Kraftwerke Oberhasli. The reservoir's vo ... at 1,849 metres. The Gelmer hut, lying at 2,412 metres above the Gelmersee, is the closest hut. It is a common base for climbers. References External linksDiechterhorn on Summitpost Mountains of the Alps Alpine three-thousanders Mountains of Switzerland Mountains of the canton of Bern {{Bern-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trift Glacier
The Trift Glacier (german: Triftgletscher) is a long glacier (2005) in the Urner Alps near Gadmen, in the extreme east of the canton Berne in Switzerland. Morphology In 1973 glacier was 5.75 km long, 3 km wide at the top and around 500 m wide at it tongue. Overall it covered an area of including glacier sides. Triftgletscher Gadmen, Schweizerisches Gletschermessnetz Since the end of the Little Ice Age, the Trift Glacier is shrinking. The valley in which lake ''Triftsee'' is today used to be filled by a large mass of ice well into the 20th century. In the 1990s small puddles of melt water began to form at the glacier tongue and gradually became larger. In the hot summer of 2003, the lake quickly grew and the glacier tongue sank into the melt water and dissolved in it, which led to a shrinkage of the glacier of more than 136 m within a year. Since 1861, the glacier has shrunk a total of 2771 meters. Tourist attractions At an altitude of 2520 meters above sea level is ... [...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] |
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] |
