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Petersgrat
The Petersgrat is a mountain of the Bernese Alps, located on the border between the Swiss cantons of Bern and Valais. It consists of a large ridge, which is entirely covered by ice. The northern side belongs to the basin of the large Kander Glacier. On the southern side (Lötschental The Lötschental is the largest valley on the northern side of the Rhône valley in the canton of Valais in Switzerland. It lies in the Bernese Alps, with the Lonza running down the length of the valley from its source within the Langgletsch ...) the glacier is smaller and is named ''Tellingletscher''. The Petersgrat is a popular destination for heliskiing and snow landing. References External links Petersgrat on Hikr Bernese Alps Mountains of the Alps Alpine three-thousanders Mountains of Switzerland Mountains of Valais Mountains of the canton of Bern Bern–Valais border {{bern-mountain-stub ...
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Bernese Alps
, topo_map= Swiss Federal Office of Topography swisstopo , photo=BerneseAlps.jpg , photo_caption=The Eiger, Mönch, and Jungfrau , country= Switzerland , subdivision1_type= Cantons , subdivision1= , parent= Western Alps , borders_on= , length_mi= , length_orientation= , width_mi= , width_orientation= , geology= , orogeny= , highest= Finsteraarhorn , elevation_m=4274 , range_coordinates= , coordinates= , map_image=Berner Alpen.png , map_caption=Map of Bernese Alps and their location in Switzerland (red) The Bernese Alps (german: Berner Alpen, french: Alpes bernoises, it, Alpi bernesi) are a mountain range of the Alps, located in western Switzerland. Although the name suggests that they are located in the Berner Oberland region of the canton of Bern, portions of the Bernese Alps are in the adjacent cantons of Valais, Fribourg and Vaud, the latter being usually named ''Fribourg Alps'' and ''Vaud Alps'' respectively. The highest mountain in the range, the ...
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Kander Glacier
The Kander Neve (german: Kanderfirn) is a long glacier (2005) of the Bernese Alps, situated south of Kandersteg in the canton of Berne. The glacier lies at the upper end of the Gasterental, at the foot of the Blüemlisalp and the Tschingelhorn. It borders the valley of Lauterbrunnen on the east ( Tschingel Pass) and the canton of Valais on the south (Petersgrat). In 1973 it had an area of . The glacier feeds the head waters of the Kander, a river that flows into Lake Thun, and hence into the Aare and the Rhine. See also *List of glaciers in Switzerland A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organizations * List College, an undergraduate division of the Jewish Theological Seminary of America * SC Germania List, German rugby unio ... * Swiss Alps External linksSwiss glacier monitoring network
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Lötschental
The Lötschental is the largest valley on the northern side of the Rhône valley in the canton of Valais in Switzerland. It lies in the Bernese Alps, with the Lonza running down the length of the valley from its source within the Langgletscher (lit.: Long Glacier). Geography The valley extends about from the Lötschenlücke (3178 m) at the top of the Langgletscher to the mouth of the valley at Steg/Gampel (630 m). It is surrounded by 3,000 meter high mountains, including the Bietschhorn (3,934 m), the Hockenhorn (3,293 m), the Wilerhorn (3,307 m) and the Petersgrat (3,205 m). The Jungfrau-Aletsch Protected Area is the most glaciated area in the Swiss Alps, and was declared a Natural World Heritage Site by decision of UNESCO on December 13, 2001, along with southern and eastern parts of the Lötschental. The main villages of the Lötschental are Wiler and Kippel, with 538 and 383 inhabitants respectively. Other villages in the valley include Ferden an ...
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Swisstopo
Swisstopo is the official name for the Swiss Federal Office of Topography (in German: ''Bundesamt für Landestopografie''; French: ''Office fédéral de topographie''; Italian: ''Ufficio federale di topografia''; 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 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 was ''1125 Chasseral'', in 1952. The last map published on this scale was ''12 ...
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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 ...
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Valais
Valais ( , , ; frp, Valês; german: Wallis ), more formally the Canton of Valais,; german: Kanton Wallis; in other official Swiss languages outside Valais: it, (Canton) Vallese ; rm, (Chantun) Vallais. is one of the 26 cantons forming the Swiss Confederation. It is composed of thirteen districts and its capital and largest city is Sion. The flag of the canton is made of thirteen stars representing the districts, on a white-red background. Valais is situated in the southwestern part of the country. It borders the cantons of Vaud and Bern to the north, the cantons of Uri and Ticino to the east, as well as Italy to the south and France to the west. It is one of the three large southern Alpine cantons, along with Ticino and the Grisons, which encompass a vast diversity of ecosystems. It is a bilingual canton, French and German being its two official languages. Traditionally, the canton is divided into Lower, Central, and Upper Valais, the latter region constituting the Germa ...
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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 = Federal assembly-independent directorial republic with elements of a direct democracy , leader_title1 = Federal Council , leader_name1 = , leader_title2 = , leader_name2 = Walter Thurnherr , legislature = Federal Assembly , upper_house = Council of ...
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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 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 ter ...
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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 'A ...
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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 ...
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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. ...
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Mountains Of Valais
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 terra ...
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