Cima Rossa
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Cima Rossa
Cima Rossa is a 3,161 metres high mountain in the Lepontine Alps, located on the border between the cantons of Ticino and Graubünden. On the west side it overlooks the valley of Malvaglia (Ticino) and on the east side it overlooks the valley of Calanca (Graubünden). Cima Rossa is connected to the higher massif of the Vogelberg by a four km ridge, not descending lower than 2,925 metres. A secondary summit (3,121 metres) named ''Piz Piotta'' lies north of the summit of Cima Rossa. A small glacier lies between them on the west flanks, named ''Ghiacciaio di Piotta''. References External linksCima Rossa on Hikr.org
Mountains of the Alps Alpine three-thousanders Mountains of Switzerland Mountains of Graubünden Mountains of Ticino Graubünden–Ticino border Lepontine Alps Mesocco Rossa, Switzerland {{Ticino-mountain-stub ...
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Lago Di Malvaglia
__NOTOC__ Bacino di Val Malvaglia (or Lago di Malvaglia) is a lake above Malvaglia in the canton of Ticino, Switzerland. The reservoir's surface area is 0.19 km2. Its arch dam was built in 1959 and is operated by Officine Idroelettriche di Blenio SA (Ofible). See also *List of mountain lakes of Switzerland External linksSwiss Dams: MalvagliaOfible: Bacini pericolosi
Lakes of Ticino Reservoirs in Switzerland Arch dams {{ticino-geo-stub ...
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Calanca
Calanca is a municipality in the Moesa Region in the Swiss canton of Graubünden. On 1 January 2015 the former municipalities of Arvigo, Braggio, Cauco and Selma merged to form the new municipality of Calanca.Amtliches Gemeindeverzeichnis der Schweiz
published by the Swiss Federal Statistical Office accessed 2 January 2013


History

Arvigo is first mentioned in 1453 as ''Arvicho''. Braggio is first mentioned in 1419 as ''Bragio''. It was part of the old municipality of Calanca until 1851 when it became an independent municipality. The church at Cauco is first mentioned in 1497. The village was part of the Squadra di Calanca until 1851 when it became an independent municipality ...
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Mountains Of Ticino
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 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 climate, mountains te ...
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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. T ...
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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 refers 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, Andes) it ...
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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'' , all 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 France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these 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 of the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to as the 'Alpine four-thousanders' ...
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Malvaglia
Malvaglia is a former municipality in the district of Blenio in the canton of Ticino in Switzerland. Since 15 March 2011, it is part of the municipality Serravalle. The reservoir Bacino di Val Malvaglia is located above the village of Malvaglia. History Malvaglia is first mentioned in 1205 as ''de Malvallia''. In German it used to be known as ''Manglia''. Malvaglia's development and history is closely tied to the development and history of the Blenio valley. In the settlement of Rongier, an ancient town on the Lukmanier road, a Roman coin hoard was found. The settlement is also home to the ''Casa Baggio''. ''Casa Baggio'' was built in the 16th century and expanded in the 17th. It was probably the ruling seat of the bailiff. The building is now listed as a historic building. Above the village is also the remains of ''Casa dei pagani'', a cave castle from the 11th-13th Centuries. The original, parish church was dedicated to St. Benedict and first mentioned in 1207. The c ...
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Swisstopo
Swisstopo is the official name for the Swiss Federal Office of Topography, Switzerland's national mapping agency. The current name was made official in 2002. It had been used as the domain name for the homepage of the instituteswisstopo.admin.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 was ''1125 Chasseral'', in 1952. The last map published on this scale was ''1292 Maggia'', in 1972. Since 1956, composites have been published, starting with ''2501 St. Gallen''. They have the same information, but consist of several parts of re ...
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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 above the surrounding land. A few mountains are inselberg, 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, ecosystems of mountains: different elevations hav ...
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Lepontine Alps
The Lepontine Alps (, , ) are a mountain range in the north-western part of the Alps. They are located in Switzerland (Valais, Ticino, Canton of Uri, Uri and Graubünden) and Italy (Piedmont and Lombardy). The Simplon Tunnel, Simplon rail tunnel (from Brig, Switzerland, Brig to Domodossola), the Gotthard Base Tunnel, Gotthard rail (from Erstfeld to Bodio) and Gotthard Road Tunnel, Gotthard road tunnels (from Andermatt to Airolo) and the San Bernardino (road tunnel), San Bernardino road tunnel are important transport arteries. The eastern portion of the Lepontine Alps, from the St Gotthard Pass to the Splügen Pass, is named the Adula Alps, while the western part is historically referred to as the Ticino Alps. Etymology The designation ''Lepontine Alps'', derived from the Latin name of the Valle Leventina, has long been somewhat vaguely applied to the Alpine ranges that enclose it, before being used for the whole range. Geography Following the line marking the division of the ...
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