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Ruchi, Glarus Alps
The Ruchi is a mountain in the Glarus Alps, located at an elevation of on the border between the Swiss cantons of Glarus and Graubünden. It overlooks the Muttsee () on its west side from where a trail leads to the summit. On its south-east side lies a small glacier, the ''Glatscher da Gavirolas''. The Ruchi is connected to the higher summit of the Hausstock on the north-east by a long ridge. The nearest settlements are the villages of Linthal to the north, and Andiast to the south. Administratively, the mountain lies in the municipalities of Glarus Süd and Waltensburg/Vuorz Waltensburg/Vuorz is a former municipality in the Surselva Region in the canton of Graubünden in Switzerland. On 1 January 2018 the former municipalities of Andiast and Waltensburg/Vuorz merged into the municipality of Breil/Brigels. History .... References External links *Ruchi on Hikr
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Muttsee
Muttsee is a reservoir in the Canton of Glarus, Switzerland. Its surface area is . It is used as the upper reservoir in the 1 GW pumped-storage hydroelectricity Linth–Limmern Power Stations. The 2.4 km high altitude permits a 2.2 MW Solar power in Switzerland, solar farm to supply 3.3 GWh per year, more than average power, even in winter (as the high altitude prevents fog formation, and as the snow reflects the sunlight onto the solar panels). The 6,000 photovoltaic panels were installed on the containment wall of the artificial basin in 2021, covering approximately 10,000 square meters of concrete, and stretching over almost 1 km. See also *List of lakes of Switzerland *List of mountain lakes of Switzerland References

Reservoirs in Switzerland Lakes of the canton of Glarus Linth/Limmat basin, LMuttsee {{Glarus-geo-stub ...
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Glarus Süd
Glarus Süd is a municipality in the Swiss canton of Glarus. It comprises the upper Linth valley, and the entire Sernf valley, and includes the villages of Betschwanden, Braunwald, Diesbach, Elm, Engi, Haslen, Hätzingen, Leuggelbach, Linthal, Luchsingen, Matt, Mitlödi, Nidfurn, Rüti, Schwanden, Schwändi and Sool. Glarus Süd is one of three municipalities of the canton of Glarus, the others being Glarus and Glarus Nord. History The municipality of Glarus Süd was created on 1 January 2011, incorporating the former municipalities of Betschwanden, Braunwald, Elm, Engi, Haslen, Linthal, Luchsingen, Matt, Mitlödi, Rüti, Schwanden, Schwändi and Sool. At the time of its creation, Glarus Süd was the largest Swiss municipality by area. As of 1 January 2015, it was overtaken in size by the expanded municipality of Scuol in the canton of Graubünden. Geography Glarus Süd incorporates all of the valley of the Linth river from Mitlödi, just upstream of the tow ...
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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 ...
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Mountains Of The Canton Of Glarus
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 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 ...
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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 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 ...
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Waltensburg/Vuorz
Waltensburg/Vuorz is a former municipality in the Surselva Region in the canton of Graubünden in Switzerland. On 1 January 2018 the former municipalities of Andiast and Waltensburg/Vuorz merged into the municipality of Breil/Brigels. History Waltensburg/Vuorz was first mentioned in 765 as ''Vorce''. The German name of Waltensburg is first mentioned in 1209 as ''Waltramsburg'', which was an older name of the castle ''Jörgenberg''. While the Romansh speaking population used the older, Romansh name of Vorce (meaning: "a river fork") the former name of the castle moved to include the village. At about the same time, the castle came to be known as Jörgenberg from the name of the nearby early medieval fortified Church of St George. In the Middle Ages, the nearby settlements on Ladral () and Jörgenberg belonged to Waltensburg. In the area surrounding Waltensburg/Vuorz there are three other medieval fortresses, Grünenfels ( rm, Chischlatsch), home of the Freiherren of Grünen ...
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Andiast
Andiast () is a former municipality in the Surselva Region in the Swiss canton of Graubünden. Until 1943, it was known as Andest.Amtliches Gemeindeverzeichnis der Schweiz
published by the Swiss Federal Statistical Office accessed 23 September 2009
Lying close to the ski resorts of and , Andiast is known for its winter sports. On 1 January 2018 the former municipalities of Andiast and

Hausstock
The Hausstock is a mountain in the Glarus Alps, at an elevation of on the border between the cantons of Glarus and Graubünden. It overlooks the valleys of Linth and Sernf rivers in Glarus, and the valley of the Vorderrhein river in Graubünden. The Hausstock was the site of the 1799 withdrawal of the Russian army under General Alexander Suvorov. A well-known destination already in the nineteenth century with British and American climbers, the mountain remains popular with mountain climbers and skiers. Geography and geology The Hausstock overlooks the valleys of Linth and Sernf rivers in Glarus, and valley of the Vorderrhein river in Graubünden. The nearest settlements are the villages of Linthal (in the Linth valley), Elm (in the Sernf valley) and Pigniu (on the slopes of the Vorderrhein valley). Administratively, the mountain lies in the municipalities of Glarus Süd, Ilanz/Glion and Andiast. The Richetli Pass to the north of the mountain connects the villages of Elm and L ...
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Linthal, Glarus
Linthal is a village, and former municipality, in the municipality of Glarus Süd and canton of Glarus in Switzerland. The village lies near the head of the valley of the Linth river, and at the foot of the Klausen Pass into the canton of Uri. It is the terminus of the railway line that traverses the length of Glarus. History Linthal is first mentioned in 1289 as ''Lintal''. In 1879, Linthal was connected to the Swiss railway network by the opening of the Swiss Northeastern Railway line from Weesen. The road over the Klausen Pass was built between 1895 and 1900. Construction of the Linth–Limmern hydro-electric power scheme, in the mountains above Linthal, commenced in 1957, and was fully operational by 1968. In 2011, the municipality of Linthal was merged into the new municipality of Glarus Süd. Geography The village Linthal lies at the head of the valley of the Linth river, at an altitude of approximately . It is surrounded by mountains, including Ortstock (), Clariden ...
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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 (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 ...
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