Lac De Sanetsch
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Lac De Sanetsch
__NOTOC__ Lac de Sanetsch (also ''Lac de Sénin'', German: ''Sanetsch See'') is a reservoir below Sanetsch Pass in Valais, Switzerland. Its surface area is . The Sanetsch dam was built in 1965. The gravity dam has a height of . See also *List of mountain lakes of Switzerland This is a list of high-altitude lakes in Switzerland. It includes all significant lakes, natural or artificial, with an area over 4 hectares and a height over 800 metres above sea level. This height approximately corresponds to the transiti ... External linksSwiss Dams: Sanetsch* Lakes of Valais Reservoirs in Switzerland {{Valais-lake-stub ...
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Gsteig
Gsteig bei Gstaad is a municipality in the Obersimmental-Saanen administrative district in the canton of Bern in Switzerland. Gsteig was formerly known by the French name of ''Châtelet''. History Gsteig is first mentioned in 1312 as ''Chastelet''. In 1453, it was mentioned as ''Steig''. The villages of Gsteig and Feutersoey grew up along the roads over the Col du Pillon and the Sanetsch Pass. During the Middle Ages, a castle was built in the valley to protect and control the passes. The castle is first mentioned in 1458 and today is in ruins. At one time there was a settlement at Ussers Gründ which was destroyed by a landslide. Originally Gsteig was part of the district and parish of Saanen. The village church of St. Theodul was consecrated in 1453. It became a filial church of Saanen in 1500. In the early 16th century, Bern adopted the new faith of the Protestant Reformation, however Gsteig did not convert until 1556. Traditionally the villagers practiced seaso ...
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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 cantons of Switzerland, 26 cantons forming the Switzerland, Swiss Confederation. It is composed of thirteen districts and its capital and largest city is Sion, Switzerland, 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 Switzerland, the country. It borders the cantons of Canton of Vaud, Vaud and Canton of Bern, Bern to the north, the cantons of Canton of Uri, 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 Alps, Alpine cantons, along with Ticino and the Grisons, which encompass a vast diversity of ecosystems. It is a bilingual canton, French language, French and German language, German ...
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Reservoir
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam A dam is a barrier that stops or restricts the flow of surface water or underground streams ...
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Sanetsch Pass
Sanetsch Pass (French: ''Col du Sanetsch'' or ''Col de Sénin'') (el. 2242 m) is a high mountain pass in Switzerland across the western Bernese Alps, connecting Gsteig in the canton of Berne and Sion in the canton of Valais. Although a road leads to the pass from Sion and goes further to the Lac de Sanetsch, it can not be completely traversed by car. In the summer season the pass is accessible by PostBus and can also be traversed by cable car. The highest point of the road is at 2,252 metres. The pass itself is located in Valais 4 km south of the border with Berne. It separates the massif of the Diablerets on the west from the massif of the Wildhorn on the east. The Sanetschhorn and the Arpelistock overlook the pass on the west and east side respectively. The Col du Sanetsch is a popular destination because of the view over the Pennine Alps and the nearby Tsanfleuron Glacier. See also * List of highest paved roads in Europe * List of mountain passes This is a list of moun ...
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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 = 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 ...
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Gravity Dam
A gravity dam is a dam constructed from concrete or stone masonry and designed to hold back water by using only the weight of the material and its resistance against the foundation to oppose the horizontal pressure of water pushing against it. Gravity dams are designed so that each section of the dam is stable and independent of any other dam section. Characteristics Gravity dams generally require stiff rock foundations of high bearing strength (slightly weathered to fresh), although in rare cases, they have been built on soil foundations. The bearing strength of the foundation limits the allowable position of the resultant force, influencing the overall stability. Also, the stiff nature of the gravity dam structure is unforgiving to differential foundation settlement, which can induce cracking of the dam structure. Gravity dams provide some advantages over embankment dams, the main advantage being that they can tolerate minor over-topping flows without damage, as the concre ...
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List Of Mountain Lakes Of Switzerland
This is a list of high-altitude lakes in Switzerland. It includes all significant lakes, natural or artificial, with an area over 4 hectares and a height over 800 metres above sea level. This height approximately corresponds to the transition between the foothill zone and the montane zone, in the Alps and in the Jura Mountains. Lakes can be found up to elevations of almost 3000 metres, where is the climatic snow line in the Alps. For each lake, the culminating point of the drainage basin is indicated, along with the river basin of which it is part. For a list of artificial lakes only, see List of dams and reservoirs in Switzerland. For a general list of lakes, see List of lakes of Switzerland. Distribution of mountain lakes by canton Main list See also * List of glaciers in Switzerland * List of mountains of Switzerland * List of lakes of Switzerland Notes and references External linksMountain lakes (MySwitzerland.com) {{Portal bar, Geography, Mountains, Switzerlan ...
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Lakes Of Valais
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ic ...
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