Ricken Pass
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Ricken Pass
The Ricken Pass is a mountain pass in the canton of St. Gallen in eastern Switzerland. At a maximum altitude of , it connects the Linth valley and the Toggenburg. The pass is crossed by a road, which has a maximum gradient of 9%. The Ricken Tunnel The Ricken Tunnel (german: Rickentunnel) is an long rail tunnel under the Ricken Pass in eastern Switzerland. It is on the Swiss Federal Railway Uznach–Wattwil line, between Kaltbrunn station and Wattwil station. The tunnel, which accommoda ..., an long rail tunnel, runs under the pass. References Mountain passes of Switzerland Mountain passes of the canton of St. Gallen Toggenburg {{StGallen-geo-stub ...
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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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Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ...
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Canton Of St
Canton may refer to: Administrative division terminology * Canton (administrative division), territorial/administrative division in some countries, notably Switzerland * Township (Canada), known as ''canton'' in Canadian French Arts and entertainment * Canton (band), an Italian synth pop group * "Canton" (song) by Japan * Canton, a fictional town in " Jaynestown", an episode of ''Firefly'' Design * Canton (building), a corner pilaster * Canton (flag), an emblem placed in the top left quarter of a flag * Canton (heraldry), a square or other charge (symbol) occupying the upper left corner of a coat of arms * Canton porcelain, Chinese ceramic ware People * Canton (surname), and list of people with the surname * Canton Jones, American Christian music/hip-hop artist Places Canada * Canton, New Brunswick, a community in Drummond Parish, New Brunswick * Canton, Ontario China * Guangdong (Canton Province), province in southern China * Guangzhou (Canton City), capita ...
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Linth
The Linth (pronounced "lint") is a Swiss river that rises near the village of Linthal in the mountains of the canton of Glarus, and eventually flows into the Obersee section of Lake Zurich. It is about in length. The water power of the Linth was a main factor in the creation of the textile industry of the canton Glarus, and is today used to drive the Linth–Limmern power stations in its upper reaches. The river and its upper valley forms the boundary between the mountain ranges of the Glarus Alps, to its east and south, and the Schwyzer Alps, to its west. Course of the river The river rises to the south-west of the village of Linthal, at the foot the Tödi mountain (elevation ). It collects the water from several glaciers, including the Clariden Glacier and the Biferten Glacier, as well as various tributary streams, including the ''Oberstafelbach'', the ''Bifertenbach'', the ''Sandbach'', the ''Walenbach'' and the ''Limmerenbach''. The last of these is dammed to create t ...
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Toggenburg
Toggenburg is a region of Switzerland. It corresponds to the upper valley of the river Thur and that of its main tributary, the Necker. Since 1 January 2003, Toggenburg has been a constituency (''Wahlkreis'') of the canton of St. Gallen ( SFOS number 1727). Geography The valley descends in a northwestern direction from the watershed between the Rhine and the Thur, and is enclosed on the northeast by the chain of the Säntis () and on the southwest by that of the Churfirsten () and of the Speer (). It is a fertile valley of about in length from the source of the river to Wil. At Wildhaus, the highest village (), the house wherein Huldrych Zwingli, the Swiss Reformer, was born in 1484, is still shown. Other villages are Lichtensteig, Kirchberg and Wattwil. History There are traces of the paleolithic Mousterian Industry throughout the Appenzell Alps, in the Toggenburg notably in Wildenmannlisloch cave. The upper Thur valley was part of the province of Raetia in the Roman ...
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Ricken Tunnel
The Ricken Tunnel (german: Rickentunnel) is an long rail tunnel under the Ricken Pass in eastern Switzerland. It is on the Swiss Federal Railway Uznach–Wattwil line, between Kaltbrunn station and Wattwil station. The tunnel, which accommodates a single track through, is relatively straight and has a constant incline of 15.75 ‰ from Kaltbrunn to Wattwill. The Ricken Tunnel was constructed between 1904 and 1910, and was initially used by steam-hauled trains. Following a fatal incident on 4 October 1926 in which nine railway employees died as a result of carbon monoxide poisoning in the poorly ventilated tunnel, the line and tunnel were both electrified during 1927. The geology surrounding the tunnel is somewhat unfavourable, the rocks being prone to swelling and damaging the tunnel walls over time, necessitating repeated repairs and the occasional closure. During the 1990s, equipment for capturing geothermal energy was installed within the tunnel and has been used sinc ...
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Mountain Passes Of Switzerland
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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Mountain Passes Of The Canton Of St
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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