Linth in the context of "Glärnisch"

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⭐ Core Definition: Linth

The Linth (pronounced [ˈlɪnt] "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 50 kilometres (31 mi) 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.

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👉 Linth in the context of Glärnisch

The Glärnisch is a mountain massif of the Schwyz Alps, overlooking the valley of the Linth in the canton of Glarus, Switzerland. It consists of several summits, of which the highest, the Bächistock, is 2,915 metres (9,564 ft) above sea level. Until 2013, the highest point was considered to be an unnamed point with a summit cross at 2,914 m (9,560 ft) (until 2013: 2,915 metres). The other main summits are the Vrenelisgärtli (lit.'Little Verena's Little Garden' at 2,904 m [9,528 ft]) and the Ruchen (2,901 m [9,518 ft]).

The massif of the Glärnisch consists of two ridges of either side of the firn named Glärnischfirn, culminating at the Ruchen to the west, rising more than 2,000 metres (6,600 ft) above the Klöntalersee, and at the Bächistock to the southwest. The Vrenelisgärtli is the closest peak to Schwanden. East of the Glärnisch is located the lower Vorder Glärnisch.

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Linth in the context of Glarus

Glarus (Swiss Standard German: [ˈɡlaːrʊs] ; Alemannic German: Glaris; French: Glaris [ɡlaʁis]; Italian: Glarona; Romansh: Glaruna) is the capital of the canton of Glarus in Switzerland. Since 1 January 2011, the municipality of Glarus incorporates the former municipalities of Ennenda, Netstal and Riedern.

Glarus lies on the river Linth between the foot of the Glärnisch (part of the Schwyzer Alps) to the west and the Schilt (Glarus Alps) to the east. Very few buildings built before the fire of 1861 remain. Wood, textile, and plastics, as well as printing, are the dominant industries. The symbol of the city is the neo-Romanesque city church.

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Linth in the context of Glarus Alps

The Glarus Alps (German: Glarner Alpen) are a mountain range in central Switzerland. They are bordered by the Uri Alps and the Schwyz Alps to the west, the Lepontine Alps to the south, the Appenzell Alps to the northeast. The eastern part of the Glarus Alps contains a major thrust fault that was declared a geologic UNESCO World Heritage Site (the Swiss Tectonic Arena Sardona).

The Glarus Alps extend well beyond the canton of Glarus, including parts of the cantons of Uri, Graubünden, and St Gallen. Conversely, not all the mountains in the canton of Glarus are part of the Glarus Alps, with those to the north of the Urner Boden and to the west of the valley of the river Linth considered to be part of the Schwyz Alps.

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Linth in the context of Limmat

The Limmat is a river in Switzerland. The river commences at the outfall of Lake Zurich, in the southern part of the city of Zurich. From Zurich it flows in a northwesterly direction, continuing a further 35 km until it reaches the river Aare. The confluence is located north of the small town of Brugg and shortly after the mouth of the Reuss.

The main towns along the Limmat Valley downstream of Zurich are Dietikon, Wettingen, and Baden. Its main tributaries are the Linth, Wägitaler Aa and Jona, all via Lake Zurich, the Sihl in Zurich, and the Reppisch in Dietikon.

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Linth in the context of Vorder Glärnisch

The Vorder Glärnisch (lit.'Anterior Glärnisch') is a mountain of the Schwyzer Alps, overlooking the valley of the Linth above the town of Glarus in the canton of Glarus, Switzerland. Its summit is at 2,327 metres (7,635 ft) above sea level.

It lies north-east of the higher Glärnisch (2,914 m [9,560 ft]). Unlike its higher neighbour, the Vorder Glärnisch can be ascended via a trail, which is on its north-west side.

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Linth in the context of Klöntalersee

Klöntalersee is a natural lake in the Klöntal valley in the canton of Glarus, Switzerland. It was formed by a rockslide and has served as a reservoir for hydroelectric power generation since 1908. The lake is impounded by the Rhodannenberg earthfill dam, which supplies water to a hydroelectric power station near Netstal.

Located at an elevation of 848 metres above sea level, the lake covers an area of approximately 3.3 square kilometres. It is considered the oldest major reservoir in Switzerland and is known for its frequently mirror-like surface that reflects the surrounding mountains. The primary inflow is the Klön stream, and the outflow is the Löntsch, which flows into the Linth near Netstal.

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Linth in the context of North-Eastern Swiss Alps

This article focuses on the part of the Alps and Pré-Alps that is located in North-Eastern Switzerland and compromises the Schwyzer Alps and the Appenzell Alps. This region is bordered by: Lake Lucerne in the south-west; the Klausen Pass, upper Linth valley and Lake Walen in the south; the Rhine valley in the east; Lake Constance in the north.

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Linth in the context of Siwellen

The Siwellen (2,307 m [7,569 ft]) is a mountain of the Glarus Alps, located east of the town of Glarus in the canton of Glarus. It lies on the range between the Linth valley and the Murgtal, north of the Gufelstock.

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