Concept

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 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. 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 the Limmerensee, a part of the Linth–Limmern hydro-electric scheme. The river then flows north to the village of Linthal, the highest significant settlement on the river, and onwards through the canton of Glarus villages of Rüti, Betschwanden, Diesbach, Hätzingen, Luchsingen, Leuggelbach, Haslen, Nidfurn and Schwanden. In Schwanden, the Linth is joined by one of its principal tributaries, the Sernf, which drains the south-eastern part of the canton of Glarus. From Schwanden, the river continues to flow north through the villages of Mitlödi and Ennenda and the town of Glarus before reaching the village of Netstal. In Netstal, the Linth is joined by the Löntsch, which drains the Klöntalersee. The Linth then flows between the villages Näfels and Mollis, from where it formerly flowed in a northerly direction to a confluence with its tributary outfall from Lake Walen (Walensee) on the Linth Plain, and then across that plain in a westerly direction to its mouth at the head of the Obersee section of Lake Zurich. As a result of the river regulation works (see below), the river is today diverted down an artificial channel in an easterly direction into Lake Walen.

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