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Water Body Attractions In Canton of Glarus

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The canton of Glarus, also canton of Glaris is a canton in east central Switzerland. The capital is Glarus. The population speaks a variety of Alemannic German. The majority of the population identifies as Christian, about evenly split between the Protestant and Catholic denominations.
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Water Body Attractions In Canton of Glarus

  • 1. Klontalersee Glarus
    Klöntalersee is a natural lake in the canton of Glarus, Switzerland and covers the major part of the Klöntal valley floor. Since 1908, it has been used as a reservoir for electricity production. The dam's construction substantially increased the lake's volume. Klöntalersee is drained by the Löntsch, a left tributary of the Linth.
    From Wikipedia, the free encyclopedia.
  • 2. Lake Brienz Brienz
    Lake Brienz is a lake just north of the Alps, in the canton of Berne in Switzerland. It has a length of about 14 kilometres , a width of 2.8 kilometres and a maximum depth of 260 metres . Its area is 29.8 square kilometres , and the surface is 564 metres above the sea-level. It is fed, among others, by the upper reaches of the Aare at its eastern end, the Giessbach at its southern shore from steep, forested and rocky hills of the high Faulhorn and Schwarzhoren more than 2,000 metres above the lake, and by the Lütschine, flowing from the valleys of Grindelwald and Lauterbrunnen, at its south-western corner. It flows out into a further stretch of the Aare at its western end. The culminating point of the lake's drainage basin is the Finsteraarhorn at 4,274 metres above sea level.The village ...
    From Wikipedia, the free encyclopedia.
  • 3. Caumasee Flims
    Caumasee is a lake near Flims, in the Grisons, Switzerland. It is one of the lakes on the Flims Rockslide deposits. The lake is fed from underground sources. Its surface area is 10.3194 ha. The level of the lake varies by approximately 4 to 5 meters along with the varying underground water flow during the year, hence reaches its minimum by the end of April when snow melting in the mountains increases. A maximum level is reached by mid July but may be topped in August even after previous falling due to summer rain. The very western bay never freezes in winter, probably showing a maximum water flow in this area. When the lake is at a low level, with a small volume of water, it warms up sooner than most lakes in the region, so people can be seen starting to swim the lake in April while bigger...
    From Wikipedia, the free encyclopedia.

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