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Valser Rhine: Difference between revisions






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Coordinates: 46°312.4N 9°220.1E / 46.517333°N 9.038917°E / 46.517333; 9.038917

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The Valser Rhine has many rapids and waterfalls and is very popular with canoeists.

The Valser Rhine has many rapids and waterfalls and is very popular with canoeists.



{{Equivalent|German|Valser Rhein}}

{{iw-ref|de|Valser Rhein}}



[[Category:Rivers of Europe]]

[[Category:Rivers of Europe]]


Revision as of 05:16, 23 September 2013

Valser Rhine
Physical characteristics
MouthConfluence with GlennerinSuraua 46°42′11N 9°10′51E / 46.70306°N 9.18083°E / 46.70306; 9.18083
Basin features
ProgressionGlennerAnterior RhineRhineNorth Sea
River systemRhine

The Valser Rhine is a source of the river Rhine in the Swiss canton of Graubünden. The river originates from the Länta glacier and the Grauhorn glacier at the northern foot of the Rheinwaldhorn and initially flows through the Länta valley before it flows into the Zervreilasee reservoir. Before the construction of the reservoir, the brooks Hornbach and Canalbach would flow into Valser Rhine from the right at the village of Zervreila. Today, the brooks flow into the reservoir, as does the Finsterbach, also from the right.

Below the Zervreila dam, the Valser Rhine flows through the Valser valley and the municipality of Vals. Before the village of Vals, the Peiler Bach joins the Valser Rhine, below the village, the Tomülbach from Tomül Pass joins from the right. The Valser Rhine the flows past St. Martin and joins the GlenneratSuraua. Several kilometers downstream, the Glenner flows into the Anterior Rhine.

The Valser Rhine has many rapids and waterfalls and is very popular with canoeists.

Template:Iw-ref


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    Categories: 
    Rivers of Europe
    Rivers of Switzerland
    Alpine Rhine basin
    Graubünden geography stubs
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    Short description is different from Wikidata
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    This page was last edited on 23 September 2013, at 05:16 (UTC).

    This version of the page has been revised. Besides normal editing, the reason for revision may have been that this version contains factual inaccuracies, vandalism, or material not compatible with the Creative Commons Attribution-ShareAlike License.



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