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Geological Formation

Val d'Anniviers

Valleys

Val d'Anniviers is a Swiss Alpine valley in the district of Sierre in the canton of Valais, extending south from the Rhône Valley on the northern slopes of the Pennine Alps. It is a U-shaped valley, the classic form left by glacial erosion, running about 35 kilometers from Chippis at 550 meters elevation up toward the Weisshorn, which reaches 4,500 meters. The Navizence river drains the valley, which was historically made up of six municipalities, Ayer, Chandolin, Grimentz, Saint-Jean, Saint-Luc and Vissoie, before they merged into the single municipality of Anniviers in January 2009. The valley is subject to significant natural hazards, including seismic activity and avalanches. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Val d'Anniviers

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Val d'Anniviers
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Val d'Anniviers
Sources
Val d'Anniviers (Wikipedia)
Lead section
Quote, Lead section
The Val d'Anniviers (old name in German Eifischtal) is a Swiss Alpine valley, situated in the district of Sierre in Valais, which extends south of the Rhône Valley, on the northern slopes of the Pennine Alps.
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Wikidata: Val d'Anniviers
Wikidata Q672472, class allow-list match (w-wdresolver-0926)View the Source
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