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Geological Formation

Val Calanca

Valleys

The Val Calanca is a valley of the Swiss Alps in the Lepontine Alps. It is drained by the Calancasca, a tributary of the Moesa that it joins at Roveredo, and it is bordered by the Puntone dei Fracion and the Zapporthorn, the highest mountains in the surrounding area. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

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 Calanca

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 Calanca
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Val Calanca
Sources
Val Calanca (Wikipedia)
Lead section
Quote, Lead section
The Val Calanca is a valley of the Swiss Alps, located in the Lepontine Alps.
View the Source
Wikidata: Val Calanca
Wikidata Q672814, class allow-list match (w-wdresolver-0926)View the Source
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