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Geological Formation

Gastern Valley

Valleys

Gastern Valley (Gasterntal) is a valley near Kandersteg in the Bernese Oberland, Switzerland, with its rear basin at about 1,600 meters elevation and its exit at about 1,350 meters, drained by the Kander river. It is inhabited only during the summer months, though its rear section, called Selden, once supported year-round residents and offered two inns for travelers crossing the mountain passes; the Lötschberg Tunnel and Lötschberg Base Tunnel both run beneath the valley floor. 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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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: Gastern Valley

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: Gastern Valley
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Also in Geography Atlas: where this subject is found.

Source Wikidata: Gastern Valley
Sources
Gastern Valley (Wikipedia)
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Quote, Lead section
The Gastern Valley ('Gasterntal') is a valley near Kandersteg in the Bernese Oberland in Switzerland.
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Wikidata: Gastern Valley
Wikidata Q1495421, class allow-list match (w-wdresolver-0926)View the Source
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