The Rhine Glacier was a glacier that existed during the last glacial period in what is now Switzerland. Its movement and retreat were responsible for carving out the basin that became Lake Constance. 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
Wikidata P31 formation-type mapped to formative process Glaciation via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Rhine Glacier
In Discipline
Wikidata P31 formation-type mapped to discipline Glaciology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Rhine Glacier
In the Other Atlases
Sources
Rhine Glacier (Wikipedia)
Lead sectionQuote, Lead section
The Rhine Glacier was a glacier during the last glacial period and was responsible for the formation of the Lake Constance.
View the Source Wikidata: Rhine Glacier
Wikidata Q454095, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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