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Geological Formation

Bossons Glacier

Glaciers and Ice Formations

The Bossons Glacier is one of the larger glaciers of the Mont Blanc massif in the Alps, in the Chamonix valley of France Haute-Savoie department. Fed by icefields on the northern side of Mont Blanc, it descends close to the Aiguille du Midi and ends on the southern side of the Arve valley near the town of Chamonix. It has the largest altitudinal drop of any alpine glacier in Europe and once extended much further down the valley than it does today, now running about 7.5 kilometers long with a surface area of roughly 10 square kilometers. 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

Glaciation, Processes

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: Bossons 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: Bossons Glacier
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Bossons Glacier (Wikipedia)
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Quote, Lead section
The Bossons Glacier is one of the larger glaciers of the Mont Blanc massif of the Alps, found in the Chamonix valley of Haute-Savoie département, south-eastern France.
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Wikidata: Bossons Glacier
Wikidata Q549647, class allow-list match (w-wdresolver-0926)View the Source
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