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Bossons Glacier

glacier in France

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionOct 9, 2025
Entity authorityQ549647 ↗
Source-derived summary

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. It is fed from icefields lying on the northern side of Mont Blanc, and descends close to the Aiguille du Midi and ends on the southern side of the Arve valley, close to the town of Chamonix.

It has the largest altitudinal drop of all the alpine glaciers in Europe, and formerly extended much further down the valley than it does today.

It is now approximately 7.5 km long, with a surface area of approximately 10 km2.

In the 17th century the Bossons glacier extended right down into Chamonix, reaching the settlement of Le Fouly, engulfing farmland, barns and houses. Local bishops were called upon to exorcise the demons within the glacier. In 1777 the traveller and correspondent, William Coxe, observed in his letters that "we mounted by the side of the glacier of Bosson, to les Murailles de Glace, so called from their resemblance to walls: they form the large ranges of ice of prodigious thickness and solidity, rising abruptly and parallel to each other. Some of these ranges appeared about a hundred feet high. Near them were pyramids and cone of ice of all forms and sizes, shooting to a very considerable height, in the most beautiful and fantastic shapes." He then noted that, on his return in 1785, "these murailles de glace no longer existed".

By around 1784 the glacier had started to retreat, although there was a renewed surge around 1815 and the frightened community erected a cross in front of its snout, which served as a marker for glacial retreat for the next 100 years.

Editorial summary

Begin with the source’s own compact description: “Bossons Glacier” is glacier in France. The dossier treats that line as a proposition to test through Bossons, Glacier and glacier, not as a finished interpretation.

Editorial reviewA concise reference frame for defining the subject, testing terminology and identifying the institution closest to the evidence. The current lead gives the account dated anchors—1777, 1785, 1784, 1815—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Bossons, Glacier and glacier is the immediate research focus.
Editorial analysis

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Vocabulary and entity names are the principal evidence signals here, because they determine the precision of every later search. The source revision retrieved here is dated Oct 9, 2025. The linked authority identifier is Q549647. VIAF identifies the subject as 235607714. The Library of Congress control number is sh2002008647. Authority coordinates are 45.883, 6.867. 2 of 3 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1777, 1785, 1784 and 1815.

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This entry incorporates text from “Bossons Glacier” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.