Photos de cryo-carbonates découvert au front du glaciers de Bossons (Mont-Blanc, Alpes, France). Ces cryo-carbonates permettent d’enregistrer une phase de retrait glaciaire important su l’optimum climatique Holocène, il y a environs 6000 ans (voir notre article)
Si vous trouvez des structures similaires au front des glaciers merci de me contacter.

Global warming is currently responsible for a spectacular drop in glacier surface area in the Mont-Blanc massif. Yet researchers suspect that since the last ice age, there have been periods during which these areas may have been even smaller. They collected rock samples to assess and date these periods of glacier shrinkage.

