The Glacier des Bossons is an expanse of ice that falls from the summit of Mont-Blanc, at an altitude of 4,810 metres, and ends at an altitude of 1,420 metres. It is 7.3 km long and features numerous seracs, while crevasses are visible in certain steep areas. The Glacier des Bossons is renowned for the cascades of ice that form in certain areas.
The Bossons glacier is thought to have appeared during the last ice age, around 11,700 BC. However, it was in 9,700 BC that this glacier separated from the other glaciers. Its maximum advance was recorded in 1818, when it reached an altitude of 1,100 metres. Since then, the Glacier des Bossons has continued to advance and retreat. Finally, in 2015, a major avalanche was recorded in this area, bringing down more than 200,000 cubic metres of ice, which was dragged for a kilometre.