The "Mer de Glace" has had this name since the 18th century, due to the numerous crevasses that look like frozen breakers. Arriving from the Col du Midi, this glacier descends towards the valley and meets the Glacier du Géant before merging further down into the Glacier du Tacul. Its main basin, upstream, is known as the Vallée Blanche. Its distinctive appearance is due to the small waves that are visible to the naked eye, iridescent with darker hues. The Mer de Glace gives the impression of being zebra-striped, alternating between white and darker bands, known as the Forbes stripes.
It is thought to have originated during the last ice age, when the ice cap covering the Alps melted. The Mer de Glace is therefore thought to have originated around 11,700 BC.