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Gorge du Cé
At the end of the last ice age, the glacier from the Combe de Biolland flowed straight to Mont-Saxonnex, where the river split into two torrents. One being more important than the other, the western torrent cut the rock deeper than the eastern torrent (Gorge du Cé). The latter was naturally neglected over the years. Today, the Bronze crosses the village to finish its course on the left bank of the Arve, in Bonneville.
