Lac des Brenets
CharacteristicsThe depression in which the lake lies was formed by the movements of a glacier, while the lake itself was formed by a natural barrier around 12,000 years ago. At the downstream end is a waterfall known as the Saut du Doubs. A few hundred metres away, a bridge connects the French and Swiss sides of the lake. The lake was effectively dried out completely during the European drought of 2022, causing all ship operations to cease.[1] PhotographsSee alsoReferences
External linksWikimedia Commons has media related to Lac des Brenets.
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