Cascade du Pain de sucre

The Pain de Sucre waterfall drops roughly 35 meters and flows over a crescent-shaped limestone formation. The water from the Bèze River collects in a deep circular basin at the bottom.

The limestone formation beneath the waterfall formed over millions of years through mineral deposits from flowing water. Continuous water flow shaped the distinctive form visible today.

The name refers to the shape of the limestone deposits that resemble a sugarloaf. Visitors can observe this natural formation up close when standing at the base of the falls.

A stairway path leads to the waterfall with parking available about 200 meters from the intersection area. The route is relatively short and easy to follow if you head toward Songieu or Brénaz.

The water flows over a crescent-shaped structure before collecting in a perfectly round, deep blue basin. This unusual geometry formed naturally through the way water eroded the limestone layers over long periods.

Location: Champagne-en-Valromey

GPS coordinates: 45.93900,5.71387

Latest update: December 14, 2025 09:45