뇌샤텔‬에서 가장 멋진 ‪11‬개의 폭포

Just a few hundred meters from the edge of the village is the entrance (or, coming from the other direction, the exit) of the Poëta Raisse Gorge. It can be visited and hiked free of charge. There are a few parking spaces, a large log cabin for picnics, and a signpost.

The Saut du Doubs is a 27-meter-high waterfall located along the Doubs River, which forms the border between France and Switzerland here. The waterfall is the result of a paleohistoric landslide that filled the narrow, gorge-like Doubs Valley, which cuts deep into the limestone formations of the Folded Jura, about 14,000 years ago.

Cool places

Follow the path of the Gorges de l'Areuse to discover this magnificent landscape carved by the waters that descend from the Jura. This part of the gorge is very narrow, animated by the narrow cliffs and numerous waterfalls.

An interesting hiking experience to have two viewpoints 5m away and not be able to cross. The view is actually better on the French side 😉 The "Saut du Doubs" is a 27-meter-high waterfall on the Doubs, which is located on the French-Swiss border. During periods of flooding on the Doubs, kayak records have been set here for overcoming the waterfall.

The Saut de Brot bridge is certainly one of the most beautiful places in the Areuse Gorge. The old stone bridge takes you to the other side of the Areuse and makes a fantastic photo opportunity.

The Vaux stream is nestled among the trees of the Bernese Jura forest, and flows between Lignières and La Neuveville. From the Combe du Pilouvi trail, the view of the falls is breathtaking. It is a natural site full of magic, where witches once came to bathe in the sparkling water of the pools.

The Areuse karst spring is a natural spring which emerges from limestone rocks and forms the Areuse river. You can start your hike from the village of Noiraigue and go up the river to the source, located at the foot of the Clusette cliffs. Along the way, you will enjoy views of gorges, bridges and waterfalls. The Areuse karst source is a good example of underground water circulation in a karst system.