The waterfall is fed by two main springs, the 'Fontaine de la Doue' and the 'Fontaine du Pissieu'.
The drop of the waterfall is recorded at exactly 60 meters in height.
The Gland stream eventually feeds into the nearby Rhône River.
The geological composition of the area is primarily limestone, which is prone to karstification.
Cascade de Glandieu is a 60-meter-tall waterfall located in the Bugey region of France. The waterfall is fed by the Gland stream, which originates from the limestone cliffs of the plateau. It drops in two distinct tiers into a pool before flowing toward the Rhône River. A concrete viewing platform at the base allows visitors to stand near the plunge zone. The site is situated within the commune of Brégnier-Cordon. The water volume fluctuates significantly based on seasonal rainfall and snowmelt. The location serves as a local geological landmark displaying the intersection of the stream and the surrounding rock formations.
The designated concrete viewing platform directly in front of the waterfall base provides the most stable and centered frame.
Wear footwear with good grip, as the area surrounding the viewing platform can be slippery due to constant mist.
Combine your visit with a trip to the nearby Maison d'Izieu, which is located in the same geographic sector.
Do not attempt to climb the rocks surrounding the waterfall, as they are unstable and moss-covered.
Stay behind the designated barriers on the viewing platform to avoid the splash zone and slippery rocks.
