The waterfalls are formed by the Rickenbach, which plunges over a massive layer of Nagelfluh, a sedimentary rock composed of cemented pebbles.
The geological formation is part of the 'Allgäu Nagelfluh ridges,' shaped by ice-age glaciers that carved the current landscape.
The site includes a 'Geology Trail' that illustrates the transition from the Tertiary period to modern topography.
The water volume is subject to seasonal variation, often thinning during dry summer periods.
The Scheidegger Wasserfälle are a series of geological cascades formed by the Rickenbach river as it drops over a 20-meter limestone ledge. The site is noted for its accessible viewing platforms that offer perspective on the tiered waterfall structure. Visitors follow a descending path that leads into a narrow gorge area. The geology is characterized by layers of Nagelfluh rock, a conglomerate typical of the northern Alpine foothills. The area features a reptile zoo and a geological trail that explains the formation of the local landscape. The falls are situated within a managed park area that maintains safety railings along the cliff edges.
The main viewing platform at the base of the primary waterfall.
Wear footwear with strong grip as the paths and stairs can become slippery near the mist.
Bring a light waterproof jacket even in warm weather, as the waterfall basin is often cooler and damp.
Plan to explore the nearby nature trail to see the full extent of the riverbed geography.
Attempting to climb off the designated paths or over safety railings, as the limestone rocks can be unstable.
The park is seasonal, typically opening in spring and closing for the winter months due to ice hazards.
Sturdy, closed-toe walking shoes are required for safety; keep dogs on a leash at all times.
