
Ruinaulta
Interesting facts
- In 2024 researchers dated an oak drowned by the newly dammed lake to 7469 BC, give or take two years, the most precise date yet for the rockslide.
- The rockslide moved roughly as much rock as there is water in Lake Lucerne, about 300 times the volume of the historic Swiss landslide at Goldau.
- One estimate puts the energy released by the collapse at about 45 megatons of TNT, comparable to a magnitude 8.3 earthquake.
- The debris dammed the Vorderrhein and created Lake Ilanz, which persisted at around 820โ840 metres above sea level for at least a thousand years.
- Even today the Rhine still flows on landslide rubble and has not yet cut back down to the valley floor that existed before the collapse.
- The forest that took over the barren debris gave the upper valley its name: Surselva means "above the forest" in Romansh.
- More than 350 butterfly species have been recorded in the gorge, and peregrine falcons breed on its crumbling cliffs.
- The Il Spir viewing platform near Conn is shaped like a common swift, cantilevered out over the edge of the gorge.
- Swiss federal judges blocked a continuous riverside trail to protect floodplain where common sandpipers nest; seven viewing platforms line the rims instead.
- The Glacier Express runs through the gorge, and the bridge at Valendas-Sagogn is the only road crossing of the Rhine between Ilanz and Reichenau.
Why it is worth it
Ruinaulta, the Rhine Gorge, is the canyon the Vorderrhein has cut through the debris of the Flims rockslide, one of the greatest landslides known in the Alps. Almost 10,000 years ago the mountainside above today's Flims gave way, and more than ten billion cubic metres of rock came down and buried the valley of the young Rhine. The river then slowly sawed its way through the rubble, and the result is a gorge about 13 km long and up to 400 m deep between Ilanz and Reichenau, whose pale walls look more like a desert canyon than anything one expects in green Graubรผnden.
The name is Romansh โ ruina for the scree and broken rock, aulta for high โ and it describes the landscape precisely. The walls are not solid bedrock but compacted landslide material, mostly shattered limestone, and erosion has sculpted them into towers, pinnacles and sharp gullies that glow white and ochre in the sun. Forest clings to every ledge, and at the bottom the milky green river winds in loops over gravel banks. There is no road along the floor: the only continuous route through the gorge is the Rhaetian Railway, which follows the river past small halts at Trin, Versam-Safien and Valendas-Sagogn.
The classic viewpoint is Il Spir, a viewing platform designed by Corinna Menn in 2006 on the edge of the gorge near Conn, above Flims, giving a bird's-eye view straight down to the river bends. From the railway halts, trails climb along the rims and down to the water, and the river is run by rafts, which is perhaps the best way to feel the scale of the walls rising on both sides.
Getting there
The gorge begins about 17 km west of Chur, the capital of Graubรผnden. Rhaetian Railway trains stop at Trin, Versam-Safien and Valendas-Sagogn, the starting points for walks in the gorge, while the Il Spir platform is reached on foot from Conn above Flims. The nearest airport is St. GallenโAltenrhein (ACH), about 78 km away; most travellers arrive by rail via Chur.
Plan your visit
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Nearby places
- Therme Vals 23.1 km ยท thermal-bath
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From the encyclopaedia
Ruinaulta, also known as the Rhine Gorge, is a canyon in the canton of Graubรผnden (Grisons), Switzerland, carved by the Anterior Rhine between the villages of Ilanz/Glion and Reichenau. It was formed by the prehistoric Flims rockslide, which blocked the river and eventually gave rise to the present-day gorge.
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