Infolge Bauarbeiten wird der Bahnbetrieb zwischen Lauterbrunnen und Wengen jeweils in den Nächten 12./13.04. - 15./16.04. & 19./20.04. - 22./23.04. & 26./27.04. - 29./30.04. & 17./18.05. - 20./21.05.2021 unterbrochen sein. Letzte Abfahrt in Lauterbrunnen um 22:30 Uhr, letzte Abfahrt in Wengen um 22:03 Uhr. Erste Abfahrt in Lauterbrunnen um 05:24 Uhr, erste Abfahrt in Wengen um 05:40 Uhr
Vertical rock faces and delightful terraces, framed by snow mountains: the Lauterbrunnen valley fascinates mountain and extreme sportsmen- as well as gourmets. Glaciers have shaped this scenery in thousands of years.
It's cold. Freezing cold. Even if the sun is shining. Ice covers the mountainous landscape and the V-shaped notches that streams have previously dug into the rock. Even where today the Lauterbrunnen Valley with the sun terraces of Wengen and Mürren is situated. Only the highest peaks rise out of the ice. We are in the Bernese Oberland, 25,000 years ago.
Ice and gravel
It's the ice age. Everything is frozen. Nothing seems to move. But appearances are deceptive. Under their enormous weight the ice masses, which are up to over 1000 meters thick, are moving on the slopes of the Jungfraumassiv. Its pressure heats the glacier bottom so that the ice begins to glide on the melting water. The glaciers are set back 20 to 200 meters per year. And they transport huge amounts of rubble - from small pebbles to huge boulders, today's boulders.
Pushing, sanding and scraping
At the bottom of the ice rivers gravel sticks, which acts like oversized sandpaper. The millions of tons of glaciers planted rock from the ground and from the flanks. It is a permanent rubbing, pushing, sanding and scraping. It is a powerful force which forces the V-shaped valley slowly to a new shape. Very slow, but all the more sustainable.
Valley milling machine from the Ice Age
The glacier, which flows downwards from the Jungfrau, acts brutally, especially in its center. Its enormous weight properly mills a wide nut into the landscape. Vertical, several hundred-meter-high rock walls bound a flat valley floor on both sides. From the V-shape becomes a U-shape, from the "Kerbtal" a "Trogtal".
The force of the ice stream at its edges is significantly lower. There are terrasse-like, gently inclined plateaus, so-called "Trogschultern", and often also "Hohlkehlen", which mark the peak of the glacier. The mountains rise steeply again.
Hikers, winter sports enthusiasts and Wingsuiter
Since the last Ice Age, the ice masses have melted, a landscape that made life possible at all and which is so rare in Europe. This has been discovered by tourists from all over the world.
Strollers take the easy paths around Mürren and Wengen. Hikers wander through forests and over-flowered Alps. Miners dare to climb steeper passages. Wintersporters swing on slopes and down the snowy slopes. Basejumper and Wingsuiter plunge from the troughs into the Lauterbrunnen valley. And quiet gourmets simply sit down on a bench.
All together is the enthusiasm for one of the most beautiful valleys in the Alps with its 72 waterfalls. It is also a succession of the valley-forming glaciers of the last Ice Age.