ユンギンゲンの峡谷・トップ10

A geological peculiarity is included in the tour.

The Hohenzollern Graben is a geological fault line that stretches from southwest Germany to Austria. It was created by tensions in the Earth's crust that led to shifts millions of years ago. The rift is particularly striking along the Swabian Alb, where it clearly shapes the landscape. Rock layers are exposed here that would otherwise remain hidden. The area is of great interest to geologists because it provides deeper insights into the development of Central Europe.

A beautiful forest path that connects directly to Bolberg. Depending on weather conditions, you'll need to be sure-footed for this trail, as it descends quite steeply.

Very rocky section. Danger of slipping in wet weather. Good footwear would be good.

There are always impressive cracks on the edge of the cliff, but these have nothing to do with the Zollerngraben. The fault zone even runs across the Albtrauf and is actually higher than the surrounding area.

Be careful when wet - risk of slipping.

The name “eaves edge” requires no further explanation.

The Hohenzollern Graben was formed 15 million years ago as a result of the tectonic tensions caused by the folding of the Alps under the pressure of the African plate and the associated uplift of the Swabian Alb. The enormous forces created cracks, crevices and trenches. Although it is a collapse area, the terrain inside the graben towers above its surroundings. This so-called relief reversal is particularly evident in the example of the Hohenzollern, where a height difference of up to 350 meters is reached. As a witness mountain, it owes its position and formation to the harder, more erosion-resistant types of rock inside the graben. On the Alb plateau, too, the hilly, wooded terrain along the graben stands out from the flatter, unforested surroundings outside the graben. Source: https://de.wikipedia.org/wiki/Hohenzollerngraben#Entstehung If the above is correct, this is nothing more than a crack/cleft but not the Zollerngraben.