Vettweißの峡谷・トップ13

Above Abenden, there are more beautiful rock formations, a little off the main hiking trail. However, the path is sometimes very narrow (marked as T2), and at times you feel like a machete would be helpful, as the blackberry bushes and stinging nettles overgrow the path on both sides. However, there are fewer hikers around, and you can admire the rocks in peace.

Beautiful hiking trail with some interesting rock formations made of red sandstone.

Very beautiful rock formations! The rust-red rock bastions along the valley slopes dominate the landscape in the Rur valley. But how did these impressive rock walls and towers come into being? The rocks are made of rubble and sand that was formed by weathering in a hot, desert-like landscape in the early Mesozoic during the Triassic period, more precisely in the formation of the "Buntsandstein" around 240 million years ago. Weathering under tropical climatic conditions is also the reason for the red color of the rocks. In these deserts there were violent storms from time to time, which transported the sand and rubble masses via large rivers into depressions and deposited them there. During transport in the river, the larger stones were ground down into rounded pebbles. Today, embedded in the sand that has solidified over millions of years, they can be clearly seen in the rocks. In geology, these types of rocks are known as "conglomerates". When the Eifel gradually rose millions of years later, having eroded into a low-lying plain, the larger rivers, such as the Rur, cut deeper and deeper into the sedimentary rocks, particularly during the ice ages, thus exposing the rock formations that can be seen today. Source: biostation-dueren.de/schutzgebiete/buntsandsteinfelsen-im-rurtal

Very beautiful rock formations! The rust-red rock bastions along the valley slopes dominate the landscape in the Rur valley. But how did these impressive rock walls and towers come into being? The rocks are made of rubble and sand that was formed by weathering in a hot, desert-like landscape in the early Mesozoic during the Triassic period, more precisely in the formation of the "Buntsandstein" around 240 million years ago. Weathering under tropical climatic conditions is also the reason for the red color of the rocks. In these deserts there were violent storms from time to time, which transported the masses of sand and rubble via large rivers into depressions and deposited them there. During transport in the river, the larger stones were ground down into rounded pebbles. Today, embedded in the sand that has solidified over millions of years, they can be clearly seen in the rocks. In geology, these types of rocks are known as "conglomerates". When the Eifel gradually rose millions of years later, having eroded into a low-lying plain, the larger rivers, such as the Rur, cut deeper and deeper into the sedimentary rocks, particularly during the ice ages, thus exposing the rock formations that can be seen today. Source: biostation-dueren.de/schutzgebiete/buntsandsteinfelsen-im-rurtal

Very beautiful hiking trail on the edge of the rocky plateau of Nideggen Castle in the Rur Valley.

Wonderful path over the rocks of Nideggen with great views.

A really great landscape, impressive rock formations and very beautiful narrow hiking trails - hardly any wide asphalt paths, so absolutely recommendable hikes.

Simply impressive rocky landscape in the Eifel with great views.