메체니히‬에서 가장 멋진 ‪16‬개의 협곡

https://youtu.be/mEVYFY4H16E?is=iVsbnNE_vRx3Jngy

하이킹과 사이클링을 위한 매우 좋은 계곡입니다. 길은 모든 마을로 이어집니다. 여기서 Nettersheim, Blankenheim, Tondorf 등으로 문제없이 갈 수 있습니다. 모든 길은 포장되어 있습니다. 타르 또는 자갈.

The Genfbach Valley is located in the Eifel region on the so-called Nettersheim-Marmagen Plateau and is a region of particular ecological importance. Its name comes from the Genfbach, a stream approximately ten kilometers long that rises above Blankenheim and meanders largely naturally through the landscape until it finally flows into the Urft River in Nettersheim. Large parts of the Genfbach Valley, particularly the section southeast of Nettersheim, are protected and designated as a protected area of European importance. This is due to the biotope and species diversity still typical of a low mountain range. It features species-rich wet meadows, near-natural stream floodplains, limestone marshes, and alder-ash forests. These habitats provide shelter for a rich variety of wildlife, including rare bird species such as the whinchat, kingfisher, and meadow pipit. Larger mammals such as the wildcat also use the valley as an important migration corridor. The botanical diversity is equally remarkable, with rare plants such as broad-leaved marsh orchid, devil's claw, and, in large numbers, wood cranesbill thriving in the colorful valley meadows. In the heart of the Genfbach Valley, approximately halfway between the source and mouth, lies the historic Ahe Chapel. Dedicated to Bishop Saint Servatius, the chapel was built around 1330. It is the only remaining building from the lost village of Ahe and boasts a long tradition as a place of pilgrimage. Inside the chapel is a 15th-century wooden statue of Saint Servatius. Every year on May 13, the saint's feast day, a procession takes place to the chapel. For hikers, the Genfbach Valley is accessible via several hiking trails, such as the Eifel Loop Ahe Chapel, offering a varied route through expansive meadows and picturesque forests.

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.

A very beautiful, idyllic stream valley. This is the perfect place for a relaxing hike.

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