ディナンのおすすめ登山＆山歩きルート

岸を変えるための重要な機会

A large rock in the middle of the center.

A beautiful bridge with a view of the castle

Concave and convex bend. That's what an information sign says along the path in this photogenic bend of the Ourthe River. The concave bank is on the outside of the meander and has (therefore) been eroded by the current. This is ideal for birds that like to make their burrows in vertical bank edges. Think of the kingfisher, and the sand martin. The convex bank is therefore on the inside of the bend. Because the water flows more slowly there, the river deposits sediments here. That's why you see gravel zones. And that, in turn, is pleasant for trout, because they like to lay their eggs there. You can walk along a beautiful path along a beautiful bend. And read about these beautiful bends. Information sign photo with the photos.

Beautiful view with a relatively easy climb

Beautiful and stately, gorgeous

On the side of the bridge, you'll find a four-language (FR/NL/DE/UK) information board with the information about the bridge Herwig mentions. It could use replacing. Other interesting facts about the bridge with visible remains: the metal cross, surmounted by a cast and painted iron statue of Christ on the railing, dates from the eighteenth century. As mentioned, the limestone base inscribes the construction years of the various successive bridges: 1725, 1909, and 1954. The base of the cross itself has also been replaced. The previous one, also part of the city's small heritage, stands on the side of the church next to the old graves. This stone stood there between 1909 and 1940 and was blown up during the war. It was replaced in 1954, just like the bridge. If you go down the stairs towards the parking lot on the other side of the bridge (the side with the information board), you will see another reminder, remains and information about the mill.

At approximately 37 meters, the top of the Anticline, also known as the Homalius Rock and especially the Falize Rock, is literally the highest point in Durbuy. It has been a highlight for many visitors for years, thanks in part to the surroundings and beautiful water features. The rock is somewhat older than the average visitor. It's said to be more than 300 million years old. However, the rock layers are much older: around 375 million years old. The name Anticline comes from the geological phenomenon known as an anticline. It's the opposite of a syncline. While the former is a fold formed over many years, with the innermost layers being the oldest and the folds running downwards, synclines have folds running downwards. Such folds can form for various reasons and range from very small to large, as seen here. Originally, everything was, of course, horizontal. The inverted U-shape created by uplift in Durbuy is not only beautiful to see but also special. And Durbuy has beautifully highlighted this. Another beautiful anticline can be found in Han-sur-Lesse, also in the Famenne-Ardenne region, albeit in the province of Namur (here we are in Luxembourg), where it has been given the name "Tête de bouc" (Tick of the Rock). There's a waterfall and a large water feature at the end of the expansive pond in front of the rock, which you can also climb. And everywhere there's space to admire it all while sitting and relaxing—or enjoying the water. Don't forget the many smaller works of art and curiosities, and take a look in the water.