ヴァルケンブルク・アーン・デ・カウルの峡谷・トップ16

Along the rippling Geul River, an impressive marlstone wall rises, a silent witness to Limburg's underground landscape. These calcareous rocks were used for centuries for construction and crafts and now offer a fascinating sight for hikers and nature lovers. The wall forms a natural boundary along the water and, in some places, harbors small caves and niches where flora and fauna have found a home. The contrast of the white marl against the green foliage and the glistening water of the Geul makes this a particularly photogenic and tranquil spot during your walk.

There are old flint quarries in this area: the “Carrières de silex du Thier des Vignes”.

Beautiful part of the walk along the Geul

A mysterious flint cave on the edge of the Albert Canal, near the locks at Klein Ternaaien. You reach the entrance via a steep path through the woods. The caves are dark, cool, and full of atmosphere—perfect for those who love hidden natural spaces. Bring a flashlight and good walking shoes!

When the path that has been running between slopes and sloping forest on one side and the Geul on the other side suddenly starts to rise a bit, you know what is coming: part of the marl crops out and offers you a glimpse of what you can discover if you take one of the paths away from the Geul: quarries and marl.

Impressive, you can see some caves.

Wonderful single track with deliciously scented wild garlic on both sides.

The Trichterberg quarry is located in the forest to the left of the steep Eckelraderweg, between Gronsveld and Eckelrade. Diagonally opposite are dole chambers. The quarry has been designated as a “Geological Monument”. Steep limestone walls with here and there sawn surfaces and a few small corridor remains are the only remains. Not much is known about the Trichterberg quarry. That is why Peter Jennekens, Kevin Amendt and Rob Habets wrote a source overview for the magazine of the Study Group Underground Limestone Quarries - Natural History Society in Limburg. Based on this, they cautiously conclude that the origin of the quarry must lie somewhere between the years 1846 and 1867. The entire PDF with all sources can be found at https://www.sok.nl (November 2013 edition).