가장 멋진 아이즈덴-마르그라텐 주변 자연유산 20곳
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마지막 업데이트: 3월 10, 2026
베멜러베르그 오르막
하이라이트 (구간) • 등반
With the racing bike, it's all about dividing the effort. After the cornering, it's still climbing.
With the Tour bike, it's about finding a good rhythm and enjoying it.
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하이라이트 • 전망대
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하이라이트 • 동굴
The green, sloping Bemelerberg has a marl wall on one side like on a postcard. Here the yellow limestone rises high into the air and …
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we tried to return to Maastricht using the Arriva bus. However, it was a small bus and only 3 seats were available. My friends walked.
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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.
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Beautiful part of the walk along the Geul
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Here you have a view of old marl quarries. You can see a marl wall with meadows, cows, or sheep.
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The Strooberggroeve is a Limburg marl quarry in the Dutch municipality of Eijsden-Margraten. The underground quarry is located north of Bemelen under the Bemelerberg on the north side of the mouth of the dry valley Koelbosgrub in the Meuse valley. The quarry is located on the western edge of the Plateau of Margraten in the transition to the Meuse valley. At this point, the plateau drops steeply for a few meters. https://nl.wikipedia.org/wiki/Strooberggroeve
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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.
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The Geul is an idyllic stream that meanders considerably, or winds through the landscape. Because the Geul flows fast on this part, the water erodes the bank in the outer bends. In the inner bends, the water flows less fast and the sand and mud that has been carried along remains there. In the outer bends, there is a steep bank and in the inner bends a flat bank.
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