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개의 천연기념물과 상세 정보를 살펴본 후에 방문하고 싶은 천연기념물을 다음 모험 계획에 추가해보세요!

마지막 업데이트: 10월 13, 2026

하터르트세와 오버라셀트세 벤넨

하이라이트 • 호수

The Hatertse and Overasseltse Vennen is an area of approximately 520 hectares in the municipalities of Heumen and Wijchen, province of Gelderland. The area consists of about twenty named pools. …

번역자 Google •

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베다프세 베르헨 모래언덕

하이라이트 • 자연

Walk the winding paths between the ancient trees or over the drifting dunes (loose sand). Do put on sturdy shoes!

번역자 Google •

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최고의 싱글 트랙, 봉우리 및 다양한 흥미로운 야외 장소에 대한 추천을 받아보세요.

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Beautiful walk through quiet (even cycling is not allowed) wooded area.

번역자 Google •

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잔드페르스퇴빙 베다프

하이라이트 • 자연 기념물

Beautiful high sand dunes. From above you have a good view over the sand drift. You can take wonderful walks here.

번역자 Google •

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우덴 근처의 필란트 단층

하이라이트 (구간) • 자연 기념물

Due to the very slow pushing up of mountains such as the Ardennes and the Eifel, tensions arose that caused cracks and fragmentation in the gently sloping earth crust.

번역자 Google •

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부르곤디스 브라란트 - 20개의 맛있는 자연 산책로

하이킹 컬렉션 에 의해

Marieke Duchatteau

커뮤니티 팁

Wappie
12월 6, 2025, Peelrand Fault Near Uden

The Peelrand fault near Uden is one of the most recognizable fault zones in Brabant and cuts across the landscape between the Bedafse Bergen and the Annabos. This geological fault causes a height difference of several meters, but more importantly, a difference in water management that is immediately visible in the terrain. On the higher side of the fault, mineral-rich groundwater rises, making this higher part wetter than the lower-lying zone adjacent to it. This inverse pattern of wet and dry is both indicative and unique to this area. Along the fault line, you can see how the dry drifting sand of the Bedafse Zandduinen abruptly transitions into dark, moist soil where seepage water surfaces. The water often has a reddish-brown hue due to the iron carried from the deeper layers. This transition is clearly visible in the field: a few meters further, the landscape changes completely, from dry and light sand to wet, boggy terrain with alders, sedges, and other moisture-loving plants. The Peelrand fault near Uden is therefore a significant geological feature that shapes the entire area. Without it, the Bedafse Bergen wouldn't be so dry and drifting, and the Annabos wouldn't be so wet and seepage-prone. The fault makes this part of Uden one of the best places to see the "wisp" phenomenon in person, and it gives the hiking trail a scenic quality found in few other places.

번역: Google•

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The Bedafse Bergen form a striking drifting sand area between Uden and Vorstenbosch. The landscape was created by centuries of sand drift after the original forests were cleared for agriculture and firewood in the Middle Ages. The wind carried the loose sand and accumulated it into hills and sand ridges—the present-day sand dunes of the Bedafse Bergen. The area consists of open drifting sand, low and high sand hills, dry heathland, and small transitions to forest. The dunes have remained active because managers keep sections open, thus preserving the character of a true drifting sand area. The higher ridges offer clear views over the undulating sand landscape, which differs significantly from the typical Brabant forests and farmland. The Bedafse Bergen are one of the few remaining places in North Brabant where this type of landscape can still be seen so clearly: a rugged, dry, and dynamic terrain with natural elevation changes. This makes it both scenically unique and physically challenging, especially when you hike up and down the steep sandy slopes several times. Today, it's a protected nature reserve and a popular hiking area due to its unique dune landscape, open vistas, and stark contrast with the surrounding landscape.

번역: Google•

0

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The Bedafse Bergen form a striking drifting sand area between Uden and Vorstenbosch. The landscape was created by centuries of sand drift after the original forests were cleared for agriculture and firewood in the Middle Ages. The wind carried the loose sand and accumulated it into hills and sand ridges—the present-day sand dunes of the Bedafse Bergen. The area consists of open drifting sand, low and high sand hills, dry heathland, and small transitions to forest. The dunes have remained active because managers keep sections open, thus preserving the character of a true drifting sand area. The higher ridges offer clear views over the undulating sand landscape, which differs significantly from the typical Brabant forests and farmland. The Bedafse Bergen are one of the few remaining places in North Brabant where this type of landscape can still be seen so clearly: a rugged, dry, and dynamic terrain with natural elevation changes. This makes it both scenically unique and physically challenging, especially when you hike up and down the steep sandy slopes several times. Today, it's a protected nature reserve and a popular hiking area due to its unique dune landscape, open vistas, and stark contrast with the surrounding landscape.

번역: Google•

2

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Beautiful area. The paths are sometimes narrow.

번역: Google•

1

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Beautiful nature and wonderfully quiet.

번역: Google•

1

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My absolute highlight in this area - small but beautiful. Pure nature - suitable for hikers and cyclists.

번역: Google•

3

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The Bedafse Bergen is a special piece of primeval territory where you can wander freely and where it feels as if time has stood still.

번역: Google•

2

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Idyllic.. peace.. nature.. everything your heart desires

번역: Google•

4

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