가장 멋진 베겔 주변 자연유산 20곳

Largest burial mound in the Netherlands.

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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.

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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.

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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.

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This is an archaeological monument.

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A nice explanation of the burial mounds found here. Everything clearly explained on signs. I found the drawings on the viaduct more impressive.

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Orbital grounds are rare and almost unheard of elsewhere in Europe. Fractures in a subsurface made up of layers of clay

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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.

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Holiday park Sandberghe is located against the sand dunes of Bedaf. Here you will encounter the beautiful surroundings of the Maashorst nature reserve. Sniff the fresh forest air and enjoy the varied nature. Rest and relax, go on an adventure and experience. How nice is it to forget the daily grind and get lost in the moment. Being in a different environment. See and do other things. A week for yourself, your family and your friends. Discover, de-stress, unwind, relax, meet... Yes, meet. It's nice not having to. That is Sandberghe. A nice place to get lost. And the wide choice of comfortable holiday homes and spacious tents surprised this guest: “We were very happy and had such…

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

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narrow access only on foot

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The Wijstgronden in Uden are three small nature reserves on the road from Uden to Vorstenbosch in the province of North Brabant. The Loose Beemden, the Raktse Beemden and the Kooldert together cover an area of approximately 41 hectares. Staatsbosbeheer is the owner. Source: Wikipedia

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Surprising piece of nature after walking through arable land for a long time.

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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. The best-known fault is De Peelrand fault east of the Asten-Deurne-Milheeze-Erp line. When this landscape was formed, the area of what is now Brabant was still below sea level. About two million years ago, in the late Tiglian, this area was covered with silt from the Rhine River. The last ice age and the subsequent period modeled the Brabant landscape as we know it today over this primeval landscape. More information: https://www.brabantserfgoed.nl/page/5639/brabantse-landschappen?gclid=Cj0KCQjw2NyFBhDoARIsAMtHtZ6Rn8xgJq3tq-bVstJtalFr3nbkB_dUgaEacnV3LZzO4IuyaAlBEvQwYYcEal-4

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Very varied landscape with beautiful sand dunes to wet wijsgronden. In this area there is a natural fault line, namely the Peelrandbreuk. Because of this fault there are high sand dunes and a little further there is a strip of very wet ground, this is the Peelrandbreuk which is clearly visible because the water rises to the surface due to upward pressure. A beautiful natural phenomenon with the difference from what we are used to that here the higher ground is wetter than the lower ground.

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

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Once upon a time there was a very large trailer camp here.

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The archaeological monuments Vorstengraf Oss and De Zevenbergen are two areas with burial mounds, urn fields and flat graves from the Bronze Age and early Iron Age, which today are separated by highways but possibly once formed a larger complex. The Vorstengraf near Oss is the largest burial mound in the Netherlands. The hill was three meters high and had a diameter of 54 meters. The grave was discovered and investigated in 1933 and rediscovered in 1997. The Vorstengraf and De Zevenbergen are located at the Paalgraven junction. This junction is named after the wreaths surrounded burial mounds that were found near the Zevenbergen. These graves were constructed in the period from the Early Bronze Age to the Early Iron Age, so from 2000 BC. up to 700 BC. (Wikipedia)

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