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마지막 업데이트: 6월 12, 2026
하이라이트 • 트레일
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하이라이트 (구간) • 트레일
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뷔트겐바흐 주변 인기 장소
Three countries, one experience – borderless cycling in the Aachen region
Heights, castles, moors – RURschleifen by bike
Cycling the tracks of the Vennbahn – the Vennbahnschleifen
Trail rush through the East Belgian Ardennes
Fens, forests and water – cycling Tours in the Rur Eifel Region
벨기에의 벤바흐 사이클 루트에서 끝없는 사이클링 즐거움
Leisure Tours on enchanted paths – hiking in East Belgium
Ovelo cycle Tours in East Belgium – railway paths and natural beauty
Fantastic regional footpaths — GR hiking paths in East Belgium
Little adventures — kids on Tour in East Belgium
At this point there is a larger moor lake, which makes a nice photo motif, especially in fog. Above this, this moor lake is regularly visited by waterfowl such as wild ducks. If there are few people on the jetties and you approach the lake(s) quietly, there is a high probability that the animals will not be startled and scared away.
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The peat that can be found everywhere in the bog and fen areas is the result of a process of incomplete decomposition. Usually, dead plants are gradually decomposed by small animals (such as earthworms), bacteria and fungi. This process applies to well-drained soils. On impervious acidic soils that do not contain many bacteria and in humid climates, plants such as peat moss are only partially decomposed. Their superimposition forms the peat layer. This peat layer can be up to 7 m in certain places here in the Brackvenn. 1 mm layer of peat takes 1 year to form. With a peat layer of 7 m, for example, we are talking about a period of 7,000 years.
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Anyone who sees the beauty of the raised and low moors will never be able to let it go. The colors of the landscape, indeed the entire appearance of the High Fens, change dramatically every season. Even in winter - a breathtakingly beautiful landscape.
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What is often called a lake in the Fens is often e.g. Palsas. The palsen or pingos in the High Fens were formed around 10,000 to 11,000 years ago at the end of the last ice age. When the ground froze deep down during the cold winters of the Ice Age, the wet ground expanded and frost mounds developed. Over the years these mounds grew and the soil material that was on top slid down the sides of the mounds and over time formed a ring-shaped wall around the mound of frost. With the end of the ice age, the ice melted, the frost mound sagged and the wall was preserved. The water in the middle is called bog scour or bog eye. Source: euregio-im-bild.de/fotos/palsen-im-brackvenn-bei-m-tzenich.html
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What a unique landscape! Warning: hiking in the High Fens can be addictive :-)
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The Trôs-Marets valley, a wonderful valley landscape with uniquely beautiful hiking trails, which fascinates every hiker.
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The Fagnes are breathtakingly beautiful at any time of the year. You really have to have been here once.
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Great rocks. Challenging but very nice to walk. Good shoes and sure-footedness are an advantage.
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