ウェームが誇る美しい風景を見てみたいなら、ウェームの素晴らしい天然記念物・トップ20
に行ってみましょう。あなたにぴったりの場所が見つかるよう、素晴らしい天然記念物を探索するために必要なすべての情報を集めました。次のアウトドアの冒険に出かける計画の参考にしましょう。
最終更新日: 6月 12, 2026
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ウェーム周辺で人気
ベルゴーラのウルアラール在の長のスルダルックの国か
自然と歴史をドイツ=ベルギー国境で-思い出の道
Cycling the tracks of the Vennbahn – the Vennbahnschleifen
Belgian Ballads – winter hiking in the Belgian Ardennes
A Vennbahn voyage - bikepacking through three countries in three days
High moor to fairytale forest – three autumn days on the Venntrilogie
グラン・トレイル・デ・ラク&シャトー - オート・ファーニュのほうすいとしろより冬のランニング
Venntrilogie – 東ベルギーのプレミアムハイキング体験
ベルギーのヴェンバーンサイクルルートでの無限のサイクリング楽しみ
Leisure Tours on enchanted paths – hiking 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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これらのガイドで、最高の洞窟を探す範囲を広げましょうウェームでの: