가장 멋진 호수 20곳

Paved, no cars, partly sun and shade, quiet

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superb in good weather!

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The Lion, created by Félix-Antoine Bouré, is one of the major attractions. Height: 13.5m – her weight: 130 tons. 183 blocks that fit together like a puzzle were completely dismantled and rebuilt to mark the raising of the dam. The lion looks in the direction of Eupen, then Prussia, barely 5 kilometers away. Source: https://www.tourismejalhaysart.be/nl/attraction/barrage-du-lac-de-la-gileppe-jalhay-hautes-fagnes-spa/

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This work of art, made from granite, was the first of its kind in Belgium. The dam was built between 1867 and 1875. Between 1967 and 1971 it was consolidated and the capacity of the reservoir was increased to 26.4 million m³ of water. The lake is fed by the Gileppe, the Louba and the Soor. Two 75m high collection towers direct the water to turbines. The famous Lion, created by Félix-Antoine Bouré, is one of the major attractions. Height: 13.5m – her weight: 130 tons. 183 blocks that fit together like a puzzle were completely dismantled and rebuilt to mark the raising of the dam. The lion looks in the direction of Eupen, then Prussia, barely 5 kilometers away. Source: https://www.tourismejalhaysart.be/nl/attraction/barrage-du-lac-de-la-gileppe-jalhay-hautes-fagnes-spa/

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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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