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마지막 업데이트: 5월 19, 2026
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The Statte Valley Stream (French: ruisseau de la Statte) is a small but characteristic river/mountain stream in the Ardennes, located in the province of Liège (Wallonia, Belgium). It flows through the beautiful Hautes-Fagnes-Eifel Nature Park, a protected nature reserve known for its forests, heathlands, fens, valleys, and streams. The Statte is a natural stream, approximately 6 km long, that originates near the Haie Henquinet, south of the Hautes Fagnes high moor, and flows downstream through forests and meadows. Along its course, you'll see typical Ardennes landscapes: shady woodlands, rock formations, and small riverbanks. It's ideal for those who enjoy tranquility, nature, and hiking. The Statte ultimately flows into the Hoëgne River near the hamlet of Parfondbois in the municipality of Jalhay (province of Liège). The Statte Valley offers beautiful hiking opportunities and is often included in longer circular walks through the nature park. There are routes that take you along the Statte as part of larger hikes through the river landscapes of the Hautes Fagnes-Eifel, such as combination routes with the Hoëgne and Sawe valleys. Popular hikes start at the Vallée de la Statte car park (a rustic parking lot on the edge of the nature park). From here, you can take various loop routes through the valley, and wooded paths, waterways, and tranquil nature await you. At the confluence of the Statte and the Hoëgne, the stream is a beautiful spot for photos and a coffee break in nature. The nature park itself is the largest nature reserve in Belgium and a mix of raised bogs, forests, valleys, and waterways that together create one of the most authentic Ardennes experiences. Hiking in the Statte valley is a perfect way to discover the quiet, mysterious side of this nature park, and why many hikers include these routes in their Ardennes adventure.
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Truly stunningly beautiful. The parking lot already boasts a major attraction.
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Sturdy shoes are necessary, it can be slippery and wet.
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In the rivers of the Venn you can find slate and quartzite basins from the younger Cambrian period (545 to 505 million years ago). They are among the oldest layers in the core of the Venn saddle. Their original sediments were planktonic clay and sand deposits from a deep sea. After they had solidified, they were tectonically deformed as clay and sandstones, i.e. folded, slated and placed upright. Today, the originally black Revin rocks bleach when exposed to air due to the oxidation of their carbon compounds. Source: Wandern im Venn, Walter / Von Hoegen
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A pristine stream valley in a fantastic landscape. Nature lovers will get their money's worth here.
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