Nature in Belgium
A guide to 203 Nature in Belgium — with descriptions, photos and traveler visits from the NextOnTrip community. Locations spread across 144 cities and towns. Most visited by the community: Waggelwaterpark, Hof ter Musschen Park, Beislovenpark.
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Schmerling Caves
Flémalle
Schmerling Caves form a modest but scientifically remarkable group of karst caves on the right bank of the Awirs stream, near the village of Awirs, within the municipality of Flémalle in Wallonia, Belgium. Though the site itself offers little in the way of visitor infrastructure today, it played a pivotal role in the early history of human paleontology. Where does the name come from? The caves take their name from Philippe-Charles Schmerling, a Belgian physician and naturalist who carried out excavations here in 1829. His findings would only be fully understood decades later, once the broader scientific community had the context to recognize their significance. What was found in the lower cave? In the lower cave, known also as Trô Cwaheur or Trou Caheur, Schmerling uncovered the remains of two individuals. One of them, now referred to as Engis 2, turned out to be a Neanderthal fossil — in fact, it is regarded as the very first Neanderthal fossil ever discovered anywhere, even though its true nature wasn't recognized at the time. The other set of remains belonged to a Neolithic Homo sapiens. The presence of two individuals from such different periods of prehistory at a single site makes Schmerling Caves an unusually significant location for the study of human evolution in Europe. What happened to the caves? The fate of the different caves in this complex varied considerably. The lower cave, site of the most important discovery, has since collapsed and is no longer accessible in its original form. A third cave in the group was destroyed entirely due to quarrying operations at the adjacent site, the Ancienne Carrière des Awirs (Former Awirs Quarry). While this industrial activity damaged part of the site, the quarrying also indirectly exposed geological layers that drew the attention of nineteenth-century researchers in the first place. Why does this site matter to science? The importance of Schmerling Caves extends well beyond local history in Flémalle. The discovery of Engis 2 predates the very coining of the term "Neanderthal" — full recognition of what Schmerling had found only came after later discoveries in the Neander Valley in Germany in the mid-nineteenth century. Today, archaeologists and paleoanthropologists widely regard Schmerling's excavations as pioneering work in the study of human origins, even though, at the time, he lacked the methodological tools and scientific context to grasp the full weight of what he had unearthed. Frequently asked questions Can Schmerling Caves be visited today? Because the lower cave has collapsed and a third cave was destroyed by quarrying, the site today holds mainly historical and scientific value rather than being a developed tourist attraction. Who was Philippe-Charles Schmerling? He was a Belgian physician and naturalist who conducted excavations in this area in 1829, uncovering remains that would later prove fundamental to understanding human prehistory. What is Engis 2? It's the name given to the Neanderthal remains found by Schmerling in the lower cave — considered the first Neanderthal fossil ever discovered anywhere in the world. Where exactly are the caves located? In the municipality of Flémalle, in the Wallonia region of Belgium, on the right bank of the Awirs stream, close to the village of Awirs.
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Trou Lecoq
Sprimont
Trou Lecoq is a karst cave, known locally as a "chantoir," located in the municipality of Sprimont in Belgium's Liège province, near the village of Louveigné and close to the boundary with the neighbouring municipality of Aywaille. It is one of roughly seventy chantoirs catalogued within the Vallon des Chantoirs, a karst valley that stretches across both municipalities. What is a chantoir, and how did Trou Lecoq form? A chantoir is the local Belgian term for a spot where a surface stream disappears underground into limestone bedrock. The area containing Trou Lecoq marks the northern edge of the Calestienne, a band of Middle Devonian limestone that runs roughly 130 kilometres southward, extending into France. Within this limestone, water has carved out a network of underground channels over time, producing the sinkholes and caves that make up the valley, Trou Lecoq among them. Hydrological studies of this karst system have shown that the waters vanishing into the valley's various chantoirs converge underground into a single common collector. That water only reappears at the surface in the Remouchamps caves, where it flows as an underground river known as the Rubicon. What has been discovered inside the cave? The exploration history of Trou Lecoq stretches back to the mid-twentieth century. The same underground chamber that later drew further investigation was first reached by Fernand Lambert and Guy de Bellefroid in September 1950, and again by the caving group Les Taxis in September 1966. A breakthrough came in June 1993, when Patrick Hamers of the SC Avalon club and Michel Antoine of CASA passed through a siphon — a passage section completely filled with water — and came upon a previously unexplored part of the cave. Beyond the siphon they found a meandering passage that, after about 25 metres, opened into a small chamber. Further exploration revealed considerably larger features. Cavers discovered the Salle de la Batterie, a spacious and very tall chamber reached by climbing an eight-metre section. They also found a tall, diagonal fissure (a diaclase) with several side passages branching off it, as well as an impressive cylindrical chimney with clay walls that required artificial climbing techniques to ascend. Altogether, the newly discovered section measured 102 metres in length. Why did exploration of the cave come to a halt? Exploration work at Trou Lecoq stopped in 1994 for two reasons. First, rising water levels once again blocked the siphon that the 1993 team had passed through, cutting off access to the newly found sections. Second, a local Dutch tour operator installed a gate at the cave entrance, which effectively brought further exploration to an end. To move through the different parts of the cave system, the cavers relied on ladders measuring ten, five, and five metres, needed for the various descents and climbs encountered along the way. Frequently asked questions Where exactly is Trou Lecoq located? The cave lies within the municipality of Sprimont in Liège province, near the village of Louveigné, inside the karst valley known as the Vallon des Chantoirs. Can Trou Lecoq be visited today? A gate installed by a local Dutch tour operator has restricted free access to the cave's interior since 1994. Where does the water that vanishes into Trou Lecoq end up? The underground water from the valley's chantoirs converges into a shared collector and re-emerges at the Remouchamps caves, flowing as an underground river called the Rubicon.
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Belle-Roche cave
Sprimont
Belle-Roche cave is a fossil cave and a Middle Pleistocene archaeological and paleontological site located in the municipality of Sprimont, in the province of Liège, Wallonia, Belgium. The cave sits on the right slope of the Amblève valley, south of the village of Fraiture, roughly 2 km from the point where the Amblève meets the Ourthe, near Comblain-au-Pont. The entrance lies at an altitude of about 160 meters, some 60 meters above the current level of the river. How was the cave discovered? The site was uncovered by chance in 1980, during blasting work at a nearby quarry. The explosion exposed sediment-filled karst passages that researchers quickly recognized as an exceptionally rich deposit of fossilized remains. The discovery triggered years of excavation and research, carried out by scientific teams until 1999. Why is this site so significant? The deposits found at Belle-Roche date from the Early Middle Pleistocene, corresponding to a phase known as the Upper Cromerian — roughly 500,000 years old. This makes the cave the oldest known Middle Quaternary deposit in the country and a reference point of major importance on a European scale. Among the sediments, researchers identified traces of primitive stone technology — worked pebbles, or pebble tools — representing by far the oldest known evidence of human presence in the Benelux region. What was found inside the cave? More than 30,000 fossils have been recovered and catalogued from the Belle-Roche sediments, representing about fifty distinct animal species — evidence of an unusually rich and varied fauna from half a million years ago. Alongside the animal bones, researchers also recovered worked flint, confirming human presence in the area at this extremely early date. Notably, some of the flint tools did not originate inside the cave itself: they were carried in by the Belle-Roche karst network, having eroded out of archaeological sites originally located further upstream in the Amblève valley. Together with the tools, tens of thousands of animal bones were swept into the cave and preserved within its sediments for hundreds of thousands of years. What sets Belle-Roche apart from other sites in the region? What distinguishes Belle-Roche from other caves and prehistoric sites in the Amblève and Ourthe valleys is the combination of an exceptionally well-preserved fossil fauna with some of the oldest traces of human activity known in the area. Finding both rich paleontological and archaeological material together, dated to half a million years, is rare not only in Belgium but across the wider Benelux region. Frequently asked questions Where exactly is Belle-Roche cave located? In the municipality of Sprimont, province of Liège, on the right slope of the Amblève valley, south of the village of Fraiture, near Comblain-au-Pont. When was the cave discovered? In 1980, as a result of blasting work at a nearby quarry. How old are the finds from Belle-Roche? The deposits are dated to roughly 500,000 years ago, corresponding to the Early Middle Pleistocene (Upper Cromerian). What exactly was found in the cave? More than 30,000 fossils representing about fifty animal species, along with worked flint tools evidencing human presence. Can Belle-Roche cave be visited? The site is primarily a scientific research location of major importance; visitor access depends on current arrangements made by local authorities and the institutions managing the site.
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Grotte La Merveilleuse
Dinant
Grotte La Merveilleuse is a limestone cave in Dinant, in Belgium's Namur province, regarded as one of the most beautiful caves in Europe. Its name — "the Marvellous One" — is no exaggeration once you step underground and take in the scale and detail of its formations. How was the cave discovered? The discovery is surprisingly recent for a geological site. The cave was uncovered in 1904 during construction work on a railway line linking Dinant to Florennes: workmen digging a trench broke through into an underground network of galleries roughly 500 meters from Dinant's train station. The site was opened to the public just a year later, in 1905, making it one of the region's longest-running tourist attractions. What can visitors see inside? The cave spreads across three levels and is known for the richness of its formations. Inside, visitors find monumental galleries, stalactites, stalagmites, columns, and dramatic rock draperies, along with water trickling and jumping along the rock surfaces — giving the interior a notably dynamic feel compared to many other karst caves. The standout geological feature is an oblique stalactite, considered the tallest formation of its kind in Europe. Its distinctive slanted shape formed as a result of strong air currents moving through that section of the tunnel — a phenomenon rarely seen at this scale. What historical role has the cave played? Beyond its natural features, Grotte La Merveilleuse played a meaningful role during the Second World War, when its underground passages served as a shelter for local residents during combat operations, offering protection from shelling and bombardment. It's a striking contrast to picture these same quiet chambers once serving as a wartime refuge. The cave is also tied to Dinant's musical heritage: the town is the birthplace of Adolphe Sax, inventor of the saxophone. In a nod to that tradition, the cave regularly hosts concerts and musical performances, with the acoustics of its underground chambers lending the events a distinctive character. Where is Grotte La Merveilleuse located? The cave sits right next to the town of Dinant, picturesquely set along the Meuse river in Wallonia's Namur province. Its proximity to both the train station and the town center means it's easy to reach without much planning — one reason it has remained a popular stop on regional itineraries for more than a century. Frequently asked questions When was Grotte La Merveilleuse discovered? It was discovered in 1904 during construction of the Dinant–Florennes railway line and opened to the public the following year, in 1905. What is the cave's most distinctive formation? An oblique stalactite, considered the tallest of its kind in Europe, shaped by air currents moving through the tunnel. What role did the cave play during World War II? It served as a shelter for Dinant's residents during combat operations. How many levels does the cave have? The cave extends across three levels, featuring galleries, stalactites, stalagmites, and rock draperies.
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Caves Sainte-Anne
Esneux
Caves Sainte-Anne is a karst cave system located between the villages of Tilff and Méry, within the municipality of Esneux, in the province of Liège in Wallonia, Belgium. The cave sits along the road connecting Esneux and Tilff, on the right bank of the river Ourthe, about a kilometre before entering Tilff. How did the cave form? Caves Sainte-Anne was carved out by an underground river, which can still be followed for several hundred metres up to a siphon fed by waters coming from the Chawresse cave and the Trou des Manants. The lower level of the system remains active and water-filled, and can become difficult to navigate during periods of high water. The upper levels, abandoned long ago by flowing water, are considered "fossil" passages — a common stage in the life cycle of karst caves, where erosion migrates progressively deeper underground while older galleries dry out. How large is the cave system? The system extends over roughly 1,542 metres in total length and reaches a depth of 35 metres across four superimposed levels. This multi-level structure makes Caves Sainte-Anne one of the more substantial cave networks in this part of Belgium, even though it remains relatively unknown to the general public compared with more touristic caves in the region. Can visitors enter on their own? No. The cave entrance was, in the past, subject to repeated damage from visitors who did not respect the underground environment — including harm to rock formations and disturbance of the natural ecosystem. To address this, since 1991 the entrance has been secured with a locked door managed by the Belgian Union of Speleology (UBS – Union Belge de Spéléologie). How can a group arrange a visit? Access to the cave is limited to organised groups and requires prior authorisation from the UBS. Requests can be made through the union's office at rue Belvaux 93 in Liège, or by phone at +32 (0)4 342 61 42. This management model — common for ecologically and geologically valuable karst caves across Western Europe — allows the interests of speleologists and visitors to be balanced against the need to protect a fragile underground environment, including its rock formations and any cave-dwelling fauna. What should visitors know before planning a trip? Caves Sainte-Anne is primarily a site for those interested in speleology rather than a conventional show cave with a marked route and lighting. Exploring it requires proper physical preparation and equipment, particularly in the sections with active water flow, where difficulty varies with the season and rainfall levels. For anyone exploring the area around Esneux and Tilff along the river Ourthe, the cave is a notable point of geological interest in the region, though a visit depends on prior contact with the organisation that manages access. Frequently asked questions Is the cave open to individual tourists? No, the entrance is secured with a lock, and access is limited to groups that have obtained authorisation from the UBS. How deep is the cave? The system reaches a depth of 35 metres across four levels and totals approximately 1,542 metres in length. Where exactly is the cave located? Between Tilff and Méry, within the municipality of Esneux, along the Esneux-Tilff road, on the right bank of the river Ourthe, about a kilometre before Tilff. Who manages access to the cave? The Belgian Union of Speleology (UBS), based at rue Belvaux 93 in Liège.
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Neptune Caves
Couvin
Neptune Caves, also known by their French name Grottes de l'Adugeoir, are a series of natural caves in the region of Wallonia, near the village of Petigny, within the municipality of Couvin in Belgium. The caves lie along the Eau Noire river, a tributary of the Meuse, in an area characteristic of the karst landscapes found across southern Belgium. Where exactly are the caves located? Neptune Caves sit at coordinates 50.06614, 4.51205, in the province of Namur — a part of Belgium well known for its limestone formations and network of caves. The valley of the Eau Noire, which runs close to the site, adds a scenic backdrop, with the surrounding hills framing the underground system. Why is the Couvin area known for its caves? The municipality of Couvin and its surroundings sit on limestone bedrock that, over long geological timescales, gave rise to extensive cave systems. Rivers like the Eau Noire have carved through the rock over thousands of years, leaving behind passages and chambers that today draw the interest of both casual visitors and speleology enthusiasts. The French name Grottes de l'Adugeoir reflects the local, French-speaking naming conventions typical of natural sites in this part of Belgium. What should visitors know before planning a trip? Since Neptune Caves are a natural cave system rather than a fully commercialized showcase cave on the scale of Belgium's largest tourist grottoes, it is worth checking local information about access and any entry restrictions before visiting. The Couvin area is well connected to other attractions in southern Wallonia, making it easy to combine a visit to the caves with other stops on a regional itinerary. How can you get to Neptune Caves? The village of Petigny, within the municipality of Couvin, serves as the main reference point for reaching the caves. From there, local roads following the Eau Noire valley provide access to the site. The region lies in the province of Namur, relatively close to the French border, making it a convenient stop for travelers exploring the Franco-Belgian borderland. Frequently asked questions Where exactly are Neptune Caves located? In Wallonia, near Petigny, in the municipality of Couvin, along the Eau Noire river, a tributary of the Meuse. What is another name for these caves? They are also known by their French name, Grottes de l'Adugeoir. Which river runs near the caves? The Eau Noire, a tributary of the Meuse. In which Belgian province are the caves found? In the province of Namur, in the Wallonia region. Are there other attractions nearby? The Couvin area and the Eau Noire valley are known for their karst landscape, so travelers can expect other cave formations and natural viewpoints typical of southern Wallonia in the vicinity.
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Scladina
Andenne
Scladina, also known as Sclayn Cave, is an archaeological site in Wallonia, in the town of Sclayn, tucked into the Andenne hills in Belgium. Over the decades it has become one of the region's most significant sources of information about Neanderthal life, and its finds have entered the international scientific literature on Stone Age Europe. What has been found inside Scladina? Systematic excavations at Scladina have been carried out since 1978. During that time, researchers have recovered an exhaustive collection of over thirteen thousand Mousterian stone artifacts from the cave's sediment layers. The Mousterian is a Middle Paleolithic stone tool tradition, and the sheer scale of this collection makes Scladina one of the key sites of its kind in the Andenne area. Why is Scladina so important? The cave's international reputation rests largely on a discovery made in 1993, when excavators uncovered the fossilized remains of an especially ancient Neanderthal within the cave's layers. The find became known as the "Scladina child." Together with the thousands of stone tools recovered on site, it turned the cave into one of the essential reference points for understanding how Neanderthals lived in Europe thousands of years ago. Where exactly is Scladina located? The cave lies in the Andenne hills, in Belgium's Namur province, close to the village of Sclayn. Its geographic coordinates are approximately 50.4843°N, 5.0252°E, placing it precisely within the hilly countryside of Wallonia. The surrounding landscape is rural, with the cave set into the slopes above the Meuse valley. What should visitors know before going? Scladina is first and foremost a scientific site rather than a fully developed tourist attraction — its significance comes from the archaeological research conducted here since 1978, not from dramatic scenery. For anyone interested in archaeology and human prehistory, though, it remains a place of real value: layer by layer, excavations here have revealed evidence of Neanderthal presence in what is now Belgium. Frequently asked questions Where is Sclayn Cave located? In Wallonia, in the town of Sclayn, within the Andenne hills in Belgium. Since when has the site been excavated? Archaeological excavations have been ongoing without interruption since 1978. What was discovered at Scladina? Over thirteen thousand Mousterian stone artifacts, along with the fossilized remains of an especially ancient Neanderthal found in 1993, known as the "Scladina child." What is the "Scladina child"? It is the name given to the remains of an unusually ancient Neanderthal individual discovered in the cave in 1993, one of the site's most important finds. What kind of place is this? Scladina is primarily an active archaeological site, valued for its scientific discoveries rather than for extensive visitor infrastructure.
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Grotte de Spy
Jemeppe-sur-Sambre
Spy is a small village in the municipality of Jemeppe-sur-Sambre, in the province of Namur, Wallonia, known worldwide for a cave that became one of the most decisive sites in the history of human evolution research. The village lies along the Orneau River, which flows through the province of Namur and, after a course of roughly 25 kilometres, joins the Sambre right at Jemeppe-sur-Sambre. What is the cave at Spy? The cave, locally known as the Betche aux Rotches, sits above the left bank of the Orneau. It is a limestone cave that has been the focus of intensive archaeological and anthropological research since the late 19th century. Its importance reaches far beyond Belgium, placing it among the most significant Palaeolithic sites in all of Europe. Why is the Spy cave so important to science? In 1886, researchers Maximin Lohest and Marcel de Puydt uncovered two nearly complete Neanderthal skeletons — a man and a woman — at a depth of about 4.9 metres, alongside numerous Mousterian-type stone tools. The discovery carried enormous scientific weight: it provided compelling evidence that Neanderthals were a distinct, archaic human species rather than a pathological variant of modern humans, a theory some scholars had favoured before. The two skeletons, known as Spy I and Spy II, were dated for decades to around 36,000 years before present. More recent Bayesian analysis, published in 2014, suggests the remains are likely older than 40,000 years. The Spy finds played a key role in shaping the modern understanding of where Neanderthals fit into human evolution, and they remain the subject of ongoing study — including taphonomic analysis of peri-mortem trauma on the skeletons, aimed at determining whether the individuals died by accident or by violence. What is the legacy of Spy today? Because of its scientific significance, the Spy cave is today classified as one of the foremost heritage sites of the Walloon Region. Research at the site has continued for more than 125 years, spanning multiple disciplines from archaeology and anthropology to geology and palaeontology, with findings published in international scholarly works, including a multi-volume monograph dedicated entirely to the site. The village of Spy itself remains a small settlement within the municipality of Jemeppe-sur-Sambre, which counted just under 18,000 inhabitants as of 2006. It is a quiet, rural corner along the Orneau whose fame far outstrips its size — for archaeologists and prehistory enthusiasts alike, the name "Spy" has stood for well over a century as shorthand for a landmark discovery about our closest evolutionary relatives. Frequently asked questions What was discovered in the Spy cave? In 1886, researchers found two nearly complete Neanderthal skeletons together with Mousterian stone tools. How old are the remains found at Spy? They were traditionally dated to around 36,000 years old, though a 2014 Bayesian analysis suggests they may be more than 40,000 years old. Where exactly is Spy located? It is a village within the municipality of Jemeppe-sur-Sambre, in the province of Namur, Wallonia, situated along the Orneau River. Why was the discovery at Spy so significant? It helped scientifically confirm that Neanderthals were a distinct human species rather than diseased modern humans.
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Lake Warfaaz
Nivezé
Lake Warfaaz is an artificial lake in Wallonia, in the Ardennes region of Belgium, situated right next to the thermal town of Spa. It was formed when a dam was built across the Wayai river in 1892, and it has since become one of the best-known spots in the immediate surroundings of Spa, drawing both locals and visitors exploring this part of the Ardennes. How big is the lake? Lake Warfaaz is modest in scale, covering an area of about 0.08 km² and holding a water volume of roughly 360,000 m³. Despite its compact size, it has functioned as a local tourist draw for well over a century, fitting neatly into the hilly, forested landscape typical of the Ardennes. What can visitors do at Lake Warfaaz? The lake is geared toward outdoor leisure. Pedalo rides are one of the main activities on offer, letting visitors get out onto the water at a relaxed pace. Fishing is another popular pursuit here, appealing to both Spa residents and travelers who come specifically for a few hours by the water. Between the water sports and the fishing, Lake Warfaaz offers something for people looking for light activity as well as those after a quieter afternoon outdoors. Why was the dam built here? The dam across the Wayai was completed in 1892, a piece of 19th-century hydraulic engineering that turned a stretch of river into a retention basin. Projects like this were common in the period, often built to manage water flow and secure a reliable supply for nearby towns. Spa itself was already established as a spa town by then, drawing visitors for its thermal waters, and a water feature so close to the town added another reason for people to stay and explore the surrounding area. Where exactly is Lake Warfaaz located? The lake sits in Wallonia, the French-speaking part of Belgium, right beside Spa — a town whose name became so associated with thermal bathing and wellness that it eventually lent its name to "spas" everywhere. Its setting in the Ardennes means it's surrounded by the rolling hills, forests, and rivers typical of the region, giving the lake a scenic backdrop for the recreational activities it hosts. Frequently asked questions Can you ride a pedalo on Lake Warfaaz? Yes, pedalo boats are one of the main water activities available at the lake. Is Lake Warfaaz natural or man-made? It's an artificial lake, created by damming the Wayai river in 1892. How close is the lake to the town of Spa? Lake Warfaaz is located right next to Spa, making it an easy destination for anyone staying in town. Is fishing allowed at Lake Warfaaz? Yes, fishing is one of the popular activities at the lake.
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Casinoweiher
Kelmis - La Calamine
Casinoweiher Casinoweiher is an artificial pond in Neu-Moresnet, one of the three villages that make up the municipality of Kelmis (La Calamine) in East Belgium, close to the German and Dutch borders. Covering roughly 5 hectares, the pond is today one of the more popular excursion destinations in the region. Where does the name come from and what is the pond's history? The pond was created in 1862 as a dammed reservoir on the Tülje stream. Its original purpose had nothing to do with leisure — the water from the Göhl stream, used to wash the zinc ore extracted around Kelmis, was not sufficient to keep the washing operations running continuously, so an additional retention reservoir was built on the Tülje. The name "Casinoweiher" (literally "Casino Pond") comes from a casino building that once stood on its shore, used by the managerial staff of Vieille-Montagne for their leisure activities. Vieille-Montagne was one of Europe's largest zinc mining and processing companies at the time, and the area around Kelmis lived off zinc-lead ore extraction — known locally as calamine — throughout the 19th century. What can visitors see there today? Together with the neighboring Altenberg spoil heap, the pond is a living record of the area's former mining activity — the site has been fully redeveloped and renatured and is now a protected conservation area. The region is known for its calamine flora: specialized plants such as the calamine violet and calamine pennycress that have adapted to survive in soils heavily loaded with heavy metals. The best time to observe this rare vegetation is between May and September, when the plants are in bloom. Numerous walking paths and hiking trails run around Casinoweiher, fitted with information panels explaining the history of calamine mining and its importance for Kelmis and the surrounding area. The parking area by the pond serves as a convenient starting point for walkers heading out into the surrounding nature. Why is it worth a visit? Casinoweiher brings together several layers of the region's history — its industrial past tied to zinc mining, the leisure heritage of Vieille-Montagne's former management, and its present-day role as a conservation area where nature has reclaimed a site once shaped by mining. It's a place where a quiet walk by the water can be combined with a lesson in Kelmis's industrial history and a look at plant life found in few other corners of Belgium. Frequently asked questions How big is Casinoweiher? The pond covers approximately 5 hectares. When was the pond created? It was built in 1862 as a dam on the Tülje stream, originally to serve the local mining industry. Where does the pond's name come from? From a casino building that once stood on its bank, used by the managerial staff of the Vieille-Montagne company. What else is worth seeing nearby? The neighboring Altenberg spoil heap and its distinctive calamine flora, best seen between May and September.
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Schulensmeer
Herk-de-Stad
Schulensmeer is an artificial lake in the Belgian province of Limburg, situated in the valley of the river Demer on the territory of Herk-de-Stad (sub-municipality Schulen) and Lummen (sub-municipality Linkhout). It takes its name from the village of Schulen, which lies on the road between Hasselt and Diest. It is Flanders' largest man-made lake, roughly 2.8 km long and about 180 m wide, covering close to 94 hectares with around 10 kilometers of accessible shoreline. How did the lake come to be? In the early 1970s, planners needed a site to mine sand for the construction of the E314 motorway between Lummen and Aarschot. At the same time, a retention basin was being planned in the nearby Schulensbroek to help manage the waters of the Demer. Combining both needs meant agricultural land only had to be sacrificed in one location, and the sand extraction that shaped the lake basin took place in 1976. Before that, the area was an extensive floodplain that was submerged several times a year during river floods. What feeds the lake? The Demer is the lake's main water source, but the same valley also carries several other streams: the Mangelbeek, Zwarte Beek, Herk, Gete, Velpe and Begijnenbeek. This makes Schulensmeer an important buffer basin, absorbing excess water during periods of high river levels in the region. How deep is the lake? Depths in Schulensmeer reach up to about 7 meters in places, with the lakebed varying across different sections of the water body — a factor that matters both for its ecology and for anyone practicing water sports here. What can visitors do at the lake? Over the years Schulensmeer has developed into a multi-activity recreation site. Sailing, windsurfing and kayaking are all practiced on the water, and fishing is permitted during daytime hours. Anglers can catch species such as bass, bream, whitefish, carp, catfish, eel, roach, pike-perch, pike and tench. Walking and cycling routes circle the lake, allowing visitors to explore the surrounding nature at their own pace. What surrounds the lake? The lake forms part of the roughly 200-hectare Schulensbroek nature reserve, which preserves the Demer's former floodplain. A visitor center dedicated to the lake and its ecology operates nearby, offering more information on how the lake was created and on ongoing conservation work, including the LIFE Delta project. Frequently asked questions Is Schulensmeer a natural lake? No, it is an artificial lake created in 1976 through sand extraction combined with the construction of a retention basin for the river Demer. Where exactly is the lake located? In the western part of Limburg province, across the municipalities of Herk-de-Stad (Schulen) and Lummen (Linkhout). Can you fish here? Yes, fishing is allowed during the day, and the lake holds species such as pike, pike-perch, carp and catfish. How big is the lake? About 94 hectares in surface area, roughly 2.8 km long and 180 m wide, with depths reaching around 7 meters.
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Kleine Geul
Assenede
Kleine Geul is a small creek — a former water arm typical of the coastal polder landscape of Flanders — located in the municipality of Assenede, in East Flanders, within the Meetjesland region. It sits right at the heart of the local krekengebied, a network of historic creeks that gives this corner of Belgium its distinctive flat, water-laced character. Where did Kleine Geul come from? The creek originated in the 15th and 16th centuries as a side branch of a larger watercourse, the Vliet. When the Nicasiuspolder dyke was built between 1519 and 1520, Kleine Geul was cut off from its parent channel and absorbed into the polder system. Since then it has functioned as a self-contained, closed body of water rather than part of an active river system — which explains its calm, still character today. What does it look like today? Kleine Geul lies just south of its larger counterpart, Grote Geul, together forming part of the wider creek network around Assenede. Its banks are lined with a relatively species-poor reed fringe, typical of this kind of standing water within a polder. The entire creek is now used as a fishing pond, making it a spot visited mainly by local angling enthusiasts rather than by mass tourism. Why is the area protected? Part of the area where Kleine Geul is located falls under European protection as part of the Natura 2000 site "Polders" (code BE2500002). The Assenede krekengebied as a whole is considered a landscape and ecologically valuable part of the Meetjesland region: the mosaic of creeks, polders and farmland provides important habitat for waterfowl and wetland vegetation. How to explore the surroundings? Kleine Geul itself has no dedicated visitor infrastructure — it's best understood as one piece of the broader creek landscape around Assenede, which is best explored on foot or by bike. Walking routes in the area trace the network of creeks, linking Grote Geul, Kleine Geul and other former water branches, offering a way to see how centuries-old hydraulic engineering shaped today's landscape. Frequently asked questions Is Kleine Geul a river or a lake? Technically it's a creek — a former water arm now cut off from the main river system and functioning as a closed body of water within a polder. Can you fish there? Yes, the entire creek is used as a fishing pond. Is the surrounding area protected? Part of it belongs to the Natura 2000 site "Polders" (BE2500002), underlining the ecological value of this landscape. What else is worth seeing nearby? The neighbouring, larger Grote Geul creek and the rest of the Assenede krekengebied, together forming a network of walking routes through the region's historic water landscape.
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Rode Geul
Assenede
Rode Geul is a small yet remarkably scenic creek located in the municipality of Assenede, in East Flanders, right in the heart of the tidal-creek landscape known as the Meetjesland kreken. Covering only around 10 hectares, it punches well above its size when it comes to natural and historical interest. Where does this creek come from? Rode Geul is a remnant of a former tidal branch of the river Vliet, an inlet that took shape in the 15th and 16th centuries when seawater regularly flooded these low-lying lands during storms and high tides. When the surrounding Rode Polder was diked and drained in 1555, this particular creek survived intact, left behind as a living trace of the area's older, water-shaped landscape amid what is now farmland and pasture. Why is it called "Rode Geul"? The name of the creek, shared with the neighboring Rode Polder, refers to the distinctive reddish-brown tint of its water. That color comes naturally from iron compounds dissolved in the ground and surface water, giving the creek and its surroundings a rusty hue that is especially noticeable when water levels are low. Where exactly is it situated? Rode Geul lies as an extension of the larger Grote Geul creek, separated from it by an embankment known as the Sint-Nicasiusdijk. The two creeks are roughly similar in length, but Rode Geul stands out for being far more secluded. Unlike many other water bodies in the region, the land around it remains privately owned and is not open for public access — which, somewhat paradoxically, is exactly what makes it so valuable ecologically. What role does it play for nature? Precisely because of its restricted access and the near-total absence of human interference, Rode Geul has become a genuine refuge for wildlife. Undisturbed aquatic and bankside vegetation, calm waters, and a setting far from foot traffic make it attractive to numerous species of waterfowl and marsh birds, as well as small fauna typical of creek ecosystems. It is this combination of rare plant communities and rich small-animal life that makes Rode Geul one of the more valuable natural fragments of the Meetjesland landscape. Can visitors explore it? The creek itself, being private land, cannot be entered directly. However, its surroundings can be appreciated from nearby walking routes — this area is crossed by stage 22 of the long-distance Grenslandpad trail, which runs between Boekhoute and Sas van Gent. Hikers following this route pass through the characteristic creek landscape of Assenede, including the vicinity of Rode Geul, without setting foot on the private grounds themselves. Frequently asked questions Is Rode Geul a lake? No — it is a creek, meaning it is the remnant of a former tidal inlet rather than an artificially created body of water. Why does the water look reddish? The color comes from iron compounds present in the water, which give it its characteristic rusty tint — hence the name "Rode" (red). Can you walk into the creek area? No, the land is privately owned and not open to the public. The surroundings can only be viewed from nearby trails such as the Grenslandpad. How large is Rode Geul? It covers roughly 10 hectares, similar in length to the neighboring Grote Geul, from which it is separated by the Sint-Nicasiusdijk embankment. What makes this place ecologically valuable? Its isolation and the absence of human disturbance have allowed rare plant species to survive and created a haven for birds and small wildlife.
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Zillebekevijver
Ypres
Zillebekevijver is a 28-hectare lake sitting right beside the village of Zillebeke, part of the municipality of Ypres in Belgium's West Flanders province. Found at coordinates 50.83722, 2.91, it's a quiet corner of the flat Flemish countryside where water, woodland and layers of history come together — a spot visited both by locals and by travellers passing through Ypres in search of a break from the town centre. How did this lake come to exist? The lake isn't entirely a natural feature — it was formed by damming the valley of the Zillebeek stream. Ponds around Ypres were already being built in the 13th century, created to supply the town with drinking water, to support the booming cloth industry, and to feed the town's canals. Zillebekevijver took on its present shape toward the end of that century, once the valley was closed off by a dam. As early as 1217, records mention five ponds in the area around Ypres, a network that was adjusted and reworked over time as the town's needs changed. Does the lake still serve its original purpose? It does, and in a very concrete way. In the early 14th century, a second pond of similar design was built at Dikkebus, alongside Zillebeke — both intended to supply Ypres with drinking water. That role hasn't disappeared: a pumping and purification station on the western bank of Zillebekevijver still produces roughly four to five thousand cubic metres of drinking water every day. It's unusual for medieval water infrastructure to still be doing real work for a modern town, and that continuity is part of what makes this lake worth a second look. What is the lake's connection to the First World War? The countryside around Ypres is among the most heavily marked by war in Europe, and the area around Zillebekevijver is no exception. During the First World War, the path running along the lake's shore was used by troops moving up toward the front line. Right next to it lies Bellewaerde Ridge, a strategically important high point fiercely contested during the war. Walking the same path today, it's hard not to think about the columns of soldiers who passed this way more than a century ago. What can visitors do at Zillebekevijver today? The lake and its surroundings are mostly a destination for a quiet walk or bike ride. A route circles the water and continues through the surrounding woods, including the area of the former Bellewaerde Ridge. The place carries several layers at once — practical water infrastructure that has served the town for centuries, a calm lake-and-forest landscape, and the weight of wartime history that is never far away anywhere around Ypres. Where exactly is Zillebekevijver located? The lake lies next to the village of Zillebeke, part of the municipality of Ypres in West Flanders province, western Belgium. It's fed by the Zillebeek stream, from which it takes its name. Its location makes it an easy stop both for people exploring Ypres itself and for those wanting to spend more time among the surrounding battlefield sites and the rural landscape of West Flanders. Frequently asked questions How big is Zillebekevijver? The lake covers roughly 28 hectares. Is the lake's water still used today? Yes — a pumping and purification station on the western bank produces several thousand cubic metres of drinking water a day for Ypres. When was the lake created? Pond-building around Ypres began in the 13th century, and Zillebekevijver took its current shape near the end of that century, after the Zillebeek valley was dammed. What is its link to the First World War? The path around the lake was used by troops heading to the front, and the nearby Bellewaerde Ridge was a key strategic position during the fighting.
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Dikkebusvijver
Ypres
Dikkebusvijver is an artificial lake located right next to the village of Dikkebus, a few kilometers southwest of Ypres (Ieper) in the Belgian province of West Flanders. Covering roughly 36 hectares, it ranks among the larger bodies of water in this part of the region and was formed by damming the Kemmelbeek stream. How did this lake come to be? The story of the reservoir goes back to the Middle Ages. Permission to dig it was granted by the Count of Flanders on 23 July 1310, with the aim of securing enough water for the cloth industry in Ypres, at the time one of Europe's leading textile centers. Acquiring the necessary land took around ten years, and the whole project was completed and fully operational by about 1323. From the very start, the lake served a clearly practical, economic purpose tied to the city's needs. How did the lake supply the city with water? For centuries, Dikkebusvijver served as the main source of drinking water for Ypres. Water initially reached the city through urban waterways and channels, and this system was later replaced by wooden pipelines capable of carrying water over greater distances. It wasn't until 1926 that a modern pumping station was built, modernizing the entire distribution process. Remarkably, the reservoir still fulfills this supply role today — water from Dikkebusvijver continues to feed into the drinking water network of Ypres, though this function is now accompanied by a far more prominent recreational role. What can visitors do at Dikkebusvijver today? Today the lake is primarily known as a popular recreation spot for both locals and visitors. A quiet walking path and a cycling route, lined with oaks and poplars that provide shade on warmer days, circle the reservoir. The best-known hiking route is a loop of roughly 6.4 km (4.0 miles) that follows the perimeter of the central pond — an easily accessible trail suitable for most visitors regardless of fitness level. The area draws cyclists, runners, and anyone looking for a quiet escape from the busier center of Ypres. Are there World War I remnants nearby? Yes — the surroundings of Dikkebusvijver, like much of the region around Ypres, carry visible traces of the First World War. Nearby, on the grounds of Kemmelberg, four concrete bunkers from that era have survived, built in the spring of 1917 by British soldiers. They stand as a reminder of the intense fighting that took place across this part of West Flanders and attract visitors interested in the region's military history. Is Dikkebusvijver worth a visit? Dikkebusvijver brings together several layers of interest at once: a site with centuries of economic history, a still-active piece of the city's water infrastructure, a popular destination for walks and bike rides, and a place connected to the legacy of the First World War. For anyone exploring Ypres, it offers a calm alternative to the busier town center — a spot where nature and local history meet. Frequently asked questions How large is Dikkebusvijver? The reservoir covers approximately 36 hectares. When was the lake created? Permission to build it was granted in 1310, and it became fully operational around 1323. Is the lake's water still used today? Yes, Dikkebusvijver still supplies Ypres with drinking water, although its recreational role is now equally important. How long is the walking route around the lake? The most popular loop around the reservoir is about 6.4 km (4.0 miles) and is accessible to most visitors.
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Grote Geul
Assenede
Grote Geul is a "kreek" — a creek left behind by historic sea floods — located in the Belgian municipality of Assenede, in the Meetjesland region of East Flanders. Covering roughly 14 hectares, it winds for more than two kilometres through the surrounding polder land, forming one of the defining features of the so-called krekengebied, the creek area around Assenede. Where did this creek come from? Grote Geul began life as a side branch of the river Vliet during the 15th and 16th centuries, at a time when storm surges and tidal floods regularly reshaped this low-lying coastal landscape. Its present form dates back to the diking of the Nicasiuspolder in 1519–1520, when the creek was cut off from the main course of the Vliet and became a self-contained body of water, fed partly by fresh water and partly by brackish seepage rising from below ground. What can visitors see here today? Although the land remains privately owned, it has been leased and managed by the nature organisation Natuurpunt since 1957, which has turned Grote Geul into a functioning nature reserve. The landscape is shaped by pollarded willows — trees traditionally pruned into a distinctive rounded crown — alongside extensive reed beds and wet alder woodland. The mix of fresh and brackish water supports salt-tolerant plant species that are unusual to find so far inland. Why does the reed here matter historically? For centuries, the reed growing along the banks of creeks in this region served a practical purpose: it was harvested for thatching roofs and used as a natural windbreak to protect crops from erosion. Grote Geul, together with the neighbouring Rode Geul and the twin creeks Grote Kil and Kleine Kil, ranks among the most significant of these creeks in the area around Assenede. How can you explore Grote Geul? The creek area around Assenede, including Grote Geul, is accessible via marked walking trails that lead through the polder landscape. Walking along the creek lets visitors take in its calm, wide stretch of water framed by the region's characteristic wetland vegetation, and, in the breeding season, spot waterbirds that favour the reed beds and alder groves. Frequently asked questions Is Grote Geul a lake? No — it is a "kreek," a remnant of a former tidal inlet shaped by centuries of flooding, rather than a conventional lake. Is the site open to the public? The creek itself remains privately owned, but it has been managed by Natuurpunt since 1957, and surrounding footpaths allow visitors to take in the landscape from a respectful distance. What sets Grote Geul apart from other creeks in the region? Its size (14 hectares) and length of over two kilometres, along with its unusual mix of fresh and brackish water, which supports rare salt-loving plant life this far inland. Where does the name krekengebied come from? It refers to the whole cluster of creeks around Assenede, which besides Grote Geul includes Rode Geul, Grote Kil and Kleine Kil — all formed in a similar way through historic floods and polder embankments.
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Gezusterskreken
Assenede
Gezusterskreken is a pair of intersecting waterways, the Grote Kil and Kleine Kil, located in the northern part of the municipality of Assenede in East Flanders, within the Meetjesland region of Belgium. A dam separates the two branches, carrying the Gezustersstraat road across it — which is where the combined name of the site comes from. How did these creeks come to be? These channels aren't natural in the strictest sense: they're remnants of former tidal gullies that were left behind once the surrounding polder land was drained and diked. The turning point came in 1612, when the Scheurhoekdijk was raised, enclosing the area now known as Sint-Albertpolder. Further polders followed in 1663 and 1690, and as a result the Scheurhoekdijk lost its role as the main line of sea defense — the water retreated further north. Today that historic dike marks the border between Belgium and the Netherlands, while the old tidal channels, cut off from the sea, remained as a network of inland creeks, Gezusterskreken among them. Why is the area worth a visit? The landscape around Gezusterskreken is classic Meetjesland polder country: flat, open fields threaded with ribbons of water, dikes, and small stands of trees. Wetlands of this kind, tucked into former coastal polders, tend to carry real ecological value, and this stretch is no exception — it's protected as part of the Natura 2000 network, covering both the Habitats Directive and the Birds Directive. Management is shared between nature conservation bodies and private landowners, a common arrangement in Belgian polder areas where conservation and agricultural land use sit side by side. What else is nearby? Gezusterskreken sits close to other creeks of the same tidal origin — the Rode Geul and Grote Geul, considered the largest in the region — while the Grote Kil and Kleine Kil extend the pattern further, together forming a broad mosaic of water and land. This combination of channels, dikes, and damp meadows draws birdwatchers as well as anyone simply looking for a quiet, open landscape away from built-up areas. How best to explore it? The area is best explored on foot or by bike: the flat terrain and network of local roads along the dikes make it well suited to long walks or cycling trips through Meetjesland. Spring and summer bring the most bird activity along the meadows and creek edges, though the landscape's core appeal — stillness, open space, sky reflected in water — holds up in any season. Frequently asked questions What's the difference between Grote Kil and Kleine Kil? They're two branches of the same former tidal channel, separated by a dam that carries the Gezustersstraat — together they make up the Gezusterskreken complex. Is the area protected? Yes, it forms part of the Natura 2000 network, covered by both the Habitats Directive and the Birds Directive. Where did the creeks come from? They're remnants of tidal channels that predate the diking of the polders, starting with the Scheurhoekdijk built in 1612. Does the Scheurhoekdijk still serve as a sea defense? Not in its original role — after later polders were added in the 17th century it lost its function as the main line of sea defense, and today it marks the Belgium-Netherlands border.
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Damvallei
Destelbergen
Damvallei is a nature area of more than one hundred hectares straddling the municipalities of Destelbergen and Laarne in East Flanders, Belgium, and forming part of Nationaal Park Scheldevallei. The site developed from the silting-up of former meanders of the river Scheldt, which gave rise to a low-lying peat landscape now bordered by wet meadows and reedbeds. The area sits at roughly 51.05°N, 3.82°E. What makes Damvallei protected? Damvallei is safeguarded as part of the European Natura 2000 network, within the designated site covering the Scheldt and Durme estuary from the Dutch border to Ghent. Management of the area is handled by the nature conservation organisation Natuurpunt vzw, which has carried out long-term restoration work to preserve the site's wetland habitats. What kind of wildlife can visitors expect? The area is known for its exceptional diversity of dragonflies and damselflies — a 2006 survey recorded twenty-eight species here, including several considered rare at a regional level. Damvallei is also home to around one hundred spider species, among them the heavily threatened marsh pajama spider. Its waters shelter rare and endangered fish such as the weatherfish and the bitterling. Birdlife is one of the area's main draws. Overlooking the Damvalleimeer, the main body of water within the site, a bird hide gives visitors a view over the many ducks that overwinter there — a spectacle that becomes especially striking during frosty spells, when birds concentrate on the remaining unfrozen patches. From the same hide, ospreys can be observed from late April onward raising their young on purpose-built breeding platforms, while the resident cormorant colony grows larger every year. How can visitors plan a walk through Damvallei? Several marked walking routes cross the site, leading through flower-rich meadows and past the results of ongoing conservation management. The main route, the Bergenmeersenpad, is a 6-kilometre trail that can be shortened to 3 kilometres, starting near the town hall of Destelbergen along the N445 road. Two bird hides are positioned along the route, allowing visitors to watch wading birds on the shallow waters. The area is freely accessible year-round, though only the stretch running alongside the Damvalleimeer is suitable for wheelchairs and strollers. Sturdy walking shoes are recommended on the remaining paths, which can be wet and uneven. Frequently asked questions Where exactly is Damvallei located? The area lies on the border between the municipalities of Destelbergen and Laarne in the province of East Flanders, Belgium, right next to Ghent. Is there an entrance fee? No, the area is freely accessible to visitors throughout the year, with no admission charge. When is the best time for birdwatching? In winter, when large numbers of ducks gather on the Damvalleimeer, and from late April, when ospreys raise their young on the breeding platforms. Is the route suitable for families with strollers? Only the path along the Damvalleimeer is suitable for wheelchairs and strollers — the other paths require sturdy footwear.
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waterfall of Chaudière
Sougné-Remouchamps
The waterfall of Chaudière is one of the best-known cascades in the Belgian Ardennes, tucked into a wooded gorge along the Ninglinspo, a tributary of the Amblève river, close to the village of Sougné-Remouchamps in the municipality of Aywaille (Liège province). Water drops roughly ten metres over a rocky ledge, forming a small natural pool at its base. Where does the name come from? The French word "chaudière" means kettle or cauldron, and the name refers to the shape of the rock basin where the water swirls after tumbling over the ledge, evoking a boiling pot. This kind of descriptive naming is common across the Ardennes, where geographic features are often named directly after their appearance. Can you swim here? Yes — at the foot of the falls lies a small, cool pool locally known as the "bain de Diane" (Diana's bath). The Ninglinspo's water stays clear but cold even in summer, since the river runs through dense forest shade and is fed by numerous springs along its course. It's a popular spot to cool off during a hike, though the rocky, sometimes slippery riverbed calls for caution. How do you get to the waterfall? The falls sit along a walking trail that follows the Ninglinspo valley, one of the most visited hiking routes in this part of the Ardennes. A popular loop of about 9.7 km (6 miles) starts in Sougné-Remouchamps and links the Chaudière waterfall with nearby natural rock pools known as "Venus' bath." The path is narrow and stony along the riverbank, occasionally requiring hikers to cross stepping stones or footbridges, making it more demanding than a flat stroll, though still manageable for anyone with average fitness. What else is there to see along the way? The Ninglinspo valley is known for its wild, almost mountainous character: the river winds between boulders, forming small cascades, eddies and rocky steps along its entire course, not just at the main waterfall. The dense deciduous forest lining the riverbed provides natural shade in summer, while autumn foliage adds an extra layer of colour to the scenery. The wider area around Aywaille and Sprimont offers additional viewpoints and trails, making it easy to combine a visit to the Chaudière with a longer day out in the region. Who is this destination for? The waterfall of Chaudière appeals both to families looking for an easy, scenic walking destination and to more experienced hikers planning a full day along the Ninglinspo valley. Because of the rocky, uneven stretches of trail, sturdy hiking shoes are recommended, especially for those continuing on to Venus' bath. Frequently asked questions Is the Chaudière waterfall easy to reach? Reaching it requires walking part of the riverside trail over partly rocky, uneven ground — it's not a spot you can drive straight up to. How high is the waterfall? The water falls roughly ten metres. Are there other attractions nearby? Yes, the natural rock pools known as Venus' bath lie close by, and the whole Ninglinspo valley is dotted with smaller cascades and rock formations. When is the best time to visit? Summer is ideal for swimming, though autumn brings extra charm to the valley thanks to the colours of the foliage.
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waterfall of Reinhardstein
Ovifat
The Waterfall of Reinhardstein is regarded as Belgium's highest cascade, tucked into the Warche river valley right below the walls of Reinhardstein Castle, in the village of Ovifat within the municipality of Robertville, Liège province. The water drops roughly 60 metres down a steep, moss-covered rock face, forming a narrow, ribbon-like cascade rather than a broad, thundering torrent. Dense ancient forest wraps around the ravine, so visitors rarely get to see the entire drop from a single vantage point — the falling water reveals itself in glimpses between tree trunks and rocky outcrops. Where exactly is the waterfall located? The site sits within the Hautes Fagnes (High Fens) region, in the German-speaking Community of Belgium, close to the German border. The Warche valley cuts deep into rugged terrain here, and it was on this same rocky ground that Reinhardstein Castle was built in the Middle Ages — its walls still loom over the valley directly above the cascade. What does the cascade look like? Unlike broad, gently sloped waterfalls found elsewhere, Reinhardstein's drop follows a near-vertical rocky channel. The water pushes through rock ledges and tangled tree roots, breaking into several smaller steps rather than falling in one even sheet. The damp, shaded surroundings, with moss clinging to every rock, give the spot an almost fairy-tale atmosphere, especially in spring when snowmelt pushes the water level to its highest. Is it worth combining with another nearby attraction? Yes — close by, near the village of Longfaye, sits the Bayehon waterfall, about nine metres high and considered Belgium's second-largest. Many visitors combine both sights into a single walking route through the Warche valley and the forests surrounding the Hautes Fagnes plateau. How do you get to the waterfall? Access is via a hiking trail that descends into the valley from the area around Reinhardstein Castle. The path can be rocky and slippery, particularly after rain, so sturdy, grippy footwear is recommended. The walk itself is short, but it crosses uneven forest terrain, so it isn't a route suited to those looking for fully paved paths. Frequently asked questions Can you see the waterfall from the castle? Partially — some viewpoints near the castle offer a glimpse of the cascade further down the valley, but a full view requires following the trail closer to the riverbed. Is this really the highest waterfall in Belgium? Yes, the Waterfall of Reinhardstein is considered the country's highest, with a drop of around 60 metres. Are there other waterfalls worth seeing nearby? Yes, a few kilometres away near the village of Longfaye lies the Bayehon waterfall, Belgium's second-largest, with a height of about nine metres. When is the best time to visit? Spring, after the snow has melted, and after periods of heavy rain, when the Warche river's flow is strongest and the cascade at its most dramatic.
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VVV-toren
Tessenderlo
VVV-toren is a metal lookout tower in Tessenderlo, standing on the Zandberg (Sand Hill) — an old sand dune at the heart of the Gerhagen nature park. The tower rises 18.75 meters, and a spiral staircase of 100 steps leads visitors to the top. Where does the name come from and what is the tower's history? The name VVV-toren refers to the former local tourism organisation VVV-Tessenderlo, which from the 1960s onwards developed the area around the Zandberg into a tourist hub. That period saw the creation of the Ter Scoete café, the Forest Museum (Bosmuseum), walking and horse-riding paths, and rest benches. The first lookout tower was built on the dune in 1969 and was a concrete structure. Over time the concrete deteriorated and suffered from concrete rot, so the tower was demolished towards the end of the 1990s. In 1999 a new tower was erected on the same spot — a metal construction, taller than its predecessor, which is the one still standing today. What can you see from the top? From the viewing platform, at a height of almost 19 meters, visitors get a wide panorama over the Gerhagen forests and the surrounding Kempen landscape. On a clear day the view extends to the mining terrils of Beringen, the abbey of Averbode, and even the basilica of Scherpenheuvel in the distance. On April 11, 2014, a telescope was installed on the platform to help visitors pick out these distant landmarks. What else is there to see around the tower? The VVV-toren sits at the heart of the Gerhagen nature park, surrounded by forest and the sandy hills typical of the Kempen region. At the foot of the tower there is a playground, making it a popular stop for families. Nearby is the Forest Museum mentioned above, along with a network of marked walking and cycling routes running through the park. Frequently asked questions How tall is the VVV-toren? The tower is 18.75 meters high, with the viewing point situated at roughly 19 meters above ground. How many steps are there to the top? A spiral staircase of 100 steps leads to the viewing platform. Is today's tower the same one built in the 1960s? No. The original concrete tower dates from 1969, but it was demolished towards the end of the 1990s after the concrete deteriorated. In 1999 it was replaced by a newer, taller metal tower. What can you see from the viewing platform? A panorama of the Gerhagen forests, and on clear days the mining terrils of Beringen, the abbey of Averbode, and the basilica of Scherpenheuvel — made easier to spot thanks to the telescope installed in 2014. Is there anything for children near the tower? Yes, there is a playground right at the base of the tower.
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Spioenkop
Wenduine
Spioenkop is a distinctive white pavilion with a red roof standing atop one of the highest dunes on the Belgian coast, in Wenduine — the seaside district of the municipality of De Haan. At 31 meters, the dune is the second highest along the entire Belgian coastline, trailing "De Hoge Blekker" in Koksijde by just two meters, which makes Spioenkop one of the most recognizable viewpoints on the Flemish coast. Where does the name come from? The name refers to the Battle of Spion Kop, fought in January 1900 during the Second Boer War in the Natal province of South Africa, where Boer farmers won a victory over British forces. The dune in Wenduine had already been used as a strategic observation point since 1770, and the name "Spioenkop" was later adopted for this location precisely because of its watch-post function, echoing the famous battle on the other side of the world. What is the history of the pavilion? The first observation pavilion on top of the dune was built in March 1902. During the First World War, the German occupying forces set up a reinforced observation post here, underlining the hill's military significance. After the war, in 1922, the structure was rebuilt with a slate roof. The current pavilion, made of concrete and brick, dates from 1955, and it is this version — known today as Le Pavillon Elisabeth — that visitors see when they climb the dune. The building is a protected heritage monument and is considered one of the most famous dune pavilions on the Belgian coast. What can you see from the top? From the viewing terrace, visitors enjoy a wide, nearly 360-degree panorama that takes in the North Sea, the surrounding coastal dunes, and the flat polder landscape further inland. It is precisely this combination — coastline on one side, open countryside on the other — that has drawn walkers and visitors here for decades in search of the best vantage point over the area. How do you get to the top? Several footpaths lead up the dune, along with a staircase built directly into the slope. The route is also accessible to wheelchairs and strollers, though the steep climb requires more effort than a stroll along the seafront promenade. At the foot of the dune lies De Rotonde, a popular gathering spot for sunbathers, anglers, and boules players, making the area around Spioenkop appealing both to those chasing a view and to those who prefer to relax lower down, closer to the lively seafront. Frequently asked questions Is it free to visit the Spioenkop? Yes, access to the pavilion and the viewpoint is free — it is a public walking area within the Wenduine dunes. Is it accessible with a stroller or wheelchair? Yes, the path can be used with strollers and wheelchairs, though the steep section leading up may require extra assistance. Where does the name Spioenkop come from? It refers to the Battle of Spion Kop, fought in 1900 during the Second Boer War in South Africa — the local dune took on this name because of its historical role as a watch and observation post. How old is the current pavilion? The building standing on the dune today dates from 1955, although the site's history as an observation point goes back to the late 18th century.
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National Park Bosland
Lommel
National Park Bosland is a vast wilderness area in the north of the Belgian province of Limburg, spread across the municipalities of Hechtel-Eksel, Lommel and Pelt. The site was officially designated a national park in 2023 — the first of its kind in Flanders — and currently covers roughly 6,500 hectares. Authorities plan to keep expanding the protected area, with the goal of surpassing 10,000 hectares within a few years. What does the landscape of Bosland look like? What sets Bosland apart is the sheer variety of landscapes packed into a relatively compact area. Visitors move from wet marshes and heathland to dry, sandy dunes, and from open, sunlit clearings to dense pine and mixed forests. This mosaic of habitats makes the park unusually rich in plant and animal species, and each season reveals a different face of the terrain — from blooming heather in late summer to winter mist drifting over the bogs. Why have wolves returned to Bosland? The park's biggest natural draw is its wild wolf pack — the only one permanently established anywhere in Flanders. The predator's return, after decades of absence from the region, is widely seen as a sign that the ecosystem is recovering and that a natural balance is being restored to the local food chain. Spotting tracks, signs or howls of the wolves (direct sightings remain rare) has become one of the reasons nature lovers and tourists are increasingly drawn to this corner of Limburg. What can visitors do in the park? Bosland was designed so that nature conservation and visitor experience go hand in hand. An extensive network of trails supports walking, cycling and longer hiking routes across sandy paths and forest tracks. The trails pass through the park's most distinctive stretches — heathland, inland dunes and old pine stands — giving visitors a full cross-section of northern Limburg's landscapes. Because the park spans three neighbouring municipalities, it's easy to plan longer routes that link different parts of the protected area. Why is Bosland worth visiting? Bosland combines raw, untamed nature with a level of visitor accessibility rarely found in protected areas of this size. In a single day, it's possible to pass through several completely different ecosystems without straying far from civilisation. For nature enthusiasts, its status as "the only place in Flanders with a wild wolf pack" makes it a genuinely unique spot on Belgium's map, and ongoing plans to expand the protected area suggest its ecological importance will only keep growing. Frequently asked questions Where exactly is National Park Bosland located? The park lies in the northern part of Limburg province, across the municipalities of Hechtel-Eksel, Lommel and Pelt, close to the border with the Netherlands. Can you encounter wolves in the park? Bosland is home to the only wild wolf pack in Flanders, though direct encounters are rare since the animals avoid contact with people. How large is the park? Currently around 6,500 hectares, with plans to expand to more than 10,000 hectares in the coming years. What activities are available in Bosland? The park offers walking and cycling trails through heathland, dunes and forests, suitable for visitors of different fitness levels.
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Scheldt Valley National Park
Waasmunster
Scheldt Valley National Park (Nationaal Park Scheldevallei) is a Belgian national park stretching along the River Scheldt between Ghent and Antwerp, covering parts of the East Flanders and Antwerp provinces. It received official national park status in 2023, after its application for recognition as one of Flanders' national parks was approved. The town of Waasmunster sits right on its edge and serves as one of the convenient starting points for exploring the area. What kind of landscape does the park protect? The park covers roughly 8,000 hectares and is the result of centuries of interaction between people and nature — the Scheldt has shaped the surrounding land for generations, while local communities adapted to the river by building polders, sluices and flood defences. The outcome is a dynamic floodplain landscape where meadows, forests, marshes and wetlands sit alongside farmland and picturesque villages. One especially distinctive feature is the river's tidal character, a rarity in this part of Europe, producing mudflats and salt marshes (known locally as "schorre") along parts of the waterway. What sub-areas make up the park? The park is divided into seven smaller sub-areas, each with its own natural and scenic character. These include the Kruibeke polders, the Durme and Dam valley, the Kalkense Meersen meadows together with Lake Donkmeer, the Klein-Brabant region, the surroundings of the town of Dendermonde, and the so-called Rupelstreek along the River Rupel. This variety means the park encompasses everything from wide open wetland meadows to more wooded stretches and typically agricultural land, all within a single protected area. What can visitors do around Waasmunster? A circular walking trail leads from the centre of Waasmunster towards Lokeren, taking visitors through a varied stretch of the park's landscape, from open fields to more wooded sections of the valley. Starting points along the route are easy to reach both by car and by public transport, making Waasmunster a practical base for people exploring the park without their own vehicle. Across the wider park, an extensive network of walking and cycling trails connects historic castles, wetland meadows and riverside forests. What makes this park stand out among protected areas in the region? The Scheldt Valley National Park's distinctiveness lies in the way its natural richness sits alongside clear traces of human history — castles, villages and old water-management systems coexist here with habitats that are valuable from a nature-conservation perspective. The tidal, brackish character of parts of the floodplain makes this ecosystem uncommon at a continental scale, adding further ecological and scientific significance to the whole area. Frequently asked questions Where is Scheldt Valley National Park located? It stretches along the River Scheldt between Ghent and Antwerp, across the provinces of East Flanders and Antwerp, including the area around the town of Waasmunster. Since when has this area held national park status? It gained this status in 2023, when its application for official recognition was approved. How big is the park? It covers an area of around 8,000 hectares. Can you start a hike directly from the centre of Waasmunster? Yes, a circular trail leads from Waasmunster towards Lokeren, with starting points reachable on foot, by car or by public transport.
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