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Warche
The Warche is a river in eastern Belgium (province of Liège). From its source at Losheimergraben on the Belgian-German border, it flows roughly west about , across the south of the Hautes Fagnes region. It passes through the town of Malmedy, and the artificial lakes of Robertville and of Bütgenbach are formed by dams on the Warche. It is a right tributary of the river Amblève, which it joins east of Stavelot. In the past the Warche used to flow northward from Bévercé, following the current Trô Maret valley, to continue through the current Eau Rouge valley. This last valley is much larger than can be expected from such a small flow, still representing the original Warche valley. In that time the Warche confluenced with the Amblève at Stavelot. Later on, probably during the last ice age the Warche adopted its current position, flowing through the Malmedy graben. References eastbelgium.com: « sentier de découverte » dans la vallée de la Warche(in French French (fre ...
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Warche - Malmedy
The Warche is a river in eastern Belgium (province of Liège (province), Liège). From its source at Losheimergraben on the Belgian-Germany, German border, it flows roughly west about , across the south of the Hautes Fagnes region. It passes through the town of Malmedy, and the artificial lakes of Lake Robertville, Robertville and of Bütgenbach are formed by dams on the Warche. It is a right tributary of the river Amblève (river), Amblève, which it joins east of Stavelot. In the past the Warche used to flow northward from Bévercé, following the current Trô Maret valley, to continue through the current Eau Rouge valley. This last valley is much larger than can be expected from such a small flow, still representing the original Warche valley. In that time the Warche confluenced with the Amblève at Stavelot. Later on, probably during the Wisconsin glaciation, last ice age the Warche adopted its current position, flowing through the Malmedy graben. References eastbelgium.com ...
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Malmedy
Malmedy (; german: Malmünd, ; wa, Måmdiy) is a city and municipality of Wallonia located in the province of Liège, Belgium. On January 1, 2018, Malmedy had a total population of 12,654. The total area is 99.96 km2 which gives a population density of 127 inhabitants per km2. The municipality consists of the following districts: Bellevaux-Ligneuville, Bévercé (including the hamlets of Baugnez and Xhoffraix), and Malmedy. Under the complex administrative structures of Belgium, which has separate structures for territorial administration and for language community rights, Malmedy is part of Wallonia and of the French Community of Belgium. But since it has a German speaking minority, it is one of Belgium's municipalities with language facilities (or "municipalities with facilities"). Malmedy and Waimes are the two municipalities in the French-speaking part of Wallonia with facilities for German speakers. The population of Malmedy is approximately 95% French speakers a ...
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Lake Robertville
Lake Robertville is an artificial lake located in Wallonia near the city of Malmedy in Belgium. The water volume is 8,000,000 m³ and the area is 0,62 km². The lake is located in the High Fens park. The dam on the river Warche was built in 1928. Lake Robertville is situated in the municipality of Waimes Waimes (; german: Weismes, ; wa, Waime) is a municipality of Wallonia located in the province of Liège, Belgium. On January 1, 2006, Waimes had a total population of 6,728. The total area is 96.93 km2 which gives a population density of 6 .... It is named after the village of Robertville. {{DEFAULTSORT:Robertville Ourthe basin Reservoirs in Belgium Lakes of the Ardennes (Belgium) Lakes of Liège Province Lake Robertville Reservoirs in the Eifel ...
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Rivers Of Belgium
These are the main rivers of Belgium. All of Belgium is drained into the North Sea, except the municipality of Momignies (Macquenoise), which is drained by the river Oise into the English Channel. Rivers that flow into the sea are sorted alphabetically. Rivers that flow into other rivers are sorted by the proximity of their points of confluence to the sea. Some rivers (e.g. Moselle, Rhine, Seine) do not flow through Belgium themselves, but they are mentioned for having Belgian tributaries. They are given in ''italics''. Below, the Belgian rivers are given alphabetically. See also :Rivers of Belgium. If the names are different in French, Dutch or German, they are given in parentheses (only given if the river comes into French, Dutch or German-speaking territory). Note for additions: Please remember to add the city where the river meets for each river. For an alphabetical overview of rivers of Belgium, see the category :Rivers of Belgium. By basin Meuse *'' Grevelingen, K ...
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Robertville Reservoir
Lake Robertville is an artificial lake located in Wallonia near the city of Malmedy in Belgium. The water volume is 8,000,000 m³ and the area is 0,62 km². The lake is located in the High Fens park. The dam on the river Warche was built in 1928. Lake Robertville is situated in the municipality of Waimes. It is named after the village of Robertville. {{DEFAULTSORT:Robertville Ourthe basin Reservoirs in Belgium Lakes of the Ardennes (Belgium) Lakes of Liège Province Lake Robertville Lake Robertville is an artificial lake located in Wallonia near the city of Malmedy in Belgium. The water volume is 8,000,000 m³ and the area is 0,62 km². The lake is located in the High Fens park. The dam on the river Warche was built in ... Reservoirs in the Eifel ...
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Eau Rouge
The Eau Rouge is a small, stream in the Belgian province of Liège. It is a right tributary of the Amblève. It starts in the Hautes Fagnes ("High Fens") and ends in Challes, near Stavelot in the river Amblève. The French words mean "red water", and the river gets its name from the reddish coloration of the stones and riverbed due to the presence of iron-oxide deposits. The Eau Rouge is particularly geomorphologically interesting, as it appears to be using the old Warche river stream bed. The Eau Rouge has been a border river for several periods in its existence, including an administrative boundary under the Roman Empire between Cologne and Tongeren, and the state border between the Netherlands and Prussia from 1815 to 1839 and then between Belgium and Prussia from 1839 to 1919. Eau Rouge and the F1 circuit The Eau Rouge has lent its name to the Eau Rouge corner, one of the best-known corners in Formula One race tracks in the Circuit de Spa-Francorchamps The Ci ...
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Amblève (river)
The Amblève (French, ) or Amel (German, ) is a long river in eastern Belgium in the province of Liège. It is a right tributary of the river Ourthe. It rises near Büllingen in the High Fens or ''Hoge Venen'' ( Dutch), ''Hohes Venn'' (German), and ''Hautes Fagnes'' (French), close to the border with Germany. Tributaries of the Amblève are the rivers Chefna, Ninglinspo, Warche, Eau Rouge, Salm and Lienne. The Amblève flows through the towns of Amel, Stavelot, Trois-Ponts, Remouchamps, and Aywaille. The Amblève joins the river Ourthe in Comblain-au-Pont. Sites At the village of Coo (near Trois-Ponts) is the Coo Waterfall, which at tall is not the highest but one of the better known waterfalls in Belgium. The waterfall was created artificially in the 18th century when local monks cut through a bend in the river to feed a watermill. The dried out river bed is now used as the lower storage basin for the Coo-Trois-Ponts Hydroelectric Power Station. A curiosity of L ...
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Hautes Fagnes
The High Fens (german: Hohes Venn; french: Hautes Fagnes; nl, Hoge Venen), which were declared a nature reserve in 1957, are an upland area, a plateau region in Liège Province, in the east of Belgium and adjoining parts of Germany, between the Ardennes and the Eifel highlands. The High Fens are the largest nature reserve or park in Belgium, with an area of ; it lies within the German-Belgian natural park ''Hohes Venn-Eifel'' (), in the Ardennes. Its highest point, at above sea level, is the Signal de Botrange near Eupen, and also the highest point in Belgium. A tower high was built here that reaches above sea level. The reserve is a rich ecological endowment of Belgium covered with alpine sphagnum raised bogs (not "fens" as the name would imply) both on the plateau and in the valley basin; the bogs, which are over 10,000 years old, with their unique subalpine flora, fauna and microclimate, are key to the conservation work of the park. In 1966, the European Council awarde ...
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East Belgium
The German-speaking Community (german: links=no, Deutschsprachige Gemeinschaft, or DG; french: links=no, Communauté germanophone; nl, links=no, Duitstalige Gemeenschap), since 2017 also known as East Belgium (german: links=no, Ostbelgien), is one of the three federal communities of Belgium. Covering an area of within the Liège Province in Wallonia, it includes nine of the eleven municipalities of Eupen-Malmedy. Traditionally speakers of Low Dietsch, Ripuarian, and Moselle Franconian varieties, the local population numbers 77,949about 7.0% of Liège Province and about 0.7% of the national total. Bordering the Netherlands, Germany and Luxembourg, the area has its own parliament and government at Eupen. The German-speaking Community of Belgium is composed of the German-speaking parts of the lands that were annexed in 1920 from Germany. In addition, in contemporary Belgium there are also some other areas where German is or has been spoken (the difference line between German, D ...
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Rivers Of The Ardennes (Belgium)
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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French Language
French ( or ) is a Romance languages, Romance language of the Indo-European languages, Indo-European family. It descended from the Vulgar Latin of the Roman Empire, as did all Romance languages. French evolved from Gallo-Romance, the Latin spoken in Gaul, and more specifically in Northern Gaul. Its closest relatives are the other langues d'oïl—languages historically spoken in northern France and in southern Belgium, which French (Francien) largely supplanted. French was also substratum, influenced by native Celtic languages of Northern Roman Gaul like Gallia Belgica and by the (Germanic languages, Germanic) Frankish language of the post-Roman Franks, Frankish invaders. Today, owing to France's French colonial empire, past overseas expansion, there are numerous French-based creole languages, most notably Haitian Creole language, Haitian Creole. A French-speaking person or nation may be referred to as Francophone in both English and French. French is an official language in ...
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Graben
In geology, a graben () is a depressed block of the crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German, meaning 'ditch' or 'trench'. The word was first used in the geologic context by Eduard Suess in 1883. The plural form is either ''graben'' or ''grabens''. Formation A graben is a valley with a distinct escarpment on each side caused by the displacement of a block of land downward. Graben often occur side by side with horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced from parallel normal faults, where the displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between graben; the bounding faults of a horst typically dip away from the center line of the horst. Single or multiple graben can produce a rift valley. ...
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