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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 In geology, a graben () is a depression (geology), depressed block of the Crust (geology), crust of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Malmedy
Malmedy (; , historically also ; ) 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 and 5% ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 (; ; ) is a Municipalities of Belgium, municipality of Wallonia located in the Liège Province, 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 popul .... It is named after the village of Robertville. The lake is an official swimming lake in Wallonia. References {{DEFAULTSORT:Robertville Ourthe basin Reservoirs in Belgium Lakes of the Ardennes (Belgium) Lakes of Liège Province Lake Robertville Reservoirs in the Eifel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Belgium
These are the main rivers that flow wholly or partially in Belgium or have Belgian tributaries. 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 flows in 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 :Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. The lake is an official swimming lake in Wallonia. References {{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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Circ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amblève (river)
The Amblève (French language, French, ) or Amel (German language, German, ) is a long river in eastern Belgium in the province of Liège (province), Liège. It is a right tributary of the river Ourthe. It rises near Büllingen in the High Fens or ''Hoge Venen'' (Dutch language, Dutch), ''Hohes Venn'' (German language, German), and ''Hautes Fagnes'' (French language, French), close to the border with Germany. Tributaries of the Amblève are the rivers Chefna, Ninglinspo, Warche, Eau Rouge, Salm River (Belgium), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hautes Fagnes
The High Fens (; ; ), 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 northwestern 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 (watered only by precipitation, instead of surface water, as the appellation “ fens” 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Belgium
The German-speaking Community (, , DG), also known as East Belgium ( ), is one of the three federal communities of Belgium. The community is composed of nine municipalities in Liège Province, Wallonia, within the Eupen-Malmedy region in Eastern Belgium. The primary language of the community is German, making this one of the three official languages in Belgium. Traditionally the community and the wider area around it forms an intersection of various local languages and/or dialects, namely Limburgish, Ripuarian and Moselle Franconian varieties. The community has an area of , and has a population of around 79,000 (as of January 2024)about 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 was annexed in 1920 from Germany. There are also some other areas where German is spoken that belonged to Belgium before 1920, but the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of The Ardennes (Belgium)
A river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
French Language
French ( or ) is a Romance languages, Romance language of the Indo-European languages, Indo-European family. Like all other Romance languages, it descended from the Vulgar Latin of the Roman Empire. French evolved from Northern Old Gallo-Romance, a descendant of the Latin spoken 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 language, Francien) largely supplanted. It was also substratum (linguistics), influenced by native Celtic languages of Northern Roman Gaul and by the Germanic languages, Germanic Frankish language of the post-Roman Franks, Frankish invaders. As a result of French and Belgian colonialism from the 16th century onward, it was introduced to new territories in the Americas, Africa, and Asia, and numerous French-based creole languages, most notably Haitian Creole, were established. A French-speaking person or nation may be referred to as Fra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Graben
In geology, a graben () is a depression (geology), depressed block of the Crust (geology), crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German language, German, meaning 'ditch' or 'trench'. The first known usage of the word in the geologic context was 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 Horst (geology), horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced by sets of normal faults that have parallel fault traces, 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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
