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North Eifel
The North Eifel (german: Nordeifel), the northern part of the Eifel, a low mountain range in Germany and East Belgium, comprises the following six sub-regions: * Venn Foreland, * Hohes Venn, * Rur Eifel, *Limestone Eifel, * Our Valley and * High Eifel. All elements belong to the Hohes Venn – Eifel Nature Park. The raised bog of the Hohes Venn is particularly noteworthy. It was designated as a world heritage site by UNESCO. The Eifel Lake Plateau with the second largest dam in Germany, the Rur Valley Dam, lies in the centre of the North Eifel. Also within the North Eifel are: *Eifel National Park, *Monschau Hedegerow Country (''Monschauer Heckenland''), *Kermeter, *Hürtgen Forest and *Zitter Forest The Zitter Forest (german: Zitterwald) is located in the Eifel region in the German district of Euskirchen (North Rhine-Westphalia) and in the Belgian province of Liège (Wallonia). Its highest point is . The Zitter Forest lies in the North Eifel .... External links Hohes Venn - ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifel
The Eifel (; lb, Äifel, ) is a low mountain range in western Germany and eastern Belgium. It occupies parts of southwestern North Rhine-Westphalia, northwestern Rhineland-Palatinate and the southern area of the German-speaking Community of Belgium. The Eifel is part of the Rhenish Massif; within its northern portions lies the Eifel National Park. Geography Location The Eifel lies between the cities of Aachen to the north, Trier to the south and Koblenz to the east. It descends in the northeast along a line from Aachen via Düren to Bonn into the Lower Rhine Bay. In the east and south it is bounded by the valleys of the Rhine and the Moselle. To the west it transitions in Belgium and Luxembourg into the geologically related Ardennes and the Luxembourg Ösling. In the north it is limited by the Jülich-Zülpicher Börde. Within Germany it lies within the states of Rhineland-Palatinate and North Rhine-Westphalia; in the Benelux the area of Eupen, St. Vith and Luxembour ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zitter Forest
The Zitter Forest (german: Zitterwald) is located in the Eifel region in the German district of Euskirchen (North Rhine-Westphalia) and in the Belgian province of Liège (Wallonia). Its highest point is . The Zitter Forest lies in the North Eifel between Hellenthal (north), Dahlem (east), Kronenburg (south) and the Belgian village of Büllingen (west). The Zitter Forest is part of the Hohes Venn – Eifel Nature Park. To the north the Eifel National Park borders on the Zitter Forest; to the south the river Kyll is the border with the Schnee Eifel. In the thinly populated and predominantly wooded uplands of the Zitter Forest between 500 and lie the sources of the Olef, Urft and Kyll. Its highest elevation is on the Weißer Stein (692 m; with ski slopes) southwest of Udenbreth; amongst the other hills within the Zitter Forest are the Bärbelkreuz (662.8 m), Hühnerhöhe (659.9 m), Kamberg (637.8 m). The Hellenthal villages and settlements — like Giesch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hürtgen Forest
The Hürtgen forest (also: Huertgen Forest; german: Hürtgenwald) is located along the border between Belgium and Germany, in the southwest corner of the German federal state of North Rhine-Westphalia. Scarcely in area, the forest lies within a triangle outlined by the German towns of Aachen, Monschau, and Düren. The Rur River runs along the forest's eastern edge. Geography The Hürtgen Forest lies at the northern edge of the Eifel mountains and High Fens – Eifel Nature Park; its terrain is characterized by plunging valleys that carve through broad plateaus. Unlike many areas of Germany in which the valleys are farmed and hilltops are wooded, the Hürtgen Forest's deep valleys are thickly wooded and the hilltop plateaus have been cleared for agriculture. The forest's rough terrain starkly contrasts with that of the adjoining Rhine Valley. Roads in the forest are few, winding, and narrow. Battle of Hürtgen Forest During World War II the rugged terrain of this area ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifel National Park
The Eifel National Park (german: Nationalpark Eifel) is the 14th national park in Germany and the first in North Rhine-Westphalia. The park was founded in 2004, and is classified as a "national park in development". Eifel National Park is part of the much larger High Fens – Eifel Nature Park, a cross-border protection between Germany and Belgium established in 1960. General The aims of the Eifel National Park accord with those set out by the International Union for Conservation of Nature and Natural Resources, IUCN. These require that at least 75 percent of the national park's area must be left to develop naturally – i.e. must not be given over to human use – within 30 years of the foundation of the park. Aims, mechanisms and executive bodies are laid down in the National Park Regulation (''Nationalpark-Verordnung'' or ''NP-VO''). The relatively young national park lies in the north of the Eifel region between Nideggen in the north, Gemünd in the south and the Bel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rur Valley Dam
The Rur or Roer (german: Rur ; Dutch and li, Roer, , ; french: Rour) is a major river that flows through portions of Belgium, Germany and the Netherlands. It is a right (eastern) tributary to the Meuse ( nl, links=no, Maas). About 90 percent of the river's course is in Germany. It is not to be confused with the rivers Ruhr and Röhr, which are tributaries of the Rhine in North Rhine-Westphalia. Geography The Rur rises in the High Fens, near the high Signal de Botrange in Belgium at an elevation of above sea level. South of Monschau it flows into Germany, through North Rhine-Westphalia. It flows first through the northern part of the Eifel mountains. After it reaches the Rur Reservoir, the second-largest artificial lake in Germany. After approximately it flows into the Netherlands, and at its mark it flows into the river Meuse in the town of Roermond. Major tributaries of the Rur include the Inde and the Wurm. The towns along the Rur are Monschau, Heimbach, Ni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
UNESCO
The United Nations Educational, Scientific and Cultural Organization is a specialized agency of the United Nations (UN) aimed at promoting world peace and security through international cooperation in education, arts, sciences and culture. It has 193 member states and 12 associate members, as well as partners in the non-governmental, intergovernmental and private sector. Headquartered at the World Heritage Centre in Paris, France, UNESCO has 53 regional field offices and 199 national commissions that facilitate its global mandate. UNESCO was founded in 1945 as the successor to the League of Nations's International Committee on Intellectual Cooperation.English summary). Its constitution establishes the agency's goals, governing structure, and operating framework. UNESCO's founding mission, which was shaped by the Second World War, is to advance peace, sustainable development and human rights by facilitating collaboration and dialogue among nations. It pursues this objectiv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raised Bog
Raised bogs, also called ombrotrophic bogs, are acidic, wet habitats that are poor in mineral salts and are home to flora and fauna that can cope with such extreme conditions. Raised bogs, unlike fens, are exclusively fed by precipitation (ombrotrophy) and from mineral salts introduced from the air. They thus represent a special type of bog, hydrologically, ecologically and in terms of their development history, in which the growth of peat mosses over centuries or millennia plays a decisive role. They also differ in character from blanket bogs which are much thinner and occur in wetter, cloudier climatic zones. Raised bogs are very threatened by peat cutting and pollution by mineral salts from the surrounding land (due to agriculture and Industrial sector, industry). The last great raised bog regions are found in western Siberia and Canada. Terminology The term raised bog derives from the fact that this type of bog rises in height over time as a result of peat formation. They a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Eifel
The High Eifel (german: Hocheifel (Ost) or ''Hohe Eifel'') forms part of the Eifel Mountains in the German state of Rhineland-Palatinate. The landscape here between Adenau, Mendig and Daun rises to a height of 747 m. The region is not to be confused with the western ''Hocheifel'', better known as the Schnee Eifel. Nürburg Castle and the famous Nürburgring racing track are located in the northwest of the area. Climate Despite being between 600 m and 700 m high the High Eifel lies in the rain shadow of the Schneifel to the west. Its annual precipitation lies between 800 mm and 1000 mm. Mountains/castles * Hohe Acht (747 m) * Nürburg Castle (678 m) * Hochkelberg (675 m) * Dreiser Höhe (611 m) See also * Maifeld * Pellenz * Vordereifel * Vulkan Eifel The Volcanic Eifel or Vulkan Eifel (german: Vulkaneifel) is a region in the Eifel Mountains in Germany that is defined to a large extent by its volcanic geological history. Characteristic o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Germany
Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Our River
The Our (; , ) is a river in Belgium, Luxembourg and Germany. It is a left-hand tributary of the river Sauer/Sûre. Its total length is . The source of the Our is in the High Fens in southeastern Belgium, near Manderfeld. It flows southwards, more or less along the German-Belgian border, and after Ouren, along the German-Luxembourg border. The historic town of Vianden lies on the Our. The Our empties into the Sauer in Wallendorf. Course The river rises in the eastern Ardennes and western Eifel on Belgian soil. Its source near the village of Losheimergraben lies northeast of the ''Eichelsberg'' mountain (653 m) at 643 m near the B 265. Just a few hundred metres away is the source of the River Kyll. The Our initially follows the B 265, which is also the Belgian-German state border. The river continues alternating between Belgium and Germany. From the tripoint by the Europa Monument between Ouren (B), Sevenig (D) and Lieler (L) it runs almost entirely on th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Eifel
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limestone c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
