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Eifel
The Eifel (; , ) is a low mountain range in western Germany, eastern Belgium and northern Luxembourg. 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. The Eifelian stage in geological history is named after the region because rocks of that period reach the surface in the Eifel at the Wetteldorf Richtschnitt outcrop. The inhabitants of the Eifel are known as Eiflers or Eifelers. 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 Ardenn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifel National Park
The Eifel National Park () 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 (Schleiden), Gemünd in the south and the Belgium, Be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eifelian
The Eifelian is the first of two faunal stages in the Middle Devonian Epoch. It lasted from 393.3 ± 1.2 million years ago to 387.7 ± 0.8 million years ago. It was preceded by the Emsian Stage and followed by the Givetian Stage. North American subdivisions of the Eifelian Stage include Southwood, and part of Cazenovia (or Cazenovian). Name and definition The Eifelian is named after the Eifel Mountains of Western Germany, which exposed the GSSP section at the Wetteldorf Richtschnitt outcrop. The base of the Eifelian is defined by the start of the '' Polygnathus partitus'' conodont zone. This layer lies within the Upper Heisdorf Formation, below the base of the Lauch Formation. Major events The earliest forest is known from the Eifelian stage. Cladoxylopsid trees including '' Calamophyton'' and other plants have formed the forest landscape in what is now England. Extinctions The end of the Eifelian was marked by a biological crisis known as the Kačák Event, a two-pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Booser Doppelmaar
The Booser Doppelmaar ("Double Maar of Boos") comprises two maars that have silted up and, today, form shallow depressions in the countryside. They lie on the territory of the village of Boos (in the collective municipality of Vordereifel), a few hundred metres west of the village itself. The two maars were formed 10,150 to 14,160 years ago and belong to the Quaternary volcano field of the Volcanic Eifel.Volcanic Eifel in the sense of a natural historical space or a region, not in the sense of a natural regional unit. From a natural region perspective it lies in the south of the Hohe Acht Upland (which belongs to the natural regional major unit of the Eastern High Eifel), ca. 7.8 km south (more precisely half west-by-south or 185.625º) of the summit of the Hohe Acht. The maars The two maars form large, circular basins surrounded by tuff embankments that lie on a line running west-southwest to east-northeast and thus follow the Variscan strike of the terrain. The west-s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhenish Slate Mountains
The Rhenish Massif, Rhine Massif or Rhenish Uplands (, : 'Rhenish Slate Uplands') is a geologic massif in western Germany, eastern Belgium, Luxembourg and northeastern France. It is drained centrally, south to north by the river Rhine and a few of its tributaries. West of the indent of the Cologne Bight it has the Eifel and the Belgian and French Ardennes; east is its greatest German component, the Süder Uplands. The Hunsrück hills form its southwest. The Westerwald is an eastern strip. The Lahn-Dill area is a small central zone and the Taunus Mountains form the rest, the south-east. The massif hosts the Middle Rhine Valley ( Rhine Gorge), a UNESCO World Heritage site linked to the lowest parts of the Moselle (, ). Geology Geologically the Rhenish Massif consists of metamorphic rocks, mostly slates (hence its German name), deformed and metamorphosed during the Hercynian orogeny (around 300 million years ago). Most of the massif is part of the Rhenohercynian zone of thi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ardennes
The Ardennes ( ; ; ; ; ), also known as the Ardennes Forest or Forest of Ardennes, is a region of extensive forests, rough terrain, rolling hills and ridges primarily in Belgium and Luxembourg, extending into Germany and France. Geologically, the range is a western extension of the Eifel; both were raised during the Givetian age of the Devonian (382.7 to 387.7 million years ago), as were several other named ranges of the same greater range. The Ardennes proper stretches well into Germany and France (lending its name to the Ardennes department and the former Champagne-Ardenne region) and geologically into the Eifel (the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany); most of it is in the southeast of Wallonia, the southern and more rural part of Belgium (away from the coastal plain but encompassing more than half of the country's total area). The eastern part of the Ardennes forms the northernmost third of the Grand Duchy of Luxembourg, also called ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohe Acht
The Hohe Acht () is the highest mountain () in the Eifel mountains of Germany. It is located on the boundary between the districts of Ahrweiler and Mayen-Koblenz in Rhineland-Palatinate. Geography and geology The Hohe Acht is located in the High Eifel east of Adenau. The mountain is a Tertiary volcano, whose cone is composed of Lower Devonian rock and whose summit is made of basalt. Emperor William Tower In 1908/09 the Emperor William Tower (''Kaiser-Wilhelm-Turm'') was erected on the Hohe Acht. The occasion for the construction of this stone observation tower, based on plans by the architect, Freiherr von Tettau of Berlin, was the silver wedding of Emperor William II and Empress Augusta Victoria as well as the commemoration of Emperor William I The tower is high and its walls are one metre thick at ground level. The work was carried out by master masons, Karl and Johannes Leidinger, from Adenau using local stone. The cost of construction was 18,000 marks. The towe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
German-speaking Community Of Belgium
The German-speaking Community (, , DG), also known as East Belgium ( ), is one of the three Communities, regions and language areas of Belgium, 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 language, Limburgish, Ripuarian language, Ripuarian and Moselle Franconian dialects, 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 Treaty of V ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moselle
The Moselle ( , ; ; ) is a river that rises in the Vosges mountains and flows through north-eastern France and Luxembourg to western Germany. It is a bank (geography), left bank tributary of the Rhine, which it joins at Koblenz. A small part of Belgium is in its drainage basin, basin as it includes the Sauer and the Our River, Our. Its lower course "twists and turns its way between Trier and Koblenz along one of Germany's most beautiful river valleys."''Moselle: Holidays in one of Germany's most beautiful river valleys'' at www.romantic-germany.info. Retrieved 23 Jan 2016. In this section the land to the north is the Eifel which stretches into Belgium; to the south lies the Hunsrück. The river flows through a region that was cultivated by the Romans. Today, its hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aachen
Aachen is the List of cities in North Rhine-Westphalia by population, 13th-largest city in North Rhine-Westphalia and the List of cities in Germany by population, 27th-largest city of Germany, with around 261,000 inhabitants. Aachen is located at the northern foothills of the High Fens and the Eifel Mountains. It sits on the Wurm (Rur), Wurm River, a tributary of the Rur (river), Rur, and together with Mönchengladbach, it is the only larger German city in the drainage basin of the Meuse. It is the westernmost larger city in Germany, lying approximately west of Cologne and Bonn, directly bordering Belgium in the southwest, and the Netherlands in the northwest. The city lies in the Meuse–Rhine Euroregion and is the seat of the Aachen (district), district of Aachen ''(Städteregion Aachen)''. The once Celts, Celtic settlement was equipped with several in the course of colonization by Roman people, Roman pioneers settling at the warm Aachen thermal springs around the 1st cen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Rhine-Westphalia
North Rhine-Westphalia or North-Rhine/Westphalia, commonly shortened to NRW, is a States of Germany, state () in Old states of Germany, Western Germany. With more than 18 million inhabitants, it is the List of German states by population, most populous state in Germany. Apart from the city-states (Berlin, Hamburg and Bremen), it is also the List of German states by population density, most densely populated state in Germany. Covering an area of , it is the List of German states by area, fourth-largest German state by size. North Rhine-Westphalia features 30 of the 81 German municipalities with over 100,000 inhabitants, including Cologne (over 1 million), the state capital Düsseldorf (630,000), Dortmund and Essen (about 590,000 inhabitants each) and other cities predominantly located in the Rhine-Ruhr metropolitan area, the largest urban area in Germany and the fourth-largest on the European continent. The location of the Rhine-Ruhr at the heart of the European Blue Banana make ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
