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Eifel
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Eifel
The Eifel (German: [ˈaɪfl̩] ⓘ; Luxembourgish: Äifel, pronounced [ˈæːɪ̯fəl]) 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.
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 Luxembourg. Its highest point is the volcanic cone of the Hohe Acht (746.9 m; 2,450 ft). Originally the Carolingian Eifelgau only covered the smaller region roughly around the sources of the rivers Ahr, Kyll, Urft and Erft. Its name was more recently transferred to the entire region.
The Eifel belongs to that part of the Rhenish Massif whose rolling plateau is categorised as peneplain highland (Rumpfhochland), which was formed by the erosion of the ancient mountains of the Variscan mountain building phase and subsequent further uplifting. Individual mountain chains, up to 700 m (2,300 ft), such as the Schneifel and High Fens, run through the western part of the plateau. In the eastern part, in the High Eifel and Volcanic Eifel, individual cinder cones and basalt kuppen, like the Hohe Acht and the Ernstberg, emerged as a result of volcanicity in the Tertiary and Quaternary periods and rise above the undulating countryside.
The rivers draining into the Moselle, Rhine and Meuse, such as the Our, Kyll, Ahr, Brohlbach and Rur, have cut deep into the edge of the Eifel and formed larger valleys.
The Eifel covers an area of 5,300 km2 (2,000 sq mi) and is geographically divided into the North and South Eifel. It is further divided into several natural regional landscapes, some with further subdivisions.
Since 2004, part of the North Eifel has been designated as the Eifel National Park. There are also four nature parks in the Eifel (from north to south): Rhineland, High Fens-Eifel, Volcanic Eifel, and South Eifel, although the first extends only partly into the northern foothills of the Eifel.
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Eifel AI simulator
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Eifel
The Eifel (German: [ˈaɪfl̩] ⓘ; Luxembourgish: Äifel, pronounced [ˈæːɪ̯fəl]) 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.
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 Luxembourg. Its highest point is the volcanic cone of the Hohe Acht (746.9 m; 2,450 ft). Originally the Carolingian Eifelgau only covered the smaller region roughly around the sources of the rivers Ahr, Kyll, Urft and Erft. Its name was more recently transferred to the entire region.
The Eifel belongs to that part of the Rhenish Massif whose rolling plateau is categorised as peneplain highland (Rumpfhochland), which was formed by the erosion of the ancient mountains of the Variscan mountain building phase and subsequent further uplifting. Individual mountain chains, up to 700 m (2,300 ft), such as the Schneifel and High Fens, run through the western part of the plateau. In the eastern part, in the High Eifel and Volcanic Eifel, individual cinder cones and basalt kuppen, like the Hohe Acht and the Ernstberg, emerged as a result of volcanicity in the Tertiary and Quaternary periods and rise above the undulating countryside.
The rivers draining into the Moselle, Rhine and Meuse, such as the Our, Kyll, Ahr, Brohlbach and Rur, have cut deep into the edge of the Eifel and formed larger valleys.
The Eifel covers an area of 5,300 km2 (2,000 sq mi) and is geographically divided into the North and South Eifel. It is further divided into several natural regional landscapes, some with further subdivisions.
Since 2004, part of the North Eifel has been designated as the Eifel National Park. There are also four nature parks in the Eifel (from north to south): Rhineland, High Fens-Eifel, Volcanic Eifel, and South Eifel, although the first extends only partly into the northern foothills of the Eifel.
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