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The Eifel 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.
Vulkaneifel is a district (Kreis) in the northwest of the state Rhineland-Palatinate, Germany. It is the least densely populated district in the state and the fourth most sparsely populated district in Germany. The administrative centre of the district is in Daun. Neighboring districts are Euskirchen, Ahrweiler, Mayen-Koblenz, Cochem-Zell, Bernkastel-Wittlich, and Bitburg-Prüm.
A monogenetic volcanic field is a type of volcanic field consisting of a group of small monogenetic volcanoes, each of which erupts only once, as opposed to polygenetic volcanoes, which erupt repeatedly over a period of time. The small monogenetic volcanoes of these fields are the most common subaerial volcanic landform.
A volcanic field is an area of Earth's crust that is prone to localized volcanic activity. The type and number of volcanoes required to be called a "field" is not well-defined. Volcanic fields usually consist of clusters of up to 100 volcanoes such as cinder cones. Lava flows may also occur. They may occur as a monogenetic volcanic field or a polygenetic volcanic field.
A maar is a broad, low-relief volcanic crater caused by a phreatomagmatic eruption. A maar characteristically fills with water to form a relatively shallow crater lake which may also be called a maar. The name comes from a Moselle Franconian dialect word used for the circular lakes of the Daun area of Germany.
Daun is a town in the Vulkaneifel district in Rhineland-Palatinate, Germany. It is the district seat and also the seat of the Verbandsgemeinde of Daun.
Laacher See, also known as Lake Laach or Laach Lake, is a volcanic caldera lake with a diameter of 2 km (1.2 mi) in Rhineland-Palatinate, Germany, about 24 km (15 mi) northwest of Koblenz, 37 km (23 mi) south of Bonn, and 8 km (5.0 mi) west of Andernach. It is in the Eifel mountain range, and is part of the East Eifel volcanic field within the larger Volcanic Eifel. The lake was formed by a Plinian eruption approximately 13,000 years BP with a Volcanic Explosivity Index (VEI) of 6, on the same scale as the Pinatubo eruption of 1991.
Rockeskyll is an Ortsgemeinde – a municipality belonging to a Verbandsgemeinde, a kind of collective municipality – in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the Verbandsgemeinde of Gerolstein, whose seat is in the like-named town.
Schönbach is an Ortsgemeinde – a municipality belonging to a Verbandsgemeinde, a kind of collective municipality – in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the Verbandsgemeinde of Daun, whose seat is in the like-named town.
The Eifel hotspot is a volcanic hotspot in Western Germany. It is one of many recent volcanic formations in and around the Eifel mountain range and includes the volcanic field known as Volcanic Eifel. Although the last eruption occurred around 10,000 years ago, the presence of escaping volcanic gases in the region indicates that it is still weakly active.
The Volcanic Eifel or Vulkan Eifel is a region in the Eifel Mountains in Germany that is defined to a large extent by its volcanic geological history. Characteristic of this volcanic field are its typical explosion crater lakes or maars, and numerous other signs of volcanic activity such as volcanic tuffs, lava streams and volcanic craters like the Laacher See. The Volcanic Eifel is still volcanically active today. One sign of this activity is the escaping gases in the Laacher See.
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.
The Volcano Park in Mayen-Koblenz is a geopark in the rural district of Mayen-Koblenz in the eastern Vulkan Eifel, Germany. It was founded in 1996 and wraps around the Laacher See. Together with the Volcano Park, Brohltal/Laacher See and the Vulkan Eifel Nature and Geo-Park, it forms part of the national Eifel Volcano Land Geo-Park. The three parks are connected by the 280-kilometre-long German Volcano Route.
The Booser Doppelmaar 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, 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. From a natural region perspective it lies in the south of the Hohe Acht Upland, ca. 7.8 km south of the summit of the Hohe Acht.
The Volcano Museum in the old district administrative office (Landratsamt) in Daun, Germany, was set up as an extension of the existing 'geopaths' at Hillesheim, Manderscheid and Gerolstein and is part of the Volcanic Eifel Nature and Geopark.
The Volcanic Eifel Nature Park lies in the counties of Bernkastel-Wittlich, Cochem-Zell and Vulkaneifel in the German state of Rhineland-Palatinate. The nature park, which is in the Eifel mountains, and which is also a geopark, was inaugurated on 31 May 2010 and has an area of 1,068.24 km².> Its sponsor is the Natur- und Geopark Vulkaneifel GmbH.
The German Volcano Route or, less commonly, German Volcano Road is a 280-kilometre-long tourist route from the River Rhine to the mountains of the High Eifel. It links 39 sites within the Geopark Vulkanland Eifel in the Volcanic Eifel (Vulkaneifel), at which geological, cultural-historical and industrial-historical nature and cultural monuments on the subject of volcanicity in the Eifel are located.
The Nerother Kopf is the conical hill of an extinct volcano near Neroth in the Eifel mountains. It is 651.7 m above sea level (NHN) and situated in the county of Vulkaneifel in the German state of Rhineland-Palatinate.
The Vulkanland Eifel Geopark is a German national geopark in the Volcanic Eifel region that was established on 19 April 2005. Covering an area of 2,200 km², the geopark extends from the Belgian border in the west over the Eifel mountains to the River Rhine in the east. The countryside here which has been shaped by the volcanism of the past contains numerous maars, cinder cones, lava flows lava domes calderas and bubbling springs. The largest caldera was formed by the Laacher See volcano that last erupted about 13,000 years ago. A sign of continuing volcanic activity in this region are the volcanic gases that are still visibly being discharged into the atmosphere.
The Hochstein is a volcanic cone, 563 m above sea level (NHN), in the Eifel near Obermendig in the German state of Rhineland-Palatinate and county of Mayen-Koblenz.
References
- Siebert L, Simkin T (2002–present). Volcanoes of the World: an Illustrated Catalog of Holocene Volcanoes and their Eruptions. Smithsonian Institution, Global Volcanism Program Digital Information Series, GVP-3 (http://www.volcano.si.edu).
- ↑ Cools, Sebastien; Juvigne, Etienne; Pouclet, Andre. "Composition of tephra of the Goldberg volcano (West Eifel, Germany) and search for its dispersion" (PDF). Core. Core. Retrieved 19 September 2022.