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Uersfeld
Uersfeld 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 Kelberg, whose seat is in the like-named municipality. Geography Location The municipality lies in the Vulkaneifel, a part of the Eifel known for its volcanic history, geographical and geological features, and even ongoing activity today, including gases that sometimes well up from the earth. Geology Like the rest of what is now the Eifel, the place that is now Uersfeld was underwater about 400,000,000 years ago, at the bottom of a Devonian sea. This is witnessed by fossils of sea creatures. Such things were found many years ago by Franz Krämer from Kölnische Höfe (a hamlet now belonging to Kaperich) near Uersfeld's railway station. About 200,000,000 years ago, the Eifel was not only no longer underwater, but also considerably drier than it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaperich
Kaperich 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 Kelberg, whose seat is in the like-named municipality. Geography Location The municipality lies in the Vulkaneifel, a part of the Eifel known for its volcanic history, geographical and geological features, and even ongoing activity today, including gases that sometimes well up from the earth. Neighbouring municipalities Kaperich’s neighbours are Lirstal, Höchstberg and Uersfeld. Constituent communities Kaperich has an outlying hamlet called Kölnische Höfe, which is home to roughly 25 people. This hamlet is sometimes also called “Pochtener Höfe”. History In feudal times, Kaperich belonged until 1794 to the Electoral-Cologne ''Amt'' of Nürburg. Under Prussian administration, Kaperich became a municipality in the Adenau district a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vulkaneifel
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 (district), Euskirchen (North Rhine-Westphalia), Ahrweiler (district), Ahrweiler, Mayen-Koblenz, Cochem-Zell, Bernkastel-Wittlich, and Bitburg-Prüm. Location The county of Vulkaneifel lies in the western part of the eponymous region which lies at heights between 150 and 700 metres above sea level. As a result of former volcanism numerous mineral springs (''Sauerbrunnen'') have formed. The Kyll flows through the county from north to south. The German Wildlife Route and the German Volcano Route also cross the county as does the Eifelsteig hiking trail. History The district was created in 1815 when the Eifel became part of Prussia. As most of the local industries had thei ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kelberg (Verbandsgemeinde)
Kelberg is a ''Verbandsgemeinde'' ("collective municipality") in the district Vulkaneifel, in Rhineland-Palatinate, Germany. The seat of the ''Verbandsgemeinde'' is in Kelberg. The ''Verbandsgemeinde'' Kelberg consists of the following ''Ortsgemeinden'' ("local municipalities"): {{Authority control Verbandsgemeinden in Rhineland-Palatinate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ortsgemeinde (Germany)
A (; plural ) is a low-level administrative division, administrative unit in the Germany, German States of Germany, federal states of Brandenburg, Rhineland-Palatinate and Saxony-Anhalt. A is typically composed of a small group of Municipalities of Germany, municipalities. Rhineland-Palatinate The state of Rhineland-Palatinate is divided into 163 , which are municipal associations grouped within the 24 Districts of Germany, districts of the state and subdivided into 2,257 Ortsgemeinden (singular Ortsgemeinde) which comprise single settlements. Most of the were established in 1969. Formerly the name for an administrative unit was ''Amt (political division), Amt''. Most of the functions of municipal government for several municipalities are consolidated and administered centrally from a larger or more central town or municipality among the group, while the individual municipalities (Ortsgemeinden) still maintain a limited degree of local autonomy. Saxony-Anhalt The 11 distric ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mosbrucher Weiher
The Mosbrucher Weiher, also called the ''Mosbrucher Maar'', is a silted up maar east of the municipal boundary of the village of Mosbruch in the county Vulkaneifel in Germany. It is located immediately at the foot of the 675-metre-high Hochkelberg, a former volcano. The floor of the maar is in the shape of an elongated oval and is about 700×500 metres in size, its upper boundary has a diameter of about 1,300 × 1,050 metres. This makes the Mosbrucher Maar the third largest of the maars in the western Eifel region. The Üßbach stream flows past and close to the Mosbrucher Weiher. Origin According to pollen analysis studies, the crater was formed about 11,000 years ago by a volcanic eruption. In the area around the maar there are very few volcanic tuffs in comparison to other Eifel maars; only in two places are there greater accumulations of tuff; the rest of the surrounding area is covered only by a thin layer. Either most of the tuffs have already been removed, or the eruption ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Eifel
The High Eifel ( 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 () consists of three areas of volcanic activity, known as the West Eifel, High Eifel, and East Eifel volcanic fields. Volcanic Eifel is a region in the Eifel Mountains in Germa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tertiary Period
The Tertiary ( ) is an obsolete Period (geology), geologic period spanning 66 million to 2.6 or 1.8 million years ago. The period began with the extinction of the non-bird, avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic, Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene, Pliocene Epoch. The Tertiary has not been recognised by the International Commission on Stratigraphy (ICS) since the late 1980s, with the timespan of the Tertiary now being split in to the earlier Paleogene and the more recent Neogene periods, though the Tertiary continues to be used in some scientific publications. Historical use of the term The term Tertiary was first used by Giovanni Arduino (geologist), Giovanni Arduino during the mid-18th century. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in Northern Italy. Later a fourth period, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism
Volcanism, vulcanism, volcanicity, or volcanic activity is the phenomenon where solids, liquids, gases, and their mixtures erupt to the surface of a solid-surface astronomical body such as a planet or a moon. It is caused by the presence of a heat source, usually internally generated, inside the body; the heat is generated by various processes, such as radioactive decay or tidal heating. This heat partially melts solid material in the body or turns material into gas. The mobilized material rises through the body's interior and may break through the solid surface. Causes For volcanism to occur, the temperature of the mantle must have risen to about half its melting point. At this point, the mantle's viscosity will have dropped to about 1021 Pascal-seconds. When large scale melting occurs, the viscosity rapidly falls to 103 Pascal-seconds or even less, increasing the heat transport rate a million-fold. The occurrence of volcanism is partially due to the fact that melted materi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maar
A maar is a broad, low-relief volcanic crater caused by a phreatomagmatic eruption (an explosion which occurs when groundwater comes into contact with hot lava or magma). A maar characteristically fills with water to form a relatively shallow crater lake, which may also be called a maar.David S.G. Thomas and Andrew Goudie (eds.), ''The Dictionary of Physical Geography'' (Oxford: Blackwell, 2000), 301. . Maars range in size from across and from deep. Most maars fill with water to form natural lakes. Most maars have low rims composed of a mixture of loose fragments of volcanic rocks and rocks torn from the walls of the diatreme. Etymology The name ''maar'' comes from a Moselle Franconian dialect word used for the circular lakes of the Daun area of Germany. The word evolved from its first use in German in the modern geological sense in 1819 and is now used in English and in the geological sciences as the term for the explosion crater, even if water from rainfall might alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Stone Age
The Neolithic or New Stone Age (from Greek 'new' and 'stone') is an archaeological period, the final division of the Stone Age in Mesopotamia, Asia, Europe and Africa (c. 10,000 BCE to c. 2,000 BCE). It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. The term 'Neolithic' was coined by Sir John Lubbock in 1865 as a refinement of the three-age system. The Neolithic began about 12,000 years ago, when farming appeared in the Epipalaeolithic Near East and Mesopotamia, and later in other parts of the world. It lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BCE), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places, the N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ulmener Maar
The Ulmener Maar is a maar in the Eifel mountains of Germany in the immediate vicinity of the town of Ulmen in the state of Rhineland-Palatinate. The lake is up to 37 metres deep and is surrounded by an embankment of tuff with an average height of 20 metres, which was formed from the erupted material of the former volcano. By the southern edge of the embankment are the ruins of a knight's castle, Ulmen Castle dating to the 11th century. IUGS geological heritage site In respect of it being the 'youngest volcano in central Europe, situated in Vulkaneifel, the volcanic region where the model of formation of maars by phreatomagmatic eruptions was established', the International Union of Geological Sciences (IUGS) included 'The Holocene Ulmen Maar' in its assemblage of 100 'geological heritage sites' around the world in a listing published in October 2022. The organisation defines an IUGS Geological Heritage Site as 'a key place with geological elements and/or processes of internation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rotliegend
The Rotliegend, Rotliegend Group or Rotliegendes () is a lithostratigraphic unit (a sequence of rock strata) of latest Carboniferous to Guadalupian (middle Permian) age that is found in the subsurface of large areas in western and central Europe. The Rotliegend mainly consists of sandstone layers. It is usually covered by the Zechstein and lies on top of regionally different formations of late Carboniferous age. The name Rotliegend has in the past not only been used to address the rock strata themselves, but also the time span in which they were formed (in which case the Rotliegend was considered a series or subsystem of the Permian). This time span corresponds roughly with the length of the Cisuralian epoch. Facies and formation In large parts of Pangaea, the last phases of the Hercynian orogeny were still ongoing during the start of the Permian. At the same time local crustal extension formed intramontane basins such as the large Permian Basin which covered parts of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
