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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 and ... [...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 (North Rhine-Westphalia), 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 their traditional markets in France, the distri ... [...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 Kelberg 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 like-named ''Verbandsgemeinde'', and .... The ''Verbandsgemeinde'' Kelberg consists of the following ''Ortsgemeinden'' ("local municipalities"): {{Authority control Verbandsgemeinde in Rhineland-Palatinate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ortsgemeinde (Germany)
A Verbandsgemeinde (; plural Verbandsgemeinden) is a low-level administrative unit in the German federal states of Rhineland-Palatinate and Saxony-Anhalt. A Verbandsgemeinde is typically composed of a small group of villages or towns. Rhineland-Palatinate The state of Rhineland-Palatinate is divided into 163 Verbandsgemeinden, which are municipal associations grouped within the 24 districts of the state and subdivided into 2,257 Ortsgemeinden (singular Ortsgemeinde) which comprise single settlements. Most of the Verbandsgemeinden were established in 1969. Formerly the name for an administrative unit was ''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 districts of Saxony-Anhalt are divided into ''Verwaltungsgemein ... [...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 p ... [...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 of thi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tertiary
Tertiary ( ) is a widely used but obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non-avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The time span covered by the Tertiary has no exact equivalent in the current geologic time system, but it is essentially the merged Paleogene and Neogene periods, which are informally called the Early Tertiary and the Late Tertiary, respectively. The Tertiary established the Antarctic as an icy island continent. Historical use of the term The term Tertiary was first used by 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, the Quaternary, was applied. In the early d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism
Volcanism, vulcanism or volcanicity is the phenomenon of eruption of molten rock (magma) onto the surface of the Earth or a solid-surface planet or moon, where lava, pyroclastics, and volcanic gases erupt through a break in the surface called a vent. It includes all phenomena resulting from and causing magma within the crust or mantle of the body, to rise through the crust and form volcanic rocks on the surface. Magmas, that reach the surface and solidify, form extrusive landforms. Volcanic processes Magma from the mantle or lower crust rises through the crust towards the surface. If magma reaches the surface, its behavior depends on the viscosity of the molten constituent rock. Viscous (thick) magma produces volcanoes characterised by explosive eruptions, while non-viscous (runny) magma produce volcanoes characterised by effusive eruptions pouring large amounts of lava onto the surface. In some cases, rising magma can cool and solidify without reaching the surface. Inste ... [...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. The name comes from a Moselle Franconian dialect word used for the circular lakes of the Daun area of Germany. Notes: * According to German Wikipedia's ''"Maar"'' article, in 1544 in his book ''Cosmographia'', Sebastian Münster (1488–1552) first applied the word "maar" (as ''Marh'') to the Ulmener Maar and the Laacher See. See: Sebastian Münster, ''Cosmographia'' (Basel, Switzerland: Heinrich Petri, 1544)p. 341. From p. 341: ''"Item zwen namhafftiger seen seind in der Eyfel / einer bey de schloß Ulmen / und ein ander bey dem Closter züm Laich / die seind sere tieff / habe kein ynflüß aber vil außflüß / die nennet man Marh unnd seind fischreich."'' (Also two noteworthy lakes are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Stone Age
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. 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. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in the ... [...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 (Eifel), 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 o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rotliegend
The Rotliegend, Rotliegend Group or Rotliegendes (german: the underlying red) is a lithostratigraphy, 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 formation (stratigraphy), 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 (stratigraphy), series or subsystem of the Permian). This time span corresponds roughly with the length of the Cisuralian Epoch (reference date), epoch. Facies and formation In large parts of Pangaea, the last tectonic phase, phases of the Hercynian orogeny were still ongoing during the start of the Permian. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
