Oberstadtfeld
Oberstadtfeld 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. Geography Location Oberstadtfeld lies 6 km southwest of Daun on ''Bundesstraße'' 257 in the valley of the Kleine Kyll river in the Volcanic Eifel, 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 Oberstadtfeld's neighbours are Pützborn (a constituent community of Daun), Neroth, Niederstadtfeld, Üdersdorf and Wallenborn. Geology Among geologists, Oberstadtfeld is well known for its varied fossils from an eventful geological past. Remnants of long-gone lifeforms, which have been preserved despite all the changes that have taken plac ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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OBERSTADTFELD Nieder
Oberstadtfeld 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. Geography Location Oberstadtfeld lies 6 km southwest of Daun on '' Bundesstraße'' 257 in the valley of the Kleine Kyll river in the Volcanic Eifel, 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 Oberstadtfeld's neighbours are Pützborn (a constituent community of Daun), Neroth, Niederstadtfeld, Üdersdorf and Wallenborn. Geology Among geologists, Oberstadtfeld is well known for its varied fossils from an eventful geological past. Remnants of long-gone lifeforms, which have been preserved despite all the changes that have tak ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Niederstadtfeld
Niederstadtfeld 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. Geography Location The municipality lies in the Volcanic Eifel, a part of the Eifel known for its volcanic history, geographical and geological features. Volcanic activity continues even today, including gases that sometimes well up from the earth. Niederstadtfeld lies roughly 8 km southwest of Daun, southwestwards towards Bitburg, near ''Bundesstraße'' 257, and can be reached directly over ''Landesstraße'' (State Road) 27. The original village (now the village centre) stands on a ridge between the Kälberbach and Schwemmbach valleys in a side valley of the Kleine Kyll river. The Kleine Kyll valley is part of the protected area ''Zwischen Uess und Kyll''. The newer built-up area today stretc ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Kleine Kyll
The Little Kyll german: Kleine Kyll, pronounced: "kill") is a orographically right-hand tributary of the Lieser. Geography Course The Little Kyll rises northeast of Neroth on the heights of the Neroth woods in the county of Vulkaneifel in the German state of Rhineland-Palatinate. It flows in a southerly direction through the municipalities of Neroth, Oberstadtfeld, Niederstadtfeld and Schutz and empties into the Lieser south of Manderscheid, Bernkastel-Wittlich. Tributaries The tributaries of the Little Kyll include the following (in a downstream direction): Recreation In the area between Oberstadtfeld and Bleckhausener Mühle/Meerfeld the cycleway runs parallel to the Kleine Kyll. At the confluence with the Horngraben, south of Manderscheid is the gorge of Wolfsschlucht [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Üdersdorf
Üdersdorf 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. 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. Üdersdorf is a state-recognized recreational resort (''Erholungsort'') and offers a great many hiking trails in thickly wooded surroundings. The maars (crater lakes) and the Lieser valley are right nearby. Not much farther away lie the spa towns of Daun and Manderscheid as well as the Nürburgring. Constituent communities Üdersdorf's two outlying '' Ortsteile'' are Tettscheid and Trittscheid. History In 1287, Üdersdorf had its first documentary mentio ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 dist ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Daun (Verbandsgemeinde)
Daun is a collective municipality (''Verbandsgemeinde'') in the Vulkaneifel district of Rhineland-Palatinate, Germany. The seat of the Daun Verbandsgemeinde is in the municipality of Daun. Constituent municipalities # Betteldorf # Bleckhausen # Brockscheid # Darscheid # Daun # Demerath #Deudesfeld #Dockweiler # Dreis-Brück # Ellscheid # Gefell #Gillenfeld #Hinterweiler # Hörscheid # Immerath # Kirchweiler # Kradenbach #Mehren # Meisburg # Mückeln # Nerdlen # Niederstadtfeld # Oberstadtfeld # Sarmersbach #Saxler # Schalkenmehren # Schönbach # Schutz # Steineberg # Steiningen # Strohn #Strotzbüsch #Udler #Üdersdorf Üdersdorf 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, who ... # Utzerath # Wallenborn # Weidenbach # Winkel References {{Authority ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Central Europe
Central Europe is an area of Europe between Western Europe and Eastern Europe, based on a common historical, social and cultural identity. The Thirty Years' War (1618–1648) between Catholicism and Protestantism significantly shaped the area's history. The concept of "Central Europe" appeared in the 19th century. Central Europe comprised most of the territories of the Holy Roman Empire and those of the two neighboring kingdoms of Poland and Hungary. Hungary and parts of Poland were later part of the Habsburg monarchy, which also significantly shaped the history of Central Europe. Unlike their Western European (Portugal, Spain et al.) and Eastern European (Russia) counterparts, the Central European nations never had any notable colonies (either overseas or adjacent) due to their inland location and other factors. It has often been argued that one of the contributing causes of both World War I and World War II was Germany's lack of original overseas colonies. After ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lava
Lava is molten or partially molten rock ( magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''l ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Himmerod Abbey
Himmerod Abbey (Kloster Himmerod) is a Cistercian monastery in the community of Großlittgen in the ''Verbandsgemeinde'' of Manderscheid in the district of Bernkastel-Wittlich, Rhineland-Palatinate, Germany, located in the Eifel, in the valley of the Salm. First foundation Himmerod Abbey was founded in 1134 by Saint Bernard and is a direct foundation of Clairvaux. In its turn it founded a daughter house, Heisterbach Abbey, in 1189. The Baroque church was completed in 1751, but after secularisation from 1802 under French occupation fell into ruin. Second foundation In 1922 the monastery was re-founded by the settlement here of German Cistercian monks from the former monastery of Mariastern in the present Bosnia. The church was re-built under Abbot Vitus Recke (abbot from 1937 to 1959), and completed in 1962, and contains a famous organ by Johannes Klais. The new abbey founded the Abbey of the Holy Cross, Itaporanga near São Paulo in Brazil, in 1936. The abbey has a m ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, Rain and snow mixed, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called shower (precipitation), showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezi ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Fossil
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the abs ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |