Black Moor (Rhön)
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Black Moor (Rhön)
The Black Moor (german: Schwarzes Moor) is an important internationally recognised wetland located in the Bavarian Rhön Mountains at the tripoint of the German states of Hesse, Thuringia and Bavaria. It is part of UNESCO's Rhön Biosphere Reserve and has an area of 66.4 hectares. It is thus the largest bog complex in the Rhön. Much of the moor is a largely undisturbed and intact raised bog. It is part of the Europe-wide conservation system, Natura 2000, and one of the most important raised bogs in Central Europe. The Black Moor lies on the watershed between the Rhine and Weser rivers. In 2007 the Black Moor was included in the List of the 100 most beautiful geotopes in Bavaria. The Black Moor is an eccentric, cupola-shaped, raised bog. Its surface appearance resembles that of the northern kermi bogs. From its central plateau which lies near the higher edge of the bog in the north, where the peat is up to 8 metres thick in places, the surface of the terrain falls away ...
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Rhine
), Surselva, Graubünden, Switzerland , source1_coordinates= , source1_elevation = , source2 = Rein Posteriur/Hinterrhein , source2_location = Paradies Glacier, Graubünden, Switzerland , source2_coordinates= , source2_elevation = , source_confluence = Reichenau , source_confluence_location = Tamins, Graubünden, Switzerland , source_confluence_coordinates= , source_confluence_elevation = , mouth = North Sea , mouth_location = Netherlands , mouth_coordinates = , mouth_elevation = , progression = , river_system = , basin_size = , tributaries_left = , tributaries_right = , custom_label = , custom_data = , extra = The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label= Sursilvan, Rein, rm, label= Sutsilvan and Surmiran, Ragn, rm, label=Rumantsch Grischun, Vallader and Puter, Rain; it, Reno ; gsw, Rhi(n), inclu ...
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High Rhön Road
The High Rhön Road (german: Hochrhönstraße) runs through the Bavarian Rhön from Bischofsheim an der Rhön to Fladungen (south to north). It bears the Landesstraße, state road number St 2288, is 25 kilometres long, runs over the central highlands of the Rhön, known as the Long Rhön, and is an important communication link in the High Rhön. In winter the High Rhön Road in the Long Rhön is often closed due to heavy snowfall and winds that block the road with snowdrifts. History The High Rhön Road was planned in the 1930s and construction began at the outset of the Second World War. The work was carried out by the Reichsarbeitsdienst, but it was gravelled and not tarmacked until after the end of the war. The counties of Landkreis Bad Neustadt an der Saale, Bad Neustadt and Landkreis Mellrichstadt, Mellrichstadt agreed in 1958 to take over the road and upgrade it. With considerably help from the treasury of the Free State of Bavaria Bavaria ( ; ), officially the F ...
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Fladungen
Fladungen is a town in the Rhön-Grabfeld district, in Bavaria, Germany. It is situated in the Rhön Mountains, 11 km northwest of Ostheim, 20 km west of Meiningen, and 33 km east of Fulda. It is the northernmost town in Bavaria, bordering Hesse to the northwest and Thuringia to the northeast. Fladungen lies at the southern edge of the Rhön Mountains, and the Rhön Biosphere Reserve begins a few kilometers outside of town. It is at the head of the river Streu, which flows southeast through it to join the Franconian Saale near Bad Neustadt. The region around the town is popular for hiking and cycling, especially in the summer and early autumn. The town is a service center for the surrounding agricultural region. There are also some small industries, including a cement factory and a biogas plant. The 2009 population was estimated at just over 2,100. History Fladungen first appears in a public record in 789 AD; the town was granted "Stadtrechte" (city r ...
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Hausen (Rhön)
Hausen may refer to: Places in Germany Bavaria *Hausen, Miltenberg, in the Miltenberg district * Hausen, Lower Bavaria, in the Kelheim district *Hausen, Upper Franconia, in the Forchheim district * Hausen, Rhön-Grabfeld, in the Rhön-Grabfeld district * Hausen, Villenbach * Hausen, Greding, a locality in Greding, district of Roth *Hausen bei Würzburg, in the Würzburg district *Hausen bei Aindling, a locality of Aichach-Friedberg *Hausen bei Augsburg, a locality in Diedorf, district of Augsburg *Hausen bei Bad Kissingen, a locality in Bad Kissingen Baden-Württemberg *, in Sigmaringen district, in the former Principality of Fürstenberg *Hausen am Tann, in Zollernalbkreis district *Hausen vor Wald, in Schwarzwald-Baar-Kreis district *Hausen im Wiesental, in Lörrach district *, in Heilbronn district on the Württemberger Weinstraße *Hausen an der Möhlin, ''Ortsteil'' of Bad Krozingen, Breisgau-Hochschwarzwald Hesse *Hausen (Frankfurt am Main); a city district of Frankfurt ...
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Lower Franconia
Lower Franconia (german: Unterfranken) is one of seven districts of Bavaria, Germany. The districts of Lower, Middle and Upper Franconia make up the region of Franconia. History After the founding of the Kingdom of Bavaria the state was totally reorganised and, in 1808, divided into 15 administrative government regions (German: , singular ), in Bavaria called (singular: ). They were created in the fashion of the French departements, quite even in size and population, and named after their main rivers. In the following years, due to territorial changes (e. g. loss of Tyrol, addition of the Palatinate), the number of Kreise was reduced to 8. One of these was the Untermainkreis (Lower Main District). In 1837 king Ludwig I of Bavaria renamed the Kreise after historical territorial names and tribes of the area. This also involved some border changes or territorial swaps. Thus the name Untermainkreis changed to Lower Franconia and Aschaffenburg, but the city name was dropped in the ...
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Flark
A flark is a depression or hollow within a bog. Flarks typically occur as a series of parallel depressions, separated by intervening ridges known as strings. Early theories suggested that flarks were formed by frost heaving, but flarks have since been found in areas where frost heaving does not occur. Flarks are now thought to form when the peat Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficien ... that forms the base of the bog becomes so thick that it slides downslope due to its own weight. Irregularities in the underlying terrain halt the slide of the peat, causing flarks to form downslope from the obstruction as the downslope peat tears away from the portion of the peat mass held back by the underlying obstruction. Another theory suggests that flarks are formed by areas within ...
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Rectangular
In Euclidean geometry, Euclidean plane geometry, a rectangle is a quadrilateral with four right angles. It can also be defined as: an equiangular quadrilateral, since equiangular means that all of its angles are equal (360°/4 = 90°); or a parallelogram containing a right angle. A rectangle with four sides of equal length is a ''square''. The term "wikt:oblong, oblong" is occasionally used to refer to a non-square rectangle. A rectangle with Vertex (geometry), vertices ''ABCD'' would be denoted as . The word rectangle comes from the Latin ''rectangulus'', which is a combination of ''rectus'' (as an adjective, right, proper) and ''angulus'' (angle). A #Crossed rectangles, crossed rectangle is a crossed (self-intersecting) quadrilateral which consists of two opposite sides of a rectangle along with the two diagonals (therefore only two sides are parallel). It is a special case of an antiparallelogram, and its angles are not right angles and not all equal, though opposite angles ...
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Cupola (geometry)
In geometry, a cupola is a solid formed by joining two polygons, one (the base) with twice as many edges as the other, by an alternating band of isosceles triangles and rectangles. If the triangles are equilateral and the rectangles are squares, while the base and its opposite face are regular polygons, the triangular, square, and pentagonal cupolae all count among the Johnson solids, and can be formed by taking sections of the cuboctahedron, rhombicuboctahedron, and rhombicosidodecahedron, respectively. A cupola can be seen as a prism where one of the polygons has been collapsed in half by merging alternate vertices. A cupola can be given an extended Schläfli symbol representing a regular polygon joined by a parallel of its truncation, or Cupolae are a subclass of the prismatoids. Its dual contains a shape that is sort of a weld between half of an -sided trapezohedron and a -sided pyramid. Examples The above-mentioned three polyhedra are the only non-trivial convex ...
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