Gsengetstein
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Gsengetstein
{{Infobox mountain , name = Gsengetstein , photo = Gsengetstein mit Kirchdorf im Wald.JPG , photo_size = 282px , photo_alt = , photo_caption = The Gsengetstein and village of Kirchdorf im Wald , elevation = {{Höhe, 951, , link=false ({{convert, 951, m, ft, disp=output only, abbr=on) , elevation_ref = , isolation = , isolation_ref = , prominence = , prominence_ref = , listing = , range = Bavarian Forest , parent_peak = , location = Bavaria , map = Germany Bavaria , map_image = , map_alt = , map_caption = , map_relief = , map_size = , label = , label_position = , coordinates = {{coord, 48.9318, 13.2581, type:mountain_region:DE-BY, format=dms, display=inline,title , topo = , type = , geology = Gneiss , volcanic_arc/ ...
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Rinchnach
Rinchnach is a municipality in the Lower Bavarian district of Regen, of Germany. As of 2000, the population was 3,261. Geography Rinchnach is in the midst of the Bavarian Forest, just 7 kilometers southeast of the town Rain, and 9 kilometers south of Zwiesel. The village spreads over a wide, sunny valley at the foot of the Gsengetstein Mountain. The river Rinchnacher Ohe flows through Rinchnach. History Saint Gunther, a Benedictine monk from the Niederaltaich Abbey, created the first settlement in the central Bavarian Forest when he founded the Rinchnach monastery in 1011. The community's history is closely connected with the monastery. The municipality was destroyed and looted in the ''Rinchnach Thirty Years' War'' in 1641. This happened again in 1703 by the Swedes in the War of Spanish Succession, and yet again by the Austrians in 1742-1744 during the War of Austrian Succession War is an intense armed conflict between states, governments, societies, or paramili ...
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Bavarian Forest
The village of Zell in the Bavarian Forest The Bavarian Forest (German: ' or ''Bayerwald''; bar, Boarischa Woid) is a wooded, low-mountain region in Bavaria, Germany that is about 100 kilometres long. It runs along the Czech border and is continued on the Czech side by the Bohemian Forest (Czech: ''Šumava''). Most of the Bavarian Forest lies within the province of Lower Bavaria, but the northern part lies within Upper Palatinate. In the south it reaches the border with Upper Austria. Geologically and geomorphologically, the Bavarian Forest is part of the Bohemian Forest - the highest of the truncated highlands of the Bohemian Massif. The area along the Czech border has been designated as the Bavarian Forest National Park (240 km2), established in 1970 as the first national park in Germany. Another 3,008 km2 has been designated as the Bavarian Forest Nature Park, established 1967, and another 1,738 km2 as the Upper Bavarian Forest Nature Park, established in 1 ...
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Bavaria
Bavaria ( ; ), officially the Free State of Bavaria (german: Freistaat Bayern, link=no ), is a state in the south-east of Germany. With an area of , Bavaria is the largest German state by land area, comprising roughly a fifth of the total land area of Germany. With over 13 million inhabitants, it is second in population only to North Rhine-Westphalia, but due to its large size its population density is below the German average. Bavaria's main cities are Munich (its capital and largest city and also the third largest city in Germany), Nuremberg, and Augsburg. The history of Bavaria includes its earliest settlement by Iron Age Celtic tribes, followed by the conquests of the Roman Empire in the 1st century BC, when the territory was incorporated into the provinces of Raetia and Noricum. It became the Duchy of Bavaria (a stem duchy) in the 6th century AD following the collapse of the Western Roman Empire. It was later incorporated into the Holy Roman Empire, became an ind ...
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Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ...
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Kirchdorf Im Wald
Kirchdorf im Wald is a municipality in the district of Regen in Bavaria in Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe .... References Regen (district) Lower Bavaria {{Regendistrict-geo-stub ...
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Frauenau
Frauenau is a municipality in the district of Regen, in Bavaria, Germany. It is known for its artificial lake, which is used as a water supply of the area around Deggendorf and Passau Passau (; bar, label=Central Bavarian, Båssa) is a city in Lower Bavaria, Germany, also known as the Dreiflüssestadt ("City of Three Rivers") as the river Danube is joined by the Inn from the south and the Ilz from the north. Passau's popu .... References Regen (district) Bavarian Forest {{Regendistrict-geo-stub ...
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Summit Cross
A summit cross (german: Gipfelkreuz) is a cross on the summit of a mountain or hill that marks the top. Often there will be a summit register (''Gipfelbuch'') at the cross, either in a container or at least a weatherproof case. Various other forms of marking or symbol such as cairns, prayer flags or ovoos may be found around the world on passes and hills, in particular on sacred mountains. In the Italian Alps a Madonna is sometimes placed at the summit instead of a cross. Summit crosses are normally about two to four metres high and are usually made of wood or metal. In April 2010, the world's first glass summit cross was erected on the ''Schartwand'' (2,339 m) in Salzburg's Tennengebirge mountains. Summit crosses are mainly found in Catholic regions of the Alps, especially in Austria, Switzerland and Bavaria, mountainous regions of Poland, but also in America. They usually stand on mountains whose summits are above the tree line, but they are also found in the German Central ...
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Bundesstraße 85
The Bundesstraße 85 (abbr. B 85) runs southeast through Thuringia and Bavaria, from Kyffhäuser to Passau, near the Austrian border. B85 is approximately long. Cities and towns along B85: Berga (Kyffhäuser) – Bad Frankenhausen – Kölleda – Weimar – Rudolstadt – Saalfeld/Saale – Kronach – Kulmbach – Bayreuth – Pegnitz – Auerbach in der Oberpfalz – Sulzbach-Rosenberg – Amberg – Schwandorf – Roding – Cham – Viechtach – Regen – Schönberg (Lower Bavaria) – Passau B85 is the successor to Reichsstraße R 85, which followed a similar route: Berga (Kyffhäuser) – Bayreuth – Vilseck – Amberg – Passau. See also List of federal highways in Germany The following is a list of the German federal highways or ''Bundesstraßen''. This does not include the autobahns. Numbering system The ''Bundesstraßen'' do not have a numbering system like that used for German ''autobahns'' (motorways), but th ... External links The B85 as t ...
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Mountains Under 1000 Metres
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Mountains Of Bavaria
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Mountains Of The Bavarian Forest
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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