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Rauenstein (mountain)
The Rauenstein is a table hill in Saxon Switzerland in Germany. It rises west of the Elbe inside the Elbe loop near Rathen. It has a height of and drops steeply to the north into the Elbe valley. It has a deeply incised structure and is about long and wide. It thus rises almost over the surrounding area. The Rauenstein is almost completely wooded, but has several dominant sandstone rock faces. The sandstone here is very soft and heavily weathered. Location and area On the eastern side is the village of Weißig in the borough of Struppen. On the north and east side there are various climbing towers, the best known being the ''Nonne'' or ''Nonnenstein'', that is situated 200 metres from the eastern side of the Rauenstein. The rock was the site of a medieval In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the Post-classical, post-classical period of World history (field), gl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saxon Switzerland
Saxon Switzerland (german: Sächsische Schweiz) is a hilly climbing area and national park around the Elbe valley south-east of Dresden in Saxony, Germany. Together with the Bohemian Switzerland in the Czech Republic it forms the Elbe Sandstone Mountains. Saxon Switzerland alone has some 1,000 climbing peaks, as well as several hollows. The area is popular with local and international climbers. The administrative district for the area is Sächsische Schweiz-Osterzgebirge. The fortress of Königstein is a well-known landmark. Etymology The German name for Saxon Switzerland, ''Sächsische Schweiz'', appeared in the 18th century. Two Swiss artists, Adrian Zingg and Anton Graff, were appointed in 1766 to the Dresden Academy of Art. They felt the landscape was reminiscent of their homeland, the Swiss Jura, and reported in their exchange of letters on the difference between their homeland and "Saxon Switzerland". Previously, the Saxon part of the Elbe Sandstone Mountains h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saxony
Saxony (german: Sachsen ; Upper Saxon: ''Saggsn''; hsb, Sakska), officially the Free State of Saxony (german: Freistaat Sachsen, links=no ; Upper Saxon: ''Freischdaad Saggsn''; hsb, Swobodny stat Sakska, links=no), is a landlocked state of Germany, bordering the states of Brandenburg, Saxony-Anhalt, Thuringia, Bavaria, as well as the countries of Poland and the Czech Republic. Its capital is Dresden, and its largest city is Leipzig. Saxony is the tenth largest of Germany's sixteen states, with an area of , and the sixth most populous, with more than 4 million inhabitants. The term Saxony has been in use for more than a millennium. It was used for the medieval Duchy of Saxony, the Electorate of Saxony of the Holy Roman Empire, the Kingdom of Saxony, and twice for a republic. The first Free State of Saxony was established in 1918 as a constituent state of the Weimar Republic. After World War II, it was under Soviet occupation before it became part of the communist East Ger ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Table (landform)
A table or tableland is a butte, flank of a mountain, or mountain, that has a flat top. This kind of landform has numerous names, including: * Butte * Mesa * * Potrero * Tepui * Terrace * Tuya A tuya is a flat-topped, steep-sided volcano formed when lava erupts through a thick glacier or ice sheet. They are rare worldwide, being confined to regions which were covered by glaciers and had active volcanism during the same period. As lava ... Description The term "flat" is relative when speaking of tables, and often the naming or identification of a table (or table hill or mountain) is based on the appearance of the terrain feature from a distance or from below it. An example is Mesa Verde, Colorado, where the "flat top" of the mountain is both rolling terrain and cut by numerous deep canyons and arroyos, but whose rims appear quite flat from almost all directions, terminating in cliffs. External links * Landforms Mountains Geography terminology {{To ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rathen
Rathen is a village in the Elbe Sandstone Mountains, in Saxony, Germany, about southeast of Dresden. The village occupies both banks of the river Elbe and, as of 2020, has 339 inhabitants. Rathen is a popular tourist destination, the main sights are the Bastei cliffs, the Amselsee (a lake), and the outdoor theater ''"Felsenbühne Rathen"''. History Rathen was founded in the 13th century around 1261 as place for a castle fortress. During World War II, a subcamp of Flossenbürg concentration camp was located here. Tourism The state-recognised climatic spa of Rathen is not only the base for tours in the western part of Saxon Switzerland, but also for the world-famous Bastei rocks. Other popular destinations in the local Amselgrund valley are the lake of Amselsee and the Rathen Open Air Stage. There are a good 400 inhabitants on both sides of the Elbe, linked by the historic Rathen Ferry, which is a protected monument. In addition to the Old Mill of 1567, which was nearly d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Struppen
Struppen is a municipality in the Sächsische Schweiz-Osterzgebirge district, in Saxony, Germany. References Populated places in Saxon Switzerland {{SächsischeSchweizOsterzgebirge-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nonne (rocks)
The Nonne (also ''Nonnenstein'') is a roughly 18-metre-high, isolated, standing sandstone rock and climbing peak in Saxon Switzerland in Germany. The rock is located southeast of Rathen, east of the rock chain of Rauenstein. In the Middle Ages the rock was used in the 15th century as a watchtower (''Burgwarte''), similar to that on the other side of the Elbe, Neurathen Castle. To that end the rock crevice below the summit plateau was widened into an artificial cave, used as a guardhouse. On the eastern side there are more traces of hammers. In addition, an artificial, earth embankment, about 35 m long, was built. Archaeological investigations ins 1963 brought to light pieces of ceramic, the spindle whorl of a spindle, the site of a hearth and fragments of charcoal. In 1888 the Nonne was climbed for the first time for fun and without using ladders. Hitherto the rocks had always been climbed with the aid of ladders even after the watchtower had closed. The ''Alte Weg'' ("Old Way", ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Medieval
In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the Post-classical, post-classical period of World history (field), global history. It began with the fall of the Western Roman Empire and transitioned into the Renaissance and the Age of Discovery. The Middle Ages is the middle period of the three traditional divisions of Western history: classical antiquity, the medieval period, and the modern history, modern period. The medieval period is itself subdivided into the Early Middle Ages, Early, High Middle Ages, High, and Late Middle Ages. Population decline, counterurbanisation, the collapse of centralized authority, invasions, and mass migrations of tribes, which had begun in late antiquity, continued into the Early Middle Ages. The large-scale movements of the Migration Period, including various Germanic peoples, formed new kingdoms in what remained of the Western Roman Empire. In the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lilienstein
Lilienstein is a highly distinctive mountain in Saxon Switzerland, in Saxony, southeastern Germany, and was once the site of a Bohemian castle. It is one of the few table mountains on the east of the river Elbe and constitutes the symbol of the Saxon Switzerland National Park. Name The name is not related to the flower lily (German: Lilie) but is probably derived from St. Gilgen or St. Ilgen (earlier names of the mountain were „Ylgenstein“ und „Illgenstein“). These names refer to Saint Giles. Location The Lilienstein is located 15 km east of Pirna and 5 km west of Bad Schandau. It overlooks the river Elbe, which forms a 180° loop around the mountain. The Königstein Fortress Königstein Fortress (german: Festung Königstein), the "Saxony, Saxon Bastille", is a hilltop fortress near Dresden, in Saxon Switzerland, Germany, above the town of Königstein, Saxony, Königstein on the left bank of the River Elbe. It is one ... is located opposite on the left b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weißig (Struppen)
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Weißig is the name of the following places: in Saxony: * Weißig am Raschütz, municipality in the district of Meißen * Weißig (Dresden), quarter of Dresden * Weißig (Freital), municipal subdivision of Freital * Weißig (Kubschütz) quarter of Kubschütz * Weißig (Lohsa), quarter of Lohsa * Weißig (Nünchritz), quarter of Nünchritz * Weißig (Oßling), quarter of Oßling * Weißig (Struppen), quarter of Struppen in Thuringia: * Weißig (Gera), quarter of Gera in Poland: * Wysoka, Zielona Góra County * Wysokie, Lower Silesian Voivodeship Wysokie is a village in the administrative district of Gmina Rudna, within Lubin County, Lower Silesian Voivodeship, in south-western Poland. It lies approximately east of Rudna, north-east of Lubin, and north-west of the regional capital W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Saxon Switzerland
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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