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Externsteine
The Externsteine () is a distinctive sandstone List of rock formations, rock formation located in the Teutoburg Forest, near the town of Horn-Bad Meinberg in the Lippe district of the German state of North Rhine-Westphalia. The formation is a Tor (rock formation), tor consisting of several tall, narrow columns of rock which rise abruptly from the surrounding wooded hills. The Hermannsweg, a long-distance hiking trail, passes through the formation. In a popular tradition going back to an idea proposed to Hermann Hamelmann in 1564, the Externsteine are identified as a sacred site of the pagan Saxons, and the location of the Irminsul idol reportedly destroyed by Charlemagne; there is however no archaeological evidence that would confirm the site's use during the relevant period. The stones were used as the site of a hermitage in the Middle Ages, and by at least the high medieval period were the site of a Christian chapel. The Externsteine relief is a medieval depiction of the Desc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Externsteine Relief
The Externsteine relief is a monumental rock relief depiction of the Descent from the Cross scene, carved into the side of the Externsteine sandstone formation in the Teutoburg Forest. The Externsteine are located near Detmold, now in the German state of North Rhine-Westphalia but in the Middle Ages in the Duchy of Saxony. It is the oldest relief of this type known north of the Alps, dated to the high medieval period (likely the 12th century).Otto Schmitt: "Zur Datierung des Externsteinreliefs". In: Oswald Goetz (ed.): ''Beiträge für Georg Swarzenski zum 11. Januar 1951''. Mann, Berlin 1951, S. 26–38; Fritz Saxl: "English Sculptures of the 12th Century." ed. Hanns Swarzenski. Faber & Faber, London 1954; Otto Gaul: "Neue Forschungen zum Problem der Externsteine". In: Westfalen. 32 (1955), S. 141–164. dissenting view: Walther Matthes / Rolf Speckner. Das Relief an den Externsteinen. Ein karolingisches Kunstwerk und sein spiritueller Hintergrund. Ostfildern 1997. Descript ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Irminsul
An Irminsul (Old Saxon 'great pillar') was a sacred, Column, pillar-like object attested as playing an important role in the Germanic paganism of the Saxons. Medieval sources describe how an Irminsul was destroyed by Charlemagne during the Saxon Wars. A church was erected on its place in 783 and blessed by Pope Leo III. Sacred trees and groves in Germanic paganism and mythology, Sacred trees and sacred groves were widely venerated by the Germanic peoples (including Donar's Oak), and the oldest chronicle describing an Irminsul refers to it as a tree trunk erected in the open air.d'Alviella (1891:112). Etymology The Old Saxon word compound means 'great pillar'. The first element, ('great') is cognate with terms with some significance elsewhere in Germanic mythology. Among the North Germanic peoples, the Old Norse form of is , which just like is one of the List of names of Odin, names of Odin. Yggdrasil (Old Norse 'Yggr's horse') is a Norse cosmology, cosmic tree from which Odin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Horn-Bad Meinberg
Horn-Bad Meinberg (; Low German: '' Häoern-Möomag '') is a German city in the Lippe district in the north-east of North Rhine-Westphalia on the edge of the Teutoburg forest. The district Bad Meinberg is a spa resort. It has 17,263 inhabitants (2019). It was formed in 1970 by merging various other municipalities that had grown together, including Bad Meinberg and Horn - the new entity's original name was Bad Meinberg-Horn, before taking its present name. Horn-Bad Meinberg is the location of the Externsteine, a rock formation consisting of several tall, narrow columns. Geography In the municipality are the two highest peaks of the Eggegebirge, the Lipp Velmerstot (441 m) and the Prussian Velmerstot with about (464 m) above sea level and the highest elevation of the Teutoburg forest, the Barnacken with (446 m). The deepest point of the metropolitan area is (125 m). Between the districts Horn and Holzhausen-Externsteine is the most famous natural monument of the Teutob ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Rhine-Westphalia
North Rhine-Westphalia or North-Rhine/Westphalia, commonly shortened to NRW, is a States of Germany, state () in Old states of Germany, Western Germany. With more than 18 million inhabitants, it is the List of German states by population, most populous state in Germany. Apart from the city-states (Berlin, Hamburg and Bremen), it is also the List of German states by population density, most densely populated state in Germany. Covering an area of , it is the List of German states by area, fourth-largest German state by size. North Rhine-Westphalia features 30 of the 81 German municipalities with over 100,000 inhabitants, including Cologne (over 1 million), the state capital Düsseldorf (630,000), Dortmund and Essen (about 590,000 inhabitants each) and other cities predominantly located in the Rhine-Ruhr metropolitan area, the largest urban area in Germany and the fourth-largest on the European continent. The location of the Rhine-Ruhr at the heart of the European Blue Banana make ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teutoburger Wald
The Teutoburg Forest ( ; ) is a range of low, forested hills in the German states of Lower Saxony and North Rhine-Westphalia. Until the 17th century, the official name of the hill ridge was Osning. It was first renamed the ''Teutoburg Forest'' in 1616 in commemoration of the Battle of the Teutoburg Forest in 9 AD, which most likely took place at Kalkriese instead. Geography The Teutoburg Forest is a peripheral section in the north of the German Central Uplands, and forms a long narrow range of hills (comprising three ridges) extending from the eastern surroundings of Paderborn in the south to the western surroundings of Osnabrück in the northwest. South of the city centre of Bielefeld, a gap called the Bielefeld Pass bisects the range into the ''Northern Teutoburg Forest'' (two thirds) and ''Southern Teutoburg Forest'' (one third). In addition, the northeastern and southwestern ridges are cut by the exits of the longitudinal valleys between the ridges. The geologically oldest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teutoburg Forest
The Teutoburg Forest ( ; ) is a range of low, forested hills in the German states of Lower Saxony and North Rhine-Westphalia. Until the 17th century, the official name of the hill ridge was Osning. It was first renamed the ''Teutoburg Forest'' in 1616 in commemoration of the Battle of the Teutoburg Forest in 9 AD, which most likely took place at Kalkriese instead. Geography The Teutoburg Forest is a peripheral section in the north of the German Central Uplands, and forms a long narrow range of hills (comprising three ridges) extending from the eastern surroundings of Paderborn in the south to the western surroundings of Osnabrück in the northwest. South of the city centre of Bielefeld, a gap called the Bielefeld Pass bisects the range into the ''Northern Teutoburg Forest'' (two thirds) and ''Southern Teutoburg Forest'' (one third). In addition, the northeastern and southwestern ridges are cut by the exits of the longitudinal valleys between the ridges. The geologically ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Detmold
Detmold () is a city in North Rhine-Westphalia, Germany, with a population of . It was the capital of the small Principality of Lippe from 1468 until 1918 and then of the Free State of Lippe until 1947. Today it is the administrative center of the district of Lippe and of the Regierungsbezirk Detmold. The Church of Lippe has its central administration located in Detmold. The Reformed Redeemer Church is the preaching venue of the state superintendent of the Lippe church. History Iron Age About to the southwest of Detmold is the hill with a prehistoric circular rampart and the Hermann monument (). The monument commemorates the so-called Battle of the Teutoburg Forest, a battle in 9 AD which may or may not have been fought close to the present location of Detmold. In this encounter, Germanic tribes led by Hermann () defeated Roman legions under the command of Publius Quinctilius Varus. Middle Ages Detmold was first mentioned as ''Theotmalli'' in 783, the year of a battle be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hermannsweg
The Hermannsweg is a long hiking trail which follows the ridge of the Teutoburg Forest, running from Rheine to Velmerstot in Germany. It is marked by signposts showing a white H on a black background. The Hermannsweg is named for Arminius (German name: ''Hermann''), a Cherusci chief who defeated the Romans in the Battle of the Teutoburg Forest in 9 AD. Together with the long Eggeweg, this long-distance hiking trail forms the Hermannshöhen. It is maintained by the ''Teutoburger-Wald-Verein e.V.'', located in Bielefeld. History Parts of the way along the ridge of the Teutoburg Forest were already used by hunter-gatherers and traders in the Mesolithic period, as evidenced by findings of flint tools. In the Middle Ages, the Hermannsweg connected surrounding areas to travelling and trading routes of interregional importance such as the Westphalian ''Hellweg'' and the ''Frankfurter Weg''. The hiking trail was officially established in 1902, 25 years after the construction of the ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Rock Formations
A rock formation is an isolated, scenic, or spectacular surface rock outcrop. Rock formations are usually the result of weathering and erosion sculpting the existing rock. The term ''rock formation'' can also refer to specific sedimentary strata or other rock unit in stratigraphic and petrologic studies. A rock structure can be created in any rock type or combination: * Igneous rocks are created when molten rock cools and solidifies, with or without crystallisation. They may be either plutonic bodies or volcanic extrusive. Again, erosive forces sculpt their current forms. * Metamorphic rocks are created by rocks that have been transformed into another kind of rock, usually by some combination of heat, pressure, and chemical alteration. * Sedimentary rocks are created by a variety of processes but usually involving deposition, grain by grain, layer by layer, in water or, in the case of terrestrial sediments, on land through the action of wind or sometimes moving i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Folk Etymology
Folk etymology – also known as (generative) popular etymology, analogical reformation, (morphological) reanalysis and etymological reinterpretation – is a change in a word or phrase resulting from the replacement of an unfamiliar form by a more familiar one through popular usage. The form or the meaning of an archaic, foreign, or otherwise unfamiliar word is reinterpreted as resembling more familiar words or morphemes. The term ''folk etymology'' is a loan translation from German ''Volksetymologie'', coined by Ernst Förstemann in 1852. Folk etymology is a productive process in historical linguistics, language change, and social interaction. Reanalysis of a word's history or original form can affect its spelling, pronunciation, or meaning. This is frequently seen in relation to loanwords or words that have become archaic or obsolete. Folk/popular etymology may also refer to a popular false belief about the etymology of a word or phrase that does not lead to a change in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust and then sediment transport, transports it to another location where it is deposit (geology), deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by Solvation, dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and Wind wave, waves; glacier, glacial Plucking (glaciation), plucking, Abrasion (geology), abrasion, and scour; areal flooding; Aeolian processes, wind abrasion; groundwater processes; and Mass wastin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
