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Externsteine
The Externsteine () is a distinctive sandstone 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 consisting of several tall, narrow columns of rock which rise abruptly from the surrounding wooded hills. 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 Descent from the Cross. It remains controversial whether the site was already used for Christian worship in the 8th to early 10 ...
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Externsteine Relief 1862
The Externsteine () is a distinctive sandstone 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 consisting of several tall, narrow columns of rock which rise abruptly from the surrounding wooded hills. 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 Descent from the Cross. It remains controversial whether the site was already used for Christian worship in the 8th to early 10 ...
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Externsteine Am Wiembecke-Teich
The Externsteine () is a distinctive sandstone 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 consisting of several tall, narrow columns of rock which rise abruptly from the surrounding wooded hills. 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 Descent from the Cross. It remains controversial whether the site was already used for Christian worship in the 8th to early 10t ...
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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 ...
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Irminsul
An Irminsul (Old Saxon 'great pillar') was a sacred, 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 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 names of Odin. Yggdrasil (Old Norse 'Yggr's horse') is a cosmic tree from which Odin sacrificed himself, and which connects the Nine worlds. 19th century scholar Jakob Grimm connects the name ...
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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 Teutoburg For ...
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North Rhine-Westphalia
North Rhine-Westphalia (german: Nordrhein-Westfalen, ; li, Noordrien-Wesfale ; nds, Noordrhien-Westfalen; ksh, Noodrhing-Wäßßfaale), commonly shortened to NRW (), is a States of Germany, state (''Land'') in Western Germany. With more than 18 million inhabitants, it is the List of German states by population, most populous state of Germany. Apart from the city-states, 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, Dortmund and Essen (all about 600,000 inhabitants) 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 h ...
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Teutoburger Wald
The Teutoburg Forest ( ; german: Teutoburger Wald ) 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. ...
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Teutoburg Forest
The Teutoburg Forest ( ; german: Teutoburger Wald ) 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. ...
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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 (german: Hermannsdenkmal). 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 ( la, Arminius) defeated Roman legions under the command of Publius Quinctilius Varus. Middle Ages Detmold was first mentioned as ''Theotma ...
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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 ice. Ero ...
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Hermann Hamelmann
Hermann Hamelmann (1526 – 26 June 1595) was a German Lutheran theologian and the reformer of Westphalia. Born in Osnabrück, he became the priest at Kamen in 1552. While a priest, he converted to the Evangelical Lutheran faith and announced it publicly on Trinity Sunday, 1553, and as a result he was forced to leave the town. During a stay at Wittenberg, he discussed the Lord's Supper with Philipp Melanchthon. In August 1553, he became the pastor at Bielefeld, and in 1556 he became the pastor at St. Mary's Church in Lemgo. He became General Superintendent at Bad Gandersheim in 1560, where he introduced the Reformation into Braunschweig. He was instrumental in bringing the Lutheran faith to Oldenburg after becoming Superintendent there in 1573. Along with Nikolaus Selnecker, he wrote the Oldenburg Church Order Church order is the systematically organized set of rules drawn up by a qualified body of a local church. P. Coertzen. ''Church and Order''. Belgium: Peeters. From the point ...
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