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Öhringen
Öhringen (East Franconian: ''Ähringe'') is the largest town in Hohenlohe (district) in the state of Baden-Württemberg, in southwest Germany, near Heilbronn. Öhringen is on the railline to Schwäbisch Hall and Crailsheim. With a population of 24,374 (2019), the town is diverse. It is a quaint medieval place, and, among its ancient buildings, boasts a fine Evangelical church (german: Stiftskirche) containing carvings in cedar-wood from the 15th century and numerous interesting tombs and monuments; a Renaissance town hall; the building, now used as a library, which formerly belonged to a monastery, erected in 1034; and a palace, the former residence of the princes of Hohenlohe-Öhringen. ''Vicus Aurelii'' to the Romans. Eastwards of it runs the old limes Roman frontier wall, and numerous remains and inscriptions dating from the days of the Roman settlement have been discovered, including traces of three camps. Geography Geographical location Öhringen is located in the wes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Öhringen Keuperaufschluss
Öhringen (East Franconian: ''Ähringe'') is the largest town in Hohenlohe (district) in the state of Baden-Württemberg, in southwest Germany, near Heilbronn. Öhringen is on the railline to Schwäbisch Hall and Crailsheim. With a population of 24,374 (2019), the town is diverse. It is a quaint medieval place, and, among its ancient buildings, boasts a fine Evangelical church (german: Stiftskirche) containing carvings in cedar-wood from the 15th century and numerous interesting tombs and monuments; a Renaissance town hall; the building, now used as a library, which formerly belonged to a monastery, erected in 1034; and a palace, the former residence of the princes of Hohenlohe-Öhringen. ''Vicus Aurelii'' to the Romans. Eastwards of it runs the old limes Roman frontier wall, and numerous remains and inscriptions dating from the days of the Roman settlement have been discovered, including traces of three camps. Geography Geographical location Öhringen is located in the weste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Öhringen Stiftskirche-schloss
Öhringen (East Franconian: ''Ähringe'') is the largest town in Hohenlohe (district) in the state of Baden-Württemberg, in southwest Germany, near Heilbronn. Öhringen is on the railline to Schwäbisch Hall and Crailsheim. With a population of 24,374 (2019), the town is diverse. It is a quaint medieval place, and, among its ancient buildings, boasts a fine Evangelical church (german: Stiftskirche) containing carvings in cedar-wood from the 15th century and numerous interesting tombs and monuments; a Renaissance town hall; the building, now used as a library, which formerly belonged to a monastery, erected in 1034; and a palace, the former residence of the princes of Hohenlohe-Öhringen. ''Vicus Aurelii'' to the Romans. Eastwards of it runs the old limes Roman frontier wall, and numerous remains and inscriptions dating from the days of the Roman settlement have been discovered, including traces of three camps. Geography Geographical location Öhringen is located in the weste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohenlohe
The House of Hohenlohe () is a German princely dynasty. It ruled an immediate territory within the Holy Roman Empire which was divided between several branches. The Hohenlohes became imperial counts in 1450. The county was divided numerous times and split into several principalities in the 18th century. In 1806 the Princes of Hohenlohe lost their independence through mediatisation initialized by Napoleon, and their lands became parts of the kingdoms of Bavaria and of Württemberg by the Act of the Confederation of the Rhine (12 July 1806), a confederation of client states of the First French Empire. In 1806 the area of Hohenlohe was 1,760 km² and its estimated population was 108,000. Having lost their Imperial immediacy, the Princes of Hohenlohe still kept their private possessions. Until the German Revolution of 1918–19, just as other mediatized families, they also retained important political privileges. They were considered equal by birth (''Ebenbürtigkeit'') to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heilbronn
Heilbronn () is a List of cities and towns in Germany, city in northern Baden-Württemberg, Germany, surrounded by Heilbronn (district), Heilbronn District. With over 126,000 residents, it is the sixth-largest city in the state. From the late Middle Ages, it developed into an important trading centre. At the beginning of the 19th century, Heilbronn became one of the centres of early industrialisation in Württemberg. Heilbronn's old town was completely destroyed during the air raid of 4 December 1944 and rebuilt in the 1950s. Today Heilbronn is the economic centre of the Heilbronn-Franconia, Heilbronn-Franken region. Heilbronn is known for its wine industry and is nicknamed ''Käthchenstadt'', after Heinrich von Kleist's ''Das Käthchen von Heilbronn''. Geography Heilbronn is located in the northern corner of the Neckar Sedimentary basin, basin at the bottom of the Wartberg (Heilbronn), Wartberg (308 m). It occupies both banks of the Neckar, and the highest spot inside city limit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohenlohe (district)
The Hohenlohe (german: Hohenlohekreis ) is a ''Landkreis'' (district) in the north of Baden-Württemberg, Germany. Neighboring districts are (from north clockwise) Neckar-Odenwald, Main-Tauber, Schwäbisch Hall and Heilbronn. Künzelsau is the administrative centre of the district. Industry and companies The Hohenlohekreis is host to many internationally active companies in the screws and ventilation industries. * Würth * Stahl History The district was created in 1973 by merging the previous districts of Öhringen and Künzelsau. It was named after the Hohenlohe family, who had once ruled most of the area until 1806, when they lost their independence as this area became part of the Kingdom of Württemberg. Geography The two main rivers of the districts are the Kocher and Jagst, both tributaries of the Neckar. The highest elevation in the district, at , is the Mühlberg, near Waldenburg. Partnerships Since 1990, the district has had a partnership with the County Limeric ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waldenburg, Baden-Württemberg
Waldenburg is a hilltop town in south central Germany, eastwards of Heilbronn in the Hohenlohe (district) of Baden-Württemberg. The town is the site of Waldenburg Castle and some hilltop churches. Records first mention Waldenburg in the year 1253, but the town was destroyed in April 1945, at the end of World War II, and it has been rebuilt since. Geography Geographical form Waldenburg covers part of the natural Schwäbisch-Fränkische forest-hills and the Hohenloher-Haller Ebene. City outline Waldenburg includes the village of Waldenburg proper and the 2 sections Obersteinbach (173 people, as of 31 March 2006) and Sailach (222 people). History of Waldenburg dates from 1253. By 1330 it was a free city. Plague and war reduced the population during the Thirty Years' War. The Confederation of the Rhine of 1806 annexed Waldenburg into the Kingdom of Württemberg under the process of "mediatisation", and the town has been part of the Federal Republic of Germany state of Baden ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ohrn
Ohrn is a river of Baden-Württemberg, Germany. It is a left tributary of the Kocher near Öhringen. See also *List of rivers of Baden-Württemberg A list of rivers of Baden-Württemberg, Germany: A * Aal * Aalbach *Aalenbach * Ablach * Ach *Acher *Adelbach *Aich *Aid * Aischbach, tributary of the Kinzig * Aischbach, tributary of the Körsch * Aitrach, tributary of the Danube * Aitrach, tri ... References Rivers of Baden-Württemberg Mainhardt Forest Rivers of Germany {{BadenWürttemberg-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haller Plain
The Haller Ebene is a plain in the German state of Baden-Württemberg which forms part of the Hohenlohe Plain and stretches from Bad Mergentheim via Rothenburg, Uffenheim, Crailsheim, Öhringen as far as Schwäbisch Hall Schwäbisch Hall (; "Swabian Hall"; from 1802 until 1934 and colloquially: ''Hall'' ) is a city in the German state of Baden-Württemberg located in the valley of the Kocher river, the longest tributary (together with its headwater Lein) of the .... The Haller Ebene specifically refers to that region of the Hohenloher Ebene around the town of Schwäbisch Hall. Natural regions of Germany Regions of Baden-Württemberg Natural regions of the Neckar and Tauber Gäu Plateaus {{BadenWürttemberg-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muschelkalk
The Muschelkalk (German for "shell-bearing limestone"; french: calcaire coquillier) is a sequence of sedimentary rock strata (a lithostratigraphic unit) in the geology of central and western Europe. It has a Middle Triassic (240 to 230 million years) age and forms the middle part of the tripartite Germanic Trias, that give the Triassic its name, lying above the older Buntsandstein and below the younger Keuper. The Muschelkalk (" mussel chalk") consists of a sequence of limestone and dolomite beds. In the past, the time span in which the Muschelkalk was deposited could also be called "Muschelkalk". In modern stratigraphy, however, the name only applies to the stratigraphic unit. Occurrence The name ''Muschelkalk'' was first used by German geologist Georg Christian Füchsel (1722-1773). In 1834, Friedrich August von Alberti included it into the Triassic system. The name indicates a characteristic feature of the unit, namely the frequent occurrence of lenticular banks composed o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keuper
The Keuper is a lithostratigraphic unit (a sequence of rock strata) in the subsurface of large parts of west and central Europe. The Keuper consists of dolomite, shales or claystones and evaporites that were deposited during the Middle and Late Triassic epochs (about ). The Keuper lies on top of the Muschelkalk and under the predominantly Lower Jurassic Lias or other Early Jurassic strata. The Keuper together with the Muschelkalk and the Buntsandstein form the Germanic Trias Group, a characteristic sequence of rock strata that gave the Triassic its name. "Muschelkalk (geology)", Britannica Online Encyclopedia, October 2010, webpage: EB-39 Exposure The Upper Triassic is well exposed in Swabia, Franconia, Alsace and Lorraine and Luxembourg; it extends from Basel on the east side of the Rhine into Hanover, and through England into Scotland and north-east Ireland; it appears flanking the central plateau of France and in the Pyrenees and Sardinia. The Keuper sequence is li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Franconian German
East Franconian (german: Ostfränkisch) or Mainfränkisch, usually referred to as Franconian (') in German, is a dialect which is spoken in Franconia, the northern part of the federal state of Bavaria and other areas in Germany around Nuremberg, Bamberg, Coburg, Würzburg, Hof, Bayreuth, Meiningen, Bad Mergentheim, and Crailsheim. The major subgroups are ' (spoken in Lower Franconia and southern Thuringia), ' (spoken in Upper and Middle Franconia) and ' (spoken in some parts of Middle Franconia and Hohenlohe). In the transitional area between Rhine Franconian in the northwest and the Austro-Bavarian dialects in the southeast, East Franconian has elements of Central German and Upper German. The same goes only for South Franconian German in adjacent Baden-Württemberg. East Franconian is one of the German dialects with the highest number of speakers. The scope of East Franconian is disputed, because it overlaps with neighbouring dialects like Bavarian and Swabian in the sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
