|
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] |
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] |
Bauland Region
The Bauland is a Gäu landscape in the northeast of the German state of Baden-Württemberg. It is a natural region within the Neckar and Tauber Gäu Plateaus (major unit 12) in the South German Scarplands. Location The Bauland is a Gäu landscape in the northeast of the German state of Baden-Württemberg. It is a natural region within the Neckar and Tauber Gäu Plateaus (major unit 12) in the South German Scarplands. It lies between the Odenwald forest and the Tauber, Jagst and Neckar rivers within the counties of Main-Tauber-Kreis and Neckar-Odenwald-Kreis. It also reaches into Hohenlohekreis and the county of Heilbronn. The Bauland is no. 128 in the classification system of the ''Handbook of Natural Region Divisions of Germany''. Etymology The name ''Bauland'' goes back to the word ''Ponland'' which meant a "strip of land in which beans are cultivated" (from the Middle High German ''pône''). The Bauland is colloquially known as Baden Siberia (''Badisch Sibirien'') due to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neckar
The Neckar () is a river in Germany, mainly flowing through the southwestern state of Baden-Württemberg, with a short section through Hesse. The Neckar is a major right tributary of the Rhine. Rising in the Schwarzwald-Baar-Kreis near Schwenningen in the ''Schwenninger Moos'' conservation area at a height of above sea level, it passes through Rottweil, Rottenburg am Neckar, Kilchberg, Tübingen, Wernau, Nürtingen, Plochingen, Esslingen, Stuttgart, Ludwigsburg, Marbach, Heilbronn and Heidelberg, before discharging on average of water into the Rhine at Mannheim, at above sea level, making the Neckar its 4th largest tributary, and the 10th largest river in Germany. Since 1968, the Neckar has been navigable for cargo ships via 27 locks for about upstream from Mannheim to the river port of Plochingen, at the confluence with the Fils. From Plochingen to Stuttgart, the Neckar valley is densely populated and heavily industrialised, with several well-known companies. Between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rapeseed
Rapeseed (''Brassica napus ''subsp.'' napus''), also known as rape, or oilseed rape, is a bright-yellow flowering member of the family Brassicaceae (mustard or cabbage family), cultivated mainly for its oil-rich seed, which naturally contains appreciable amounts of erucic acid. The term ''canola'' denotes a group of rapeseed cultivars which were bred to have very low levels of erucic acid and are especially prized for use as human and animal food. Rapeseed is the third-largest source of vegetable oil and the second-largest source of protein meal in the world. Description ''Brassica napus'' grows to in height with hairless, fleshy, pinnatifid and glaucous lower leaves which are stalked whereas the upper leaves have no petioles. ''Brassica napus'' can be distinguished from ''Brassica nigra'' by the upper leaves which do not clasp the stem, and from ''Brassica rapa'' by its smaller petals which are less than across. Rapeseed flowers are bright yellow and about across. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...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] |
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] |
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] |
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] |
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] |
.jpg "Click for more on -> Karst")
