Keltern (Baden)
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Keltern (Baden)
Keltren is a municipality in the district of Enz in Baden-Württemberg in Germany. History The oldest documentary records for the constituent towns of Keltern are from 827 or 830 for Dietenhausen, 919 for Ellmendingen, sometime in the 11th century for Dietlingen, 1219 for Weiler, and around 1300 for Niebelsbach. The towns of Dietenhausen, Dietlingen, Ellmendingen, and Weiler were for most of their history part of Baden. They were assigned to Pforzheim's jurisdiction in 1803 when the state became the Grand Duchy of Baden. When the districts were shuffled in 1809, the four towns were assigned to the second Pforzheim Oberamt, and again remained under Pforzheim when the district was recreated as on 25 June 1938. Niebelsbach was ceded on 17 October 1806 to the Kingdom of Württemberg, under whom it was assigned to until 1 October 1938, when it was reassigned to Calw. Dietenhausen was incorporated into Ellemendingen on 1 July 1971. On 30 March 1972, all five townships were joined t ...
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Enz (district)
Enzkreis is a ''Landkreis'' (district) in the northwest of Baden-Württemberg, Germany. Neighboring districts are (from west clockwise) Karlsruhe, Heilbronn, Ludwigsburg, Böblingen and Calw. The district-free Pforzheim area in the south is nearly completely surrounded by Enz. History The district was created in 1973, when the previous district Pforzheim was merged with parts of the neighboring districts Vaihingen, Leonberg and Calw. Some part of the district Pforzheim was included into the city Pforzheim. The district Pforzheim dates back to 1939, when the ''Bezirksamt Pforzheim'' was split into the district and the district-free city. Geography The south of the Enz district covers the northern part of the Black Forest. In the north-west of the district is the Kraichgau, a mainly agricultural area. The main river is the Enz, a tributary of the Neckar. International relations Twin towns — Sister cities Since March 1993 the district has an official partnership with the Itali ...
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Black Forest
The Black Forest (german: Schwarzwald ) is a large forested mountain range in the state of Baden-Württemberg in southwest Germany, bounded by the Rhine Valley to the west and south and close to the borders with France and Switzerland. It is the source of the Danube and Neckar rivers. Its highest peak is the Feldberg with an elevation of above sea level. Roughly oblong in shape, with a length of and breadth of up to , it has an area of about 6,009 km2 (2,320 sq mi). Historically, the area was known for forestry and the mining of ore deposits, but tourism has now become the primary industry, accounting for around 300,000 jobs. There are several ruined military fortifications dating back to the 17th century. History In ancient times, the Black Forest was known as , after the Celtic deity, Abnoba. In Roman times (Late antiquity), it was given the name ("Marcynian Forest", from the Germanic word ''marka'' = "border"). The Black Forest probably represented the bo ...
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Wine Press
A winepress is a device used to extract juice from crushed grapes during wine making. There are a number of different styles of presses that are used by wine makers but their overall functionality is the same. Each style of press exerts controlled pressure in order to free the juice from the fruit (most often grapes). The pressure must be controlled, especially with grapes, in order to avoid crushing the seeds and releasing a great deal of undesirable tannins into the wine. Wine was being made at least as long ago as 4000 BC; in 2011, a winepress was unearthed in Armenia with red wine dated 6,000 years old. Press types Basket A basket press consists of a large basket filled with the crushed grapes. Pressure is applied through a plate that is forced down onto the fruit. The mechanism to lower the plate is often either a screw or a hydraulic device. The juice flows through openings in the basket. The basket style press was the first type of mechanized press to be developed, and i ...
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Viticulture
Viticulture (from the Latin word for ''vine'') or winegrowing (wine growing) is the cultivation and harvesting of grapes. It is a branch of the science of horticulture. While the native territory of ''Vitis vinifera'', the common grape vine, ranges from Western Europe to the Iran, Persian shores of the Caspian Sea, the vine has demonstrated high levels of adaptability to new environments, hence viticulture can be found on every continent except Antarctica. Duties of the viticulturist include monitoring and controlling Pest (organism), pests and Plant pathology, diseases, fertilizer, fertilizing, irrigation (wine), irrigation, canopy (grape), canopy Glossary of viticultural terms#Canopy management, management, monitoring fruit development and Typicity, characteristics, deciding when to harvest (wine), harvest, and vine pruning during the winter months. Viticulturists are often intimately involved with winemakers, because vineyard management and the resulting grape characteristics ...
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Federal Ministry Of The Interior, Building And Community
The Federal Ministry of the Interior and for Community (german: Bundesministerium des Innern und für Heimat, ; ''Heimat'' also translates to "homeland"), abbreviated , is a cabinet-level ministry of the Federal Republic of Germany. Its main office is in Berlin, with a secondary seat in Bonn. The current minister of the Interior and Community is Nancy Faeser. It is comparable to the British Home Office or a combination of the US Department of Homeland Security and the US Department of Justice, because both manage several law enforcement agencies. The BMI is tasked with the internal security of Germany. To fulfill this responsibility it maintains, among other agencies, the two biggest federal law enforcement agencies in Germany, the Federal Police and the Federal Criminal Police Office. It is also responsible for the federal domestic intelligence agency, the Federal Office for the Protection of the Constitution. History The ''Reichsamt des Innern'' (Imperial Office of th ...
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Remchingen
Remchingen () is a municipality in the Enz district, in Baden-Württemberg, Germany, situated on the river Pfinz, 14 km southeast of Karlsruhe, and 12 km northwest of Pforzheim. History Older history * 1st millennium BC: Celtic settlement (grave finds 1947 in Singen) * Roman settlement between 80 and 90 AD (numerous finds, including two pillars of denial from Nöttingen, two four-god stones immured in the churches of Nöttingen, inscription plate from the settlement Vicus Senotensis) * After the Romans fled their flight around 260 AD, the Alamanni settled the land to the right of the Rhine, but a little over two centuries later, after a great battle in 496, they were forced by the Franconian tribe to give up the Kraichgau and the landscape up to vacate the Murg. * The first written mentions of Remchingen districts date from the 8th century: On June 1, 769 in “Sigincheim im Pfinzgau” (first mention of Singen), four Franks gave Lorsch monastery a farmyard, 34 ac ...
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Normalnull
("standard zero") or (short N. N. or NN ) is an outdated official vertical datum used in Germany. Elevations using this reference system were to be marked (“meters above standard zero”). has been replaced by (NHN). History In 1878 reference heights were taken from the Amsterdam Ordnance Datum and transferred to the New Berlin Observatory in order to define the . has been defined as a level going through an imaginary point 37.000 m below . When the New Berlin Observatory was demolished in 1912 the reference point was moved east to the village of Hoppegarten (now part of the town of Müncheberg, Brandenburg, 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 betwe ...).S. German: ''Was ist "Normal-Null"?''. In: ''Physikalische Blätter'' 1958, vol 14, issue 2, p. ...
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Upper Rhine Plain
The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben (German: ''Oberrheinische Tiefebene'', ''Oberrheinisches Tiefland'' or ''Oberrheingraben'', French: ''Vallée du Rhin'') is a major rift, about and on average , between Basel in the south and the cities of Frankfurt/Wiesbaden in the north. Its southern section straddles the France–Germany border. It forms part of the European Cenozoic Rift System, which extends across Central Europe. The Upper Rhine Graben formed during the Oligocene, as a response to the evolution of the Alps to the south. It remains active to the present day. Today, the Rhine Rift Valley forms a downfaulted trough through which the river Rhine flows. Formation The Upper Rhine Plain was formed during the Early Cenozoic era, during the Late Eocene epoch. At this time, the Alpine Orogeny, the major mountain building event that was to produce the Alps, was in its early stages. The Alps were formed because the continents of Europe and Africa colli ...
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Rift
In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. Where rifts remain above sea level they form a rift valley, which may be filled by water forming a rift lake. The axis of the rift area may contain volcanic rocks, and active volcanism is a part of many, but not all, active rift systems. Major rifts occur along the central axis of most mid-ocean ridges, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates. ''Failed rifts'' are the result of continental rifting that failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to the poi ...
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Pfinz
The Pfinz is a right tributary of the Rhine in Baden-Württemberg. Its origin is located at the northern edge of the Black Forest near the Straubenhardt borough of Pfinzweiler. Near Durlach it enters the Upper Rhine Plain and continues, splitting into several beds and canals, in northwesterly direction through several towns and villages north of Karlsruhe for example Staffort. The Pfinz discharges into the Rhine near Dettenheim-Rußheim. Over the course of its path the Pfinz crosses underneath two canals: one near the Karlsruhe borough of Hagsfeld and one by Dettenheim-Rußheim. The river flows through Pfinztal and lent its name to the town of Pfinztal. The town was created by combining four previously independent villages on or near the Pfinz during the Baden-Württemberg district reform in the 1970s. The area along the river is traditionally referred to as the Pfinzgau. References External links Photos and informationabout the irrigation system in the Hardt north of K ...
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Buntsandstein
The Buntsandstein (German for ''coloured'' or ''colourful sandstone'') or Bunter sandstone is a lithostratigraphy, lithostratigraphic and allostratigraphy, allostratigraphic unit (a sequence of rock strata) in the Subsurface (geology), subsurface of large parts of west and central Europe. The Buntsandstein predominantly consists of sandstone layers of the Lower Triassic series (stratigraphy), series and is one of three characteristic Triassic units, together with the Muschelkalk and Keuper that form the Germanic Trias Supergroup (geology), Supergroup. The Buntsandstein is similar in age, sedimentary facies, facies and lithology with the Bunter (geology), Bunter of the British Isles. It is normally lying on top of the Permian Zechstein and below the Muschelkalk. In the past the name Buntsandstein was in Europe also used in a chronostratigraphy, chronostratigraphic sense, as a subdivision of the Triassic system. Among reasons to abandon this use was the discovery that its base lies a ...
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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 ...
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