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Dechenhöhle
The Dechen Cave (german: Dechenhöhle) in Iserlohn, Germany is one of the most visited show caves in Germany. It is located in the northern part of the Sauerland at Iserlohn (Grüne district). 360 metres of the 870-metre long cave have been laid out for visitors, beginning at the spot where, in 1868, the cave was discovered by two railway workers. The workers dropped a hammer into a rock crevice which turned out to be the entrance to a dripstone cave when they were searching for the lost tool. The cave is named after ''Oberberghauptmann'' Heinrich von Dechen (1800–1889), in recognition of his contribution to researching the geology of the Rhineland and Westphalia. Owner Due to its discovery by rail workers, the cave was first owned by the local railway company – which built the Letmathe–Fröndenberg railway – and later on by the National railway company, the last one was the Deutsche Bundesbahn. In 1983 the cave was taken over by the Mark Sauerland Touristik GmbH. Rail ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Letmathe–Fröndenberg Railway
The Letmathe–Fröndenberg railway is a two-track, partially electrified and partially disused branch line in the German state of North Rhine-Westphalia. For over 100 years it ran from Letmathe via Iserlohn station, Iserlohn, Hemer and Menden (Sauerland) station, Menden to Fröndenberg station, Fröndenberg. The section between Hemer and Iserlohn and the branch line from Hemer to Sundwig have been closed and dismantled. History The construction of its first inter-regional line by the Bergisch-Märkische Railway Company (''Bergisch-Märkische Eisenbahn-Gesellschaft'', BME) bypassed various nearby towns such as Iserlohn. In the second half of the 19th Century the BME began to provide connections from its main line, the Elberfeld–Dortmund railway, to isolated places in the western Sauerland. Iserlohn-Letmathe–Iserlohn First, the BME opened a branch line to Iserlohn station on 31 March 1864. This is also locally called the ''Iserlohner Bahn'' (Iserlohn Railway). This branc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sauerland
The Sauerland () is a rural, hilly area spreading across most of the south-eastern part of North Rhine-Westphalia, in parts heavily forested and, apart from the major valleys, sparsely inhabited. The Sauerland is the largest tourist region in North Rhine-Westphalia, in particular for mountain biking and cycling, water sports and scenic recreation. The town and Skiliftkarussell of Winterberg in the Hochsauerlandkreis is a major winter sport resort. Etymology The name ''Sauerland'' is first mentioned as ''Suderland'' in an official document from 1266. After 1400 the letter 'd' started to disappear. Therefore, Sauerland = ''southern country'' is the most convincing meaning, opposed to the theory that Sauer is from the German word ''sauer'' meaning ''sour'' (poor "sour" soil). Linguistically, "suder-“ is similar to the Old Saxon ''sûðar'' (southbound). History Before 1800 the western part of the Sauerland was part of the County of the Mark based in Altena; the eastern p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ruhr-Sieg-Express
The Ruhr-Lenne-Express (RE 16) is a Regional-Express service in the German state of North Rhine-Westphalia, running from Essen via Bochum, Witten, Bochum, Hagen and Iserlohn-Letmathe to . It is operated by DB Regio NRW hourly. History In the summer of 2001, DB Reise&Touristik abandoned InterRegio line 22, which ran from Frankfurt on the Ruhr–Sieg railway to Düsseldorf (until the summer of 1999 to Münster), continuing once a day to Norddeich Mole). The RE 16 (''Ruhr-Sieg-Express'') service was established to replace it from the timetable change of 10 June 2001 by the transport association of the Rhine-Ruhr, Ruhr-Lippe and Westfalen-Süd. The newly created service ran initially via Siegen to Au (Sieg); this branch was taken over in December 2002 by the RB 95 ( Sieg-Dill-Bahn) service operated by Deutsche Bahn and operated since December 2004 under the brand name of DreiLänderBahn. In 2004, the operations of the RE 16 was tendered together with the RB 40 (''Ruhr-Lenne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iserlohn
Iserlohn (; Westphalian: ''Iserlaun'') is a city in the Märkischer Kreis district, in North Rhine-Westphalia, Germany. It is the largest city by population and area within the district and the Sauerland region. Geography Iserlohn is located at the north end of the Sauerland near the Ruhr river, in West-Central Germany. History The Pancratius church (also called Bauernkirche) is believed to have been founded in around 985, but the first written document mentioning ''lon'' dates only from 1150. In 1237 the Count of the Mark gave Iserlohn municipal rights. In 1975 the city, which had been an urban district before, incorporated the surrounding ex-municipalities of Letmathe, Hennen, Sümmern and Kesbern, and became part of the district "Märkischer Kreis". As a larger mid-sized city, Iserlohn, however, still has a special status compared to most other municipalities in the district. This means that the city takes on tasks more usually performed by the district, such as social ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of North Rhine-Westphalia
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Formations Of Germany
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 earlie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Caves
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 limestone c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of Germany
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Show Caves In Germany
The list of show caves in Germany contains all 51 show caves in Germany which are hosted by the German Speleological Federation. (german: Verband der Deutschen Höhlen- and Karstforscher) Background As of 2008, there have been 51 show caves in Germany, which are hosted by the German Speleological Federation (german: Verband der Deutschen Höhlen- and Karstforscher). A show cave is defined as any cave equipped for tourists, by having walkways or steps, fitted with lighting, or supplying gear, as examples. Show caves have regular opening times, usually with regular guided tours of about 30 to 45 minutes duration and are almost all electrically lighted. Only the Easter Cave and the Schellenberg Ice Cave still use carbide lamps. In 1884 the Olga Cave was the first German show cave to be equipped with electrical lighting and the second in the world to be thus fitted. Only the Kraus Cave in the Styria in Austria was equipped earlier, in 1883. Not included on this list are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Abellio Deutschland
Abellio Deutschland is a public transit operator in Germany operating bus and rail networks. Headquartered in Berlin, it is a subsidiary of the Dutch state-owned Abellio. History Abellio Deutschland was formed by the Essen public transit company ( EVAG, today part of Ruhrbahn) in 2004. In 2005, British investment company Star Capital Partners purchased a 75% share in Abellio from the City of Essen. In December 2008, both sold their shares to NedRailways. The Abellio brand was later rolled out to replace the NedRailways brand internationally. Operations Rail As of December 2016, Abellio Deutschland operated 18 lines over 978 kilometres with a fleet of 86 trains.Welcome to Abellio Abellio February 2017 Abellio Rail NRW Abellio Rail NRW was founded i ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deutsche Bundesbahn
The Deutsche Bundesbahn or DB (German Federal Railway) was formed as the state railway of the newly established Federal Republic of Germany (FRG) on 7 September 1949 as a successor of the Deutsche Reichsbahn-Gesellschaft (DRG). The DB remained the state railway of West Germany until after German reunification, when it was merged with the former East German Deutsche Reichsbahn (DR) to form Deutsche Bahn, which came into existence on 1 January 1994. Background After World War II, each of the military governments of the Allied Occupation Zones in Germany were ''de facto'' in charge of the German railways in their respective territories. On 10 October 1946, the railways in the British and American occupation zones formed the ''Deutsche Reichsbahn im Vereinigten Wirtschaftsgebiet'' (German Imperial Railway in the united economic area), while on 25 June 1947, the provinces under French occupation formed the Südwestdeutsche Eisenbahn. With the formation of the FRG these succe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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