Eberstadt Stalactite Cave
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Eberstadt Stalactite Cave
The Eberstadt Stalactite Cave (or Eberstadter Tropfsteinhöhle) is a German show cave located in Bauland at the transition of Southeastern Odenwald forest in the North of Baden-Württemberg. It is near Eberstadt, a District of Buchen, around east of Heidelberg and north of Stuttgart. The cave is around long, lies above sea level and is estimated to be 3 to 5 million years old. It was discovered in December 1971 after blasting operations in a Muschelkalk quarry, and opened to the public in 1973. Since then it has been used as a show cave and is one of the attractions of the "Geo-Nature park Bergstrasse-Odenwald". The cave entrance is angled several times and in some instances only high, and has halls up to high. It lies in the lower Muschelkalk and contains rich stalactite ornaments such as slender and cone-like stalagmites and sinterflags, sinterterraces and crystals. As the cave was closed after its discovery and guided tours have only used electric light, the dripstones hav ...
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Buchen
Buchen (South Franconian: ''Buche'') is a town in the German state of Baden-Württemberg. It is situated in the Odenwald low mountain range, 23 km northeast of the regional center Mosbach. Geography Buchen is situated on the seam between the south-eastern Odenwald and the Bauland area, along the Upper Germanic-Rhaetian Limes. It lies geographically in the triangle formed by the cities of Mannheim, Würzburg and Heilbronn. The precincts of the municipality lie in the Natural Park of the Neckar Valley and the Odenwald and in the Geo-Natural Park of Bergstrasse-Odenwald, at an altitude of between 250 and 500 metres. Structure of the city The municipality of Buchen (Odenwald) consists of 14 city areas: Bödigheim, Buchen-City (Buchen-Stadt), Eberstadt, Einbach, Götzingen, Hainstadt, Hettigenbeuern, Hettingen, Hollerbach, Oberneudorf, Rinschheim, Stürzenhardt, Unterneudorf and Waldhausen. The city areas cover the same areas that were occupied by the former townships with ...
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Stalactites
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground". Another example is that ''stalactites'' "hang on ''T''ight" and ''stalagmites'' "''M''ight grow up" â ...
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Show Caves In Germany
Show or The Show may refer to: Competition, event, or artistic production * Agricultural show, associated with agriculture and animal husbandry * Animal show, a judged event in the hobby of animal fancy ** Cat show ** Dog show ** Horse show ** Specialty show, a dog show which reviews a single breed *Show, an artistic production, such as: ** Concert ** Radio show ** Talk show ** Television show ** Theatre production * Trade fair or trade show Arts, entertainment, and media Films * ''The Show'' (1922 film), starring Oliver Hardy * ''The Show'' (1927 film), directed by Tod Browning * ''The Show'' (1995 film), a hip hop documentary * ''The Show'' (2017 film), an American satirical drama * ''The Show'' (2020 film), a British mystery film Album * ''Show'' (The Cure album), 1993 * ''Show'' (The Jesus Lizard album), 1994 * ''The Show'' (album), a 2008 album by eMC Songs * "The Show" (Doug E. Fresh song) * "The Show" (Girls Aloud song) * "The Show" (Lenka song) * "The ...
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Landforms Of Baden-Württemberg
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, Stratum, 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 Waterbody, waterbodies and sub-surface features. Mountains, hills, Plateau, plat ...
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Springs Of Germany
Spring(s) may refer to: Common uses * Spring (season), a season of the year * Spring (device), a mechanical device that stores energy * Spring (hydrology), a natural source of water * Spring (mathematics), a geometric surface in the shape of a helically coiled tube * Spring (political terminology), often used to name periods of political liberalization * Springs (tide), in oceanography, the maximum tide, occurs twice a month during the full and new moon Places * Spring (Milz), a river in Thuringia, Germany * Spring, Alabel, a barangay unit in Alabel, Sarangani Province, Philippines * Șpring, a commune in Alba County, Romania * Șpring (river), a river in Alba County, Romania * Springs, Gauteng, South Africa * Springs, the location of Dubai British School, Dubai United States * Springs, New York, a part of East Hampton, New York * Springs, Pennsylvania, an unincorporated community * Spring, Texas, a census-designated place * Spring District, neighborhood in Bellevue, Wash ...
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Karst Caves
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. ...
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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 ...
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Wilfried Rosendahl
Wilfried Rosendahl (born 1966) is a German bioarchaeologist, geoscientist, and cultural manager, general director of the Reiss-Engelhorn-Museums in Mannheim, and honorary professor at the Institute of History at the University of Mannheim. Life and education Wilfried Rosendahl studied geology, paleontology, prehistory and early history, and zoology at the University of Cologne The University of Cologne (german: Universität zu Köln) is a university in Cologne, Germany. It was established in the year 1388 and is one of the most prestigious and research intensive universities in Germany. It was the sixth university to ... from 1986 to 1992. Directly after receiving his diploma in 1992, he began his doctoral studies, which he completed in 1994. While still a student, Rosendahl worked on various projects at museums and curated exhibitions on natural and cultural history topics. From 1994 to 1996, Rosendahl completed a scientific traineeship at the Hessisches Landesmuseu ...
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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 th ...
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Natural Monument
A natural monument is a natural or natural/cultural feature of outstanding or unique value because of its inherent rarity, representative of aesthetic qualities or cultural significance. Under World Commission on Protected Areas guidelines, natural monuments are level III, described as: :"Areas are set aside to protect a specific natural monument, which can be a landform, sea mount, submarine cavern, geological feature such as a cave or even a living feature such as an ancient grove. They are generally quite small protected areas and often have high visitor value." This is a lower level of protection than level II (national parks) and level I (wilderness areas). The European Environment Agency's guidelines for selection of a natural monument are: * The area should contain one or more features of outstanding significance. Appropriate natural features include waterfalls, caves, craters, fossil beds, sand dunes and marine features, along with unique or representative fauna and flo ...
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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 ...
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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 ...
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