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Hermann's Cave (Harz)
Hermann's Cave (german: Hermannshöhle), together with Baumann's Cave, is one of two show caves in the village of Rübeland near the town of Wernigerode, in the district of Harz, Saxony-Anhalt, Germany. The cave was formed out of the Devonian limestone of the Elbingerode (Harz) complex during the shaping of the Bode Valley. It was discovered in 1866 during road works and was soon opened up to visitors. As a result of being protected early on its rich dripstone stalactites and stalagmites have been largely preserved. The cave is well known for, amongst other things, the discovery of numerous bones of cave bears, cave wolves and cave hyenas. The cave was comprehensively surveyed by J. H. Klooß, Robert Nehring (1888) and Dr. Ing. Friedrich Stolberg (1932). Progressive exploration since 1970 has uncovered and surveyed previously unknown chambers. See also * Olm - a species of cave salamander * List of show caves in Germany The list of show caves in Germany contains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bode Valley
The Bode Gorge (german: Bodetal) is a long ravine that forms part of the Bode valley between Treseburg and Thale in the Harz Mountains of central Germany. The German term, ''Bodetal'' (literally "Bode Valley"), is also used in a wider sense to refer to the valleys of the Warme and Kalte Bode rivers that feed the River Bode. At the Bode Gorge, the River Bode, which rises on the highest mountain in the Harz, the Brocken, has cut deeply into the hard Ramberg granite rock. The ravine is about 140 m deep at Treseburg and some 280 m deep at Thale where it breaks out into the Harz Foreland. The Bode Gorge was designated a nature reserve as early as 5 March 1937; its boundaries being subsequently expanded. With an area of, currently , it is one of the largest nature reserves in Saxony-Anhalt. Geology Apart from intrusions of Ramberg granite, which rose to the surface and solidified 300 million years ago in the Upper Carboniferous Period, and their associated veins of q ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Saxony-Anhalt
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 the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caves Of The Harz
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, microorganism ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave Hyenas
The cave hyena (''Crocuta crocuta spelaea''), also known as the Ice Age spotted hyena, was a paleosubspecies of spotted hyena which ranged from the Iberian Peninsula to eastern Siberia. It is one of the best known mammals of the Ice Age and is well represented in many European bone caves. The cave hyena was a highly specialised animal, with its progressive and regressive features being more developed than in its modern African relative. It preyed on large mammals (primarily wild horses, steppe bison and woolly rhinoceros), and was responsible for the accumulation of hundreds of large Pleistocene mammal bones in areas including horizontal caves, sinkholes, mud pits and muddy areas along rivers. The cause of the cave hyena's extinction is not fully understood, though it could have been due to a combination of factors, including climate change and competition with other predators. Description and paleoecology The main difference between the spotted hyena and the cave hyena lies in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave Wolf
The cave wolf (''Canis lupus spelaeus'') is an extinct subspecies of wolf that lived during the Late Pleistocene Ice Age. It inhabited what is now modern-day western Europe. The Don wolf (''C. l. brevis'') from eastern Europe is regarded as a taxonomic synonym, which indicates that one subspecies once lived across Europe. Taxonomy The cave wolf was first described by Georg August Goldfuss in 1823 based on a wolf pup skull found in the Zoolithen Cave located at Gailenreuth, Bavaria, Germany. In the early to middle Late Pleistocene, these large wolves existed all over Europe. They have not been studied in any degree of depth, and their relationship to modern wolves has not been clarified using DNA. All of the top predators in Europe commenced going extinct with the loss of the pleistocene megafauna when conditions became colder during the peak of the Last Glacial Maximum around 23,000 years ago. The last cave wolves used the side branches of the main caves to protect their pups fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave Bear
The cave bear (''Ursus spelaeus'') is a prehistoric species of bear that lived in Europe and Asia during the Pleistocene and became extinct about 24,000 years ago during the Last Glacial Maximum. Both the word "cave" and the scientific name ''spelaeus'' are used because fossils of this species were mostly found in caves. This reflects the views of experts that cave bears may have spent more time in caves than the brown bear, which uses caves only for hibernation. Taxonomy Cave bear skeletons were first described in 1774 by Johann Friedrich Esper, in his book ''Newly Discovered Zoolites of Unknown Four Footed Animals''. While scientists at the time considered that the skeletons could belong to apes, canids, felids, or even dragons or unicorns, Esper postulated that they actually belonged to polar bears. Twenty years later, Johann Christian Rosenmüller, an anatomist at Leipzig University, gave the species its binomial name. The bones were so numerous that most researcher ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elbingerode (Harz)
Elbingerode is an ''Ortsteil'' of Oberharz am Brocken in the Harz district, in the German state of Saxony-Anhalt. The former town was incorporated into the newly established municipality on 1 January 2010. Geography It is situated in the eastern Harz mountain range, approximately south of neighbouring Wernigerode. The former municipal area comprised Elbingerode proper as well as the villages of Königshütte and Rübeland. The surrounding mountains were the site of numerous ore mines and ironworks, today the Drei Kronen & Ehrt mine and the Büchenberg Pit, run as show mines, are popular tourist destinations. Cargo train service to several surrounding limestone pits is provided on the standard gauge Rübeland Railway link to Blankenburg, opened in 1886; the former continuation to Drei Annen Hohne station and the Harz Railway line was closed in 1965. There is a large open-cast limestone mine, the ''Tagebau Felswerke'', on the edge of the town. From checkpoint 39 on the Harzer Wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baumann's Cave
Baumann's Cave (german: Baumannshöhle), located nearby Hermann's Cave, is a show cave in Rübeland in the district of Harz and is Germany's oldest show cave. The grotto was formed in the Devonian limestone of the Elbingerode Complex at least since the Bode Valley was being shaped. The cave has been visited by man since the Stone Age and not first discovered in 1536 as many written accounts suggest. The year of discovery in 1536 in combination with the tale of the miner, Baumann, who is supposed to have discovered the cave, are part of a false story dating back to Nazi times when a politically suitable jubilee date was being sought. The cave is frequently mentioned in the early scientific and travel literature as it has been open to the public with guided tours since 1649 when Valentin Wagner was installed as first cave guide. Baumann's Cave is probably the oldest regularly frequented and guided show cave, at least in Germany. Amongst its most famous visitors was Johann Wolfgang ... [...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] |
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