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Teufelsloch (Teufelsbäder)
The Teufelsloch ("Devil's Hole") is a karst spring near Osterode am Harz in the German state of Lower Saxony. Description The Teufelsloch is located southeast of Augustental in mature forest near the Karst Trail. It is a circular sinkhole with lustrous blue-green water. The stream that drains it feeds the Teufelsbäder moor to the west, and then flows through the Apenke to the river Söse. After heavy rain, other springs rise in the area around its banks that give the karst water in the Teufelsloch a brownish colour. The Teufelsloch lies within the Nature Reserve. Folk stories In earlier times, the Teufelsloch was perceived as something rather threatening. The origin of its shimmering blue waters rising from eerie depths could not be explained by the people. They talked of will-o'-the-wisps of human size, who would lure wanderers at night over a bent tree into the Teufelsloch. Others believed that the devil in the form of a giant one-eyed fish with a needle-sharp bite, lurked ...
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Teufelsloch Osterode
Teufelsloch may refer to: * Teufelsloch (Teufelsbäder), a sinkhole with a karst spring in the Harz Mountains of Germany near Osterode am Harz, Lower Saxony * Teufelsloch (doline), a doline in the southern Black Forest in Germany near Rheinfelden, Baden-Württemberg. * Teufelsloch (ravine), a ravine in the Swabian Jura near Bad Boll, Baden-Württemberg * Teufelsloch (Lattengebirge), the natural rock arch in the Lattengebirge near Berchtesgaden, Bavaria * The Teufelshöhle (Pottenstein), near Pottenstein, Bavaria, Germany * The Teufelshöhle (Steinau), near Steinau, Hesse, Germany * Průrva Ploučnice, the artificial, underground river course in Bohemia, Czech Republic * Devil's Hole Devils Hole is a geologic formation located in a detached unit of Death Valley National Park and surrounded by the Ash Meadows National Wildlife Refuge, in Nye County, Nevada, in the Southwestern United States. Devils Hole is habitat for the onl ..., the underground water reservoir in Nevada, US ...
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Söse
Söse is a river of Lower Saxony, Germany. It is a right tributary of the river Rhume and long. Geography The Söse rises on the plateau of ''Auf dem Acker'' in the district of Göttingen in the southwestern part of the Harz Mountains in Germany. From there it flows initially westwards; and is then impounded at a pre-dam and then by the Söse Dam between the Osterode village of Riefensbeek and the town of Osterode itself. In Osterode the river bends northwest, only to swing westwards near Badenhausen and then southwards near Eisdorf just a few kilometres west of the Harz. It flows in that direction through Osterode-Dorste before entering the westward-flowing Rhume between the villages of and , both part of the borough of Katlenburg-Lindau in the district of Northeim. Tributaries * Große Söse ''("Great Söse", left headstream)'' * Kleine Söse ''("Little Söse", right headstream)'' * Große Limpig ''(right)'' * Eipenke ''(left)'' * Ospenke ''(left)'' * Lerbach ''(r ...
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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 ...
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Karst Springs
A karst spring or karstic spring is a spring (outflow of groundwater) that is part of a karst hydrological system. Description Because of their often conical or inverted bowl shape, karst springs are also known in German-speaking lands as a ''Topf'' ("pot") which is reflected in names such as Aachtopf (the source of the Radolfzeller Aach) or Blautopf (the source of the Blau river in Blaubeuren). Karst springs often have a very high yield or discharge rate, because they are often fed by underground drainage from a large catchment basin. Because the springs are usually the terminus of a cave drainage system at the place where a river cave reaches the Earth's surface, it is often possible to enter the caves from karst springs for exploration. Large karst springs are located in many parts of the world; the largest ones are believed to be in Papua New Guinea, with others located in Mediterranean countries such as Bosnia and Herzegovina, Croatia, Turkey, Slovenia, and Italy. Types ...
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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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Lower Saxon State Department For Waterway, Coastal And Nature Conservation
The Lower Saxon Department for Water, Coastal and Nature Conservation (german: Niedersächsischer Landesbetrieb für Wasserwirtschaft, Küsten- und Naturschutz) or NLWKN is a department of the state of Lower Saxony, with its headquarters in Norden (Ostfriesland) and is responsible to the Minister for the Environment and Climate Protection. Other NLWKN services * national flood reporting service in the catchment areas of the Weser, Aller and Leine The Leine (; Old Saxon ''Lagina'') is a river in Thuringia and Lower Saxony, Germany. It is a left tributary of the Aller and the Weser and is long. The river's source is located close to the town of Leinefelde in Thuringia. About downriver, t ... * national storm surge warning service for the Lower Saxon coast * current water level data ( gauge measurements) for the Weser and Ems External links Website: NLWKN Organisations based in Lower Saxony Hydraulic engineering Coastal engineering Nature conservation in Germany
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Devil
A devil is the personification of evil as it is conceived in various cultures and religious traditions. It is seen as the objectification of a hostile and destructive force. Jeffrey Burton Russell states that the different conceptions of the devil can be summed up as 1) a principle of evil independent from God, 2) an aspect of God, 3) a created being turning evil (a ''fallen angel''), and 4) a symbol of human evil. Each tradition, culture, and religion with a devil in its mythos offers a different lens on manifestations of evil.Jeffrey Burton Russell, ''The Devil: Perceptions of Evil from Antiquity to Primitive Christianity'', Cornell University Press 1987 , pp. 41–75 The history of these perspectives intertwines with theology, mythology, psychiatry, art, and literature developing independently within each of the traditions. It occurs historically in many contexts and cultures, and is given many different names— Satan, Lucifer, Beelzebub, Mephistopheles, Iblis—and at ...
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Will-o'-the-wisp
In folklore, a will-o'-the-wisp, will-o'-wisp or ''ignis fatuus'' (, plural ''ignes fatui''), is an atmospheric ghost light seen by travellers at night, especially over bogs, swamps or marshes. The phenomenon is known in English folk belief, English folklore and much of European folklore by a variety of names, including jack-o'-lantern, friar's lantern, hinkypunk and is said to mislead travellers by resembling a flickering lamp or lantern. In literature, will-o'-the-wisp metaphorically refers to a hope or goal that leads one on, but is impossible to reach, or something one finds strange or sinister. Wills-o'-the-wisp appear in folk tales and traditional legends of numerous countries and cultures; notable wills-o'-the-wisp include St. Louis Light in Saskatchewan, the Spooklight in Southwestern Missouri and Northeastern Oklahoma, the Marfa lights of Texas, the Naga fireballs on the Mekong in Thailand, the Paulding Light in Upper Peninsula of Michigan and the Hessdalen light i ...
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Apenke
The Apenke is a left tributary of the Söse in Osterode in the Harz Mountains in the German state of Lower Saxony. Course The Apenke rises south of the Feenhöhe heights in the Bärengarten. It flows initially parallel to the Eipenke stream in a southwesterly direction. Near Augustental it is joined by more water draining from the Teufelsbäder moor. For the rest of its course the Apenke flows northwest and feeds the ponds of ''Kaiserteich'' and ''Pferdeteich''. In the Osterode town district of Petershütte it empties into the Söse. History The water power of the Apenke used to be used to drive the various water wheels for gypsum, corn and saw mills. In 1991, the Apenke was polluted in Osterode by {{cvt, 8, m3 of diesel fuel. The following is a translation of the verses (rhyming in the original German) written by Manfred Kleiner about the Apenke: :''Pure and clear all silvery bright, is the Apenke's little spring on the Harz's western rim, where I found the little beck's ...
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Quelle Am Teufelsloch
Quelle may refer to: People * Horst Matthai Quelle (1912–1999), German philosopher * Quelle Chris (born 1984), American rapper Other * Quelle (Bible), a collection of Jesus' sayings * Quelle station, in Bielefeld, Germany * Quelle-Kupferheide station, located in Bielefeld, Germany * Quelle, a German department store now part of Karstadt * Quelle AG, now part of Arcandor Arcandor AG was a holding company located in Essen, Germany, that oversaw a number of companies operating in the businesses of mail order and internet shopping, department stores and tourism services. It was formed in 1999 by the merger of Kar ... See also * {{disambiguation, given name, surname German toponymic surnames ...
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Teufelsbäder
The Teufelsbäder ("Devil's Baths") is the name of a moor landscape near Osterode am Harz in the Harz Mountains of central Germany. It lies within the nature reserve of the same name southeast of Augustental on the B 243 federal road. Description The ponds and marshy depressions in the nature reserve, which covers an area of roughly , are fed by the Teufelsloch, a karst spring in the highland forest. They are the remains of an intensive deposition of Werra anhydrites and a representative part of the gypsum karst landscape of the South Harz. The Großes and Kleines Teufelsbad ("Large and Small Devil's Bath") were formed by embankments and have become silted up fishing ponds. Their runoff empties into the Apenke stream after flowing for just a few metres. in 1980 the Lower Saxon State Office of Soil Science drilled 145 metres into the karst cavities below the anhydrite. In the hole, a steel pipe was installed from which about 1.5 litres of karst water flowed per second. With th ...
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Sinkhole
A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are locally also known as ''vrtače'' and shakeholes, and to openings where surface water enters into underground passages known as ''ponor'', swallow hole or swallet. A ''cenote'' is a type of sinkhole that exposes groundwater underneath. A ''sink'' or ''stream sink'' are more general terms for sites that drain surface water, possibly by infiltration into sediment or crumbled rock. Most sinkholes are caused by karst processes – the chemical dissolution of carbonate rocks, collapse or suffosion processes. Sinkholes are usually circular and vary in size from tens to hundreds of meters both in diameter and depth, and vary in form from soil-lined bowls to bedrock-edged chasms. Sinkholes may form gradually or suddenly, and are found worldwide. Formation Natural processes Sinkholes may capture surf ...
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