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Karst Trail
The Karst Trail (german: Karstwanderweg) is a marked and signed footpath that runs for over 250 kilometres between Förste in Lower Saxony and Pölsfeld in Saxony-Anhalt through the karst landscape of the Harz, South Harz in Germany. The path runs past a number of areas of natural beauty, including caves like the Heimkehle and the Barbarossa Cave, sinkholes like the Juessee and the Schwimmende Insel (bei Pöhlde), Schwimmende Insel, depressions, moor landscapes like the Teufelsbäder, karst springs like the Rhumequelle and the Teufelsloch (Teufelsbäder), Teufelsloch, Losing stream, disappearing streams and subterranean rivers like the Bauerngraben (Harz), Bauerngraben and gypsum rocks. External linksHomepage of the Karst Trail
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Schild Karstwanderweg
Schild is a German surname meaning "shield". Notable people with the surname include: *Alfred Schild (1921–1977), American physicist *André Schild (1910–1981), Swiss linguist *Bernadette Schild (born 1990), Austrian alpine skier *Charles Schild (1902–1980), American inventor *Christina Schild, Austrian-Canadian actress *Edi Schild (born 1919), Swiss cross-country skier *Erwin Schild (born 1920), German-Canadian Conservative rabbi and author *Irving Schild, American commercial photographer *Jerry Schild, former NASCAR Cup Series driver *Marlies Schild (born 1981), Austrian alpine skier *Martina Schild (born 1981), Swiss alpine skier * Ozer Schild (1930-2006), Danish-born Israeli academic, President of the University of Haifa and President of the College of Judea and Samaria ("Ariel College"). *Rolf Schild (1924–2003), German-born British businessman *Romuald Schild (1936–2021), Polish archaeologist *Rudolph Schild, American astrophysicist *Thekla Schild (1890–1991), Germ ...
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Tourist Attractions In Lower Saxony
Tourism is travel for pleasure or business; also the theory and practice of touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tours. The World Tourism Organization defines tourism more generally, in terms which go "beyond the common perception of tourism as being limited to holiday activity only", as people "travelling to and staying in places outside their usual environment for not more than one consecutive year for leisure and not less than 24 hours, business and other purposes". Tourism can be domestic (within the traveller's own country) or international, and international tourism has both incoming and outgoing implications on a country's balance of payments. Tourism numbers declined as a result of a strong economic slowdown (the late-2000s recession) between the second half of 2008 and the end of 2009, and in consequence of the outbreak of the 2009 H1N1 influenza virus, but slowly recovered until the COVID-19 ...
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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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Hiking Trails In Germany
Hiking is a long, vigorous walk, usually on trails or footpaths in the countryside. Walking for pleasure developed in Europe during the eighteenth century.AMATO, JOSEPH A. "Mind over Foot: Romantic Walking and Rambling." In ''On Foot: A History of Walking'', 101-24. NYU Press, 2004. Accessed March 1, 2021. http://www.jstor.org/stable/j.ctt9qg056.7. Religious pilgrimages have existed much longer but they involve walking long distances for a spiritual purpose associated with specific religions. "Hiking" is the preferred term in Canada and the United States; the term "walking" is used in these regions for shorter, particularly urban walks. In the United Kingdom and the Republic of Ireland, the word "walking" describes all forms of walking, whether it is a walk in the park or backpacking in the Alps. The word hiking is also often used in the UK, along with rambling , hillwalking, and fell walking (a term mostly used for hillwalking in northern England). The term bushwalking is ende ...
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Bauerngraben (Harz)
The Bauerngraben, also called the Hungersee, is a lake in Germany between Breitungen, and Roßla in the South Harz. It is an intermittent lake of about in length and in width, into which the Glasebach disappears. A feature of this lake is its sudden disappearance from time to time, when the outlet opens due to the removal of material. The lake can then become dry for a long period. The Bauerngraben ist part of the ''Gipskarstlandschaft Questenberg'' nature reserve. The Karst Trail runs through the area. The Bauerngraben is a popular destination for day trippers and is easy to reach due to the nearby car park and easy footpaths. There is a checkpoint (no. 213) in the Harzer Wandernadel The Harzer Wandernadel is a system of hiking awards in the Harz mountains in central Germany. The hiker (or mountain biker) can earn awards at different levels of challenge by walking to the various checkpoints in the network and stamping his or ... hiking system by the lake. External links ...
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Losing Stream
A losing stream, disappearing stream, influent stream or sinking river is a stream or river that loses water as it flows downstream. The water infiltrates into the ground recharging the local groundwater, because the water table is below the bottom of the stream channel. This is the opposite of a more common ''gaining stream'' (or ''effluent stream'') which increases in water volume farther downstream as it gains water from the local aquifer. Losing streams are common in arid areas due to the climate which results in huge amounts of water evaporating from the river generally towards the mouth. Losing streams are also common in regions of karst topography where the streamwater may be completely captured by a cavern system, becoming a subterranean river. Examples There are many natural examples of subterranean rivers including: Bosnia and Herzegovina * Unac; Mušnica-Trebišnjica- Krupa/Ombla (Trebišnjica is considered to be one of the largest sinking rivers in the world; ...
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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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Rhumequelle
The Rhume Spring (german: Rhumequelle) is a large karst spring in the eastern part of the Rotenberg ridge not far from the northeastern edge of the village of Rhumspringe in the Harz mountains of Germany. It is the source of the River Rhume. Description The spring is easily accessible by a nearby road. External links – private website on the Rhume Spring (German)Description of the Rhume Springby the State Office of Mining, Energy and Geology,(pdf, 263 kb) {{Coord, 51.589656, N, 10.310175, E, type:waterbody_region:DE-NI, display=title Springs of Germany Karst springs Karst formations of Germany Landforms of Lower Saxony Eichsfeld (district) Osterode (district) Göttingen (district) Rhume Spring The Rhume Spring (german: Rhumequelle) is a large karst spring in the eastern part of the Rotenberg ridge not far from the northeastern edge of the village of Rhumspringe in the Harz mountains of Germany. It is the source of the River Rhume ...
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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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