Creux Du Van
The Creux du Van is a natural rocky cirque approximately 1,400 metres wide and 150 metres deep, on the north side of Le Soliat, in the Val de Travers district in the Swiss canton of Neuchâtel. A very well known, amphitheatre-shaped natural attraction, it is at the heart of a nature reservation area of 15.5 km2. Geology The rocky arc of Creux du Van was created in three phases: Phase 1: A glacier covered the area of today's Val de Travers around 140,000 years ago ( Würm Ice Age). The stream of meltwater eroded material, making a V-shaped valley. Phase 2: During subsequent ice ages, other glaciers were created and hollowed out the valley. In warmer periods, the material was eroded by meltwater. Phase 3: After the removal of rocks from the fault, erosion of a stronger layer from a different age was much slower. See cirque for a description of the process forming features like this. The ground beneath the Creux du Van remains permanently frozen to this day ( ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Creux Du Van
The Creux du Van is a natural rocky cirque approximately 1,400 metres wide and 150 metres deep, on the north side of Le Soliat, in the Val de Travers district in the Swiss canton of Neuchâtel. A very well known, amphitheatre-shaped natural attraction, it is at the heart of a nature reservation area of 15.5 km2. Geology The rocky arc of Creux du Van was created in three phases: Phase 1: A glacier covered the area of today's Val de Travers around 140,000 years ago ( Würm Ice Age). The stream of meltwater eroded material, making a V-shaped valley. Phase 2: During subsequent ice ages, other glaciers were created and hollowed out the valley. In warmer periods, the material was eroded by meltwater. Phase 3: After the removal of rocks from the fault, erosion of a stronger layer from a different age was much slower. See cirque for a description of the process forming features like this. The ground beneath the Creux du Van remains permanently frozen to this day ( ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Würm Ice Age
The Würm is a river in Bavaria, Germany, right tributary of the Amper. The length of the river is , or including the ''Steinbach'', the main feed of Lake Starnberg. It drains the overflow from Lake Starnberg and flows swiftly through the villages of Gauting, Krailling, Planegg, Gräfelfing and Lochham as well as part of Munich (in the borough of Pasing) before joining, near Dachau, the Amper, which soon afterwards flows into the Isar and eventually flowing into the Danube. Although the Würm is not a very large river, it is well known as it gave its name to the Würm glaciation. A small man-made channel extracts water from the river at Pasing to feed the water features at Nymphenburg Palace, before flowing on to join the Isar at the public park Englischer Garten in Munich. See also *List of rivers of Bavaria A list of rivers of Bavaria, Germany: A * Aalbach * Abens * Ach * Afferbach *Affinger Bach *Ailsbach * Aisch * Aiterach *Alpbach * Alster * Altmühl * Alz *Amper * ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountains Of The Canton Of Neuchâtel
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tourist Attractions In Switzerland
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 pa ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Noiraigue
Noiraigue was a municipality in the district of Val-de-Travers in the canton of Neuchâtel in Switzerland. On 1 January 2009, the former municipalities of Boveresse, Buttes, Couvet, Fleurier, Les Bayards, Môtiers, Noiraigue, Saint-Sulpice and Travers merged to form Val-de-Travers Val-de-Travers is a municipality in the canton of Neuchâtel in Switzerland. It was created on 1 January 2009, when the former municipalities of Boveresse, Buttes, Couvet, Fleurier, Les Bayards, Môtiers, Noiraigue, Saint-Sulpice and Travers ....Amtliches Gemeindeverzeichnis der Schweiz published by the Swiss Federal Statistical Office accessed 14 January 2010 References [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Val-de-Travers
Val-de-Travers is a municipality in the canton of Neuchâtel in Switzerland. It was created on 1 January 2009, when the former municipalities of Boveresse, Buttes, Couvet, Fleurier, Les Bayards, Môtiers, Noiraigue, Saint-Sulpice and Travers merged to form Val-de-Travers.Amtliches Gemeindeverzeichnis der Schweiz published by the Swiss Federal Statistical Office accessed 14 January 2010 The region is known for its production of . History Val-de-Travers is first mentioned in 1150 as '.Geography [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Couvet
Couvet was a municipality in the district of Val-de-Travers in the canton of Neuchâtel in Switzerland. On 1 January 2009, the former municipalities of Boveresse, Buttes, Couvet, Fleurier, Les Bayards, Môtiers, Noiraigue, Saint-Sulpice and Travers merged to form the administrative district of Val-de-Travers.Amtliches Gemeindeverzeichnis der Schweiz published by the Swiss Federal Statistical Office accessed 14 January 2010 It is claimed that Couvet was the birthplace of at the end of the 18th century and it is now the home of [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lake Neuchâtel
Lake Neuchâtel (french: Lac de Neuchâtel ; frp, Lèc de Nôchâtél; german: Neuenburgersee) is a lake primarily in Romandy, in the French-speaking part of Switzerland. The lake lies mainly in the canton of Neuchâtel, but is also shared by the cantons of Vaud, Fribourg, and Bern. It comprises one of the lakes in the Three Lakes Region (French: ''Pays des Trois-Lacs'', German: ''Drei-Seen-Land''), along with lakes Biel/Bienne and Morat/Murten. With a surface of , Lake Neuchâtel is the largest lake located entirely in Switzerland and the 59th largest lake in Europe. It is long and at its widest. Its surface is above sea level, and the maximum depth is . The total water volume is . The lake's drainage area is approximately and its culminating point is Le Chasseron at . In comparison to the Lake Geneva region, the Lake Neuchatel shoreline has experienced significant economic development with the completion of the regional motorway network. It is also known to have housed ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Saint-Aubin-Sauges
Saint-Aubin-Sauges is a former municipality in the district of Boudry in the canton of Neuchâtel in Switzerland. On 1 January 2018 the former municipalities of Bevaix, Saint-Aubin-Sauges, Gorgier, Vaumarcus, Montalchez and Fresens merged into the new municipality of La Grande-Béroche. History Saint-Aubin-Sauges is first mentioned in 1176 as ''Sancti Albini''. In 1340 it was mentioned as ''villa de Sauges''. Geography Saint-Aubin-Sauges has an area, , of . Of this area, or 47.7% is used for agricultural purposes, while or 38.3% is forested. Of the rest of the land, or 13.5% is settled (buildings or roads) and or 0.3% is unproductive land.Swiss Federal Statistical Office-Land Use Statistics 2009 data accessed 25 March 2010 Of the built ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ibex
An ibex (plural ibex, ibexes or ibices) is any of several species of wild goat (genus ''Capra''), distinguished by the male's large recurved horns, which are transversely ridged in front. Ibex are found in Eurasia, North Africa and East Africa. The name ''ibex'' comes from Latin, borrowed from Iberian or Aquitanian, akin to Old Spanish ''bezerro'' "bull", modern Spanish ''becerro'' "yearling". Ranging in height from and weighing , ibex can live 20 years. Two closely related varieties of goats found in the wild are not usually called ibex: the markhor and the feral goat. A male ibex is referred to as a buck, a female is a doe, and young juveniles are called kids. An ibex buck is commonly larger and heavier than a doe. The most noticeable difference between the sexes is the larger size of a buck's horns. The doe grows a pair of smaller, thinner horns which develop considerably more slowly than those of a buck. The ibex's horns appear at birth and continue to grow through the r ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Permafrost
Permafrost is ground that continuously remains below 0 °C (32 °F) for two or more years, located on land or under the ocean. Most common in the Northern Hemisphere, around 15% of the Northern Hemisphere or 11% of the global surface is underlain by permafrost, with the total area of around 18 million km2. This includes substantial areas of Alaska, Greenland, Canada and Siberia. It can also be located on mountaintops in the Southern Hemisphere and beneath ice-free areas in the Antarctic. Permafrost does not have to be the first layer that is on the ground. It can be from an inch to several miles deep under the Earth's surface. It frequently occurs in ground ice, but it can also be present in non-porous bedrock. Permafrost is formed from ice holding various types of soil, sand, and rock in combination. Permafrost contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide, making tundra soil a carbon sink. As global war ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Meltwater
Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater can be produced during volcanic eruptions Several types of volcanic eruptions—during which lava, tephra (ash, lapilli, volcanic bombs and volcanic blocks), and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists. These are often ..., in a similar way in which the more dangerous lahars form. When meltwater pools on the surface rather than flowing, it forms melt ponds. As the weather gets colder meltwater will often re-freeze. Meltwater can collect or melt under the ice's surface. These pools of water, known as subglacial lakes can form due to geothermal heat and friction. Water source Meltwater provides drinking water for a large proportion of the world's population, as well as pro ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |