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Gouffre Berger
The Gouffre Berger is a French cave discovered on 24 May 1953 by Joseph Berger, Bouvet, Ruiz de Arcaute and Marc Jouffrey. From 1953 to 1963, it was regarded as the deepest cave in the world at , relinquishing this title to the previous contender, Pierre Saint Martin, in 1964, after further exploration. The Gouffre Berger is now ranked 37th deepest cave in the world, and the 4th in France. To return from the bottom of the cave back to the surface can take between 15 and 30 hours, without long breaks. In 1967, Ken Pearce, a metallurgy lecturer from Britain, descended with the Pegasus Caving Club team from Nottingham UK, organised and led by Peter Watkinson, and along with a dive, reached a depth of . They emerged after 13 days underground, having set a new world record at the time. In 1968, B Leger and J Dubois reached a depth of . This record was held until July 1982, when Patrick Penez attained . In 1990, a breakthrough was made, connecting the cave to the nearby "Scialet de la ...
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Vercors Plateau
The Vercors Massif is a range in France consisting of rugged plateaus and mountains straddling the ''départements'' of Isère and Drôme in the French Prealps. It lies west of the Dauphiné Alps, from which it is separated by the rivers Drac and Isère. The cliffs at the massif's eastern limit face the city of Grenoble. Background Over time, various features of the complex geography have been recognised including, the Quatre Montagnes (four mountains), the Coulmes (gorges), the Vercors Drômois (Drome Vercors), the Hauts-Plateaux (high plateaus) and, in the foothills, Royans, Gervanne, Diois, and Trièves. The massif is sometimes called the "fortress." The movement of people tends to be between the massif and the surrounding plains rather than between the various parts of the massif itself. Until the mid twentieth century, the name ''Vercors'' was used to describe only the township of La Chapelle-en-Vercors (with Royans), and the northern area around Lans-en-Vercors, Vill ...
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Vercors Cave System
The Vercors Massif is a range in France consisting of rugged plateaus and mountains straddling the ''départements'' of Isère and Drôme in the French Prealps. It lies west of the Dauphiné Alps, from which it is separated by the rivers Drac and Isère. The cliffs at the massif's eastern limit face the city of Grenoble. Background Over time, various features of the complex geography have been recognised including, the Quatre Montagnes (four mountains), the Coulmes (gorges), the Vercors Drômois (Drome Vercors), the Hauts-Plateaux (high plateaus) and, in the foothills, Royans, Gervanne, Diois, and Trièves. The massif is sometimes called the "fortress." The movement of people tends to be between the massif and the surrounding plains rather than between the various parts of the massif itself. Until the mid twentieth century, the name ''Vercors'' was used to describe only the township of La Chapelle-en-Vercors (with Royans), and the northern area around Lans-en-Vercors, Vill ...
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Vercors Massif
The Vercors Massif is a Mountain range, range in France consisting of rugged plateaus and mountains straddling the ''département in France, départements'' of Isère and Drôme in the French Prealps. It lies west of the Dauphiné Alps, from which it is separated by the rivers Drac (river), Drac and Isère (river), Isère. The cliffs at the massif's eastern limit face the city of Grenoble. Background Over time, various features of the complex geography have been recognised including, the Quatre Montagnes (four mountains), the Coulmes (gorges), the Vercors Drômois (Drome Vercors), the Hauts-Plateaux (high plateaus) and, in the foothills, Royans, Gervanne, Diois, and Trièves. The massif is sometimes called the "fortress." The movement of people tends to be between the massif and the surrounding plains rather than between the various parts of the massif itself. Until the mid twentieth century, the name ''Vercors'' was used to describe only the township of La Chapelle-en-Vercor ...
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Cave
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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List Of Caves In France
The following article shows a List of caves in France: Caves * Bédeilhac cave * Bétharram caves * Bournillon cave, the highest cave opening in Europe. Part of the Vercors Cave System * Bruniquel Cave, an archaeological site dated at 176,000 years with stalagmite rings constructed by Neanderthal men * , near Carcassonne (city) * Chauvet Cave, and its replica (for protection) Pont-d'Arc cave * Cosquer Cave, only sub-marine access), (its replica is in construction). * Font-de-Gaume cave, near Les Eyzies-de-Tayac-Sireuil * , * Gargas caves * , near Les Eyzies-de-Tayac-Sireuil * Savonnières caves * St-Médard-de-Presque cave * Grotte des Demoiselles, near Nîmes * , near Nice (city) * Jean Bernard cave system, in competition as world's deepest cave * Grotte des Fées cave * La Mansonnière cave, one of the longest chalk caves * , near Alès (city) * La Verna cave, part of the * Lascaux Cave * Les Combarelles cave * Lombrives caves, this cave network is one of the m ...
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Metallurgy
Metallurgy is a domain of materials science and engineering that studies the physical and chemical behavior of metallic elements, their inter-metallic compounds, and their mixtures, which are known as alloys. Metallurgy encompasses both the science and the technology of metals; that is, the way in which science is applied to the production of metals, and the engineering of metal components used in products for both consumers and manufacturers. Metallurgy is distinct from the craft of metalworking. Metalworking relies on metallurgy in a similar manner to how medicine relies on medical science for technical advancement. A specialist practitioner of metallurgy is known as a metallurgist. The science of metallurgy is further subdivided into two broad categories: chemical metallurgy and physical metallurgy. Chemical metallurgy is chiefly concerned with the reduction and oxidation of metals, and the chemical performance of metals. Subjects of study in chemical metallurgy include mi ...
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Communes Of France
The () is a level of administrative division in the French Republic. French are analogous to civil townships and incorporated municipalities in the United States and Canada, ' in Germany, ' in Italy, or ' in Spain. The United Kingdom's equivalent are civil parishes, although some areas, particularly urban areas, are unparished. are based on historical geographic communities or villages and are vested with significant powers to manage the populations and land of the geographic area covered. The are the fourth-level administrative divisions of France. vary widely in size and area, from large sprawling cities with millions of inhabitants like Paris, to small hamlets with only a handful of inhabitants. typically are based on pre-existing villages and facilitate local governance. All have names, but not all named geographic areas or groups of people residing together are ( or ), the difference residing in the lack of administrative powers. Except for the municipal arrondi ...
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Engins
Engins () is a commune in the Isère department in southeastern France. Population See also *Communes of the Isère department *Parc naturel régional du Vercors The Vercors Regional Natural Park (French: ''Parc naturel régional du Vercors'') is a protected area of forested mountains in the Rhône-Alpes region of southeastern France. Geography Set upon a limestone plateau south of Grenoble, the park ext ... References External links Official site Communes of Isère Isère communes articles needing translation from French Wikipedia {{Isère-geo-stub ...
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Coupe Développée 2020 Du Réseau Du Gouffre Berger POUR Wikipédia (10)
A coupe or coupé (, ) is a passenger car with a sloping or truncated rear roofline and two doors. The term ''coupé'' was first applied to horse-drawn carriages for two passengers without rear-facing seats. It comes from the French past participle of ''couper'', "cut". __TOC__ Etymology and pronunciation () is based on the past participle of the French verb ("to cut") and thus indicates a car which has been "cut" or made shorter than standard. It was first applied to horse-drawn carriages for two passengers without rear-facing seats. These or ("clipped carriages") were eventually clipped to .. There are two common pronunciations in English: * () – the anglicized version of the French pronunciation of ''coupé''. * () – as a spelling pronunciation when the word is written without an accent. This is the usual pronunciation and spelling in the United States, with the pronunciation entering American vernacular no later than 1936 and featuring in the Beach Boys' hit ...
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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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Fernand Petzl
Fernand Petzl (April 7, 1913 – May 31, 2003) was a caver and manufacturer of outdoor equipment under the brand name Petzl. Petzl lived most of his life in the village of Saint-Ismier (near Grenoble), France at the foot of the mountain Dent De Crolles. He first went caving in Trou du Glaz in 1933, and was immediately captivated by the idea of exploring beyond the cave's known limits. Subsequent explorations there with Pierre Chevalier, Charles Petit-Didier and others culminated in connections to other caves in the massif, forming the Réseau de la Dent de Crolles which, in 1947, became the deepest cave in the world. Petzl also participated in explorations in the Gouffre Berger The Gouffre Berger is a French cave discovered on 24 May 1953 by Joseph Berger, Bouvet, Ruiz de Arcaute and Marc Jouffrey. From 1953 to 1963, it was regarded as the deepest cave in the world at , relinquishing this title to the previous contender, ..., which set a new world depth record in 1956 as the ...
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Rimstone
Rimstone, also called gours, is a type of speleothem (cave formation) in the form of a stone dam. Rimstone is made up of calcite and other minerals that build up in cave pools. The formation created, which looks like stairs, often extends into flowstone above or below the original rimstone. Often, rimstone is covered with small, micro-gours on horizontal surfaces. Rimstone basins may form terraces that extend over hundreds of feet, with single basins known up to 200 feet long from Tham Xe Biang Fai in Laos. Formation Rimstone dams form where there is some gradient, and hence flow, over the edge of a pool. Crystallization begins to occur at the air/water/rock interface. The turbulence caused by flow over the edge of the building dam may contribute to the outgassing or loss of carbon dioxide from water, and result in precipitation of mineral on this edge. When dams form under running water, they tend to be higher when the passage is steeper. Shallow-gradient dams tend to be lower a ...
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