Villars Cave
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Villars Cave
The Villars Cave, in French ''Grotte de Villars'' or ''Grotte du Cluzeau'', was occupied during the Lower Magdalenian by Cro-Magnon hunter-gatherers. The cave is part of the French commune of Villars in the northern Dordogne département. Besides its enormous wealth in beautiful stalactites, stalagmites and similar calcite deposits it contains cave paintings and some engravings. The Villars Cave and the Rouffignac Cave are the biggest known cave systems in the Dordogne. Geography and geology The Villars Cave is situated 3.5 kilometres to the northeast of Villars and about 500 metres to the north-northeast of the hamlet ''Le Cluzeau''. It can be accessed via the D 82 from Villars to Saint-Saud-Lacoussière; after a right-turn at ''Le Cluzeau'' one crosses the hamlet and reaches the ample parking area on a hill. The entry of the cave is at 170 metres above sea level, somewhat below the parking area along the left-hand slope of the little stream ''Ruisseau de l'Étang Rompu ...
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Villars (Dordogne)
Villars (; oc, Vilars) is a commune in the Dordogne department in Nouvelle-Aquitaine in southwestern France. Nearby towns include Brantôme and Nontron Nontron (; oc, Nontronh ) is a Communes of France, commune in the Dordogne Departments of France, department in Nouvelle-Aquitaine in southwestern France. History The name Nontron probably derives from the Gallo-Roman personal name ''Nantironius .... Villars' attractions include the Château de Puyguilhem, Grotte de Villars and the Abbaye de Boschaud. Population See also * Communes of the Dordogne department References Communes of Dordogne {{Dordogne-geo-stub simple:Villars ...
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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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Villars Plan
Villars may refer to: Places France * Villars, Dordogne * Villars, Eure-et-Loir * Villars, Loire *Villars, Vaucluse *Villars-les-Dombes, Ain *Villars-le-Sec, Territoire de Belfort Switzerland Canton of Jura * Villars-sur-Fontenais, Fontenais Canton of Fribourg *Villars-d'Avry in Pont-en-Ogoz *Villars-sous-Mont in Bas-Intyamon *Villars-sur-Glâne *Villars-sur-Marly, Pierrafortscha Canton of Vaud * Villars-sur-Ollon *Villars Bozon, L'Isle *Bougy-Villars *Lussery-Villars *Villars-Bramard * Villars-Burquin * Villars-Epeney *Villars-le-Comte * Villars-le-Grand * Villars-le-Terroir * Villars-Mendraz *Villars-Sainte-Croix *Villars-sous-Champvent * Villars-sous-Yens * Villars-Tiercelin People *Claude Louis Hector de Villars (1653–1734), Marshal of France *Dominique Villars (1745–1814), French botanist *Felix Villars (1921–2002), biophysicist Other uses *Villars Maître Chocolatier Villars Maître Chocolatier SA is a Swiss chocolate company founded in 1901 and based in the ...
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André Leroi-Gourhan
André Leroi-Gourhan (; ; 25 August 1911 – 19 February 1986) was a French archaeology, archaeologist, paleontology, paleontologist, paleoanthropology, paleoanthropologist, and anthropology, anthropologist with an interest in technology and aesthetics and a penchant for philosophy, philosophical reflection. Biography Leroi-Gourhan completed his doctorate on the archaeology of the Pacific Ocean, North Pacific under the supervision of Marcel Mauss. Beginning in 1933 he held various positions at museums around the world, including the British Museum and the Musée de l'Homme, as well as in Japan. Between 1940 and 1944 he worked at the Musée Guimet. In 1944 he was sent to the Château de Valençay to take care of works evacuated from the Louvre, including the Venus de Milo and the Winged Victory of Samothrace. He also participated in the French resistance, for which he received the Croix de Guerre, the Médaille de la Résistance and the Légion d'honneur. In 1956 he succeeded ...
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Henri Breuil
Henri Édouard Prosper Breuil (28 February 1877 – 14 August 1961), often referred to as Abbé Breuil, was a French Catholic priest, archaeologist, anthropologist, ethnologist and geologist. He is noted for his studies of cave art in the Somme and Dordogne valleys as well as in Spain, Portugal, Italy, Ireland, China with Teilhard de Chardin, Ethiopia, British Somali Coast Protectorate, and especially Southern Africa. Life Breuil was born at Mortain, Manche, France, and was the son of Albert Breuil, magistrate, and Lucie Morio De L'Isle. He received his education at the Seminary of St. Sulpice and the Sorbonne and was ordained in 1900, and was also given permission to pursue his research interests. He was a man of deep religious faith and learning. In 1904 Breuil had recognised that a pair of 13,000-year-old carvings of reindeer at the British Museum were in fact one composition. {{DEFAULTSORT:Breuil, Henri 1877 births 1961 deaths Catholic clergy scientists French arc ...
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Archeologist
Archaeology or archeology is the scientific study of human activity through the recovery and analysis of material culture. The archaeological record consists of Artifact (archaeology), artifacts, architecture, biofact (archaeology), biofacts or ecofacts, archaeological site, sites, and cultural landscapes. Archaeology can be considered both a social science and a branch of the humanities. It is usually considered an independent academic discipline, but may also be classified as part of anthropology (in North America – the four-field approach), history or geography. Archaeologists study human prehistory and history, from the development of the first stone tools at Lomekwi in East Africa 3.3 million years ago up until recent decades. Archaeology is distinct from palaeontology, which is the study of fossil remains. Archaeology is particularly important for learning about prehistoric societies, for which, by definition, there are no written records. Prehistory includes ove ...
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Speleology
Speleology is the scientific study of caves and other karst features, as well as their make-up, structure, physical properties, history, life forms, and the processes by which they form (speleogenesis) and change over time (speleomorphology). The term ''speleology'' is also sometimes applied to the recreational activity of exploring caves, but this is more properly known as ''caving'', ''potholing'' (British English), or ''spelunking''. Speleology and caving are often connected, as the physical skills required for ''in situ'' study are the same. Speleology is a cross-disciplinary field that combines the knowledge of chemistry, biology, geology, physics, meteorology, and cartography to develop portraits of caves as complex, evolving systems. History Before modern speleology developed, John Beaumont wrote detailed descriptions of some Mendip caves in the 1680s. The term speleology was coined by Émile Rivière in 1890. Prior to the mid-nineteenth century the scientific valu ...
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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 ...
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Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ...
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Carbon Dioxide
Carbon dioxide (chemical formula ) is a chemical compound made up of molecules that each have one carbon atom covalently double bonded to two oxygen atoms. It is found in the gas state at room temperature. In the air, carbon dioxide is transparent to visible light but absorbs infrared radiation, acting as a greenhouse gas. It is a trace gas in Earth's atmosphere at 421 parts per million (ppm), or about 0.04% by volume (as of May 2022), having risen from pre-industrial levels of 280 ppm. Burning fossil fuels is the primary cause of these increased CO2 concentrations and also the primary cause of climate change.IPCC (2022Summary for policy makersiClimate Change 2022: Mitigation of Climate Change. Contribution of Working Group III to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA Carbon dioxide is soluble in water and is found in groundwater, lakes, ice caps, ...
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Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ...
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Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ...
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