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Caves Of Arcy-sur-Cure
The caves of Arcy-sur-Cure are a series of caves located on the commune of Arcy-sur-Cure, Burgundy, France. Some of them contained archaeological artefacts, from the Mousterian to Gallo-Roman times. Some hold remarkable parietal art, the second oldest presently known after those of the Chauvet cave. Another notable characteristic of these caves is the time-long series of pollen, related to determined and consistent archaeological levels. Between 1947 and 1963, they were searched by the French prehistorians Arlette and André Leroi-Gourhan. Listed ''monument historique'' (Heritage Monument) in 1992, they are partially open to the public. Location and description Arcy-sur-Cure is south-east of Auxerre, in the Yonne departement. The caves are south of Arcy-sur-Cure, on the left bank of the river Cure. At this place the river has meandered through the coral limestone substrate, creating a valley bordered by crests standing up from the present river bed. The caves are in a mea ...
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Arcy-sur-Cure
Arcy-sur-Cure (, literally ''Arcy on Cure'') is a commune in the Yonne department in Bourgogne-Franche-Comté in north-central France. The caves of Arcy-sur-Cure, just south of the commune, hold the second-oldest cave paintings known, after those of Chauvet Cave.Grottes d'Arcy-sur-CurOfficial website Archeological remains at the Grotte du Renne were taken to provide evidence that Neanderthals had modern human behavior, but this is now doubted.Higham T, Jacobi R, Julien M, David F, Basell L, Wood R, Davies W, Ramsey CB.C (2010). Chronology of the Grotte du Renne (France) and implications for the context of ornaments and human remains within the Chatelperronian. Proc Natl Acad Sci U S A. Mellars P. (2010). Neanderthal symbolism and ornament manufacture: The bursting of a bubble? Proc Natl Acad Sci U S A. See also *Communes of the Yonne department The following is a list of the 423 communes of the Yonne Yonne () is a department in the Bourgogne-Franche-Comté region in Fra ...
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Cure (river)
The Cure () is a long river in central France, a right-bank tributary of the Yonne. Its source is in Gien-sur-Cure, in the Morvan hills. It flows into the Yonne at Cravant near Vermenton. Communes crossed It crosses the following departments and towns: (from its source to its confluence): * Anost (source, Saône-et-Loire) * Planchez (Nièvre) * Gien-sur-Cure (Nièvre) * Moux-en-Morvan (lac des Settons, Nièvre) * Montsauche-les-Settons (lac des Settons, Nièvre) * Gouloux (Nièvre) * Saint-Brisson (Nièvre) * Dun-les-Places (Nièvre) * Quarré-les-Tombes (Yonne) * Marigny-l'Eglise ( lac du Crescent, Nièvre) * Saint-Germain-des-Champs (Yonne) * Chastellux-sur-Cure (Yonne) * Saint-André-en-Morvan (Nièvre) * Domecy-sur-Cure (Yonne) * Pierre-Perthuis (Yonne) * Foissy-les-Vezelay (Yonne) * Saint-Père (near Vézelay, Yonne) * Asquins (Yonne) * Montillot (Yonne) * Givry (Yonne) * Blannay (Yonne) * Sermizelles (Yonne) * Voutenay-sur-Cure (Yonne) * Saint-Moré (Yonne) * ...
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Stalactite
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground". Another example is that ''stalactites'' "hang on ''T''ight" and ''stalagmites'' "''M''ight grow up" †...
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Stalagmite
A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). The corresponding formation hanging down from the ceiling of a cave is a stalactite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground", another is that, as with ants in the pants, the mites go up and the tights (tites) come down. Formation and type Limestone stalagmites The most common stalagmites are speleothems, which usually form in limestone caves. Stalagmite formation occurs only under certain pH conditions within the cavern. They form through deposition of calcium carbonate ...
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Megaloceros Giganteus
The Irish elk (''Megaloceros giganteus''), also called the giant deer or Irish deer, is an extinct species of deer in the genus '' Megaloceros'' and is one of the largest deer that ever lived. Its range extended across Eurasia during the Pleistocene, from Ireland to Lake Baikal in Siberia. The most recent remains of the species have been carbon dated to about 7,700 years ago in western Russia. /nowiki>International_Code_of_Zoological_Nomenclature.html" ;"title="International Code of Zoological Nomenclature">/nowiki>International Code of Zoological Nomenclature">International Code of Zoological Nomenclature">/nowiki>International Code of Zoological Nomenclature/nowiki> (article 12) to validate ''Megalocerus''." The original spelling of ''Megalocerus'' was never used after its original publication.In 1844 Richard Owen named another synonym of the Irish elk, including it within the newly named subgenus ''Megaceros'', ''Cervus'' (''Megaceros'') ''hibernicus''. This has been suggested ...
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Ochre
Ochre ( ; , ), or ocher in American English, is a natural clay earth pigment, a mixture of ferric oxide and varying amounts of clay and sand. It ranges in colour from yellow to deep orange or brown. It is also the name of the colours produced by this pigment, especially a light brownish-yellow. A variant of ochre containing a large amount of hematite, or dehydrated iron oxide, has a reddish tint known as "red ochre" (or, in some dialects, ruddle). The word ochre also describes clays coloured with iron oxide derived during the extraction of tin and copper. Earth pigments Ochre is a family of earth pigments, which includes yellow ochre, red ochre, purple ochre, sienna, and umber. The major ingredient of all the ochres is iron(III) oxide-hydroxide, known as limonite, which gives them a yellow colour. * Yellow ochre, , is a hydrated iron hydroxide (limonite) also called gold ochre. * Red ochre, , takes its reddish colour from the mineral hematite, which is an anhydrous iron ...
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Lascaux
Lascaux ( , ; french: Grotte de Lascaux , "Lascaux Cave") is a network of caves near the village of Montignac, in the department of Dordogne in southwestern France. Over 600 parietal wall paintings cover the interior walls and ceilings of the cave. The paintings represent primarily large animals, typical local contemporary fauna that correspond with the fossil record of the Upper Paleolithic in the area. They are the combined effort of many generations and, with continued debate, the age of the paintings is now usually estimated at around 17,000 years (early Magdalenian). Because of the outstanding prehistoric art in the cave, Lascaux was inducted into the UNESCO World Heritage List in 1979, as an element of the ''Prehistoric Sites and Decorated Caves of the Vézère Valley''. The original caves have been closed to the public since 1963, as their condition was deteriorating, but there are now a number of replicas. History since rediscovery On 12 September 1940, the entra ...
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Chauvet Cave
The Chauvet-Pont-d'Arc Cave (french: Grotte Chauvet-Pont d'Arc, ) in the Ardèche department of southeastern France is a cave that contains some of the best-preserved figurative cave paintings in the world, as well as other evidence of Upper Paleolithic life.Clottes (2003b), p. 214. It is located near the commune of Vallon-Pont-d'Arc on a limestone cliff above the former bed of the river Ardèche, in the Gorges de l'Ardèche. Discovered on December 18, 1994, it is considered one of the most significant prehistoric art sites and the UN’s cultural agency UNESCO granted it World Heritage status on June 22, 2014. The cave was first explored by a group of three speleologists: Eliette Brunel-Deschamps, Christian Hillaire, and Jean-Marie Chauvet for whom it was named six months after an aperture now known as "Le Trou de Baba" ("Baba's Hole") was discovered by Michel Rosa (Baba). At a later date the group returned to the cave. Another member of this group, Michel Chabaud, along with tw ...
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Radiocarbon Dating
Radiocarbon dating (also referred to as carbon dating or carbon-14 dating) is a method for determining the age of an object containing organic material by using the properties of radiocarbon, a radioactive isotope of carbon. The method was developed in the late 1940s at the University of Chicago by Willard Libby. It is based on the fact that radiocarbon () is constantly being created in the Earth's atmosphere by the interaction of cosmic rays with atmospheric nitrogen. The resulting combines with atmospheric oxygen to form radioactive carbon dioxide, which is incorporated into plants by photosynthesis; animals then acquire by eating the plants. When the animal or plant dies, it stops exchanging carbon with its environment, and thereafter the amount of it contains begins to decrease as the undergoes radioactive decay. Measuring the amount of in a sample from a dead plant or animal, such as a piece of wood or a fragment of bone, provides information that can be used to calc ...
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Grotte Du Renne
The Grotte du Renne (French for "Reindeer's cave") is one of the many caves at Arcy-sur-Cure in France, an archaeological site of the Middle/Upper Paleolithic period in the Yonne departement, Bourgogne-Franche-Comté. It contains Châtelperronian lithic industry and Neanderthal remains. Grotte du Renne has been argued to provide the best evidence that Neanderthals developed aspects of modern behaviour before contact with modern humans, but this has been challenged by radiological dates, which suggest mixing of later human artifacts with Neanderthal remains. However, it has also been argued that the radiometric dates have been affected by post-recovery contamination, and statistical testing suggests the association between Neanderthal remains, Châtelperronian artefacts and personal ornaments is genuine, not the result of post-depositional processes. Site It has 15 archaeological levels that cover a depth of about 4 m. From top to base they are labelled I to XV. Those of IV, V and ...
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Magdalenian
The Magdalenian cultures (also Madelenian; French: ''Magdalénien'') are later cultures of the Upper Paleolithic and Mesolithic in western Europe. They date from around 17,000 to 12,000 years ago. It is named after the type site of La Madeleine, a rock shelter located in the Vézère valley, commune of Tursac, in France's Dordogne department. Édouard Lartet and Henry Christy originally termed the period ''L'âge du renne'' (the Age of the Reindeer). They conducted the first systematic excavations of the type site, publishing in 1875. The Magdalenian epoch is associated with reindeer hunters, although Magdalenian sites contain extensive evidence for the hunting of red deer, horses, and other large mammals present in Europe toward the end of the last glacial period. The culture was geographically widespread, and later Magdalenian sites stretched from Portugal in the west to Poland in the east, and as far north as France, the Channel Islands, England, and Wales. It is the th ...
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Solutrean
The Solutrean industry is a relatively advanced flint tool-making style of the Upper Paleolithic of the Final Gravettian, from around 22,000 to 17,000 BP. Solutrean sites have been found in modern-day France, Spain and Portugal. Details The term ''Solutrean'' comes from the type-site of " Cros du Charnier", dating to around 21,000 years ago and located at Solutré, in east-central France near Mâcon. The Rock of Solutré site was discovered in 1866 by the French geologist and paleontologist Henry Testot-Ferry. It is now preserved as the Parc archéologique et botanique de Solutré. The industry was named by Gabriel de Mortillet to describe the second stage of his system of cave chronology, following the Mousterian, and he considered it synchronous with the third division of the Quaternary period. The era's finds include tools, ornamental beads, and bone pins as well as prehistoric art. Solutrean tool-making employed techniques not seen before and not rediscovered for mil ...
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