Creswell Crags is an enclosed limestone gorge on the border between Derbyshire and Nottinghamshire, England, near the villages of Creswell and Whitwell. The cliffs in the ravine contain several caves that were occupied during the last ice age, between around 43,000 and 10,000 years ago. Its caves contain the northernmost cave art in Europe. The evidence of occupation found in the rich series of sediments that accumulated over many thousands of years is regarded as internationally unique in demonstrating how prehistoric people managed to live at the extreme northernmost limits of their territory during the Late Pleistocene period.
The Chauvet-Pont-d'Arc Cave 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. 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.
The Aurignacian is an archaeological industry of the Upper Paleolithic associated with Early European modern humans (EEMH) lasting from 43,000 to 26,000 years ago. The Upper Paleolithic developed in Europe some time after the Levant, where the Emiran period and the Ahmarian period form the first periods of the Upper Paleolithic, corresponding to the first stages of the expansion of Homo sapiens out of Africa. They then migrated to Europe and created the first European culture of modern humans, the Aurignacian.
The Châtelperronian is a proposed industry of the Upper Palaeolithic, the existence of which is debated. It represents both the only Upper Palaeolithic industry made by Neanderthals and the earliest Upper Palaeolithic industry in central and southwestern France, as well as in northern Spain. It derives its name from Châtelperron, the French village closest to the type site, the cave La Grotte des Fées.
The Gravettian was an archaeological industry of the European Upper Paleolithic that succeeded the Aurignacian circa 33,000 years BP. It is archaeologically the last European culture many consider unified, and had mostly disappeared by c. 22,000 BP, close to the Last Glacial Maximum, although some elements lasted until c. 17,000 BP. In Spain and France, it was succeeded by the Solutrean, and developed into or continued as the Epigravettian in Italy, the Balkans, Ukraine and Russia.
The Upper Paleolithic is the third and last subdivision of the Paleolithic or Old Stone Age. Very broadly, it dates to between 50,000 and 12,000 years ago, according to some theories coinciding with the appearance of behavioral modernity in early modern humans, until the advent of the Neolithic Revolution and agriculture.
The Franco-Cantabrian region is a term applied in archaeology and history to refer to an area that stretches from Asturias, in northern Spain, to Aquitaine and Provence in Southern France. It includes the southern half of France and the northern strip of Spain looking at the Bay of Biscay.
Prehistoric France is the period in the human occupation of the geographical area covered by present-day France which extended through prehistory and ended in the Iron Age with the Roman conquest, when the territory enters the domain of written history.
The Grotte du Renne 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.
The Prehistoric Sites and Decorated Caves of the Vézère Valley is a UNESCO World Heritage Site in France since 1979. It specifically lists 15 prehistoric sites in the Vézère valley in the Dordogne department, mostly in and around Les Eyzies-de-Tayac-Sireuil, which has been called the "Capital of Prehistory". This valley is exceptionally rich in prehistoric sites, with more than 150 known sites including 25 decorated caves, and has played an essential role in the study of the Paleolithic era and its art. Three of the sites are the namesakes for prehistoric periods; the Micoquien, Mousterian, and Magdalenian. Furthermore, the Cro-Magnon rock shelter gave its name to the Cro-Magnon, the generic name for the European early modern humans. Many of the sites were discovered or first recognised as significant and scientifically explored by the archaeologists Henri Breuil and Denis Peyrony in the early twentieth century, while Lascaux, which has the most exceptional rock art of these, was discovered in 1940.
The Rouffignac cave, in the French commune of Rouffignac-Saint-Cernin-de-Reilhac in the Dordogne département, contains over 250 engravings and cave paintings dating back to the Upper Paleolithic. In conjunction with other caves and abris of the Vézère valley, the Rouffignac cave was classified a Monument historique in 1957 and a World Heritage Site in 1979 by UNESCO as part of the Prehistoric Sites and Decorated Caves of the Vézère Valley.
HaYonim Cave is a cave located in a limestone bluff about 250 meters above modern sea level, in the Upper Galilee, Israel.
The Caves of Gargas in the Pyrenees region of France are known for their cave art from the Upper Paleolithic period - about 27,000 years old.
Coliboaia Cave is located in Apuseni Natural Park, Câmpani, Bihor County, Romania. It may contain the oldest known cave paintings of Central Europe, radiocarbon dated to 32,000 and 35,000 years BP, corresponding to the Aurignacian and Gravettian cultures of the Paleolithic period.
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.
The Goyet Caves are a series of connected caves located in Wallonia in a limestone cliff about 15 m (50 ft) above the river Samson near the village of Mozet in the Gesves municipality of the Namur province, Belgium. The site is a significant locality of regional Neanderthal and European early modern human occupation, as thousands of fossils and artifacts were discovered that are all attributed to a long and contiguous stratigraphic sequence from 120,000 years ago, the Middle Paleolithic to less than 5,000 years ago, the late Neolithic. A robust sequence of sediments was identified during extensive excavations by geologist Edouard Dupont, who undertook the first probings as early as 1867. The site was added to the Belgian National Heritage register in 1976.
The Cave of Aurignac is an archaeological site in the commune of Aurignac, Haute-Garonne department in southwestern France. Sediment excavation and artefact documentation since 1860 confirm the idea of the arrival and permanent presence of European early modern humans during the Upper Palaeolithic. The eponymous location represents the type site of the Aurignacian, the earliest known culture attributed to modern humans in western Eurasia. Assemblages of Aurignacian tool making tradition can be found in the cultural sediments of numerous sites from around 45,000 years BP to around 26,000 years BP. In recognition of its significance for various scientific fields and the 19th-century pioneering work of Édouard Lartet the Cave of Aurignac was officially declared a national Historic Monument of France by order of May 26, 1921.
Paleolithic in the Iberian peninsula is the longest period of its prehistory, starting c. 1.3 million of years (Ma) ago and ending almost at the same time as Pleistocene, first epoch of Quaternary, c. 11.500 years or 11.5 ka ago. It was a period characterized by climate oscillations between ice ages and small interglacials, producing heavy changes in Iberia's orography. Cultural change within the period is usually described in terms of lithic industry evolution, as described by Grahame Clark.
Gallic horse, also known as Equus caballus gallicus, is a prehistoric subspecies of Equus caballus that lived in the Upper Paleolithic. It first appeared in the Aurignacian period because of climatic changes and roamed the territory of present-day France during the Gravettian and up to the end of the Solutrean. Its fossils, dated from 40 000 to around 15 000 years BC, are close to those of Equus caballus germanicus and may not correspond to a valid subspecies. First described by François Prat in 1968, it is around 1.40 m tall and differs from Equus caballus germanicus mainly in its dentition and slightly smaller size.
