Vestonice cluster in the context of "South Moravian Region"

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⭐ Core Definition: Vestonice cluster

Dolní Věstonice (often without diacritics as Dolni Vestonice) is an Upper Paleolithic archaeological site near the village of Dolní Věstonice in the South Moravian Region of the Czech Republic, at the base of Mount Děvín, 550 metres (1,800 ft). It dates to approximately 26,000 BP, as supported by radiocarbon dating. The site is unique in that it has been a particularly abundant source of prehistoric artifacts (especially art) dating from the Gravettian period, which spanned roughly from 27,000 to 20,000 BC. In addition to the abundance of art, this site also includes carved representations of men, women, and animals, along with personal ornaments, human burials and enigmatic engravings.

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Vestonice cluster in the context of Gravettian

The Gravettian is 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 modern-day Portugal, Spain and France, it was succeeded by the Solutrean and by the Epigravettian in Italy, the Balkans, Ukraine and Russia.

The Gravettian culture is known for their artistic works including the famous Venus figurines, which were typically carved from either ivory or limestone. The culture was first identified at the site of La Gravette in the southwestern French department of Dordogne. While historically assumed to represent a genetically homogenous group, recent analysis of ancient DNA sequences suggests that the Gravettian was produced by multiple genetically divergent groups of hunter-gatherers. Eastern Gravettian-producing groups belong to the Věstonice cluster, while western Gravettian-producing groups belong to the Fournol cluster, both of which have genetic continuity from producers of the earlier Aurignacian. Fournol cluster-related groups are thought to be the ancestors of the producers of the following Solutrean and Magdalenian cultures present in Western Europe after the Last Glacial Maximum, while the producers of the Epigravettian are genetically distinct from Gravettian-producing groups.

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