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    Human Settlements and the Last Deglaciation in the French Alps

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    Author
    Evin, Jacques
    Bintz, Pierre
    Monjuvent, Guy
    Issue Date
    1994-01-01
    Keywords
    French Alps
    Stone Age
    Paleolithic
    relative age
    ice sheets
    Wurm
    France
    archaeology
    Alps
    glacial geology
    deglaciation
    Pleistocene
    upper Pleistocene
    Europe
    Western Europe
    Cenozoic
    Quaternary
    C 14
    carbon
    isotopes
    radioactive isotopes
    absolute age
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    Citation
    Evin, J., Bintz, P., & Monjuvent, G. (1994). Human settlements and the last deglaciation in the French Alps. Radiocarbon, 36(3), 345-357.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/653323
    DOI
    10.1017/S0033822200014521
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    According to most geological and geomorphological studies, the maximal advance of the Wurmian glaciers in the French Alps occurred at least before 40 ka BP and cannot be dated by 14C. Scientists believed that this dating method could be used for dating the last glacial advance and late deglaciation in the region. The scarce and scattered 14C dating results available from geological samples do not confirm an early (ca. 18 or 20 ka BP) age for the total cooling of the ice nor do they prove that residual ice sheets remained at low elevations. Attempting to solve this chronological problem, we compiled current archaeological knowledge of the oldest Late Paleolithic sites. A review of their 14C results shows that no site older than 15 ka BP (with Gravettian, Solutrean or early Magdalenian industries) can be found east of the Saone-Rhone Valley, even at low elevations. Only rare sites, dated to ca. 14.5 ka BP, may be found close to the mountain regions that were suddenly occupied around the beginning of the Bulling period (ca. 13.5 ka BP). Thus, it seems that the eastern Alps offer no evidence for direct association between glacial retreat and human settlement or simultaneous occurrence in early or late deglaciated areas.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200014521
    Scopus Count
    Collections
    Radiocarbon, Volume 36, Number 3 (1994)

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