Late Holocene glacial and periglacial evolution in the upper Orco Valley, northwestern Italian Alps
Abstract: The sediments present in some areas of the Orco Valley provide indications on climatic variations that occurred during the last 6000 years on the southern slopes of the Alps. In particular, distribution and ages of peat layers help define periods and extent of glacial fluctuation in the la...
| Publicado en: | Quaternary Research Vol. 71; no. 1; pp. 1 - 9 |
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| Formato: | Artículo |
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Cambridge University Press
Jan2009
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| Acceso en línea: | Ver este registro en EBSCOhost |