L’évolution morphologique récente du réseau hydrographique sur les marges des glaciers Lovén, presqu’île de Brøgger (Spitsberg, 79° N)
In polar areas the post Little Ice Age warming generates paraglacial processes (Church and Ryder, 1972) marked by the prevalence of run-off over the zonal (glacial and periglacial) processes. In Spitsbergen, the retreat of the Brøgger peninsula’s glaciers induces the release of large amounts of prog...
Published in: | Norois |
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Format: | Article in Journal/Newspaper |
Language: | French |
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Presses universitaires de Rennes
2005
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Online Access: | https://doi.org/10.4000/norois.659 http://journals.openedition.org/norois/659 |