The first estimation of Fleuve Manche palaeoriver discharge during the last deglaciation: Evidence for Fennoscandian ice sheet meltwater flow in the English Channel ca 20-18 ka ago
The Fleuve Manche (English Channel) palaeoriver represents the largest river system that drained the European continent during Pleistocene lowstands, particularly during the Elsterian (Marine Isotope Stage 12) and Saalian Drenthe (MIS 6) glaciations when extensive ice advances into the North Sea are...
Published in: | Earth and Planetary Science Letters |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier Science Bv
2010
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Subjects: | |
Online Access: | https://archimer.ifremer.fr/doc/00002/11310/7858.pdf https://doi.org/10.1016/j.epsl.2009.12.050 https://archimer.ifremer.fr/doc/00002/11310/ |