Abstract : During the last glaciation, an ice sheet covered Iceland approximately 1000 m thick. A reconstruction of the ice flow lines shows that the ice sheet was partly drained through fast-flowing streams. The major drainage routes correlate with locations of geothermal anomalies, suggesting that ice stream activity was favoured by water produced in regions of high geothermal heat flux. A widening of active rift zone was also deduced revealing a coupling between deep and surface processes.
Type de document :
Communication dans un congrès
Iceland in the Central Northern Atlantic : hotspot, sea currents and climate change, May 2010, Plouzané, France
http://hal.univ-brest.fr/hal-00480686
Contributeur : Adminhal Univbrestbu
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Soumis le : mardi 4 mai 2010 - 17:11:42
Dernière modification le : jeudi 5 avril 2018 - 10:36:19
Document(s) archivé(s) le : jeudi 16 septembre 2010 - 13:12:22
Olivier Dauteuil, Olivier Bourgeois, Brigitte Van Vliet-Lanoë. Enlargement of the active rift during glaciations. Iceland in the Central Northern Atlantic : hotspot, sea currents and climate change, May 2010, Plouzané, France. 〈hal-00480686〉
