Abstracts
Abstract
The deglacial marine-limit surface is a virtual topography that shows the increase of elevation since deglaciation. The currently available set of marine-limit elevations (n = 929), about three times the number available in the most recent synthesis, allows a fairly detailed rendering of the surface across most of glaciated North America and Greenland. Certain large glacial lake-limit surfaces are analogous to marine-limit surfaces, except that their gradients were not dampened by eustatic sea-level rise. Collectively the surfaces reflect both gross ice-sheet geometry and regional to local rates of ice-marginal recession. As such, they are replication targets for glacioisostatic modelling that are supplementary to and more continuously distributed than relative sea-level curves.
Résumé
La surface de la limite marine durant la déglaciation est une topographie virtuelle illustrant l’augmentation des altitudes depuis la déglaciation. Les données disponibles sur l’altitude des limites marines (n = 929), trois fois plus nombreuses que celles publiées dans les synthèses récentes, permettent d’obtenir une surface plus détaillée de la région glaciaire de l’Amérique du Nord et du Groenland. Certaines surfaces lacustres de grande superficie sont similaires aux surfaces marines, sauf que leurs gradients ne sont pas affectés par la remontée du niveau de la mer. Ces surfaces reflètent collectivement la géométrie de la calotte glaciaire ainsi que les taux régionaux et locaux de recul des marges glaciaires. En conséquence, elles constitutent d’excellentes cibles additionnelles pour la modélisation glacio-isostatique, étant mieux distribuées que les courbes du niveau marin relatif.
Appendices
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