Cosmogenic nuclide evidence for minimal erosion across two subglacial sliding boundaries of the late glacial Fennoscandian ice sheet

• Main Authors: Harbor, J., Stroeven, A. P., Fabel, D., Clarhall, A., Kleman, J., Li, Y. K., Elmore, D., Fink, D.
• Format: Text
• Language: unknown
• Published: Purdue University 2006
• Subjects: glacial erosion; cosmogenic nuclides; ice sheet; sliding; northwestern sweden; frozen-bed; landscape; examples; surfaces; history; Ultevis; Arvestuottar; Fennoscandian; Ice Sheet; Northern Sweden
• Online Access: https://docs.lib.purdue.edu/physics_articles/161

The existence of sliding and frozen bed areas under ice sheets is significant in understanding basal thermal regimes, patterns of erosion and landform development, and in constraining boundary conditions for the reconstructions of ice sheets. Recognition of subglacial boundaries between sliding and...