Hummock corridors in the south‐central sector of the Fennoscandian ice sheet, morphometry and pattern

Abstract Subglacial conditions strongly influence the flow of ice‐sheets, in part due to the availability of melt water. Contemporary ice sheets are retreating and are affected by increased melting as climate warms. The south Swedish uplands (SSU) were deglaciated during the relatively warm Bølling‐...

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Bibliographic Details
Published in:Earth Surface Processes and Landforms
Main Authors: Peterson, Gustaf, Johnson, Mark D.
Other Authors: Sveriges Geologiska Undersökning
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2017
Subjects:
Online Access:http://dx.doi.org/10.1002/esp.4294
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