Late erosion pulse triggered by rapid melt in the cold‐based interior of the last Fennoscandian Ice Sheet, an example from Rogen
Abstract Ice sheet interiors are conventionally regarded as non‐erosive. Yet subglacial conditions may be transformed during deglaciation by the arrival of large volumes of meltwater at the ice sheet bed. The development of a dynamic meltwater drainage system and the onset of basal sliding have pote...
| Published in: | Earth Surface Processes and Landforms |
|---|---|
| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
2022
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1002/esp.5464 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.5464 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/esp.5464 |