Impact of glacio-lacustrine interactions on ice-sheet dynamics
Geological records show that large proglacial lakes existed along the land-terminating margins of the Quaternary ice sheets. The major lakes formed in basins that were left deeply depressed due to delayed glacial isostatic adjustment (GIA) when the ice sheets retreated. As the environment around the...
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Other Authors: | , |
Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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Universität Bremen
2022
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Online Access: | https://media.suub.uni-bremen.de/handle/elib/6603 https://doi.org/10.26092/elib/2018 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib66039 |