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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Bibliographic Details
Main Author: Hinck, Sebastian
Other Authors: Lohmann, Gerrit, Humbert, Angelika
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Universität Bremen 2022
Subjects:
530
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