Eastern Lomonosov Ridge: Constraints for a variable ice mass thickness during former glaciations
Here we present dense acoustic and swath bathymetry data sets as well as geological age constraints that allow a new view on past glacial processes at the Siberian termination of Lomonosov Ridge in the Arctic Ocean between 81° and 84° 20′ N. Here, the seabed is marked by three sets of streamlined gl...
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Veröffentlicht in: | Geomorphology (Amsterdam, Netherlands) Netherlands), 2022-09, Vol.413, p.108328, Article 108328 |
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