Articles | Volume 72, issue 1
E&G Quaternary Sci. J., 72, 23–36, 2023
https://doi.org/10.5194/egqsj-72-23-2023

Special issue: Subglacial erosional landforms and their relevance for the...

E&G Quaternary Sci. J., 72, 23–36, 2023
https://doi.org/10.5194/egqsj-72-23-2023
Research article
20 Jan 2023
Research article | 20 Jan 2023

Comparison of overdeepened structures in formerly glaciated areas of the northern Alpine foreland and northern central Europe

Lukas Gegg and Frank Preusser

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Cited articles

Alley, R. B., Cuffey, K. M., Evenson, E. B., Strasser, J. C., Lawson, D. E., and Larson, G. J.: How glaciers entrain and transport basal sediment: physical constraints, Quaternary Sci. Rev., 16, 1017–1038, https://doi.org/10.1016/S0277-3791(97)00034-6, 1997. 
Alley, R. B., Cuffey, K. M., and Zoet, L. K.: Glacial erosion: status and outlook, Ann. Glaciol., 60, 1–13, https://doi.org/10.1017/aog.2019.38, 2019. 
Andersen, T. R., Huuse, M., Jørgensen, F., and Christensen, S.: Seismic investigations of buried tunnel valleys on-and offshore Denmark, Geol. Soc. Spec. Publ., 368, 129–144, https://doi.org/10.1144/SP368.14, 2012. 
Andrews, J. T., Hardardóttir, J., Helgadóttir, G., Jennings, A. E., Geirsdóttir, Á., Sveinbjörnsdóttir, Á. E., Schoolfield, S., Kristjánsdóttir, G. B., Smith, L. M., Thorse, K., and Syvitski, J. P. M.: The N and W Iceland Shelf: insights into Last Glacial Maximum ice extent and deglaciation based on acoustic stratigraphy and basal radiocarbon AMS dates, Quaternary Sci. Rev., 19, 619–631, https://doi.org/10.1016/S0277-3791(99)00036-0, 2000. 
Anselmetti, F. S., Drescher-Schneider, R., Furrer, H., Graf, H. R., Lowick, S. E., Preusser, F., and Riedi, M. A.: A  180,000 years sedimentation history of a perialpine overdeepened glacial trough (Wehntal, N-Switzerland), Swiss J. Geosci., 103, 345–361, https://doi.org/10.1007/s00015-010-0041-1, 2010. 
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Erosion processes below glacier ice have carved large and deep basins in the landscapes surrounding mountain ranges as well as polar regions. With our comparison, we show that these two groups of basins are very similar in their shapes and sizes. However, open questions still remain especially regarding the sediments that later fill up these basins. We aim to stimulate future research and promote exchange between researchers working around the Alps and the northern central European lowlands.