Articles | Volume 12, issue 6
https://doi.org/10.5194/esurf-12-1371-2024
https://doi.org/10.5194/esurf-12-1371-2024
Research article
 | 
11 Dec 2024
Research article |  | 11 Dec 2024

The Aare main overdeepening on the northern margin of the European Alps: basins, riegels, and slot canyons

Fritz Schlunegger, Edi Kissling, Dimitri Tibo Bandou, Guilhem Amin Douillet, David Mair, Urs Marti, Regina Reber, Patrick Schläfli, and Michael Alfred Schwenk

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Short summary
Overdeepenings are bedrock depressions filled with sediment. We combine the results of a gravity survey with drilling data to explore the morphology of such a depression beneath the city of Bern. We find that the target overdeepening comprises two basins >200 m deep. They are separated by a bedrock riegel that itself is cut by narrow canyons up to 150 m deep. We postulate that these structures formed underneath a glacier, where erosion by subglacial meltwater caused the formation of the canyons.
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