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We observe slightly increased geothermal heat fluxes above salt structures allowing to derive a local increase of melting rates. In the investigated scenarios (with and without idealized ice motion), this process not solely causes, but reinforces tunnel valley erosion. In a future study, we will include transient effects, investigate the hydrothermal convection and couple the melting rates to the computed heat fluxes.doi:10.18154/rwth-conv-250300 fatcat:qesmns7xmna7ve7uibqulahebi