Fig. 5From: Analysis of overdeepened valleys using the digital elevation model of the bedrock surface of Northern SwitzerlandThalweg sections (A–A′ to F–F′; vertically strongly exaggerated) along the different axes of the Reuss glacier domain including the Linth-Rhine to Reuss conjunction passing the now completely hidden Richterswil—Menzingen valley (Section A′–A). All sections start at Laufenburg (for profile traces see inset and Fig. 1). Segments with identical courses of interlacing sections are partly omitted for better visibility. Arrows indicate connectivity between different profiles. Cross-sections 1–3 are oriented normal to the thalweg. The LGM and younger melting stages are shown by arrow heads. For further discussion see textBack to article page