Fig. 2From: Multiple Quaternary erosion and infill cycles in overdeepened basins of the northern Alpine forelandGeology after Isler et al. (1984), Sommerhalder (1968), Hantke (1967), and own observations. Bedrock surface model compiled by Pietsch and Jordan (2014)a Geological map of the Lower Glatt valley with locations referred to in the text. b Quaternary sediments (up to 200 m thick) are infilled into several distinct overdeepened bedrock troughs.Back to article page