Fig. 5From: Combined cosmogenic 10Be, in situ 14C and 36Cl concentrations constrain Holocene history and erosion depth of Grueben glacier (CH)3D-model of the study area including the four sampling sites and the footprint of Grueben glacier at ~1850 (Swisstopo 1865). Grub2-4 were covered by Grueben glacier during the LIA, Grub1 not. The model is based on swissALTI3D DEM and Landsat images used with permission of swisstopo (JA100120)Back to article page