Skip to main content
Fig. 9 | Swiss Journal of Geosciences

Fig. 9

From: Postglacial evolution of Lake Constance: sedimentological and geochemical evidence from a deep-basin sediment core

Fig. 9

Core section details of the prominent double event layer related to the Flimser Bergsturz event. The corresponding line-scans (colored) and CT scans (black and white) of the event layer are depicted on the left. Bright colors correspond with high density and dark colors the low density. The lower section contains green colored artificial filler-material inserted for an extracted pore-water sample (black in the CT scans). The color-coded grain size distribution [v%], mineral distribution [wt%], and the lithological constituents [wt%] are displayed in the center, with respective sample intervals separated by horizontal black lines. Two of the 14C-ages (black; with 2σ-range, Table 3) are shown in the right column in relation to a previously published Flimser Bergsturz age (blue; Deplazes et al., 2007)

Back to article page