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Fig. 6 | Swiss Journal of Geosciences

Fig. 6

From: Combined cosmogenic 10Be, in situ 14C and 36Cl concentrations constrain Holocene history and erosion depth of Grueben glacier (CH)

Fig. 6

Comparison of apparent surface exposure ages and uncertainties (1σ) calculated from 10Be, 14C and 36Cl concentrations. The dashed grey line and surrounding area mark the mean age and uncertainty of samples Grub1-3 of 9.6 ± 0.3 and of 8.1 ± 0.5 ka for Grub4, respectively. All nuclide ages agree with the corresponding mean age when the 2σ-uncertainty interval is considered

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